American Condor Resources 1-A/A Offering $20M in Equity

 

Technical Report on the Suriloma Gold-Silver Property, Department of La Libertad, Peru

Prepared for Darwin Resources Corp.

By Graham D Carman

Bluerock Geological Pty Ltd Effective Date: February 27, 2013

1

CERTIFICATE OF AUTHOR

BLUEROCK GEOLOGICAL PTY LTD

Graham Carman (FAusIMM, Ph.D.)

8 Denman Street, Turramurra NSW 2074, Australia grahamcarman@bigpond.com

I, Dr. Graham Carman, Consulting Geologist for Bluerock Geological Pty Ltd, of 8 Denman Street, Turramurra, NSW 2074, Australia carried out this assignment for Darwin Resources Corp;

This certificate applies to the technical report entitled “Technical Report on the Suriloma Gold-Silver Property, Department of La Libertad, Peru” with effective date February 27, 2013; 

I am a Fellow of Australasian Institute of Mining and Metallurgy in Australia. I graduated from Victoria University of Wellington, New Zealand with a B.Sc. (Hons) in Geology in 1987, and with a Doctorate in Geology from Monash University, Australia in 1996. The PhD study was a geological  and geochemical study of the Lihir Island epithermal gold deposit in Papua New Guinea. I have worked as a geologist in mineral exploration for gold and base metals internationally for over 20 years, and I qualify as a ‘Qualified Person’ for the purposes of National Instrument 43-101; 

I have visited the Suriloma property on four occasions from 5 to 7 May 2012, 28 to 30 June 2012, 18 to 21 September 2012, and 20 to 22 February 2013; 

I am responsible for the preparation of all sections of the “Technical Report on the Suriloma Gold- Silver Property, Department of La Libertad, Peru” dated February 27, 2013; 

I am not independent of Darwin Resources Corp. as defined in section 1.5 of National Instrument 43- 101, as I am the President and CEO of the Company. 

I have not had any involvement in the property prior to the involvement of Darwin Resources Corp.; 

I have read National Instrument 43-101 and Form 43-101F1, and this technical report has been prepared in compliance with National Instrument 43-101 and Form 43-101F1; 

As of the date of this certificate, to the best of my knowledge, information and belief, the technical report contains all scientific and technical information that is required to be disclosed to make the technical report not misleading. 

Signed by Graham Carman

 

Dr. Graham D Carman Bluerock Geological Pty Ltd FAusIMM, Ph.D.

Dated: February 27, 2013

2

Date and Signature Page

The undersigned prepared this technical report titled “Technical Report on the Suriloma Gold-Silver Property, Department of La Libertad, Peru” and dated February 27 2013, in support of the public disclosure of technical aspects of the Suriloma Property by Darwin Resources Corp. The format and content of the report are intended to conform to Form 43-101F1 of National Instrument 43-101 of the Canadian Securities Administrators.

The undersigned consents to the public filing of the Technical Report entitled “Technical Report on the Suriloma Gold-Silver Property, Department of La Libertad, Peru” .

Effective Date: February 27, 2013

Signed on February 27, 2013 by

(Signed by Dr. Graham D Carman) (signed copy on file)

Graham Carman, FAusIMM, Ph.D., B.Sc.(Hons.)

For Bluerock Geological Pty Ltd

3

Table of Contents

0.3Property Ownership12 

7.4Target areas30 

0.0.1La Puerta30 

4

List of Tables	Page
Table 1. Claims details	12
Table 2. Option payments details	12
Table 3. Significant channel results of the stockwork zone at La Puerta	30
Table 4. Significant channel results of the silver-gold-base metals veins at La Puerta	33
Table 5. Significant channel results of the silver-gold-base metals veins at Edelmira	36
Table 6. PIMA results of clay minerals	39
Table 7. Laboratory samples and Quality Control Samples	47
Table 8. Summary of gold extraction results from metallurgical leach tests	50
Table 9. Budget ($US) for Initial Drill Program at La Puerta	53
List of Figures Figure 1. Location Map	11
Figure 2. Suriloma Mineral Concession Map	13
Figure 3. Suriloma Community & infrastructure Map	17
Figure 4. Regional Geology Map	20
Figure 5. Local Geology Map	22
Figure 6. Stratigraphic Column of local geology at Suriloma	23
Figure 7. Gold Geochemistry map	25
Figure 8. Silver Geochemistry map	26
Figure 9. Copper Geochemistry map	27
Figure 10. Zinc Geochemistry map	28
Figure 11. Suriloma Target Map	29
Figure 12. La Puerta channel samples and interpretation of mineralization	31
Figure 13. Edelmira channel samples and interpretation of mineralization	38
Figure 14. PIMA clay results from channel samples from La Puerta	41
Figure 15. Genetic geological model for Suriloma	43
Figure 16. Graphic of field duplicates with results of gold and silver	48
Figure 17. Graphic of blank samples for gold	49
Figure 18. Graphic of gold standard samples inserted by Darwin	49
Figure 19. Conceptual model for stockwork epithermal mineralization at La Puerta	52
Figure 20. Proposed initial drill program for the La Puerta area	54
List of Plates Plate 1. Stockwork mineralization at the La Puerta area	32
Plate 2. Stockwork at La Puerta showing veinlets trending ESE with argillic alteration	33
Plate 3. Outcrop of hydrothermal breccia and quartz stockwork at Santa Felicita	34
Plate 4. Mina Leje area showing artisanal mine working develop on the vein	35
Plate 5. Outcrop of the Giuliana vein dipping 60 degrees to the south at Edelmira	37
Plate 6. Photomicrography of 2-phase (liquid+vapour) fluid inclusions from Edelmira	46
List of Appendices Appendix 1. Geochemical maps of Suriloma: arsenic, antimony, mercury, bismuth, lead, tin.	57-64
Appendix 2. Darwin Resources Corp Rockchip Geochemical Database	65-80

5

View of the La Puerta gold stockwork target at the Suriloma property looking north – February 2013

Stockwork gold mineralization is exposed at the top of the ridge marked by a line of trees, parked truck at middle right hand side for scale

 

6

1.0 Summary

The Suriloma property is located in the Department of La Libertad in Peru, 60km northeast of the city of Trujillo at 7° 49.2’ South and 78° 33.2’ West between 3200-3900 metres in elevation. The property lies  within a mineral belt containing several world-class gold deposits. Suriloma is 30km west of Barrick’s  Lagunas Norte mine (2011 production: 763,000 oz gold) and 50km west of Rio Alto’s La Arena gold mine (2012 production: 212,000 oz gold – Rio Alto Mining website, 2013). The Shahuindo gold-silver deposit in  the Department of Cajamarca is located 50km to the north (4 Moz gold endowment: Sulliden Gold Corporation, 2012). The huge Yanacocha gold deposit (70 Moz gold endowment: Teal and Benavides, 2010) lies 100km to the north.

Darwin Resources Corp. (“Darwin” or “The Company”) acquired the Suriloma mineral concessions during 2012, following a target generation exercise by the Company which identified the area as a target for epithermal gold - silver mineralization. Surface mapping and sampling has now identified gold and silver mineralization at a number of specific target areas at the property. This report discloses technical aspects of the property including significant exploration results to date, and outlines the basis of a future exploration program including a proposed drill program and budget.

Darwin entered into three separate agreements to earn a 100% interest in three mineral concessions at Suriloma during the period from July to September 2012. Pursuant to these agreements, Darwin can earn 100% interest in the mineral concessions by making staged payments over 3 years for a total of US$800,000. A residual 2% net smelter return (NSR) can be bought at any time on all three claims for a total of US$1.3 million. Two other concessions are 100% owned by Darwin. The Suriloma property consists of a continuous mineral concession package totalling 2,070 hectares. No past drilling is known on the property. No Mineral Resource or Mineral Reserve is known.

Two styles of mineralization occur on the property:

-Stockwork gold mineralization; 

-Quartz vein silver - gold - base metal mineralization; 

Mineralization is hosted by Calipuy Group volcanic rocks of mid-Tertiary age, and Goyllarisquizga Group quartz sandstones of Cretaceous age. The mineralization occurs over a discontinuous strike length of 7 kilometres, and over a vertical interval of some 700 metres between 3,200 metres and 3,900 metres elevation. The style of mineralization is identified as intermediate sulfidation epithermal to mesothermal vein type. Old artisanal mine workings for silver and antimony veins are present in the area.

Seven (7) target areas for gold and silver mineralization have been identified at Suriloma. Darwin has collected around 650 surface samples, most of which are continuous channel samples averaging 2m in length.

The La Puerta target is the principal gold oxide target hosted by epithermal quartz stockwork mineralization within andesite host rocks associated with argillic (illite ± smectite) alteration. A total of 309  channel samples were collected and assayed from 24 channels dug perpendicular to the strike of the gold structure over a 1km length. An epithermal gold stockwork zone has been identified in two sub-parallel mineralized zones with a combined width of up to 60 metres. Highlights of the channel sampling from the La Puerta area include 29 metres @ 1.6g/t gold + 4.5g/t silver, 26 metres @ 1.28g/t gold + 0.5g/t silver, and 16 metres @ 2.2g/t gold + 2g/t silver. The average grade of all 309 channel samples, including unmineralized samples, is

0.90 g/t  gold (ranging from  <0.005 to 12.8  g/t  Au) and 15 g/t silver  (ranging from <0.2 to 171 g/t  Ag). The

7

samples are anomalous in arsenic, and there is a strong positive correlation between gold and arsenic. Base metal values in the stockwork are low. Gold mineralization is related to the density of quartz stockwork veinlets, and is disseminated in the hydrothermally altered rocks. The stockwork mineralization is believed  to have formed at around 160 to 200 °C in a shallow epithermal environment based on the clay mineralogy. Outcrops of the stockwork are now oxidised containing no sulfide. The western end of the mineralized structure at La Puerta is interpreted to lie beneath shallow post-mineral volcanic cover.

The stockwork mineralization at the La Puerta target has the potential to host a large tonnage, low grade, oxide gold deposit. The intial conceptual target has a strike length of 1,000 metres, a depth potential of 200 metres (i.e., to the base of the mineralized volcanic unit) and width of 50+ metres. Potential exists for the gold mineralization to extend into the Mesozoic sediments that underlie the volcanic host rocks.

Other gold stockwork targets at Suriloma include the Inmaculada and Santa Felicita areas. At Santa Felicita gold mineralization is hosted in quartz sandstones, with reconnaissance samples grading up to 4.4 g/t gold in hydrothermal breccia. Further work is required to define the exploration potential at these areas. Quartz sandstones are the host of major gold deposits in the La Libertad region of Peru, including Lagunas Norte and La Arena, so these targets warrant further work.

A metallurgical cyanide leach test of representative material from surface samples at La Puerta grading 1.48 g/t gold returned a gold recovery of 90.7% gold from a cyanide bottle roll test within a 24 hour period, with cyanide consumption of 0.4 kg/t. This was a highly favourable result, indicating the vast majority of gold mineralization in surface outcrops is easily leachable with low cyanide consumption. It is noted that this was a preliminary metallurgical test from surface mineralization, and is not necessarily representative of mineralization in the sub-surface. Further metallurgical testing is recommended once drill cores are available.

Silver - gold - base metal quartz veins that vary in width from <1 metre to 4 metres occur at several areas on the property including Surupampa, La Puerta, Edelmira, Mina Leje, and Guadalupe. These veins commonly have small old artisanal workings developed along them, and can contain significant base metals and silver- antimony sulfosalts and/or stibnite while gold grades are variable from low to high. A vein at Surupampa returned the highest gold values yet at the property, 0.3 metres @ 132g/t gold + 45 g/t silver from a narrow oxidised quartz vein. A quartz vein at La Puerta returned a channel result of 2 metres @ 658 g/t silver + 1.33 g/t gold + 0.2% antimony with coarse-grained stibnite. Sulfide mineralization in the veins typically comprises around 10% by volume as pyrite, stibnite, sphalerite, galena, and silver-antimony sulfosalt minerals including polybasite. The vein gangue is mostly crystalline and drusy-textured quartz. The quartz - base metal sulfide veins are interpreted to have formed under high temperature intermediate sulfidation epithermal conditions or mesothermal conditions (250 to 300 °C). The presence of copper sulfosalts (including bournonite) and tin sulfide (stannite) in some of the quartz veins suggests a nearby mineralizing intrusion.

An exploration program is recommended including at least 2,000 metres of diamond drilling at the La Puerta area, focussing on the oxide gold potential and the epithermal stockwork mineralization. Darwin has an approval pending for a 12 platform drill program at La Puerta.  The Company expects the drill approvals to  be granted by calendar Q2 2013. Land access agreements have been signed with individual landholders for this proposed program. The drill program is estimated to cost US$761,000 including contingencies.

8

0.1Introduction 

0.2Property and Issuer 

The Suriloma mining concessions are situated in the District and Province of Otuzco in the Department of La Libertad in northern Peru, approximately 80 kilometres by road east of the city of Trujillo - Figure 1. The property consists of five contiguous mineral concessions covering 2,070 hectares (ha) including concession overlaps (the ‘Property’). Three of the mineral concessions are held under three separate option  agreements with individual concession holders, on which Darwin Resources Corp (‘Darwin’, the ‘Company’ or the ‘Issuer’) has the right to acquire 100% ownership of the mineral rights.  Darwin Peru SAC, a wholly  owned Peruvian subsidiary of Darwin, is party to the legal agreements. Two other concessions are 100% owned by Darwin Peru SAC. Darwin is a TSX Venture Exchange reporting public company.

0.3Site Visits 

The author has visited the property on four occasions from 5 to 7 May 2012, 28 to 30 June 2012, 18 to 21 September 2012, and 20 to 22 February 2013, accompanied by Company staff and/or consultants of the Company. Several rock samples were collected during these visits by the author.

0.4Principal Sources of Information 

The purpose of this technical report (the ‘report’) is to disclose technical aspects of the Suriloma gold-silver property and outline a proposed work program including drilling. This report has been prepared by Dr. Graham Carman (PhD, FAusIMM) in compliance with the disclosure requirements of the Canadian National Instrument 43-101. Dr. Carman (the ‘author’) meets the criteria of Qualified Person. The author is a full-time employee of the Company and is not considered ‘independent’ based on the definition in Section 1.5 of National Instrument 43-101. The author has reviewed available exploration results and prepared the Report in accordance with the formatting requirements of National Instrument 43-101 (‘NI 43-101’) and Form 43- 101F1 (Standards of Disclosure for Mineral Properties). This report is intended to be read in its entirety.

The author has compiled Darwin’s available geological and geochemical data on the property as of the date of this Report. Sources of data used include in-house reports and accompanying maps, sections and tables prepared by Darwin’s staff; geochemical datasets provided by the Company and the laboratory; mineralogical reports by independent consultants of samples collected by the Company; papers in the public domain on the geology and mineralization of northern Peru; and various maps, press releases and papers found on the Internet. References have been made to third party documents  where  appropriate, to the best of the author’s knowledge.

10

Figure 1. Location Map of the Suriloma project with selected large gold deposits of northern Peru

 

0.1Reliance on Other Experts 

This report has been compiled based on field observations by the author and with reference to ‘in-house’ Darwin geological reports made available to the author by professional geologists of the Company. The author has visited the property on four occasions, and has been involved in the collection of surface samples. The information, conclusions, opinions and recommendations are based upon:

Information available to the author at the time of the preparation of this report; 

Data, reports and other information provided by Darwin Resources Corp. and other sources; 

Assumptions, conditions and qualifications as set forth in this report; and 

The author’s knowledge of the subject of economic geology gained over years of experience. 

Mr. Rolando Ligarda, Exploration Manager South America for Darwin, accompanied the author during his property examinations and provided commentary on the geology at the property and the exploration results. Mr. Luis Giraldo, Project Geologist, compiled the bulk of the geochemical data and supervised the collection of the channel samples at the La Puerta area. Mr. Edgardo Guizado, Geological Consultant, supervised the mapping and sampling at the Edelmira, Santa Felicita and Surupampa areas. Mr. Georg  Winkelmann, General Manager of Darwin in Peru, provided the property ownership information relating to the mineral concessions and of the mineral rights in Peru. The available information is believed to be of good quality,  and there is no reason to consider any of the information to be inaccurate.

11

0.1Property Description and Location 

0.2Property Location and Description 

The Suriloma property is located at 7° 49.2’ South and 78° 33.2’ West between 3200m and 3900m elevation in the District and Province of Otuzco, Department of La Libertad, Peru (Figure 1). In UTM coordinates the property is centered at approximately 770000E, 9135000N (PSAD56 zone17S datum). Access is via a  bitumen road from the coastal city of Trujillo to the town of Otuzco 60km to the east. From Otuzco, access  to the property is via a gravel road heading northwards approximately 20 km from Otuzco.

The Suriloma property consists of five contiguous mineral concessions namely Surupampa III 2009, Santa Felicita 2, Edelmira, Colquiloma 1, and Colquiloma 2, which cover a total of 2,070 hectares (ha). Figure 2 shows a map of these concessions, and Table 1 documents the relevant concession information.

Table 1. Claim Details

Claim name	Ownership			Code No. concession	Status		Area (ha)
Surupampa III 2009	Jorge Juan Manuel Pinillos Cisneros			630006809	Concession Granted		800
Santa Felicita 2	Luis Carlos Alfaro Ulloa			630006209	Claim Application		660
Edelmira	Juliete Margarett Miguel Pacheco			15008317X01	Concession Granted		140
Colquiloma 1	Darwin Peru SAC			010092712	Concession Granted		600
Colquiloma 2	Darwin Peru SAC			010239812	Concession Granted		200
Total area (ha)							2,400
Area (incl. overlap)							2,070
4.2Property Ownership  Darwin has a right to earn 100% interest in the mineral rights of three (3) concessions by making staged annual cash payments for a combined $800,000 over 3 years. Annual payments to the owners of each concession are due on the anniversary dates of the execution of the respective option (see Table 2), except for the Santa Felicita 2 concession, for which the 3 year option will start once the concession is granted and the option agreement signed (expected early Q2 2013). The concession holders each retain a 2% Net  Smelter Return (NSR) royalty, which may be purchased at any time (see Table 2). Two other concessions are 100% owned by Darwin (Colquiloma 1 and Colquiloma 2). Colquiloma 1 was granted on 27 June 2012, and Colquiloma 2 on 31 October 2012. Table 2. Option Payments Details ($US)
Claim name	Payment	Payments	Payment	Payment at	Payment	Payment at	Payment	Option
	for 100%	at	at signing	12 months	at 24	exercise 36	to	Execution
	rights*	Execution	of LOI		months	months	buyout	Date
		of option					NSR
Surupampa III 2009	$300,000	$21,000+	-	$50,000	$100,000	$129,000	$500,000	13/07/2012
Santa Felicita 2*	$300,000	$13,500	$12,500+	$50,000	$95,000	$129,000	$500,000	At granting
Edelmira	$200,000	$20,000+	-	$30,000	$50,000	$100,000	$300,000	30/10/2012
TOTAL	$800,000			$130,000	$245,000	$358,000	$1,300,000
+ Payments as marked have been made * Letter of Intent (LOI) signed on 26 October 2012

12

Figure 2. Suriloma Mineral Concession Map

 

13

4.3 Mineral Rights in Peru

The General Mining Law of Peru is administered by the Ministerio de Energia y Minas. The Mining Law defines and regulates different categories of mining activity, according to the stage of development. Details of the Mining Law were consolidated in the ‘Single Revised Text of the General Mining Law’ of 1992 (Government document D.S. No. 014-92-EM). In summary, ownership of mineral claims is controlled by mining concessions that are established under UTM coordinates (PSAD zones 17, 18, or 19 S). New concessions have a maximum size of 1,000 ha and a minimum of 100 ha, with vertices to the nearest 1,000m UTM coordinate. Concessions that pre-date the new law are based on the ‘punto de partida’ system and can be of any orientation with metre coordinates of vertices given to 3 decimal places. If the old concessions overlap with new concessions granted in the graticular system, the old concession has priority.

Mining concessions are irrevocable as long as the required annual maintenance fees (‘derecho de vigencia’) are paid by 30 June each year and cannot be more than 2 years in arrears, otherwise the concessions will extinguish. The annual fee for metallic mineral concessions is US$3/ha for each concession that is either granted or under application (‘petitorio’). The concession holder must sustain a minimum level of annual commercial production no later than by the expiration of the tenth year, equivalent to one Taxation Unit (currently 3,700 Peruvian soles or approximately CDN $1,450) per year and per hectare. Otherwise, starting the first half of the eleventh year following the granting of the mining concession, the titleholder shall pay a penalty equal to 10% of the required minimum annual production per hectare and per year, until the minimum annual production has been met. The penalty must be paid in addition to the annual rental fee. If the required minimum annual production has not been met by the expiration of the fifteenth year following the granting of the mining concession granted, the mining concession will extinguish. An additional non- renewable term of up to a maximum of five years validity can be granted if the breach of the minimum annual production is caused by force majeure or by any fact not attributable to the titleholder, properly supported and approved by the competent authority. Also, the titleholder may be granted an additional non- renewable term of up to a maximum of five years validity, by paying the penalty and crediting investments in mining and / or basic infrastructure for public use, equivalent to not less than ten times the amount of the penalty which he/she is liable. In either case, if the failure continues until the twentieth year following the granting of the mining concession, it will expire.

For mining concessions granted before 2008, the former ruling on minimum annual production applies, whereby the holder must sustain a commercial annual production greater than US$100/ha in gross sales before the end of the sixth year following the granting of the concession. If the concession has not been put into production within a six year period, the annual rental increases from the first semester of the seventh year to US$9 (US$3 for derecho de vigencia, plus a US$6 penalty), until the minimum production level is met. If, by the start of the twelfth year from granting a concession, the minimum production level is not been achieved, the annual rental increases to US$23/ha (US$3 for derecho de vigencia, plus a US$20 penalty). A concession holder can, however, be exonerated from paying penalties if he/she can demonstrate that at least ten times the penalty for the total concession was invested during the previous year. The investment must be documented and it must be accompanied by a copy of the relevant annual tax statement (‘declaración jurada de impuesto a la renta’) and payment of the annual fees.

The holder of a mining concession must operate their concession in compliance with applicable safety and environmental regulations, and in so doing take all necessary steps to avoid damage to third parties. The

14

concession holder must at all times, allow free access to their concessions by those authorities responsible for assessing whether the concession holder is meeting their obligations by law.

The issue of land tenure continues to be of importance in Peru, as the owner of surface rights can prevent exploration activities from proceeding. The Government requires a concession holder to either make an appropriate agreement with the surface rights owner for access to a property, or purchase the surface rights, prior to any significant exploration activity proceeding, including drilling. If the titleholder is unable to reach an agreement on the use of surface ground, it can apply for initiation of an easement to the Government. Holders of mining concessions are protected under the Peruvian Constitution and Civil Code. A Peruvian mining concession is a property-related right, distinct and independent from the ownership of land on which it is located, even when both belong to the same person. The rights granted by a mining concession are defensible against third parties, are transferable and chargeable, and may be the subject of any transaction or contract.

All transactions and contracts relating to a mining concession need to be registered with the Public Registry of Mining (Registro Publico de Mineria) in the event of subsequent disputes in law. The two option agreements relating to the granted concessions are registered in the Public Registry of Mining in Trujillo, whilst the Letter of Intent has been signed before a notary in Trujillo and will be registered as soon as the concession title is granted.

Darwin does not control the surface rights on any of the concessions at Suriloma. All surface rights are held by individual land holders. Darwin is progressing with the necessary permits to undertake drilling activities.

Environmental issues related to industrial activities in Peru are governed by the Ministerio del Ambiente (MINAM). The Dirección General de Asuntos Ambientales of the Ministerio de Energía y Minas is the enforcing agency for mining. The General Law of Environmental Law no. 28611 of 2005 is the relevant law. Specific environmental regulations for mining exploration are contained in the Decreto Supremo 020-2008- EM. The Decreto Supremo 020-2012 establishes that an approved Environmental Impact Study (DIA) for category I drilling, an approved water permit, and the agreement with the registered owners of the surface ground must be exhibited to obtain the authorization required prior to the application for a Permit to Initiate Activities (PIA). The final PIA approval generally takes 2-3 months after the application is presented.

For more details see: http://www.minem.gob.pe/area.php?idSector=4&idArea=56&idTitular=614&idMenu=sub611&idCateg=334

5.0 Accessibility, Climate, Local Resources, Infrastructure and Physiography

The property is located in northern Peru in the Province of Otuzco, Department of La Libertad. Access is via a bitumen road from Trujillo to the town of Otuzco, located 60km to the northeast of Trujillo and about 90 minutes by vehicle along a well formed bitumen highway. From Otuzco access to the property is via a gravel road heading northwards approximately 20km by road to the project, which takes 60 minutes.

Trujillo is the third largest city in Peru and hosts an international airport with several flights a day to Lima and to other cities in Peru. The Pacific Ocean port of Salaverry is located about 15km south of Trujillo city.  Otuzco is a moderate-sized town about 10km in a straight line south of the property, with a population of around 12,000. Darwin currently is renting space in Otuzco as a base for the Company.

15

There are four communities located within the property - Figure 3. The La Libertad village is located 2km  east of the centre of the property. The Tambillo village is located 2km to the north. Surupampa village is located 3km to the northwest. Pango is located 5km to the south. The property area is generally used for cropping of potatoes, wheat and other cash crops by the local inhabitants. Farm animals include pigs, sheep, goats, llamas, chickens, horses, and donkeys. Houses are scattered around the property area.

The physiography of the Suriloma property is mountainous with the property located on the edge of a ridge between two large river systems. The Moche River drains south and west through the town of Otuzco to the coastal city of Trujillo, while the larger Chicama River drains north and northwest before turning west to the coast. Elevations within the property range from 2,900m to 4,000m with moderate to strong relief. The  areas of known gold mineralization occur from elevations of about 3,200m to 3,900m.

Vegetation consists mostly of grasses with sporadic eucalyptus trees and low perennial shrubs. The local climate is typical of a western Andes environment with cooler dry winters (April to June), and mild wet summers (December to March). Daytime temperatures range from 8 to 25 °C during the year. Exploration work can proceed on a year-round basis, although care must be taken on wet tracks during the summer.

The closest permanent water source is the river Moche (15km by road). While there is a good road access to the property, access within and between the prospects is limited. There is electricity to the nearest village 2km from the property. There appears to be adequate space to construct a mine, mill and suitable tailings ponds and waste dump sites, but these considerations are beyond the scope of this report.

6.0     History

The Suriloma property area was highlighted by a generative targeting study by Darwin geologists in early 2012. A site visit and preliminary assays returned encouraging results. This work led to return visits with more detailed sampling and mapping, and ultimately the negotiation and completion of the option agreements. No mineral resources or reserves exist on the property. To the knowledge of Darwin, no drilling or modern systematic exploration including extensive outcrop sampling or ground geophysics, appears to have taken place.

Small old mining pits up to a few metres deep have been developed on various silver - gold - base metal quartz veins at La Puerta and Inmaculada. The La Puerta workings exploited stibnite (antimony), whereas Inmaculada workings probably exploited gold - silver mineralization, with the quantity of material mined estimated to be less than 100 tonnes based on the small size of the stockpiles.

The Edelmira area has a number of quartz veins ranging between 0.2 and 4 metres in width exploited for silver at an artisanal scale during early 20^th Century times up to 1956. Some of the small scale workings may be much older. Some veins are currently being worked at an artisanal scale, in part by local landholders. In 1982 the Peruvian state-owned Banco Minero, based on a request by the current owner of the Edelmira concession, reviewed the economic potential of the veins from oxidised and mixed sulfide samples of underground workings (Banco Minero, 1982). Of the six veins described in the Banco Minero report, the Giuliana vein was described as having the potential for 10,000 tonnes of ore grading 340 g/t silver, 5.5% Pb and 4.6% Zn (no strike length was defined). Banco Minero recommended re-opening and re-sampling of the old mines to expose primary sulfides, but this work was not completed.

16

Figure 3. Suriloma Community and Infrastructure Map

 

17

0.1Geological Setting and Mineralization 

Northern Peru has a history of gold mining dating back to Inca times. Extensive modern exploration has taken place since the late 1980s, with the discovery of the Yanacocha deposit (2009 production: 2.1 million oz gold – Buenaventura website 2011) in the Department of Cajamarca, 100km north of Suriloma – see Figure 1.

Several large gold deposits occur within a 50km radius of Suriloma in the Department of La Libertad, where the Suriloma property is located. These include the Lagunas Norte gold mine operated by Barrick with 14 Moz contained gold (Barrick Gold Corporation, 2011); the La Arena gold mine with oxide Reserves + Resources of 2.3 Moz gold (Rio Alto Mining website, 2012), and the Shahuindo gold-silver oxide heap leach project currently in feasibility with oxide Reserves of 1.0 Moz gold and 11 Moz silver (Defilippi et al., 2012). Old silver mining districts within 50km radius of Suriloma include Salpo, with estimated past production of 100 Moz silver and 1Moz gold (Hollister and Entwistle, 1977), and the historic silver-base metals vein deposits of Quiruvilca.

Despite being located in a heavily mineralized gold-silver belt, the Suriloma property had seen very little modern exploration prior to Darwin’s exploration activities.

0.2Regional Geology 

The Suriloma property straddles a regional northwest-southeast trending Andean boundary between Mesozoic sedimentary rocks of Jurassic-Cretaceous age, and volcanic rocks of the Middle Tertiary  (Oligocene- mid Miocene). Mesozoic rocks lie to the north of the boundary, with Calipuy Group volcanic rocks to the south. Figure 4 shows the regional geology of the area and some of the important gold deposits in the region.

The following descriptions of the rock formations in the region are sourced largely from Navarro et al. (2010).

The basement rocks in the region belong to the Chicama Group of Jurassic age, consisting of deformed laminated lutites with interbedded sandstones and minor coal measures. Chicama Group sediments outcrop some 15km to the south and west of the project and are discussed no further here.

Middle to Upper Cretaceous age Goyllarisquizga Group rocks outcrop in the north and west of the property. Goyllarisquizga Group consists of a number of conformable, tightly folded sedimentary formations being from oldest to youngest: Chimu Formation, Santa-Carhuaz Formations, and Farrat Formation. Chimu Formation consists of quartzose sandstone (quartzite) with interbedded lutite. The Santa and Carhuaz Formations consist predominantly of impure limestone and lutite with minor sandstone. The Farrat Formation consists of interbedded quartzose sandstone and lutite. At the Suriloma property, Goyllarisquizga Group rocks are undifferentiated quartz sandstone sedimentary units which outcrop below approximately 3,250m elevation in the north and west of the property. The specific sedimentary formation name is not known at this time.

18

Regionally the Goyllarisquizga Group is unconformably overlain by limestone formations of upper Cretaceous age (Chulec and Pariatambo Formations) which outcrop some 20km north of the property and are discussed no further here. The Tablachaca Formation (also known as Huaylillas Formation) consists of red sandstone and conglomerate (‘red beds’) of late Cretaceous to early Tertiary age, forming a discordant contact above the folded Goyllarisquizga Group rocks within the project area.

The Coastal Batholith is a 50km-wide granodiorite batholith that extends continuously throughout the coastal belt of Peru for 1500km. The Coastal Batholith is of Upper Cretaceous to Lower Tertiary age. The closest outcrops of granodiorite lie 15km west of the property, and are discussed no further here.

The Calipuy Group, the dominant outcropping rock unit in the project area, is a thick (700m to >1500m) sequence of andesite and dacite pyroclastic flows (‘tuffs’) and lavas. The contact with the underlying Mesozoic sediments is discordant and/or faulted. Dating and stratigraphic classification of Calipuy Group volcanics in the region by Ingemmet (Rivera et al., 2005; Navarro et al., 2010), has designated four main eruptive stages each characterized by calc-alkaline andesite and minor dacite volcanics from Eocene to Miocene as follows (Ma = million years ago); Stage 1 (40Ma to 28Ma); Stage 2 (28Ma to 24Ma); Stage 3 (24Ma to 17Ma); and Stage 4 (17Ma to 10Ma). Calipuy Group rocks within the property are part of the Urpillao-Rushos eruption centres younger than about 24Ma, corresponding to Stage 3 of Navarro et al. (2010). The eroded Urpillao and Rushos volcanoes are believed to have been connected strata-volcanoes. A single K-Ar age date of 24 ± 1.0 Ma (i.e. Oligocene) was obtained from a diorite intrusive cutting the basal units (Stewart et al., 1974).

It is interpreted that the Calipuy Group volcanic rocks have infilled a fault-controlled basin that thickens rapidly to the south. To the north of the property, Calipuy Group rocks were probably thinly deposited and have now been eroded - see Figure 4.

0.3Property Geology 

Mineralization at Suriloma is hosted by Calipuy Group volcanic rocks and underlying undifferentiated Goyllarisquizga Group sedimentary rocks. Darwin Resources has mapped the property at a 1:5,000 scale, from which a simplified 1:25,000 scale geological map is presented in Figure 5. A stratigraphic column of the local geology is presented in Figure 6. All mapped units pre-date the gold mineralization except for andesite domes, dikes and sills which are believed to post-date mineralization.

0.3.1Mesozoic Sedimentary Rocks 

Undifferentiated Goyllarisquizga Group rocks consist of quartz sandstone and siltstone sedimentary units which outcrop below approximately 3,250m elevation in the north and west of the property. These rocks appear to be tightly folded. The sedimentary rocks host gold mineralization at the Santa Felicita and Mina Leje areas.

19

Figure 4. Regional Geology Map

20

0.3.2Calipuy Volcanic Rocks 

The Calipuy Group has a maximum thickness of 700m at the Suriloma property. The volcanic sequence has been subdivided by Darwin geologists into four mappable, relatively flat lying, laterally continuous units - see stratigraphic column (Figure 6). The dip of the sequence is 10 to 20 degrees to the southwest.  From oldest  to youngest the four units are:

1.Lower Andesite consists of purple-green coloured andesite pyroclastic flow units with minor epiclastic sandstones. The Lower Andesite sequence is up to 300m thick, with its base at about 3,300m elevation. The pyroclastic flows consist of both heterolithic and monolithic tuffs with sub- rounded to sub-angular andesite clasts up to 10cm in diameter within an andesite matrix. The Lower Andesite is an important host for the gold mineralization at the La Puerta and Inmaculada areas. 

2.Dacite consists of pale pink - cream - green coloured crystal and lithic tuffs (i.e., pyroclastic flows) with abundant 10-30% quartz phenocrysts. The lithic clasts are up to 5cm in diameter enclosed in a dacite volcanic matrix. The pyroclastic flows contain abundant flattened pumice clasts (“fiamme”). The base of the Dacite contains a quartz latite unit with approximately 5% quartz and abundant fiamme. The Dacite unit is 200m to 250m thick with its base between 3,450m and 3,600m elevation, and has been eroded from the eastern part of the property. Dacite hosts silver - gold - base metal quartz veins at Edelmira. 

3.Limestone - Chert unit is a sedimentary horizon between 10m and 30m thick consisting of limestone layers with lenses of chert, interbedded with epiclastic volcanics including sandstone and conglomerate commonly in a calcareous matrix. This unit is a key stratigraphic marker. 

4.Upper Andesite consists of brown-purple coloured andesite pyroclastic flows including lithic tuffs with clasts up to 10cm diameter in an andesite matrix, interbedded with thinner units of quartz latite containing approximately 5% quartz. Flattened pumice (‘fiamme’) is common throughout. This unit  is up to 150m thick in the Edelmira area, and has been eroded from the eastern part of the property. A volcanic conglomerate debris flow unit occurs towards the top with rounded clasts up to 1m in diameter. The Upper Andesite hosts silver-gold-base metal vein mineralization in the Edelmira area. 

0.3.3Volcanic domes and Pebble Dikes 

Pebble dikes between 1m and 10m across containing rounded to sub-rounded clasts of quartzite, siltstone, andesite and dacite in a rock flour clay matrix have been mapped cutting the Lower Andesite, Dacite and Upper Andesite units. The pebble dikes contain low levels of gold mineralization, and are interpreted as a precursor to the gold mineralization.

Small bodies of andesite displaying sub-horizontal ‘flow-banding’ textures are mapped in several locations on some of the highest hills on the property. These andesites are interpreted to be the remnants of volcanic domes and/or sills that were emplaced after the mineralization. An andesite dome is interpreted to  shallowly cover the gold mineralization at the western end of the La Puerta area.

Andesite dikes 1m to 5m across have been observed cutting the Upper Andesite, and are interpreted to be of a similar age to the andesite domes (i.e., post-mineral).

21

Figure 5. Local Geology Map of Suriloma

22

Figure 6. Stratigraphic Column of Local Geology

23

0.4Mineralization 

Two general styles of mineralization have been recognized at Suriloma by the Darwin geological team. These are (1) stockwork gold mineralization, and (2) quartz vein silver - gold - base metal mineralization. These styles are described in detail below.

Surface geochemical results from Darwin’s rock sampling at the property are summarized in geochemical maps for gold, silver, copper and zinc (Figures 7 to 10). Other geochemical maps summarizing results for arsenic, mercury, antimony, tin, bismuth, and lead are provided as Appendix 1. The full geochemical database of approximately 630 samples is provided as Appendix 2.

0.4.1Stockwork gold mineralization 

Quartz veinlet mineralization referred to as “stockwork” type, is the most important mineralization style in terms of bulk mineable gold potential at Suriloma. Gold mineralization is spatially  associated with the  quartz veinlets but also is disseminated within the altered rock. Stockwork gold mineralization is known at the La Puerta and Inmaculada areas hosted within the Lower Andesite, and in quartz sandstones at Santa Felicita associated with hydrothermal breccia. Gold mineralization of stockwork type is typically accompanied by arsenic anomalism, believed to be arsenopyrite and/or arsenian pyrite but now oxidized at surface. Silver mineralization is typically low in the stockwork (Ag:Au ratio typically <5:1), while base metals (copper, lead, zinc) are weak to not anomalous.

See Section 7.4 for a detailed description of the stockwork gold mineralization at each of the target areas.

0.4.2Silver – gold – base metal vein mineralization 

Quartz veins containing silver - gold - base metal mineralization occur throughout the property, and are concentrated in the Edelmira area where a swarm of sub-parallel veins have been worked in the past as small-scale artisanal mines. The Edelmira veins are <1m to 4m across, and contain up to 10 volume %  sulfides including pyrite, galena, sphalerite, stibnite, and various sulfosalts of silver-lead (including bournonite) and silver-bismuth minerals. The veins at Edelmira are also highly anomalous in mercury (Hg).

Copper mineralization associated with elevated levels of tin occurs in some of the quartz veins at the western end of the Edelmira area. The copper mineralization is due to the presence of copper-silver-zinc sulfosalt minerals, including polybasite. Minor tin mineralization occurs as stannite.

See Section 7.4 for a detailed description of the quartz-sulfide vein mineralization at each of the target areas.

24

Figure 7. Gold Geochemistry Map

 

25

Figure 8. Silver Geochemistry Map

 

26

Figure 9. Copper Geochemistry Map

 

27

Figure 10. Zinc Geochemistry Map

 

28

Figure 11. Suriloma Target Map

 

29

7.4Target areas
Seven (7) target areas prospective for gold, and silver - gold - base metal mineralization have been
identified at the Suriloma property. The targets are located on a map in Figure 11, and described in turn
below.
7.4.1La Puerta
The La Puerta area is believed to be prospective for a large tonnage, low grade, oxide gold deposit hosted
by quartz stockwork. The stockwork gold mineralization has been traced on the surface over a strike length
of approximately 2km.Along the central 1km zone of La Puerta where gold grades are highest,
mineralization separates into two sub-parallel east-west trending zones that have a combined width at
surface of 50-60 metres, and a vertical extent of 80 metres. Plate 1 displays a typical outcrop of the
stockwork in the central La Puerta area. The western extension of the mineralized zone is believed to be
overlain by shallow volcanic cover which is younger than the mineralization.
Quartz stockwork veinlets criss-cross the Lower Andesite unit in three preferential orientations: NE-SW
(040-060 degrees – most dominant), E-W (080-100 degrees), and N-S (350-010 degrees – least dominant).
A photo of the predominant 060 orientation is shown in Plate 2. Quartz veinlets are typically 0.2 to 0.7cm
across with a veinlet separation of 2-5cm. The host andesite is pervasively hydrothermally altered to an
assemblage of hydrothermal clay-quartz-goethite. The clays are dominantly illite and smectite or mixed-
layer  clays  (see  Section 7.5).Occasionally boulders of hydrothermal breccia are scattered about the
surface, exhibiting clasts of andesite in hydrothermal cement.
A total of 309 samples were taken by Darwin geologists from 24 hand-dug channels cutting
outcropping/subcropping zones at La Puerta. The average width of each individual sample was two metres,
with the maximum continuous channel length being 53 metres. A detailed gold and silver geochemical map
of the channel sample results is presented below - Figure 12. The edges of the mineralized zones can be
soil covered and not well defined, so there remains the possibility that mineralization could be wider than
indicated by sampling.The channel sampling results of the gold stockwork zone at La Puerta are
highlighted in Table 3.
Table 3. Significant channel results of the stockwork zone at La Puerta
Width (m)	Gold g/t	Silver g/t	Number of samples	Zone	Channel number	Date released
10.0	0.45	1	5	B	TR-22	Feb 7 2013
20.0	0.85	2	10	B	TR-19	Feb 7 2013
29.0	1.60	4.5	15	A-B	TR-15	Jan 8 2013
15.5	1.00	4	7	B	TR-12	Dec 4 2012
6.0	1.53	2.5	3	A	TR-13	Dec 4 2012
26.0	1.28	0.5	13	A	TR-14	Dec 4 2012
16.0	2.12	2	8	A	TR-09/10/11	Nov 14 2012
22.5	0.56	14	12	B	TR-09/10/11	Nov 14 2012
18.0	1.40	15	9	B	TR-06/07/08	Nov 14 2012
1.2	9.10	7.4	1	A	-	Nov 14 2012
3.0	4.80	3	3	A	Canal-02	July 9 2012
7.0	2.17	3	3	A	TR-01d	July 9 2012
1.4	7.30	2	1	B	TR-01a	July 9 2012
30

Figure 12. La Puerta channel sample highlights and interpretation of the mineralization

 

31

Sulfides are rarely seen in outcrops at La Puerta. ‘Boxwork’ textures reflect the surface weathering and oxidation of sulfide minerals.

The average grade of all 309 channel samples at La Puerta is 0.90 g/t gold (ranging from <0.005 to 12.8 g/t Au) and 15 g/t silver (ranging from <0.2 to 171 g/t Ag), including samples which are unmineralized. There is a strong positive correlation between gold and arsenic in general. The average arsenic value in the channel samples from La Puerta is 3,950ppm arsenic. Other gold pathfinder metals such as antimony, barium, and mercury are mildly anomalous at the La Puerta area (average of 365ppm Sb, 157ppm Ba, 1.5ppm Hg). Base metals such as copper, lead, and zinc are considered weak to not anomalous in the La Puerta channel samples as a whole (average 22ppm Cu, 125ppm Pb, 128ppm Zn).

Plate 1. Stockwork mineralization at the La Puerta area

32

Plate2. Stockwork at La Puerta showing veinlets trending 060 degrees with associated argillic hydrothermal alteration

 

A silver - gold - stibnite (- base metal) quartz vein between 1m to 3m wide outcrops at La Puerta trending northwest-southeast over 400m strike length. This vein was exploited for stibnite at a small scale during  the 1970s. The vein is discordant to the stockwork mineralization, and is interpreted by the author to pre- date the stockwork mineralization. The quartz vein has a number of old artisanal workings developed along it, and contains up to 10 volume % sulfide (including pyrite, arsenopyrite, stibnite, sphalerite, galena, and marcasite) encapsulated in the quartz. Antimony occurs as coarse-grained stibnite. Sulfosalt minerals were not observed. Highlights of the silver - gold – antimony – base metal channel results are shown in Table 4.

Table 4. Significant channel results from the La Puerta gold – silver – base metal quartz vein

Width (m)	Gold g/t	Silver g/t	Copper ppm	Zinc ppm	Lead ppm	Antimony ppm	Number of samples	Channel number
6.0	1.68	53	20	57	306	370	3	TR-21
10.0	0.53	133	26	383	586	481	5	TR-18
Incl. 2.0m	1.33	658	90	0.18%	0.28%	0.21%	1	TR-18
2.0	11.0	292	36	409	809	0.11%	1	TR-06/07/08
4.1	1.9	188	26	0.15%	866	0.33%	3	TR-04
Incl. 0.8m	4.0	871	319	0.75%	0.41%	1.23%	1	TR-04
3.6	4.0	15	94	406	280	0.82%	3	TR-02

A sericite alteration halo several metres wide occurs with a bright bottle-green clay mineral that is possibly paragonite.

33

0.0.1Santa Felicita 

The Santa Felicita area is prospective for stockwork gold mineralization hosted by quartz sandstones of the Goyllarisguizga Group. Exploration to date is preliminary, with only 30 surface samples approximately collected. Mineralization occurs at about 3,200 metres elevation. A photograph of hydrothermal breccia containing gold mineralization with strong sericite alteration in the sandstone is shown in Plate 3. These samples are also anomalous in arsenic, and appear to have similar geochemistry to the stockwork samples from La Puerta, including low values of silver and base metals.

Plate 3. Hydrothermal breccia in quartz sandstone at Santa Felicita. The outcrop returned 4.4 g/t gold.

Silver - gold - base metal quartz veins also occur in Dacite and Lower Andesite at Santa Felicita. Channel samples grade up to 261 g/t silver and 0.1 g/t gold over 2 metres in this area.

0.0.2Surupampa 

The Surupampa area is prospective for high-grade gold-silver vein mineralization cutting the Lower Andesite. A total of 23 rock samples have been collected to date from outcropping veins.  The highest  grade gold sample on the property taken by Darwin was at Surupampa returning 0.3m @ 132 g/t gold and 45 g/t silver (average of original sample and field duplicate) from an oxidised quartz vein outcrop in a road cut. Most of the other samples collected from this area are anomalous in gold ranging from 0.1 to 1.4g/t gold.

A small artisanal mine is currently active in one location in the Surupampa area.

34

0.0.3Inmaculada 

The Inmaculada area is prospective for gold, located about 1km west of La Puerta. Gold mineralization is hosted by the Lower Andesite. Only reconnaissance exploration has been carried out to date.

The Inmaculada stockwork is exposed over 400m of strike length in outcrops up to 5m wide. The structure consists of gossanous quartz stockwork with argillic alteration. Small old mine workings have been developed on the structure at two locations. Eleven channel and dump samples average 3.44 g/t gold (ranging from 0.005 to 11.9 g/t Au) and 17 g/t silver (ranging from 0.4 to 122 g/t Ag).

0.0.4Mina Leje 

A narrow quartz-sulfide vein less than 1 metre wide cuts siltstone at Mina Leje – see Plate 4. It is currently being exploited by a small number of artisanal miners. A channel sample 0.15m across returned 10.2 g/t gold and 269 g/t silver. The Mina Leje quartz vein contains significant pyrite and arsenopyrite (>20% by volume). Further work is required to determine if bulk mineable mineralization may exist.

Plate 4. Mina Leje area showing current artisanal mine working developed on the vein

0.0.5Edelmira 

The Edelmira area is prospective for silver- gold -base metal mineralization associated with a swarm of sub- parallel quartz veins striking approximately east-west. The veins outcrop discontinuously over several hundred metres, are south-dipping at between 45 and 75 degrees, and range from <1 to 4 metres wide. The veins are hosted within the Dacite and Upper Andesite units. The veins are exposed over 300m of vertical relief from 3500 to 3800m elevation – see channel sample map of Edelmira in Figure 13.

The veins at Edelmira are characterized by sulfide minerals which make up about 10% of the veins by volume in quartz gangue. Sulfide minerals are exposed in mine dumps or in shallow workings and include pyrite, sphalerite, galena, stibnite, various sulfosalts including bournonite (a Cu-Pb-Sb-S mineral) and polybasite (a Cu-Zn-Ag-Sb-S mineral). Silver also occurs with complex bismuth - antimony sulfosalt minerals identified in mineral studies (see Section 9.4). The gangue consists of quartz with minor manganese oxide,

35

possibly after Mn-carbonate. The quartz is crystalline and drusy. Bladed quartz “lattice” texture is common in samples, interpreted as a replacement of original bladed calcite.

Seven sub-parallel vein structures have been mapped and sampled by the Darwin geological team at Edelmira. The names used for the veins are those used in old reports (e.g., Banco Minero, 1982) – see Figure 13. Alteration halos around the veins consisting of sericite alteration which can extend up to 15 metres either side of the vein in the widest of cases, although the alteration zones appear weakly mineralized.

A total of 112 channel samples have been collected by Darwin at Edelmira – Figure 13. The highlights of the channel sampling are presented in Table 5. Approximately 50 rock samples were collected from old mine dumps and outcrops, these results are included in the Appendix 2.

The most important veins are the Giuliana vein exposed over approximately 1.5km of strike, the Petronila- Rocio, Judith, and the Anita vein exposed for about 1km of strike. A typical outcrop of Giuliana vein is shown in Plate 5. The Giuliana, Petronila and Judith samples are predominantly channel samples taken perpendicular to strike from inside the old workings which have exposed sulfides. The Anita samples are from oxidised surface outcrops or oxidised mineralization in small shallow workings.

Table 5. Significant channel results of the silver - gold - base metal veins at Edelmira

Vein	Width m	Silver g/t	Gold g/t	Copper %	Zinc %	Lead %	Tin %
Giuliana	1.50	455	0.10	0.04	0.25	0.55	-
	0.35	354	1.11	0.04	0.07	0.03	-
	5.50	46	0.06	0.01	0.10	0.40	-
	3.20	234	0.32	0.06	6.16	2.11	-
Petronila-Rocio	0.15	946	0.20	2.02	0.44	1.08	0.045
	0.30	255	0.07	0.67	0.15	0.25	0.007
Judith	0.60	161	0.05	0.05	0.06	0.61
Anita	4.0	106	0.08	0.01	1.30	0.54
	2.0	81	0.82	0.01	0.05	0.15
	1.6	117	0.50	0.03	0.03	1.17

The Petronila-Rocio vein contains copper mineralization associated with the sulfosalt minerals polybasite and bournonite. Copper is positively correlated with tin (Sn), with samples grading up to 0.045% Sn – see Table 5. The tin mineral has been identified as stannite (a sulfide of tin). The high levels of copper and tin indicate relatively hot formation temperatures for these veins, and suggest a mineralizing intrusion is nearby.

36

Plate 5. Outcrop of the Giuliana vein dipping 60 degrees southwards, Edelmira area

0.0.6Guadalupe 

The Guadalupe vein occurs 1.5km south of the La Puerta area along a sub-parallel structure that is poorly exposed. Colloform banded quartz float occurs over a strike length of approximately 400 metres. Ten samples of the Guadalupe vein contain anomalous to high levels of silver averaging 68 g/t Ag (ranging from

0.2 to 409 g/t Ag) while gold values average 0.04 g/t Au (ranging from 0.008 to 0.16 g/t Au).

37

Figure 13. Edelmira channel samples and interpretation of mineralization

 

38

0.1Hydrothermal Alteration 

7.5.1 Argillic Alteration

Hydrothermal alteration associated with quartz stockwork is typically argillic (i.e., clay dominant) with minor silicification in areas of intense stockwork veining. The argillic alteration may extend several metres into the unmineralized host rock, while the clay mineralogy changes with decreasing distance from the mineralization.

Clay minerals were identified in 20 channel samples from La Puerta using a Terraspec Portable Infrared Mineral Analyzer (PIMA) (Ligarda, 2013) in samples independently analysed for gold – see Table 6. The dominant clays at La Puerta based on the PIMA results are illite, montmorillonite (either smectite or mixed- layer illite-smectite), kaolinite, minor dickite and paragonite (a sodium muscovite). Mixed-layer illite- smectite clays, if present, were not able to be distinguished from the end member clays in the PIMA analysis. The predominant clays analysed in the PIMA at La Puerta are shown in Figure 14.

Illite-predominant samples are generally associated with higher-grade gold mineralization in the quartz stockwork (Table 6, Figure 14). Montmorillonite is the other most common clay mineral  identified.  Samples that contain predominantly montmorillonite without illite have low gold values, and are generally located beyond the stockwork in relatively impermeable, weakly mineralized areas.

Other clays present in the PIMA analyses include kaolinite, dickite, and paragonite. Kaolinite is interpreted as a low-temperature supergene alteration overprint. Dickite occurs in a few samples commonly with illite, and likely formed at higher temperatures associated with the epithermal mineralization at La Puerta. Chlorite and minor calcite are present as a propylitic alteration halo at the La Puerta area, but chlorite was not identified in the PIMA study.

Illite is known to form above about 160 °C in active geothermal systems of New Zealand (Ji and Browne, 2000). On the other hand, montmorillonite (smectite) and mixed-layer illite-smectite clays form between 100 and 200 °C in geothermal systems (Harvey and Browne, 1991). Hence samples containing illite and montmorillonite at La Puerta are interpreted to have formed in the epithermal temperature range of about 160-200 °C. The montmorillonite samples (without illite) were likely formed at lower temperatures on the edge of the system, consistent with the lower gold grades.

Table 6. PIMA results of clay minerals from samples at Suriloma ranked in decreasing abundance (Ligarda, 2013)

SAMPLE

AreaMineral 1Mineral 2Mineral 3Mineral 4Style 

Gold g/t

51000163	La Puerta	Illite	Dickite	Montmorillonite	Kaolinite	Stockwork	2.457
51000164	La Puerta	Illite	Montmorillonite	Paragonite		Stockwork	2.078
51000409	La Puerta	Illite	Montmorillonite			Stockwork	0.192
51000417	La Puerta	Illite	Montmorillonite			Stockwork	2.242
51000422	La Puerta	Illite	Montmorillonite			Stockwork	0.378
51000423	La Puerta	Illite	Montmorillonite	Dickite	Kaolinite	Stockwork	4.999
51000435	La Puerta	Illite	Montmorillonite			Stockwork	0.716
51000173	La Puerta	Kaolinite	Dickite	Paragonite		Stockwork	0.176
51000429	La Puerta	Kaolinite	Illite	Dickite	Paragonite	Stockwork	2.5
51000439	La Puerta	Kaolinite	Illite	Montmorillonite	Paragonite	Stockwork	0.147
51000122	La Puerta	Montmorillonite	Kaolinite	Dickite	Illite	Stockwork	<0.005

39

51000193	La Puerta	Montmorillonite	Illite		Stockwork	0.052
51000197	La Puerta	Montmorillonite	Kaolinite	Illite	Stockwork	0.009
51000198	La Puerta	Montmorillonite	Kaolinite		Stockwork	0.026
51000405	La Puerta	Montmorillonite	Illite		Stockwork	0.938
51000408	La Puerta	Montmorillonite	Illite		Stockwork	1.74
51000442	La Puerta	Dickite	Montmorillonite	Kaolinite	Stockwork	0.08
51000106	La Puerta	Paragonite			Stockwork	2.211
51000140	La Puerta	Paragonite	Montmorillonite		Stockwork	0.153
51000131	La Puerta	Muscovite			Vein	0.05
51000220	Edelmira	Muscovite	Paragonite		Vein	0.106
51000229	Edelmira	Muscovite			Vein	0.02

7.5.2. Sericite Alteration

Hydrothermal alteration associated with silver - gold - base metal quartz veins is sericite dominant. Sericitic alteration haloes occur up to a few metres from the veins, with the intensity of alteration diminishing with distance from the vein.

Muscovite (a well-crystallized version of sericite) was confirmed by PIMA results in three samples from Edelmira and La Puerta. The sericite (muscovite) is interpreted to have formed at a higher temperature than illite alteration areas associated with the stockwork mineralization consistent with fluid inclusion evidence (see Section 9.5).

0.1Structural Controls to Mineralization 

At this early stage in the exploration, the structural controls to the gold and silver mineralization at Suriloma are poorly known. The Company’s interpretations of the structural controls are largely  conceptual.

The main structural features are faults that trend WNW-ESE and E-W. These faults are believed to have been the main pathways for the mineralizing gold-silver bearing fluids at Suriloma. These faults are interpreted as transpressional structures (or ‘thrust’ faults) along which hydrothermal fluids have permeated and deposited gold by processes including hydrothermal brecciation, boiling, and mixing with cooler fluids. Areas where the structures have widened to disseminated zones with abundant quartz stockwork veinlets (e.g. La Puerta) are interpreted as dilational fault bends (or ‘jogs’) where hydrothermal activity has been concentrated.

Another important consideration is that the geological contact between Mesozoic sedimentary rocks and the Tertiary volcanic rocks was an important reactive boundary for precious metal hydrothermal fluids. The strongest mineralization to date occurs in the rocks that straddle the regional sediment – volcanic boundary (e.g., Lagunas Norte, La Arena).

40

Figure 14. PIMA clay results for channel samples from La Puerta

 

41

0.1Deposit Types 

The region of northern Peru has several world-class epithermal gold deposits largely discovered during the last 20 years. Epithermal deposits in northern Peru include Yanacocha (70 Moz gold endowment – Teal and Benavides, 2010), Lagunas Norte (14 Moz Au – Barrick Gold Corporation, 2011), La Arena (6 Moz – Rio Alto website, 2013) and Pierina (10 Moz Au). The Fruta del Norte gold deposit (6.1 Moz Au & 10 Moz Ag - Henderson, 2009) lies in southeastern Ecuador.

In general, epithermal deposits are formed within 1km of the surface, with or without the association with magmas, and typically accompanied by fracturing of the host rocks (e.g. Hedenquist and Henley, 1985; Henley, 1985). The classification of epithermal deposits favored by this author is a subdivision into high-, intermediate-, and low sulfidation types based on the sulfide minerals present (after Sillitoe and Hedenquist, 2003). High sulfidation deposits are typically located close to the tops of volcanic centres where they are hosted within the volcanic rocks themselves (e.g., Yanacocha, Pierina) or by Mesozoic sedimentary rocks typically quartzites (e.g., Lagunas Norte, La Arena). Gold mineralization in high sulfidation deposits in this region is typically associated with vuggy silica alteration (Navarro, 2007). This style of alteration is not observed at Suriloma.

Low sulfidation vein deposits occur with banded chalcedonic quartz and sometime with K-feldspar (adularia) and calcite (Sillitoe and Hedenquist, 2003). Economic vein deposits are typically of a low overall tonnage but can contain bonanza grade ore. Sulfide content of the ores is dominated by pyrite-marcasite and is typically less than 2 volume % (Sillitoe, 1993). This style of mineralization does not occur at Suriloma. A nearby low sulfidation occurrence at Urumalqui about 30km south of Suriloma has an Inferred Mineral Resource of 1.9 Mt tonnes grading 171 g/t Ag and 1.38 g/t Au (Kaye et al., 2011).

The gold stockwork and sulfide vein mineralization at Suriloma is typical of many characteristics of the intermediate sulfidation deposit type. Characteristics of these deposits are discussed in more detail below.

0.2Intermediate Sulfidation Deposit Model 

In Peru, intermediate sulfidation deposits include Shahuindo (4 Moz Au + 70 Moz Ag – Sulliden Gold Corporation, 2012) located 50km north of Suriloma in the Department of Cajamarca, while the old mining district of Salpo (estimated 1 Moz Au + 100 Moz Ag mined - Hollister and Entwistle, 1977) is located 20km south of Suriloma in the Department of La Libertad. These deposit types are characterised by quartz - carbonate veins and stockworks with sulfides of an intermediate sulfidation state occurring with base metals. Sulfide minerals include sulfosalts of antimony and/or arsenic (e.g., tetrahedrite-tennantite), together with galena, sphalerite, and minor chalcopyrite (Sillitoe and Hedenquist, 2003). Arsenopyrite may also occur. The deposits show a range of precious metal - base metal ratios, from very low base metal content to silver - base metal and base metal - silver deposits (Albinson et al., 2001). The quartz veins are typically crystalline and can include manganese - bearing carbonates and silicates (Sillitoe, 1993). Some intermediate sulfidation deposits show a spatial association with porphyry gold or copper systems, for example in the Hualgayoc Department of Cajamarca, Peru.

Other regional intermediate sulfidation deposits include the Quiruvilca silver district, located 33km east of Suriloma, an old mine exploited by the early Spanish miners. The Tres Cruces gold prospect located 5km from Quiruvilca is an intermediate sulfidation epithermal gold system hosted by hydrothermal breccias, quartz stockworks and disseminations within volcanic rocks and intrusions (Heyl and Livingstone, 1999).

42

A generalized geological model for Suriloma is shown in Figure 15. The model infers that intermediate sulfidation mineralization occurred beneath an argillic ‘lithocap’, but above and to the side of a buried intrusion yet to be identified. The argillic lithocap at Suriloma is interpreted to have largely been eroded.

Figure 15. Genetic model for Suriloma mineralization (modified from Sillitoe, 2010)

0.1Exploration 

Exploration by Darwin Resources Corp at Suriloma has included geological mapping and surface sampling, gold metallurgical tests of surface samples from La Puerta, mineralogical studies, PIMA clay analyses, and fluid inclusion studies of vein samples. These activities are described below.

0.2Geological Mapping 

Mapping has been carried out over most of the property by Darwin geologists at a scale of 1:5,000. A geological map of the property is presented in Figure 5. The geology is described in section 7.2.

0.3Outcrop and Mine Stockpile Sampling 

A total number of 578 rock surface samples have been collected from outcrops and old mine dumps at the property by the Darwin team. Of these samples, a total of 463 are channel samples, 49 are non-selective outcrop rock chip samples, 37 are selective rock chip samples, 24 are mine dump or stockpile samples, and 5 are float samples. The sample types are described below.

43

Quality control samples were inserted at random into the batches that went to the laboratory for assay. Quality control samples represent 49 samples, or 7.8% of the Suriloma geochemical database. Field duplicates represent 13 samples in the database. Known standards in the database are 24  in number.  Blank samples were 12 in number.

‘Channel’ samples are the most reliable sample types taken because they are considered representative of the in situ mineralization over a specified continuous outcrop interval, using a hammer and chisel. Each sample was typically 2m in length, up to 0.3m in depth (depending on depth of soil cover), and collected approximately perpendicular to the dominant vein direction. Channel sampling was restricted to surface exposures where there is little or no soil cover, in cases where soil cover was greater than about 0.3m thick no sample was taken. Whenever possible, channel samples were collected continuously without interruption over intervals of metres to tens of metres, however in most cases channel samples are interrupted due to the presence of deep soil. Channel samples represent approximately 80% of  the samples collected by Darwin at Suriloma.

‘Rock chip’ or ‘outcrop’ samples are either selective or non-selective samples taken at random or over semi-continuous intervals over outcrop widths of <1 to 5m across. These samples are believed to be generally indicative of the outcrop, but are not considered as representative as channel samples. These represent approximately 15% of the samples in the database.

‘Dump’ samples are selective rocks taken from mine dumps or stockpiles, so the exact location of the in situ mineralization may not be known. These samples can be highly selective, so do not necessarily represent the typical grades of the mineralized rock but could be ‘high-graded’. These samples represent approximately 4% of the samples collected.

‘Float’ samples are rock samples that are not in situ and may be transported a distance (often unknown) to the place of sampling. These samples represent less than 1% of the total samples taken.

Results of surface rock chip and channel sampling at each of the target areas are described in Section 7.4.

0.4Bottle-Roll Gold Metallurgical Tests 

A bottle-roll leach metallurgical test was carried out on a composite sample from a 10m-long continuous channel sample from the La Puerta area at Certimin SA Lima. See Section 13 for details of these results.

0.5Mineralogical Studies of Sulfides 

A petrographic study of two vein samples from La Puerta was carried out by Geo Services Alberto Aranda

E.I.R.L (Aranda, 2012). The aim was to identify the sulfide minerals in samples from the principal quartz - sulfide vein from the La Puerta area. Sulfides recognised were stibnite, arsenopyrite, sphalerite, galena, pyrite, and marcasite (in order of decreasing abundance). Coarse grained stibnite was recognized as a late sulfide phase replacing sphalerite.

An additional petrographic study was made of two samples by Panda Geoscience Ltd (White, 2012) comprising of quartz vein material from La Puerta, and a quartz - sulfide vein from Edelmira (the Petronila

44

vein). The La Puerta stockwork sample contained arsenopyrite overgrowing pyrite in a quartz vein, with rare sphalerite. No other sulfides were recognized.

The Petronila vein quartz-sulfide sample contained a number of intergrown sulfide species, several of which were unidentified by petrographic analysis. The sample was then sent for analysis on the JEOL 8600 electron microprobe at Otago University New Zealand. Sulfide minerals identified using a qualitative technique on the microprobe were pyrite, galena, bournonite (Cu-Pb-Sb sulfosalt), polybasite (Cu-Zn-Ag-Sb sulfosalt), stannite (tin sulfide), sphalerite, and several complex silver – bismuth sulfosalts.

0.6Fluid Inclusion Studies 

Samples of two vein specimens from La Puerta and Edelmira were submitted to Panda Geoscience Ltd, Auckland New Zealand, to determine formation temperatures of the veins (White, 2012). Thin sections of the samples where doubly polished to 0.2mm thick. The fluid inclusion samples were the same samples sent for microprobe analysis.

Fluid inclusion homogenization temperatures from 9 individual primary fluid inclusions in the Edelmira sample were found to cover a wide range of temperatures from 164-281°C, in some cases reflecting variable liquid to vapor ratios in these inclusions – see Plate 6. The median homogenization temperature was 196°C. The inclusions were interpreted by Panda Geoscience to have trapped two-phase (i.e., boiling) fluids during the formation of the quartz veins, in which case those inclusions may have been trapped at about 200°C. Evidence of boiling in fluid inclusions during vein formation is consistent with other boiling evidence (including ‘lattice texture’ where quartz has replaced bladed calcite). The high temperature samples may also have recorded a higher temperature event.

The same Edelmira sample was analysed by BISA Laboratory Lima for fluid inclusion heating and freezing measurements, and found homogenization temperatures in 26 inclusions ranging from 282-350°C, while freezing measurements found salinities of around 10 weight % NaCl equivalent.

The differences in the homogenization temperatures and textures are interpreted as evidence of two distinct hydrothermal stages in the mineralization at Suriloma; a high temperature 250-300°C stage, and a lower temperature 160-200°C stage.

The author interprets that silver - gold - base metal quartz vein mineralization was associated with high temperature fluids at 250-300°C. A later, lower temperature epithermal stage associated with boiling fluids at around 200°C overprinted the high temperature stage at both Edelmira and La Puerta. This interpretation is consistent with the sulfide mineralogy in the veins (i.e., dominated by silver and base metals), which most likely formed under relatively high formation temperature conditions, and PIMA clay analyses from the stockwork mineralization at La Puerta indicating lower epithermal temperatures of around 160-200°C.

45

Plate 6. Photomicrograph of primary 2-phase fluid inclusions from Edelmira – field of view 0.25mm.

 

10.0 Drilling

No drilling has been carried out at the Suriloma property by Darwin or any previous explorer. It is the Company’s intention to begin a drill program at La Puerta by calendar Q2 2013. Access agreements have been signed by landholders and drill permits are pending.

An initial drill program of 2,000m in approximately 12 diamond drill holes (minimum 150m drill hole depths) is recommended. This proposed program is discussed in more detail under Recommendations (Section 26).

11.0 Sample Preparation, Analyses and Security

Rock samples of surface outcrops collected in the field were generally 2.5-3.5 kg each. The geology of each sample is described by a Company geologist, UTM coordinates are noted, samples are bagged and labelled, and a batch of samples is then sent by 3^rd party transport to Lima. Sample preparation and assaying of all samples was conducted by Certimin S.A., an independent commercial laboratory in Lima, Peru, using certified standards and approved methodologies.

Certimin is an ISO 9001:2008 accredited laboratory, having received ISO 17025 accreditations for specific laboratory procedures with the Canadian Association for Laboratory Accreditation Inc. (CALA). As part of their ISO 17025 accreditation, Certimin participate in a number of international proficiency tests, such as those managed by CANMET and Geostats. Both of these agencies circulate samples for analysis twice a  year and evaluate the performance of participating laboratories.

The sample preparation used for all rock samples is method G0640. Samples are heated to 60°C to remove moisture, then dried. The entire sample is then crushed using a primary crusher (100% sample reduced to 6mm or less) and then a secondary crusher (100% sample reduced to 1.7mm or 10 mesh). The sample is then 1/8 split to approximately 400g and pulverised to approximately 90% passing 75 microns (200 mesh)

46

for geochemical analyses and stored (“pulps”). The 7/8 sample reject is stored in the original sample  bag for a period of at least 3 months (“coarse rejects”).

Gold was analysed by fire assay at Certimin using a 50g aliquot with an atomic absorption finish (method G0107). If the grade of the sample supersedes 10g/t Au, the sample is re-assayed with a gravimetric finish (method G0014). Silver and other trace and major element analyses were carried out using ICP-AES using an aqua regia digestion (method G0146). Over limits for silver (>100 ppm) were fire assayed with a gravimetric finish (method G0001). Over limits for copper, lead, zinc, arsenic and antimony (>1% for each) were re-assayed with an AAS finish (methods G0038, G0076, G0387, G0342, and G0086 respectively). Mercury was analyzed by AAS-FIMS with aqua regia digestion using the cold vapor technique (method G0137).

0.1Data Verification 

The author has reviewed all the documents, assay results, plans and sections prepared by the Darwin geological team. Thirteen days were spent by the author in the field examining surface geology, observing the sampling process, assisting with sample collection and mapping, and reviewing maps prepared by Darwin geologists on the Suriloma project.

The digital data available to the author consists of geochemical assays and geological maps. These data are believed by the author to be authentic and of good quality. Observations made by the author on site corroborate with the data that has been presented by Darwin’s geologists. The author has seen the original digital files from Certimin, and has compared these files to the database provided by Darwin with no differences noted. Although digital data can be subject to modification by anyone who has access to it or the motivation to do so, the author believes that any manipulation of the data is highly improbable.

0.2Quality Control of Analytical Data 

The author made a visit to Certimin on 26 June 2012, and was provided a tour of the sample preparation, gold fire assay and ICP analytical facilities. Based on these observations author believes that the Certimin laboratory is a high class commercial laboratory that meets world standards.

Darwin has implemented a system of quality control of samples sent to Certimin Laboratory, including the insertion of known standards and field duplicates into each batch submitted. The total of samples and Darwin control samples sent to the laboratory are shown in Table 7 below. Results of field duplicates, standards and blank samples inserted into the sample batches are presented below. These results indicate that the quality of the results are within limits of acceptable errors for all sample types, and provide confidence in the validity of results obtained.

The results of the quality control samples are considered acceptable, within analytical variation.

Table 7. Suriloma geochemical samples and Quality Control samples

Type of Sample	Quantity	%
Normal samples	578	92.8%
Field duplicates	13	2.1%
Standards	22	3.5%
Blanks	10	1.6%
TOTAL	623	100%
QA-QC	45	7.2%

47

0.2.1Field duplicates 

Field duplicates were inserted into all batches of samples sent to the laboratory. The results of the field duplicates are shown for gold and silver in Figure 16. In general, the correlation between the original sample and the duplicate sample analyses are extremely high for both gold and silver. Two of the 13 duplicate samples are beyond the 20% differential. This difference may be a function of sampling variability in the field rather than variability at the laboratory.

0.2.2Blanks 

A total of 10 blank samples were inserted into the sample batches. Gold analyses of the blanks are presented graphically in Figure 17. The results are considered acceptable.

0.2.3Standards inserted by Darwin 

A total of 22 internal standard samples were inserted by Darwin into the sample batches sent to the laboratory, with three different standards used (OREAS 52c, OREAS 54Pa, OREAS 62d). The results for gold are presented graphically in Figure 18. Assay results from Certimin are within 1-2 standard deviations of the mean, and are considered acceptable.

Figure 16. Graphic of field duplicates with results of gold and silver

48

Figure 17. Graphic of blank samples for gold

STANDARD: OREAS 22b (BLANK)

Limite < 25 ppb Au

50

40

30

20

Au ppb

Limite Au

10

0

-10

SAMPLES

Au ppb

Figure 18. Graphic of gold standard samples inserted by Darwin

49

 

13.0Mineral Processing and Metallurgical Testing 

A bottle-roll gold leach test was carried out at Certimin using a composite sample from a 10 metre continuous channel sample of outcropping quartz stockwork mineralization from the La Puerta area (Certimin, 2013). The sample is considered typical of the grade of the outcropping oxidized mineralization. The composite sample was made up of five 2m continuous samples each weighing about 3.2 kg. A 2.2 kg subsample of each original sample was split, homogenized and combined into a single 11kg bulk sample for leach testing. The head-grade of the bulk sample was 1.485 g/t Au.

Two cyanide leach bottle roll tests were carried out over a 72 hour period on a 1.5kg sample split, using a 100% minus 1.7mm size fraction, and a 90% minus 75 micron size fraction. The cyanide concentration used was 500ppm NaCN, with a pH of 10.5 and 11. The gold extraction tests, summarized in Table 8, recovered 90.7% of the total gold in both samples, indicating the vast majority of the gold in these outcrops is leachable while the cyanide consumption was low.

Table 8. Summary of gold extraction results from metallurgical leach tests

Sample	Size fraction	Gold Extraction	Time taken to maximum extraction	Cyanide consumption kg/t
Minus 10 mesh composite Minus 200 mesh composite	- 1.7mm - 75µm	90.7% 90.7%	24 hours 2 hours	0.39 0.43

A 90.7% gold recuperation level in this initial test of surface mineralization is considered highly encouraging. It is noted that Mineral Reserves or Resources have not been defined at Suriloma, and that the preliminary gold extraction test results from surface outcrops are not necessarily representative of gold mineralization in the sub-surface. More metallurgical testing is recommended once drill core is available.

14.0 Mineral Resource Estimates

At this time, there are no known Mineral Resource estimates or Mineral Reserves on the Suriloma property.

50

15.0 Mineral Reserve Estimates

Not applicable to this report.

16.0 Mining Methods

Not applicable to this report.

17.0 Recovery Methods

Not applicable to this report.

18.0 Project Infrastructure

Not applicable to this report.

19.0 Market Studies and Contracts

Not applicable to this report.

20.0 Environmental Studies, Permitting and Social or Community Impact

A Declaration of Environmental Impact (DIA) for stage 1 drilling allowing a program of up to 12 drill platforms at the La Puerta area, was submitted to the relevant authorities in Peru in early February 2013. Permits are pending as of the date of this report.

Landholder access agreements have been signed with landholders at the La Puerta area to enable this drill program to be completed.

21.0 Capital and Operating Costs

Not applicable to this report.

22.0 Economic Analysis

Not applicable to this report.

23.0 Adjacent Properties

Not applicable to this report.

24.0 Other Relevant Data and Information

There is no other current data or information that is applicable to this property or the report.

51

25.0 Interpretation and Conclusions

The Suriloma gold-silver property is situated on a regional east-west trending geological structure in a highly prospective region of northern Peru, within 50km of several multi-million ounce gold deposits including Lagunas Norte, La Arena and Shahuindo. Seven target areas have been identified by Darwin Resources Corp. for gold and silver potential at the property. It is the author’s belief that these targets are significantly under-explored.

Two styles of intermediate sulfidation mineralization have been identified at Suriloma: (1) epithermal stockwork gold mineralization and (2) silver-gold-base metal quartz veins. The principal initial exploration target for Darwin is the stockwork gold epithermal mineralization at the La Puerta area.

La Puerta has the potential to host a large, low grade, gold deposit based on the surface results.  In outcrops strong oxide gold mineralization is exposed over a strike length of at about 1000 metres, and over widths of about 50 metres. The contact between volcanic and Mesozoic sedimentary rocks is interpreted  to be 200-250 metres below the surface, and it is believed that the underlying sediments could also host gold mineralization. The base of the initial prospective target, therefore, is 200 to 250 metres, however the prospective target could potentially extend much deeper – see Figure 19 for a conceptual model.

Oxide gold mineralization at surface appears to have favourable cyanide leach characteristics based on preliminary metallurgical test work with a head grade of 1.5 g/t gold. However, more detailed metallurgical testing is needed once drill core is available to test gold recoveries from sub-surface samples.

Figure 19. Conceptual model for stockwork epithermal mineralization at La Puerta

The stockwork and hydrothermal breccia zones at Santa Felicita require further exploration including mapping and sampling, to determine the full potential of this area prior to drilling. The bonanza grade gold

- silver veins at Surupampa also offer high-grade bonanza potential.

52

Silver - gold - base metal quartz veins at Suriloma offer additional potential but at this stage should be lower in priority. The presence of base metal mineralization in veins including copper and tin at Edelmira points to a higher temperature mineralizing source, possibly a nearby porphyry intrusion.

0.1Recommendations 

Recommendations of future work are as follows:

The Company should carry out a 2,000 metre diamond drill program at La Puerta to test oxide stockwork gold mineralization to at least 150m depth in a minimum of 12 drill holes along the central part of the prospect – see Figure 20; 

Metallurgical test work is required to determine gold recovery from drill cores; 

Geophysical exploration at La Puerta is recommended, including Induced Polarization and magnetics, to assist in the targeting deep drill holes; 

Proper ealuation of the sediment hosted gold at Santa Felicita and bonanza veins at Surupampa ; 

Pending success in the initial drill holes, expansion of any drill program should occur accordingly. 

A proposed initial drill program to test the La Puerta area was submitted to the appropriate authorities in Peru in February 2013, with the Environmental Impact Statement (DIA). The proposed drill program is shown in Figure 20. The author supports the initial drill program and proposed budget.

0.2Budget 

As of the end of November 2012, a total of $129,423 had been spent by Darwin at Suriloma and capitalized on the Company’s books. This value does not include amounts paid for mineral concession acquisitions or option payments to purchase any mining concessions.

The proposed budget for the initial drilling program of 2,000 metres is presented in Table 9.

Table 9. Budget ($US) for Initial Drill Program at La Puerta

Direct drilling costs (at $200/metre)	$400,000
Mobilization/Demobilization	$15,000
Water transport for drilling	$15,000
Road and site construction	$22,000
Geology, mapping, sampling	$40,000
Assays (1,000 samples @ $25/sample)	$25,000
Camping and accommodations	$25,000
Travel expenses	$15,000
Metallurgical and petrographic studies	$10,000
Vehicle service and fuel	$20,000
Environmental studies, reclamation, etc.	$15,000
Land access costs	$30,000
Mineral tenure acquisitions and maintenance	$50,000
Office supplies and administration costs	$10,000
Sub-total	$692,000
Contingencies (10%)	$69,200
TOTAL	$761,200

53

Figure 20. Proposed initial drill program for the La Puerta area submitted for approval

54

27.0 References

Albinson,T., Norman, D., Cole, D and Chomiak, B., 2001, Controls on formation of low-sulphidation epithermal deposits in Mexico: Constraints from fluid inclusion and stable isotope data. Society of Economic Geology Special Publication 8, p. 1-32.

Aranda, A., 2012, Estudio petromineralogico de Suriloma. Darwin Resources Internal Report, May 2012, by GeoServices Alberto Aranda E.I.R.L. Lima Peru.

Banco Minero del Peru, 1982, Informe Tecnico del prospecto Edelmira por Ingeniero Esteban Miguel Corcuera. Internal Report by Banco Minero to be found in the file Edelmira. Ingemmet.

Barrick Gold Corporation, 2011, ProEXPLO Conference Presentation, Lima. Instituto de Ingenieros de Minas del Peru.

Certimin, 2013, Informe metalúrgico final: Pruebas de lixiviación de botellas de Suriloma. Prepared for Darwin Peru SAC report number ENE4005.R13. Darwin Internal Report January 2013.

Defilippi, C., Dyer, T. and Tietz, P., 2012, Technical Report on the Shahuindo Heap Leach Project Cajabamba, Peru. Prepared for Sulliden Gold Corporation Ltd. National Instrument 43-101 report by Kappes, Cassiday & Associates and Mine Development Associates, Report Date November 9 2012.

Harvey, C. C. and Browne, P.R.L, 1991, Mixed-layer clay geothermometry in the Wairakei geothermal field, New Zealand. Clay and Clay Minerals, V. 39, No.6, p. 614-621.

Heyl, D. and Livingston, W., 1999, El yacimiento Tres Cruces y la evolucion de sus modelos geneticos de geologia economica. ProExplo’99, Primer volumen de monografias de yacimientos minerals Peruanos: Historia, Exploracion y Geologia, Volumen Luis Hochschild Plaut, Instituto de Ingenieros de Minas del Peru. P. 61-71

Hedenquist, J. W. and Henley, R. W., 1985, Hydrothermal eruptions in the Waiotapu geothermal system, New Zealand: their origin, associated breccias, and relation to precious metal mineralization. Economic Geology v. 80, p. 1640-1668.

Henderson, R. D., 2009, Fruta del Norte Project, Ecuador, NI 43-101 Technical Report prepared for Kinross Gold Corporation. Effective date 31 December 2009.

Henley, R. W., 1985, The geochemical framework of epithermal deposits, in Berger, B. R. and Bethke, P. M., eds., Geology and geochemistry of epithermal system. Review in Economic Geology: Society of Economic Geologists v. 1, p. 1-24.

Hodder, R. W., 2010, The Shahuindo epithermal gold occurrence, Cajabamba Province, Peru: Petrographic reconnaissance and interpretation of shape and size. Downloaded from Sulliden Gold Corporation website, 2012.

Hollister, V. F. and Entwistle, L. P., 1977, Short Note: The Milluachaqui Epithermal Silver District of Northern Peru. Mineralium Deposita v. 12, p. 235 – 238.

55

Ji, J. and Browne, P. R. L, 2000, Relationship between illite crystallinity and temperature in active geothermal systems of New Zealand.

Kaye, C., McCrea, J. and Blanchflower, J., 2011, Technical Report Urumalqui Property, Julcán District, Department of La Libertad, Peru, Latitude 8° 05’ south by longitude 78° 29’ west. National Instrument 43-101 Technical Report for Andean Gold Ltd. and Gitennes Exploration Inc., by Mine and Quarry Engineering Services Inc. (MQes).

Ligarda, R., 2013, PIMA results of samples from Suriloma property, La Libertad, Peru. Darwin Resources Corp internal report, February 2013.

Navarro, P., 2007, Caracteristicas metalogeneticas de los yacimientos asociados al Grupo Calipuy en el norte del Peru, Departamentos de La Libertad y Ancash, INGEMMET, Sociedad Geologica del Peru Boletin 102, p. 79-100;

Navarro, P., Rivera, M., and Monge, R., 2010, Geologia y Metalogenia del Grupo Calipuy (Volcanismo Cenozoico) Segmento Santiago de Chuco, Norte del Peru: Boletin 28, Estudios Regionales, Ingemmet, Ministerio de Energia y Minas, Peru;

Rivera, M., Monge, R. and Navarro., P., 2005, Nuevos datos sobre el volcanismo Cenozoico (Grupo Calipuy) en el norte del Peru: Departamentos de La Libertad y Ancash. Boletin Sociedad Geologica del Peru  99, p. 7-21.

Sillitoe, R., 1993, Epithermal models: Genetic types, geometrical controls and shallow features. Geological Association of Canada Special Paper 40, p. 403-417.

Sillitoe, R. H., 2010, Porphyry Copper Systems. Economic Geology, v. 105, p. 3-41.

Sillitoe, R. and Hedenquist, J., 2003, Linkages between volcanotectonic settings, ore-fluid compositions, and epithermal precious metal deposits. Society of Economic Geologists Special Publication 10, Chapter 16, p. 315-343.

Stewart, J., Evernden, J. and Snelling, N., 1974, Age determinations from Andean Peru: A reconnaissance survey. Geological Society of America Bulletin, 85, p. 1107 – 1116.

Sulliden Gold Corporation, 2012, Developing a low-cost gold operation in Peru, September 2012. Corporate presentation downloaded from Sulliden website 2012.

Teal, L. and Benavides, A., 2010, History and geologic overview of the Yanacocha Mining District, Cajamarca, Peru. Economic Geology, v. 105, p. 1173-1190.

White, P., 2012, Petrology of two samples from Peru for Darwin Resources Corp by Panda Geoscience Ltd, December 2012. Darwin Resources Corp Internal Report.

56

APPENDICES

Appendix 1. Geochemical maps of Suriloma including arsenic, antimony, mercury, bismuth, lead, tin.

Appendix 2. Darwin Resources Corp. Rockchip Geochemical Database

57

Map of Arsenic geochemistry

 

58

Map of Mercury geochemistry

 

59

Map of Antimony geochemistry

 

60

Map of Tin geochemistry

 

61

Map of Bismuth geochemistry

 

62

Map of Lead geochemistry

 

63

APPENDIX 2: GEOCHEMICAL DATABASE OF SURILOMA

64

SURILOMA PROJECT GEOCHEMICAL DATA BASE FEBRUARY 2013

1de 16 

SampleID	Easting	Northing	RL	Grid	IntervalFrom	IntervalTo	Interval	SampleSubType	ChkType	ParentID	StandardID	Comments	Auppm	Auppm2	Hgppm	Agppm	Agppm2	Al%	Asppm	As%	Bappm	Beppm	Bippm	Ca%	Cdppm	Coppm	Crppm
218367	770,796.0	9,134,912.0	3,649.0	PSAD56_17S	0.00	0.30	0.30	CHIPS					1.899			26.9		0.37	6,078		389	-0.5	-5	0.04	-1	2	179
218368	770,837.0	9,134,927.0	3,654.0	PSAD56_17S	0.00	6.00	6.00	CHANNEL					1.184			7.2		0.70	10,400	1.04	182	-0.5	-5	0.05	-1	6	43
218369	770,838.0	9,134,927.0	3,654.0	PSAD56_17S	0.00	0.50	0.50	CHIPS					2.567			2.7		0.69	13,900	1.39	166	-0.5	-5	0.03	-1	7	66
218370	770,838.0	9,134,933.0	3,657.0	PSAD56_17S	0.00	1.00	1.00	CHANNEL				CANAL 01	1.258			45.7		0.58	12,600	1.26	202	-0.5	-5	0.02	-1	7	66
218371	770,837.0	9,134,933.0	3,657.0	PSAD56_17S	0.00	1.80	1.80	CHANNEL				CANAL 01	1.431			3.0		1.06	16,000	1.60	983	1.1	-5	0.15	-1	5	139
218372	770,819.0	9,134,939.0	3,657.0	PSAD56_17S	0.00	4.00	4.00	CHANNEL					0.028			-0.2		0.95	3,912		50	-0.5	-5	0.03	-1	5	15
218373	770,805.0	9,134,958.0	3,653.0	PSAD56_17S	0.00	0.20	0.20	CHIPS					1.626			3.2		0.41	8,205		42	-0.5	-5	0.04	-1	3	112
218374	770,831.0	9,134,915.0	3,652.0	PSAD56_17S	0.00	0.30	0.30	CHANNEL					1.721			165.0	165	0.40	7,149		53	-0.5	-5	0.01	-1	3	234
218375	770,892.0	9,134,895.0	3,659.0	PSAD56_17S	0.00	1.00	1.00	CHANNEL				CANAL 02	4.598			3.9		0.52	25,000	2.50	134	-0.5	-5	0.02	-1	5	71
218376	770,892.0	9,134,894.0	3,659.0	PSAD56_17S	0.00	1.00	1.00	CHANNEL				CANAL 02	6.299			3.6		0.52	23,000	2.30	586	-0.5	-5	0.04	-1	9	54
218377	770,892.0	9,134,893.0	3,659.0	PSAD56_17S	0.00	1.00	1.00	CHANNEL				CANAL 02	3.512			2.6		0.66	19,600	1.96	127	-0.5	-5	0.03	-1	8	101
218378	771,141.0	9,134,796.0	3,598.0	PSAD56_17S	0.00	0.70	0.70	CHANNEL					2.205			2.2		0.56	7,968		299	0.8	-5	0.13	-1	6	70
218379	770,794.0	9,133,513.0	3,552.0	PSAD56_17S	0.00	0.30	0.30	CHIPS					0.157			0.2		0.75	7,702		54	2.4	-5	0.02	-1	12	47
218383	770,686.0	9,133,630.0	3,570.0	PSAD56_17S	0.00	3.00	3.00	CHIPS					0.116			11.1		0.52	947		645	-0.5	-5	0.04	-1	2	172
218384	770,464.0	9,133,755.0	3,582.0	PSAD56_17S	0.00	0.30	0.30	CHANNEL					0.018			-0.2		0.42	95		915	-0.5	-5	1.69	-1	3	132
218385	770,247.0	9,133,800.0	3,579.0	PSAD56_17S	0.00	0.40	0.40	CHANNEL				CANAL 03	0.014			1.9		0.45	713		566	-0.5	-5	0.02	-1	1	85
218386	770,248.0	9,133,800.0	3,579.0	PSAD56_17S	0.00	0.80	0.80	CHANNEL				CANAL 03	0.008			3.0		0.55	658		2503	-0.5	-5	0.02	-1	1	207
218387	770,156.0	9,133,733.0	3,577.0	PSAD56_17S	0.00	0.20	0.20	FLOAT					0.009			409.0	409	0.14	40		84	-0.5	-5	0.01	6	-1	215
218388	770,086.0	9,135,293.0	3,653.0	PSAD56_17S				DUMP					1.617			190.0	190	0.15	2,815		13	-0.5	-5	-0.01	-1	3	197
218389	769,332.0	9,135,132.0	3,642.0	PSAD56_17S	0.00	0.10	0.10	CHIPS					0.005			2.2		0.18	15		51	-0.5	-5	0.04	-1	2	268
218390	769,223.0	9,135,224.0	3,620.0	PSAD56_17S	0.00	0.15	0.15	CHANNEL				CANAL 04	11.170	11.170		3.6		0.20	14,600	1.46	1826	-0.5	-5	0.12	-1	3	174
218391	769,224.0	9,135,225.0	3,620.0	PSAD56_17S	0.00	1.00	1.00	CHANNEL				CANAL 04	2.290			0.6		0.80	7,586		455	-0.5	-5	0.09	-1	4	75
218392	769,222.0	9,135,223.0	3,621.0	PSAD56_17S	0.00	1.00	1.00	CHANNEL				CANAL 04	6.283			1.8		0.38	10,500	1.05	2189	1.2	-5	0.10	-1	4	108
218393	769,168.0	9,135,254.0	3,613.0	PSAD56_17S				DUMP					0.408			3.4		0.55	5,639		116	-0.5	-5	0.03	-1	9	41
218394	769,169.0	9,135,252.0	3,614.0	PSAD56_17S	0.00	0.20	0.20	CHIPS					11.920	11.920		122.0	122	0.24	16,500	1.65	265	-0.5	-5	0.07	-1	4	296
218395	770,412.0	9,135,192.0	3,683.0	PSAD56_17S	0.00	1.20	1.20	CHANNEL					1.722			473.0	473	0.28	2,474		146	-0.5	-5	0.06	-1	3	207
218396	770,440.0	9,135,158.0	3,692.0	PSAD56_17S				DUMP					2.953			54.8		0.19	2,765		3144	-0.5	-5	0.05	-1	2	205
218397	770,481.0	9,135,120.0	3,700.0	PSAD56_17S				DUMP					2.143			448.0	448	0.12	3,754		20	-0.5	-5	-0.01	9	3	539
218398	770,526.0	9,135,084.0	3,699.0	PSAD56_17S				DUMP					2.288			51.3		0.20	4,763		24	-0.5	-5	-0.01	-1	4	204
218399	770,528.0	9,135,080.0	3,700.0	PSAD56_17S				DUMP					2.253			95.0		0.18	5,648		32	-0.5	-5	0.02	-1	3	203
218400	770,588.0	9,135,015.0	3,683.0	PSAD56_17S				DUMP					2.375			90.0		0.12	5,051		25	-0.5	-5	0.01	5	2	476
218971									STD		OREAS 52c		0.333			1.1		1.73	-3		165	-0.5	-5	1.58	-1	22	47
218972									STD		OREAS 62d		10.970	10.970		9.3		0.69	15		57	-0.5	-5	8.43	-1	8	11
218973									STD		OREAS 54Pa		2.999			4.9		1.00	-3		28	-0.5	16	1.48	-1	23	24
218974									STD		OREAS 22b		-0.005			-0.2		0.01	-3		6	-0.5	-5	-0.01	-1	3	23
218975									STD		OREAS 62d		10.930	10.930		9.6		0.72	24		57	-0.5	-5	8.90	-1	8	14
218976									STD		OREAS 22b		-0.005			-0.2		0.01	-3		6	-0.5	-5	-0.01	-1	3	20
218977									STD		OREAS 54Pa		3.057			4.7		1.00	13		29	-0.5	19	1.49	-1	24	23
218978									STD		OREAS 52c		0.325			0.6		1.71	-3		154	0.5	-5	1.55	-1	19	47
218979									STD		OREAS 62d		11.030	11.030		9.3		0.73	-3		56	-0.5	-5	8.69	-1	9	14
218980									STD		OREAS 22b		-0.005			-0.2		0.01	-3		6	-0.5	-5	-0.01	-1	2	22
218981									STD		OREAS 54Pa		3.050			4.2		1.02	-3		28	-0.5	19	1.51	-1	26	27
218982									STD		OREAS 62d		10.890	10.890		9.4		0.73	11		57	-0.5	6	8.95	-1	9	14
218983									STD		OREAS 52c		0.332			1.0		1.70	-3		158	0.5	-5	1.53	-1	17	44
218984									STD		OREAS 22b		-0.005			-0.2		0.01	-3		6	-0.5	-5	-0.01	-1	4	23
218985									STD		OREAS 54Pa		3.010			4.6		1.03	-3		28	-0.5	6	1.54	-1	24	26
218986									STD		OREAS 52c		0.321			0.9		1.72	-3		167	-0.5	-5	1.56	-1	18	46
218987									STD		OREAS 62d		10.870	10.870		8.9		0.73	35		55	0.5	-5	8.92	-1	7	13
218988									STD		OREAS 22b		-0.005			0.2		0.01	-3		6	-0.5	-5	-0.01	-1	1	20
218989									STD		OREAS 52c		0.326			0.7		1.73	-3		157	-0.5	-5	1.56	-1	18	46
218990									STD		OREAS 54Pa		3.011			4.7		0.98	-3		27	-0.5	14	1.47	-1	23	24
218991	766,852.0	9,137,558.0		PSAD56_17S	0.00	1.00	1.00	CHANNEL					0.029		0.02	-0.2		0.81	197		46	0.9	-5	0.04	-1	6	16
218992	766,705.0	9,137,479.0	3,359.0	PSAD56_17S	0.00	0.25	0.25	CHANNEL					127.000	127.000	0.46	38.6		0.92	2,556		142	0.9	16	0.04	3	12	108
218993	766,509.0	9,137,358.0	3,345.0	PSAD56_17S	0.00	0.20	0.20	CHANNEL					0.050		-0.02	-0.2		1.65	138		47	1.3	-5	-0.01	-1	18	21
218994	766,531.0	9,137,297.0	3,347.0	PSAD56_17S	0.00	2.50	2.50	CHANNEL					0.207		-0.02	0.3		0.85	404		30	-0.5	-5	0.02	-1	9	35
218995	766,528.0	9,137,279.0	3,348.0	PSAD56_17S	0.00	4.00	4.00	CHANNEL					0.161		0.03	0.6		0.46	349		23	-0.5	-5	0.02	-1	11	40
218996	766,805.0	9,135,870.0	3,746.0	PSAD56_17S				DUMP					0.330		50.00	179.0	179	0.07	753		10	-0.5	27	0.03	61	6	127
218997	766,806.0	9,135,870.0	3,746.0	PSAD56_17S				DUMP					0.142		50.00	2,206.0	2,206	0.01	5,501		12	-0.5	11	0.01	821	2	94
218998	766,806.0	9,135,871.0	3,746.0	PSAD56_17S	0.00	8.00	8.00	CHIPS					0.066		12.02	11.9		0.21	166		44	-0.5	-5	-0.01	1	3	54
219011	770,589.0	9,135,014.0	3,660.0	PSAD56_17S				DUMP					2.198			227.0	227	0.56	4,731		38	-0.5	-5	0.05	-1	2	212
219012	770,678.0	9,134,970.0	3,659.0	PSAD56_17S				DUMP					7.511			5.1		0.17	14,400	1.44	1386	-0.5	-5	0.05	-1	2	181
219013	768,976.0	9,134,801.0	3,771.0	PSAD56_17S	0.00	1.00	1.00	CHIPS					0.013			0.5		0.02	77		53	-0.5	-5	-0.01	-1	1	276
219014	769,024.0	9,134,814.0	3,774.0	PSAD56_17S	0.00	1.50	1.50	CHIPS					0.012			0.7		0.04	46		50	-0.5	-5	0.54	-1	6	594
219015	766,887.0	9,135,545.0	3,817.0	PSAD56_17S				DUMP					0.187			69.6		0.40	518		30	-0.5	14	0.04	-1	7	211
219016	771,230.0	9,134,771.0	3,574.0	PSAD56_17S	0.00	1.30	1.30	CHIPS					0.301			0.9		0.56	3,120		679	0.7	-5	0.06	-1	5	71
219017	771,420.0	9,134,669.0	3,575.0	PSAD56_17S	0.00	1.20	1.20	CHANNEL					0.523			1.2		0.65	4,547		643	-0.5	-5	-0.01	-1	2	104
219018	771,421.0	9,134,669.0	3,575.0	PSAD56_17S	0.00	0.40	0.40	CHANNEL					0.796			3.7		0.31	4,893		4890	-0.5	-5	-0.01	-1	2	150
219019	771,419.0	9,134,669.0	3,575.0	PSAD56_17S	0.00	1.20	1.20	CHANNEL					0.497			2.5		0.59	2,976		5439	-0.5	-5	0.04	-1	2	49
219020	771,462.0	9,134,645.0	3,573.0	PSAD56_17S	0.00	1.00	1.00	CHIPS					0.868			6.5		0.61	4,468		5198	-0.5	-5	0.04	-1	3	149
219021	771,593.0	9,134,551.0	3,562.0	PSAD56_17S	0.00	1.30	1.30	CHIPS					0.960			6.9		0.56	2,419		3853	-0.5	-5	0.04	-1	2	105
219022	771,654.0	9,134,523.0	3,552.0	PSAD56_17S	0.00	5.00	5.00	CHIPS					0.242			1.7		0.52	2,518		5737	-0.5	-5	0.04	-1	3	79
219023	771,739.0	9,134,480.0	3,529.0	PSAD56_17S	0.00	0.50	0.50	CHIPS					0.275			0.9		0.59	2,455		246	-0.5	-5	0.01	-1	2	126
219024	771,863.0	9,134,419.0	3,486.0	PSAD56_17S	0.00	0.10	0.10	CHIPS					0.091			0.6		0.52	573		588	-0.5	-5	0.04	-1	2	91
219025	770,477.0	9,135,042.0	3,699.0	PSAD56_17S	0.00	0.20	0.20	CHANNEL				TR-03	9.630		5.95	849.0	849	0.16	25,400	2.54	33	-0.5	-5	0.04	22	3	152
219026	771,594.0	9,134,595.0	3,567.0	PSAD56_17S	0.00	1.00	1.00	CHIPS					0.274		1.11	3.8		0.51	2,446		1819	-0.5	-5	0.08	-1	3	75
219027	771,605.0	9,134,615.0	3,566.0	PSAD56_17S	0.00	1.20	1.20	CHIPS					0.015		1.35	1.3		0.79	234		41	0.7	-5	0.03	-1	3	33
219028	771,648.0	9,134,519.0	3,545.0	PSAD56_17S	0.00	0.50	0.50	CHIPS					0.574		0.52	17.5		0.21	3,209		1112	-0.5	-5	-0.01	-1	2	140
219029	770,569.0	9,133,690.0	3,578.0	PSAD56_17S				FLOAT					0.008		0.08	0.6		0.46	29		79	-0.5	-5	0.03	-1	2	124
219030	770,504.0	9,133,743.0	3,585.0	PSAD56_17S	0.00	0.15	0.15	SUBCROP					0.031		4.16	132.0	132	0.27	84		927	-0.5	-5	0.04	1	2	127
219031	770,179.0	9,133,770.0	3,571.0	PSAD56_17S				FLOAT					0.027		6.22	116.0	116	0.18	176		29	-0.5	-5	0.02	2	-1	222
219032	769,165.0	9,135,253.0	3,607.0	PSAD56_17S				DUMP					0.054		0.07	0.7		0.73	1,880		19	0.8	-5	0.21	-1	16	16
219033	769,166.0	9,135,254.0	3,608.0	PSAD56_17S				DUMP					5.594		0.41	56.4		0.19	13,100	1.31	152	-0.5	-5	0.04	-1	5	195
219039	770,844.0	9,134,893.0	3,655.0	PSAD56_17S	0.00	1.20	1.20	CHANNEL				TR-01a	0.193		0.70	-0.2		0.62	1,367		44	-0.5	-5	0.04	-1	3	43

SURILOMA PROJECT GEOCHEMICAL DATA BASE FEBRUARY 2013

2de 16 

SampleID	Easting	Northing	RL	Grid	IntervalFrom	IntervalTo	Interval	SampleSubType	ChkType	ParentID	StandardID	Comments	Auppm	Auppm2	Hgppm	Agppm	Agppm2	Al%	Asppm	As%	Bappm	Beppm	Bippm	Ca%	Cdppm	Coppm	Crppm
219040	770,843.0	9,134,896.0	3,655.0	PSAD56_17S	1.20	2.60	1.40	CHANNEL				TR-01a	7.344		2.83	1.6		0.59	22,800	2.28	206	0.8	-5	0.04	-1	3	57
219041	770,835.0	9,134,904.0	3,655.0	PSAD56_17S	0.00	2.20	2.20	CHANNEL				TR-01b	0.114		1.33	0.3		0.63	1,713		31	-0.5	-5	0.03	-1	2	28
219042	770,835.0	9,134,906.0	3,655.0	PSAD56_17S	2.20	2.45	0.25	CHANNEL				TR-01b	7.591		2.60	11.3		0.29	22,000	2.20	185	-0.5	-5	0.03	-1	2	145
219043	770,835.0	9,134,907.0	3,655.0	PSAD56_17S	2.45	4.25	1.80	CHANNEL				TR-01b	0.377		2.35	-0.2		0.51	1,900		89	-0.5	-5	0.03	-1	4	36
219044	770,838.0	9,134,907.0	3,655.0	PSAD56_17S	4.25	5.85	1.60	CHANNEL				TR-01b	0.663		1.93	-0.2		0.63	5,586		138	-0.5	-5	0.05	-1	5	47
219045	770,832.0	9,134,914.0	3,655.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-01c	1.388		3.50	0.7		0.62	4,131		94	-0.5	-5	0.03	-1	3	44
219046	770,832.0	9,134,916.0	3,655.0	PSAD56_17S	2.00	4.00	2.00	CHANNEL				TR-01c	0.902		3.31	1.3		0.65	7,107		42	-0.5	-5	0.02	-1	7	26
219047	770,831.0	9,134,918.0	3,655.0	PSAD56_17S	4.00	7.00	3.00	CHANNEL				TR-01c	1.183		2.13	29.3		0.52	5,845		74	-0.5	-5	0.02	-1	4	66
219048	770,831.0	9,134,919.0	3,655.0	PSAD56_17S	0.00	0.40	0.40	CHANNEL					2.346		2.40	171.0	171	0.25	7,148		133	-0.5	-5	0.02	-1	-1	151
219049	770,826.0	9,134,931.0	3,656.0	PSAD56_17S	0.00	3.00	3.00	CHANNEL				TR-01d	1.966		3.00	4.6		0.50	11,300	1.13	192	-0.5	-5	0.03	-1	4	52
219050	770,826.0	9,134,934.0	3,656.0	PSAD56_17S	3.00	5.00	2.00	CHANNEL				TR-01d	2.861		1.63	2.3		0.73	10,900	1.09	692	-0.5	-5	0.07	-1	6	46
219051	770,826.0	9,134,936.0	3,656.0	PSAD56_17S	5.00	7.00	2.00	CHANNEL				TR-01d	1.768		0.78	1.5		0.50	7,688		455	-0.5	-5	0.03	-1	3	64
219052	770,826.0	9,134,938.0	3,656.0	PSAD56_17S	7.00	9.00	2.00	CHANNEL				TR-01d	0.077		1.80	-0.2		0.72	3,220		71	-0.5	-5	0.03	-1	6	24
219053	770,826.0	9,134,940.0	3,656.0	PSAD56_17S	9.00	11.00	2.00	CHANNEL				TR-01d	0.274		1.02	-0.2		0.71	4,020		105	-0.5	-5	0.03	-1	2	46
219054	770,826.0	9,134,942.0	3,656.0	PSAD56_17S	11.00	13.00	2.00	CHANNEL				TR-01d	0.347		1.38	-0.2		0.56	2,664		105	-0.5	-5	0.02	-1	3	42
219055	770,827.0	9,134,927.0	3,657.0	PSAD56_17S	0.00	0.70	0.70	CHANNEL					3.549		2.11	9.8		0.46	18,700	1.87	214	-0.5	-5	0.02	-1	4	72
219056	770,821.0	9,134,942.0	3,658.0	PSAD56_17S	0.00	3.80	3.80	CHANNEL					0.270		2.78	-0.2		0.71	3,562		90	-0.5	-5	0.03	-1	4	23
219057	770,817.0	9,134,946.0	3,658.0	PSAD56_17S	0.00	1.10	1.10	CHANNEL					0.226		3.45	0.3		0.79	2,985		140	-0.5	-5	0.08	-1	5	84
219058	770,807.0	9,134,954.0	3,657.0	PSAD56_17S	0.00	2.80	2.80	CHANNEL					-0.005		1.76	-0.2		0.87	188		18	2.0	-5	0.07	-1	5	19
219059	770,583.0	9,135,031.0	3,683.0	PSAD56_17S	0.00	1.30	1.30	CHANNEL					8.693		14.65	106.0	106	0.18	14,500	1.45	1162	-0.5	-5	0.03	3	2	140
219060	770,579.0	9,135,031.0	3,681.0	PSAD56_17S	1.60	3.60	2.00	CHANNEL				TR-02	3.789		0.65	7.9		0.46	9,471		58	-0.5	-5	0.04	-1	2	71
219061	770,580.0	9,135,033.0	3,681.0	PSAD56_17S	0.50	1.60	1.10	CHANNEL				TR-02	4.469		2.57	32.6		0.19	12,900	1.29	24	-0.5	-5	0.03	-1	4	157
219062	770,580.0	9,135,034.0	3,681.0	PSAD56_17S	0.00	0.50	0.50	CHANNEL				TR-02	4.129		1.49	5.9		0.29	8,286		14	-0.5	-5	0.02	-1	3	62
219063	770,479.0	9,135,042.0	3,690.0	PSAD56_17S	0.20	2.20	2.00	CHANNEL				TR-03	0.656		0.79	3.1		0.36	4,064		22	-0.5	-5	0.09	-1	2	56
219064	770,479.0	9,135,044.0	3,690.0	PSAD56_17S	2.20	5.20	3.00	CHANNEL				TR-03	0.088		0.95	-0.2		0.84	1,824		21	1.3	-5	0.15	-1	8	23
219065	770,482.0	9,135,056.0	3,690.0	PSAD56_17S	0.00	1.00	1.00	CHANNEL					4.803		1.02	8.8		0.40	14,900	1.49	121	-0.5	-5	0.09	-1	3	133
219066	770,482.0	9,135,060.0	3,692.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.005		2.36	-0.2		0.88	95		17	3.2	-5	0.07	-1	9	19
219067	770,512.0	9,135,091.0	3,697.0	PSAD56_17S	0.00	1.30	1.30	CHANNEL				TR-04	0.384		0.20	1.3		0.65	3,014		12	-0.5	-5	0.10	-1	3	49
219068	770,512.0	9,135,090.0	3,697.0	PSAD56_17S	1.30	2.10	0.80	CHANNEL				TR-04	3.984		7.57	871.0	871	0.15	4,449		23	-0.5	-5	0.02	31	1	141
219069	770,511.0	9,135,090.0	3,697.0	PSAD56_17S	2.10	2.60	0.50	CHANNEL				TR-04	4.274		0.62	12.1		0.41	27,200	2.72	10	-0.5	-5	0.06	-1	4	58
219070	770,510.0	9,135,088.0	3,697.0	PSAD56_17S	3.40	4.90	1.50	CHANNEL				TR-04	1.333		0.81	44.9		0.50	9,164		12	-0.5	-5	0.06	-1	4	51
219071	766,703.0	9,135,593.0	3,822.0	PSAD56_17S				DUMP					0.198		50.00	596.0	596	0.56	4,189		81	0.6	41	0.15	30	10	183
219072	772,000.0	9,134,400.0	3,434.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.088		1.03	1.2		0.46	969		271	1.9	-5	0.05	-1	7	127
219073	768,728.0	9,136,119.0	3,291.0	PSAD56_17S	0.00	2.50	2.50	CHIPS					0.063		0.42	0.8		0.56	449		41	0.8	-5	0.04	-1	8	113
219074	766,703.0	9,137,487.0	3,374.0	PSAD56_17S	0.00	0.30	0.30	CHIPS					138.000	138.000	0.36	55.3		0.58	2,754		173	0.7	29	0.02	5	8	239
219075	766,528.0	9,137,310.0	3,341.0	PSAD56_17S	0.00	0.50	0.50	CHIPS					1.445		0.09	11.3		0.08	1,263		12	-0.5	28	0.02	2	2	193
219076	766,539.0	9,137,097.0	3,352.0	PSAD56_17S	0.00	0.50	0.50	CHANNEL					0.458		0.04	1.8		1.18	111		27	-0.5	-5	0.04	-1	5	61
219077	766,328.0	9,136,731.0	3,348.0	PSAD56_17S	0.00	1.00	1.00	CHIPS					0.059		0.12	14.9		0.36	70		117	-0.5	-5	0.03	-1	12	175
219078	767,270.0	9,135,744.0	3,697.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.114		14.50	146.0	146	0.24	369		30	-0.5	308	0.03	81	6	90
219079	767,271.0	9,135,743.0	3,695.0	PSAD56_17S	0.00	0.20	0.20	CHANNEL					1.274		50.00	616.0	616	0.08	322		7	-0.5	2,801	0.03	1796	7	197
219080	766,611.0	9,135,853.0	3,690.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.125		3.98	14.2		0.26	661		21	-0.5	9	-0.01	1	6	153
219081	766,608.0	9,135,854.0	3,690.0	PSAD56_17S				DUMP					0.224		50.00	264.0	264	0.02	463		13	-0.5	20	-0.01	190	4	265
219082	766,607.0	9,135,853.0	3,690.0	PSAD56_17S				DUMP					0.385		50.00	915.0	915	0.08	1,021		7	-0.5	54	0.03	1224	10	216
219086	766,805.0	9,137,011.0	3,489.0	PSAD56_17S	0.00	3.00	3.00	CHANNEL					0.028		0.15	0.4		0.98	55		28	0.8	-5	0.01	-1	29	30
219087	767,256.0	9,137,123.0	3,352.0	PSAD56_17S	0.00	1.00	1.00	CHANNEL					0.028		0.09	1.1		0.47	104		439	1.0	-5	0.03	2	9	83
219089	770,110.0	9,135,257.0	3,670.0	PSAD56_17S	0.00	0.60	0.60	CHANNEL					2.726		1.47	29.6		0.27	4,124		102	-0.5	-5	0.11	7	2	80
219090	770,183.0	9,135,213.0	3,678.0	PSAD56_17S	0.00	0.00	0.00	SUBCROP					2.007		1.21	30.4		0.19	2,142		51	-0.5	-5	0.07	5	2	155
219091	770,060.0	9,135,300.0	3,657.0	PSAD56_17S				DUMP					1.621		1.33	9.0		0.14	970		63	-0.5	-5	0.25	1	2	70
219092	769,261.0	9,135,212.0	3,624.0	PSAD56_17S	0.00	1.00	1.00	CHANNEL					0.076		0.48	0.4		0.76	136		58	-0.5	-5	0.13	-1	4	14
219093	769,172.0	9,135,256.0	3,605.0	PSAD56_17S	0.00	2.80	2.80	CHANNEL					0.018		0.31	0.5		0.84	979		157	0.6	-5	0.25	-1	5	13
219094	768,910.0	9,135,295.0	3,600.0	PSAD56_17S	0.00	0.40	0.40	CHANNEL					0.101		0.03	1.4		0.46	1,403		315	2.3	-5	0.19	2	10	26
219095									STD		OREAS 22b		-0.005		-0.02	0.6		0.01	13		6	-0.5	-5	-0.01	-1	2	23
219096	767,353.0	9,135,724.0	3,694.0	PSAD56_17S	0.00	1.20	1.20	CHANNEL					0.118		0.31	0.5		0.22	361		16	-0.5	-5	-0.01	-1	4	92
219097	767,398.0	9,135,686.0	3,711.0	PSAD56_17S	0.00	1.00	1.00	CHIPS					0.057		0.46	6.8		0.26	316		76	-0.5	-5	0.02	-1	2	49
219098	767,480.0	9,135,609.0	3,725.0	PSAD56_17S	0.00	0.25	0.25	CHANNEL					0.875		50.00	202.0	202	0.10	7,026		8	0.5	1,208	0.09	79	16	46
219099	767,379.0	9,136,020.0	3,588.0	PSAD56_17S	0.00	0.50	0.50	CHANNEL					0.011		0.17	-0.2		0.37	148		39	1.2	-5	0.05	-1	5	57
219100	767,046.0	9,136,919.0	3,460.0	PSAD56_17S				FLOAT					0.006		0.07	-0.2		0.25	170		47	-0.5	-5	0.02	-1	1	108
219147	766,240.0	9,137,960.0	3,125.0	PSAD56_17S	0.00	2.00	2.00	OUTCROP					0.013		-0.02	-0.2		0.26	42		12	-0.5	-5	0.01	-1	3	87
219148	766,250.0	9,137,970.0	3,131.0	PSAD56_17S	0.00	1.00	1.00	OUTCROP					0.015		0.02	-0.2		0.21	46		10	-0.5	-5	-0.01	-1	7	100
219335	768,725.0	9,136,113.0		PSAD56_17S	0.00	1.00	1.00	CHANNEL					0.052		0.17	0.3		0.93	134		37	1.0	-5	0.18	-1	5	8
219336	770,076.0	9,135,475.0		PSAD56_17S	0.00	3.00	3.00	OUTCROP					0.008		3.04	-0.2		0.52	76		44	-0.5	-5	0.04	-1	-1	14
219337	769,519.0	9,135,587.0		PSAD56_17S	0.00	0.02	0.02	CHANNEL					0.472		0.15	5.9		0.49	2,630		544	1.3	-5	0.12	4	21	45
219338	769,306.0	9,135,723.0		PSAD56_17S	0.00	0.05	0.05	CHANNEL					0.219		1.90	0.7		0.14	94		17	-0.5	-5	0.03	2	-1	112
219339	770,311.0	9,133,800.0		PSAD56_17S	0.00	0.60	0.60	CHANNEL					0.064		1.32	11.2		0.32	1,684		1925	-0.5	-5	0.03	3	2	84
219401	770,579.0	9,135,029.0	3,681.0	PSAD56_17S	3.60	5.60	2.00	CHANNEL				TR-02	0.179		0.39	1.2		0.37	2,724		103	-0.5	-5	0.03	4	2	13
219402	770,580.0	9,135,026.0	3,681.0	PSAD56_17S	5.60	7.60	2.00	CHANNEL				TR-02	0.214		0.68	0.7		0.43	4,223		41	-0.5	-5	0.04	6	4	16
219403	770,580.0	9,135,026.0	3,681.0	PSAD56_17S	7.60	9.60	2.00	CHANNEL				TR-02	0.161		0.53	0.6		0.46	1,107		72	-0.5	-5	0.08	-1	3	7
219404	770,581.0	9,135,024.0	3,681.0	PSAD56_17S	9.60	11.60	2.00	CHANNEL				TR-02	0.128		0.53	-0.2		0.56	1,926		51	1.0	-5	0.10	-1	10	5
219405	770,582.0	9,135,022.0	3,681.0	PSAD56_17S	11.60	13.60	2.00	CHANNEL				TR-02	0.149		0.43	-0.2		0.55	989		43	-0.5	-5	0.09	-1	8	7
219406	770,740.0	9,134,900.0	3,640.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-05	0.110		0.54	-0.2		0.89	925		72	0.7	-5	0.11	-1	11	15
219407	770,742.0	9,134,900.0	3,640.0	PSAD56_17S	2.00	4.00	2.00	CHANNEL				TR-05	0.007		0.50	-0.2		0.50	534		46	-0.5	-5	0.09	-1	3	19
219408	770,744.0	9,134,900.0	3,640.0	PSAD56_17S	4.00	6.00	2.00	CHANNEL				TR-05	-0.005		0.89	-0.2		0.44	230		25	-0.5	-5	0.08	-1	3	20
219409	770,746.0	9,134,901.0	3,640.0	PSAD56_17S	6.00	8.00	2.00	CHANNEL				TR-05	0.045		2.37	-0.2		0.45	531		27	-0.5	-5	0.09	-1	4	16
219410	770,748.0	9,134,901.0	3,641.0	PSAD56_17S	8.00	10.00	2.00	CHANNEL				TR-05	0.076		1.17	-0.2		0.46	697		64	-0.5	-5	0.15	-1	6	21
219411	770,750.0	9,134,901.0	3,641.0	PSAD56_17S	10.00	12.00	2.00	CHANNEL				TR-05	0.029		0.65	-0.2		0.58	1,743		64	0.5	-5	0.13	1	4	16
219412	770,752.0	9,134,902.0	3,641.0	PSAD56_17S	12.00	14.00	2.00	CHANNEL				TR-05	0.233		0.85	0.3		0.92	967		135	0.6	-5	0.11	-1	8	7
219413									FDUP	219409			0.024		2.16	-0.2		0.44	539		33	-0.5	-5	0.09	-1	3	17
219414									STD		OREAS 52c		0.364		0.06	0.4		1.74	24		148	-0.5	-5	1.37	-1	18	47
219415	770,745.0	9,134,903.0	3,642.0	PSAD56_17S	0.00	2.60	2.60	CHANNEL					0.235		0.32	-0.2		0.48	1,512		37	-0.5	-5	0.10	1	4	28
51000017	766,919.0	9,135,883.0	3,752.0	PSAD56_17S	0.00	0.00	0.00	CHANNEL					0.132		1.19	30.2		0.49	536		35	-0.5	17	0.03	5	5	117
51000018	766,874.0	9,135,886.0	3,778.0	PSAD56_17S	0.00	0.00	0.00	CHANNEL					0.033		1.26	1.7		0.29	229		22	-0.5	-5	-0.01	-1	-1	81
51000019	766,863.0	9,135,730.0	3,820.0	PSAD56_17S	0.00	0.00	0.00	SELECT					0.007		0.09	0.9		0.53	127		59	0.6	-5	0.02	4	22	52
51000020	766,766.0	9,135,662.0	3,829.0	PSAD56_17S	0.00	0.00	0.00	CHANNEL					0.097		0.98	31.1		0.37	306		16	-0.5	45	0.01	-1	8	116

SURILOMA PROJECT GEOCHEMICAL DATA BASE FEBRUARY 2013

3de 16 

SampleID	Easting	Northing	RL	Grid	IntervalFrom	IntervalTo	Interval	SampleSubType	ChkType	ParentID	StandardID	Comments	Auppm	Auppm2	Hgppm	Agppm	Agppm2	Al%	Asppm	As%	Bappm	Beppm	Bippm	Ca%	Cdppm	Coppm	Crppm
51000021	766,639.0	9,135,489.0	3,872.0	PSAD56_17S	0.00	0.00	0.00	SELECT					0.311		1.60	19.8		0.30	523		149	-0.5	-5	0.04	-1	-1	152
51000022	766,729.0	9,135,480.0		PSAD56_17S	0.00	0.00	0.00	CHANNEL					0.818		12.62	80.7		0.30	1,146		33	-0.5	-5	0.02	3	-1	146
51000023	766,649.0	9,135,497.0	3,870.0	PSAD56_17S	0.00	0.00	0.00	SELECT					0.018		0.03	0.8		0.53	222		71	-0.5	-5	0.75	-1	-1	64
51000024	766,400.0	9,135,533.0	3,787.0	PSAD56_17S				DUMP					0.111		69.11	1,382.0		0.18	1,844		8	-0.5	106	0.01	99	2	185
51000025	766,476.0	9,135,681.0	3,725.0	PSAD56_17S	0.00	0.00	0.00	CHIPS					0.009		0.20	51.2		0.43	316		71	-0.5	-5	0.05	1	-1	52
51000026	767,465.0	9,135,614.0	3,742.0	PSAD56_17S	0.00	0.00	0.00	CHIPS					0.173		5.07	29.4		0.22	191		59	-0.5	29	0.04	7	3	119
51000027	767,279.0	9,135,423.0	3,824.0	PSAD56_17S	0.00	0.00	0.00	SELECT					0.232		0.36	2.4		0.51	713		37	-0.5	-5	0.06	1	1	75
51000028	767,216.0	9,135,424.0	3,836.0	PSAD56_17S	0.00	0.00	0.00	SELECT					0.342		1.79	177.0		0.39	409		21	-0.5	-5	0.02	-1	-1	82
51000029	767,216.0	9,135,426.0		PSAD56_17S				DUMP					0.753		8.38	201.0		0.61	1,210		27	0.7	25	0.04	-1	-1	152
51000030	767,092.0	9,135,440.0	3,853.0	PSAD56_17S	0.00	0.00	0.00	CHANNEL					0.493		14.25	37.3		0.58	1,193		12	-0.5	51	0.05	2	-1	76
51000031	766,856.0	9,135,464.0	3,896.0	PSAD56_17S	0.00	0.00	0.00	SELECT					3.334		2.35	21.6		0.47	1,360		18	0.6	8	0.01	-1	3	127
51000032	766,300.0	9,135,400.0	3,815.0	PSAD56_17S	0.00	0.00	0.00	CHANNEL					0.014		0.10	2.1		0.30	40		8	-0.5	-5	-0.01	-1	-1	89
51000033	766,290.0	9,135,530.0	3,764.0	PSAD56_17S				DUMP					0.127		12.06	144.0		0.29	293		35	-0.5	21	0.03	13	6	116
51000038	768,066.0	9,135,162.0	3,748.0	PSAD56_17S	0.00	0.00	0.00	SELECT					0.580		5.87	18.9		0.21	508		597	1.1	-5	0.02	4	2	184
51000039	767,787.0	9,135,230.0	3,772.0	PSAD56_17S	0.00	0.00	0.00	SELECT					0.207		2.26	31.2		0.26	390		38	-0.5	-5	0.09	4	-1	145
51000040	767,380.0	9,135,310.0		PSAD56_17S	0.00	0.00	0.00	CHANNEL					0.387		0.73	11.4		0.22	700		5	-0.5	28	0.06	2	5	218
51000041	767,714.0	9,135,450.0	3,715.0	PSAD56_17S	0.00	0.00	0.00	CHANNEL					-0.005		0.03	0.6		0.19	20		19	-0.5	-5	3.83	-1	3	377
51000042	767,786.0	9,135,470.0	3,705.0	PSAD56_17S	0.00	0.00	0.00	SELECT					0.096		6.42	20.9		0.23	160		2063	1.1	-5	0.05	41	11	183
51000043	767,866.0	9,135,474.0	3,704.0	PSAD56_17S	0.00	0.00	0.00	SELECT					0.123		6.95	8.7		0.13	210		18	-0.5	-5	0.03	2	-1	240
51000044	768,108.0	9,135,322.0	3,707.0	PSAD56_17S	0.00	0.00	0.00	CHANNEL					1.042		0.16	8.0		0.46	2,091		682	-0.5	-5	0.07	-1	13	113
51000045	766,945.0	9,135,450.0	3,875.0	PSAD56_17S				DUMP					0.551		8.33	65.3		0.13	742		11	-0.5	11	0.02	3	3	303
51000046	766,700.0	9,135,590.0	3,838.0	PSAD56_17S				DUMP					0.085		41.86	167.0	167	0.34	2,304		47	-0.5	14	0.03	14	2	111
51000047	766,750.0	9,135,575.0	3,868.0	PSAD56_17S	0.00	0.80	0.80	CHANNEL					0.057		10.34	15.8		0.71	343		28	-0.5	12	0.03	2	10	19
51000048	768,250.0	9,135,100.0	3,760.0	PSAD56_17S	0.00	5.00	5.00	CHIPS					-0.005		0.04	0.4		0.09	19		100	-0.5	-5	1.42	-1	3	286
51000049	768,440.0	9,134,950.0	3,766.0	PSAD56_17S	0.00	1.00	1.00	CHIPS					-0.005		0.05	-0.2		0.17	5		311	-0.5	-5	2.94	1	4	316
51000052	766,690.0	9,136,290.0	3,647.0	PSAD56_17S	0.00	0.15	0.15	CHANNEL					0.690		20.34	246.0	246	0.26	604		4	-0.5	10	0.02	3	4	170
51000053	766,570.0	9,136,345.0	3,623.0	PSAD56_17S	0.00	5.00	5.00	CHIPS					0.074		0.85	261.0	261	0.26	221		23	-0.5	7	0.01	-1	1	73
51000054	767,120.0	9,136,120.0	3,623.0	PSAD56_17S	0.00	5.00	5.00	CHIPS					0.153		1.53	33.6		0.26	388		21	-0.5	-5	0.03	3	1	113
51000055	767,180.0	9,136,240.0	3,590.0	PSAD56_17S	0.00	0.50	0.50	CHANNEL					0.008		0.06	0.2		0.25	53		33	-0.5	-5	0.01	-1	3	141
51000056	767,520.0	9,136,150.0	3,540.0	PSAD56_17S	0.00	2.00	2.00	CHIPS					0.204		0.27	22.4		0.39	474		1029	0.5	-5	0.04	-1	3	96
51000057	767,390.0	9,135,960.0	3,610.0	PSAD56_17S	0.00	1.00	1.00	CHIPS					0.092		0.13	1.9		0.23	295		68	0.7	-5	0.10	4	3	50
51000059	766,240.0	9,135,530.0	3,742.0	PSAD56_17S	0.00	0.50	0.50	CHANNEL					0.134		12.09	18.3		0.32	335		26	-0.5	9	0.02	-1	-1	88
51000060	766,228.0	9,135,430.0	3,766.0	PSAD56_17S	0.00	1.00	1.00	CHANNEL					0.040		0.14	2.0		0.81	326		20	-0.5	-5	0.13	-1	5	24
51000063	766,320.0	9,135,640.0	3,730.0	PSAD56_17S	0.00	2.00	2.00	CHIPS					0.056		0.17	9.7		0.33	324		71	-0.5	-5	0.02	-1	-1	58
51000064	766,450.0	9,135,670.0	3,738.0	PSAD56_17S	0.00	0.40	0.40	CHANNEL					0.145		22.91	46.1		0.19	1,698		4	0.7	75	0.01	2	11	66
51000065	766,260.0	9,135,710.0	3,696.0	PSAD56_17S	0.00	0.40	0.40	CHANNEL					0.306		3.32	1.6		0.47	1,433		3	0.7	97	0.02	7	13	17
51000066	766,240.0	9,135,725.0	3,683.0	PSAD56_17S	0.00	6.00	6.00	SELECT					0.034		0.12	6.4		0.36	296		47	-0.5	-5	0.02	-1	-1	65
51000077	766,305.0	9,135,700.0	3,690.0	PSAD56_17S	0.00	0.30	0.30	CHANNEL					0.226		22.34	83.1		0.37	1,396		29	1.7	45	0.03	5	17	42
51000078	767,820.0	9,135,970.0	3,517.0	PSAD56_17S	0.00	10.00	10.00	Chips					0.038		0.05	-0.2		1.05	101		77	0.6	-5	0.12	-1	7	11
51000079	767,660.0	9,136,030.0	3,560.0	PSAD56_17S	0.00	8.00	8.00	SELECT					0.698		0.11	1.5		0.40	934		106	1.9	6	0.08	-1	4	77
51000080	766,150.0	9,136,620.0	3,370.0	PSAD56_17S	0.00	0.80	0.80	CHANNEL					0.303		0.12	10.2		0.80	662		8	-0.5	18	0.03	-1	6	98
51000081	766,090.0	9,136,635.0	3,343.0	PSAD56_17S	0.00	5.00	5.00	Chips					0.114		0.03	4.3		0.33	221		5	-0.5	16	0.03	-1	3	181
51000082	766,320.0	9,135,380.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.241		9.25	19.7		0.23	71		8	-0.5	11	0.03	-1	1	236
51000083	766,575.0	9,135,520.0	3,822.0	PSAD56_17S	0.00	4.00	4.00	CHANNEL					0.079		25.82	106.0	106	0.16	317		13	-0.5	26	0.03	116	3	324
51000084	766,574.0	9,135,521.0	3,822.0	PSAD56_17S	0.00	0.60	0.60	CHANNEL					0.052		0.25	1.8		2.18	233		8	0.9	-5	7.72	17	23	49
51000085	766,630.0	9,135,640.0	3,794.0	PSAD56_17S	0.00	0.60	0.60	CHANNEL					0.051		38.26	161.0	161	0.23	158		20	0.9	105	0.13	4	14	412
51000086	766,710.0	9,135,715.0	3,780.0	PSAD56_17S	0.00	3.00	3.00	SELECT					0.045		2.81	7.6		1.12	436		39	-0.5	-5	0.08	2	1	56
51000087	766,640.0	9,135,720.0	3,745.0	PSAD56_17S	0.00	0.30	0.30	CHANNEL					0.066		44.27	255.0	255	0.12	2,620		4	-0.5	65	0.02	17	3	294
51000088	766,660.0	9,135,714.0	3,760.0	PSAD56_17S	0.00	0.15	0.15	CHANNEL					0.192		169.23	946.0	946	0.27	8,913		10	-0.5	599	0.03	75	-1	230
51000089	766,660.0	9,135,770.0	3,748.0	PSAD56_17S	0.00	0.10	0.10	CHANNEL					0.048		0.85	14.1		0.50	212		47	-0.5	-5	0.15	7	9	87
51000090	766,437.0	9,135,857.0	3,643.0	PSAD56_17S	0.00	4.00	4.00	SELECT					0.015		1.26	5.5		0.38	143		49	-0.5	-5	0.02	-1	1	159
51000091	766,395.0	9,135,788.0	3,657.0	PSAD56_17S	0.00	1.50	1.50	SELECT					0.039		0.26	2.8		0.47	117		115	-0.5	-5	0.03	-1	-1	51
51000092	766,415.0	9,135,745.0	3,682.0	PSAD56_17S	0.00	0.20	0.20	CHANNEL					0.010		1.23	2.2		0.35	78		51	-0.5	10	0.04	-1	-1	119
51000093	766,990.0	9,135,720.0	3,775.0	PSAD56_17S	0.00	4.00	4.00	Select					-0.005		0.17	0.5		0.85	80		58	-0.5	-5	0.11	-1	-1	54
51000094	766,688.0	9,135,854.0	3,721.0	PSAD56_17S	0.00	0.30	0.30	CHANNEL					0.206		217.21	122.0	122	0.37	293		11	-0.5	32	0.02	4	-1	108
51000101	770,451.0	9,135,037.0	3,695.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-06	0.048		1.75	-0.2		0.55	184		52	1.0	-5	0.16	-1	2	30
51000102	770,452.0	9,135,038.7	3,695.0	PSAD56_17S	2.00	4.00	2.00	CHANNEL				TR-06	0.005		1.48	-0.2		0.69	13		21	1.8	-5	0.17	-1	7	12
51000103	770,453.0	9,135,040.5	3,695.0	PSAD56_17S	4.00	6.00	2.00	CHANNEL				TR-06	0.006		1.03	-0.2		0.61	66		24	0.8	-5	0.13	-1	8	10
51000104	770,454.0	9,135,042.2	3,695.0	PSAD56_17S	6.00	8.00	2.00	CHANNEL				TR-06	3.250		17.98	21.8		0.36	10,500	1.05	28	-0.5	-5	0.11	-1	-1	86
51000105	770,455.0	9,135,043.9	3,695.0	PSAD56_17S	8.00	10.00	2.00	CHANNEL				TR-06	0.108		0.91	1.5		0.48	2,425		28	-0.5	-5	0.08	-1	2	29
51000106	770,456.0	9,135,045.7	3,695.0	PSAD56_17S	10.00	12.00	2.00	CHANNEL				TR-06	2.211		1.46	90.7		0.49	9,641		21	-0.5	-5	0.07	-1	2	72
51000107	770,457.0	9,135,047.4	3,695.0	PSAD56_17S	12.00	14.00	2.00	CHANNEL				TR-06	3.614		1.19	18.3		0.38	16,700	1.67	47	-0.5	-5	0.06	-1	2	102
51000108	770,458.0	9,135,049.1	3,695.0	PSAD56_17S	14.00	16.00	2.00	CHANNEL				TR-06	0.738		0.27	3.5		0.48	7,649		33	-0.5	-5	0.08	-1	-1	69
51000109	770,459.0	9,135,050.9	3,695.0	PSAD56_17S	16.00	18.00	2.00	CHANNEL				TR-06	0.071		0.15	-0.2		0.46	1,753		16	-0.5	-5	0.11	-1	-1	32
51000110	770,460.0	9,135,052.6	3,695.0	PSAD56_17S	18.00	20.00	2.00	CHANNEL				TR-06	0.477		0.28	0.6		0.43	4,145		38	-0.5	-5	0.14	-1	-1	23
51000111	770,461.0	9,135,054.3	3,695.0	PSAD56_17S	20.00	22.00	2.00	CHANNEL				TR-06	0.019		0.26	-0.2		0.37	859		51	-0.5	-5	0.11	-1	-1	22
51000112	770,462.0	9,135,056.1	3,695.0	PSAD56_17S	22.00	24.00	2.00	CHANNEL				TR-06	2.206		0.88	1.0		0.35	8,489		36	-0.5	-5	0.07	-1	-1	88
51000113	770,463.0	9,135,057.8	3,695.0	PSAD56_17S	24.00	27.00	3.00	CHANNEL				TR-06	0.045		0.46	-0.2		0.50	2,514		59	-0.5	-5	0.11	-1	-1	17
51000114	770,472.0	9,135,055.0	3,695.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-07	0.011		0.33	-0.2		0.71	273		15	-0.5	-5	0.12	-1	-1	31
51000115									FDUP	51000114			0.012		0.29	-0.2		0.53	238		16	-0.5	-5	0.12	-1	-1	20
51000116	770,473.0	9,135,056.7	3,695.0	PSAD56_17S	2.00	4.00	2.00	CHANNEL				TR-07	0.130		0.43	-0.2		0.52	2,564		28	-0.5	-5	0.13	-1	1	29
51000117	770,474.0	9,135,058.5	3,695.0	PSAD56_17S	4.00	6.00	2.00	CHANNEL				TR-07	0.972		1.09	14.5		0.54	6,888		66	-0.5	-5	0.15	-1	2	56
51000118	770,475.0	9,135,060.2	3,695.0	PSAD56_17S	6.00	8.00	2.00	CHANNEL				TR-07	0.085		1.18	1.4		0.48	3,506		46	-0.5	-5	0.13	-1	3	10
51000119	770,476.0	9,135,061.9	3,695.0	PSAD56_17S	8.00	10.00	2.00	CHANNEL				TR-07	0.006		0.63	-0.2		0.69	149		31	0.7	-5	0.12	-1	2	13
51000120	770,477.0	9,135,063.7	3,695.0	PSAD56_17S	10.00	12.00	2.00	CHANNEL				TR-07	0.006		0.26	-0.2		1.19	169		22	1.7	-5	0.15	-1	9	14
51000121	770,478.0	9,135,065.4	3,695.0	PSAD56_17S	12.00	14.00	2.00	CHANNEL				TR-07	-0.005		0.03	-0.2		1.20	248		37	2.9	-5	0.19	-1	14	13
51000122	770,479.0	9,135,067.1	3,695.0	PSAD56_17S	14.00	16.00	2.00	CHANNEL				TR-07	-0.005		0.03	-0.2		1.17	139		65	1.4	-5	0.24	-1	12	15
51000123	770,480.0	9,135,068.9	3,695.0	PSAD56_17S	16.00	18.00	2.00	CHANNEL				TR-07	-0.005		0.03	1.4		1.06	44		700	2.6	-5	0.25	2	55	20
51000124	770,481.0	9,135,070.6	3,695.0	PSAD56_17S	18.00	20.00	2.00	CHANNEL				TR-07	-0.005		-0.02	1.1		1.80	32		457	1.6	-5	0.53	5	34	34
51000125	770,482.0	9,135,072.3	3,695.0	PSAD56_17S	20.00	22.00	2.00	CHANNEL				TR-07	-0.005		0.04	-0.2		1.35	114		56	1.9	-5	0.32	-1	14	25
51000126	770,483.0	9,135,074.1	3,695.0	PSAD56_17S	22.00	25.00	3.00	CHANNEL				TR-07	-0.005		0.03	-0.2		1.00	127		133	1.2	-5	0.86	-1	19	14
51000127	770,494.8	9,135,094.4	3,696.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-08	0.046		1.39	0.5		0.89	609		104	2.1	-5	0.14	-1	22	37
51000128	770,495.8	9,135,096.1	3,696.0	PSAD56_17S	2.00	3.60	1.60	CHANNEL				TR-08	0.022		0.21	0.3		0.60	936		25	-0.5	-5	0.10	-1	-1	29

SURILOMA PROJECT GEOCHEMICAL DATA BASE FEBRUARY 2013

4de 16 

SampleID	Easting	Northing	RL	Grid	IntervalFrom	IntervalTo	Interval	SampleSubType	ChkType	ParentID	StandardID	Comments	Auppm	Auppm2	Hgppm	Agppm	Agppm2	Al%	Asppm	As%	Bappm	Beppm	Bippm	Ca%	Cdppm	Coppm	Crppm
51000129	770,496.6	9,135,097.5	3,696.0	PSAD56_17S	5.60	7.60	2.00	CHANNEL				TR-08	10.960	10.960	2.08	292.0	292	0.30	16,000	1.60	28	-0.5	-5	0.05	1	-1	102
51000130	770,497.6	9,135,099.3	3,696.0	PSAD56_17S	7.60	9.60	2.00	CHANNEL				TR-08	0.006		0.34	-0.2		0.73	73		16	0.6	-5	0.10	-1	9	29
51000131	770,498.6	9,135,101.0	3,696.0	PSAD56_17S	9.60	11.60	2.00	CHANNEL				TR-08	0.050		0.23	-0.2		0.74	268		18	1.5	-5	0.11	-1	10	63
51000132	770,499.6	9,135,102.7	3,696.0	PSAD56_17S	11.60	13.60	2.00	CHANNEL				TR-08	0.058		0.62	-0.2		0.69	389		24	0.7	-5	0.11	-1	17	11
51000133	770,500.6	9,135,104.5	3,697.0	PSAD56_17S	13.60	15.10	1.50	CHANNEL				TR-08	0.035		0.29	-0.2		0.63	1,107		18	0.7	-5	0.13	-1	-1	14
51000134	770,501.3	9,135,105.7	3,697.0	PSAD56_17S	15.10	17.10	2.00	CHANNEL				TR-08	-0.005		0.28	-0.2		0.58	59		14	1.0	-5	0.12	-1	5	10
51000135	770,502.3	9,135,107.5	3,697.0	PSAD56_17S	17.10	18.70	1.60	CHANNEL				TR-08	-0.005		0.25	-0.2		0.90	62		36	0.9	-5	0.35	-1	3	12
51000136									STD		OREAS 52c		0.367		0.05	0.7		1.71	15		172	-0.5	-5	1.40	-1	17	49
51000137	770,493.0	9,135,108.0	3,697.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					5.976		0.72	4.0		0.43	10,500	1.05	28	-0.5	-5	0.13	-1	2	78
51000138	770,784.0	9,134,893.0	3,645.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-09	0.713		2.62	1.3		0.80	5,265		70	0.5	-5	0.04	-1	4	53
51000139	770,784.5	9,134,894.9	3,645.0	PSAD56_17S	2.00	4.00	2.00	CHANNEL				TR-09	0.843		2.09	3.3		0.56	4,875		53	-0.5	-5	0.04	-1	-1	47
51000140	770,785.0	9,134,896.9	3,645.0	PSAD56_17S	4.00	6.00	2.00	CHANNEL				TR-09	0.153		2.23	-0.2		0.83	1,723		39	-0.5	-5	0.04	-1	-1	36
51000141	770,785.6	9,134,898.8	3,645.0	PSAD56_17S	6.00	8.00	2.00	CHANNEL				TR-09	0.143		3.58	0.2		0.76	2,347		37	-0.5	-5	0.05	-1	1	30
51000142	770,786.1	9,134,900.7	3,645.0	PSAD56_17S	8.00	10.00	2.00	CHANNEL				TR-09	1.172		2.27	41.1		0.44	6,212		72	-0.5	-5	0.05	-1	-1	76
51000143	770,786.6	9,134,902.7	3,646.0	PSAD56_17S	10.00	12.00	2.00	CHANNEL				TR-09	1.105		2.16	4.5		0.59	8,507		50	-0.5	-5	0.06	-1	-1	77
51000144	770,787.1	9,134,904.6	3,646.0	PSAD56_17S	12.00	14.00	2.00	CHANNEL				TR-09	0.587		1.27	0.4		0.59	2,655		48	-0.5	-5	0.07	-1	-1	66
51000145	770,794.0	9,134,903.0	3,646.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-10	0.257		1.32	1.1		0.72	2,418		29	-0.5	-5	0.05	-1	-1	48
51000146	770,794.7	9,134,904.9	3,646.0	PSAD56_17S	2.00	4.00	2.00	CHANNEL				TR-10	0.598		2.06	109.0	109	0.42	4,582		58	-0.5	-5	0.05	-1	-1	79
51000147	770,795.5	9,134,906.7	3,647.0	PSAD56_17S	4.00	6.00	2.00	CHANNEL				TR-10	0.534		0.75	8.3		0.56	3,220		42	-0.5	-5	0.08	-1	-1	26
51000148	770,796.2	9,134,908.6	3,647.0	PSAD56_17S	6.00	8.00	2.00	CHANNEL				TR-10	0.042		0.94	0.4		0.72	951		20	-0.5	-5	0.07	-1	-1	32
51000149									STD		OREAS 22b		-0.005		-0.02	-0.2		0.02	-3		7	-0.5	-5	-0.01	-1	-1	23
51000150	770,797.0	9,134,910.4	3,648.0	PSAD56_17S	8.00	10.00	2.00	CHANNEL				TR-10	0.604		1.57	0.5		0.44	3,471		55	-0.5	-5	0.09	-1	-1	44
51000151	770,797.7	9,134,912.3	3,648.0	PSAD56_17S	10.00	12.00	2.00	CHANNEL				TR-10	0.028		1.28	-0.2		0.62	505		30	0.6	-5	0.09	-1	5	22
51000152	770,798.5	9,134,914.1	3,648.0	PSAD56_17S	12.00	14.00	2.00	CHANNEL				TR-10	0.005		4.27	0.4		0.54	187		373	2.3	-5	0.10	-1	27	29
51000153	770,799.2	9,134,916.0	3,649.0	PSAD56_17S	14.00	16.00	2.00	CHANNEL				TR-10	0.011		0.86	-0.2		0.65	149		135	1.9	-5	0.08	-1	25	22
51000154	770,800.0	9,134,917.8	3,649.0	PSAD56_17S	16.00	18.00	2.00	CHANNEL				TR-10	0.007		2.15	0.2		0.75	27		214	1.8	-5	0.09	-1	12	30
51000155	770,800.7	9,134,919.7	3,649.0	PSAD56_17S	18.00	20.00	2.00	CHANNEL				TR-10	0.007		1.43	-0.2		0.61	52		119	1.3	-5	0.13	-1	10	31
51000156	770,801.5	9,134,921.5	3,650.0	PSAD56_17S	20.00	22.00	2.00	CHANNEL				TR-10	0.007		0.10	-0.2		0.63	61		158	1.0	-5	0.23	-1	9	25
51000157	770,802.2	9,134,923.4	3,650.0	PSAD56_17S	22.00	24.00	2.00	CHANNEL				TR-10	0.011		0.04	-0.2		0.85	86		155	0.8	-5	0.04	-1	11	30
51000158	770,803.0	9,134,925.2	3,650.0	PSAD56_17S	24.00	26.00	2.00	CHANNEL				TR-10	0.048		1.00	0.5		0.66	1,185		743	2.0	-5	0.05	-1	34	28
51000159	770,803.7	9,134,927.1	3,650.0	PSAD56_17S	26.00	28.00	2.00	CHANNEL				TR-10	0.060		1.24	-0.2		0.44	1,028		48	-0.5	-5	0.03	-1	-1	19
51000160	770,804.5	9,134,929.0	3,651.0	PSAD56_17S	28.00	30.00	2.00	CHANNEL				TR-10	0.124		3.10	-0.2		0.57	1,885		57	-0.5	-5	0.02	-1	-1	34
51000161	770,805.2	9,134,930.8	3,651.0	PSAD56_17S	30.00	32.00	2.00	CHANNEL				TR-10	0.159		2.06	-0.2		0.58	2,127		63	-0.5	-5	0.04	-1	-1	26
51000162	770,806.0	9,134,932.7	3,651.0	PSAD56_17S	32.00	34.00	2.00	CHANNEL				TR-10	0.896		3.06	1.6		0.46	5,679		257	-0.5	-5	0.03	-1	-1	31
51000163	770,806.7	9,134,934.5	3,651.0	PSAD56_17S	34.00	36.00	2.00	CHANNEL				TR-10	2.457		4.86	2.0		0.51	15,800	1.58	1100	-0.5	-5	0.03	-1	-1	57
51000164	770,807.5	9,134,936.4	3,652.0	PSAD56_17S	36.00	38.00	2.00	CHANNEL				TR-10	2.078		4.75	0.8		0.43	12,100	1.21	683	-0.5	-5	0.03	-1	3	36
51000165	770,808.2	9,134,938.2	3,652.0	PSAD56_17S	38.00	40.00	2.00	CHANNEL				TR-10	2.245		2.01	2.7		0.38	12,000	1.20	337	-0.5	-5	0.06	-1	2	49
51000166	770,812.0	9,134,938.0	3,651.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-11	2.850		3.72	2.8		0.46	13,800	1.38	485	-0.5	-5	0.02	-1	-1	87
51000167	770,812.5	9,134,939.9	3,651.0	PSAD56_17S	2.00	4.00	2.00	CHANNEL				TR-11	2.238		2.54	3.3		0.32	11,800	1.18	395	-0.5	-5	0.05	-1	-1	63
51000168	770,813.0	9,134,941.9	3,651.0	PSAD56_17S	4.00	6.00	2.00	CHANNEL				TR-11	3.243		1.86	3.8		0.55	10,300	1.03	598	-0.5	-5	0.10	-1	2	101
51000169	770,813.6	9,134,943.8	3,651.0	PSAD56_17S	6.00	8.00	2.00	CHANNEL				TR-11	0.949		2.89	0.8		0.88	7,770		350	-0.5	-5	0.08	-1	-1	27
51000170	770,814.1	9,134,945.7	3,652.0	PSAD56_17S	8.00	10.00	2.00	CHANNEL				TR-11	0.363		2.96	-0.2		0.78	9,575		187	-0.5	-5	0.06	-1	-1	21
51000171									FDUP	51000170			0.174		3.07	0.4		0.75	9,150		170	-0.5	-5	0.05	-1	-1	16
51000172	770,814.6	9,134,947.7	3,652.0	PSAD56_17S	10.00	12.00	2.00	CHANNEL				TR-11	0.014		1.52	0.3		0.75	656		31	-0.5	-5	0.05	-1	-1	52
51000173	770,815.1	9,134,949.6	3,653.0	PSAD56_17S	12.00	14.00	2.00	CHANNEL				TR-11	0.176		4.27	0.4		0.74	3,257		85	-0.5	-5	0.05	-1	-1	60
51000174	770,815.6	9,134,951.5	3,653.0	PSAD56_17S	14.00	16.00	2.00	CHANNEL				TR-11	0.044		0.96	-0.2		0.81	2,055		123	-0.5	-5	0.07	-1	-1	28
51000175	770,816.1	9,134,953.5	3,653.0	PSAD56_17S	16.00	18.00	2.00	CHANNEL				TR-11	0.027		1.89	-0.2		0.82	1,196		42	-0.5	-5	0.04	-1	-1	30
51000176	770,816.7	9,134,955.4	3,653.0	PSAD56_17S	18.00	20.00	2.00	CHANNEL				TR-11	0.011		2.26	-0.2		0.64	284		17	-0.5	-5	0.03	-1	-1	24
51000177	770,817.2	9,134,957.3	3,654.0	PSAD56_17S	20.00	22.00	2.00	CHANNEL				TR-11	0.024		4.17	-0.2		0.75	1,109		15	-0.5	-5	0.03	-1	-1	29
51000178	770,817.7	9,134,959.3	3,654.0	PSAD56_17S	22.00	24.00	2.00	CHANNEL				TR-11	0.010		1.38	-0.2		0.87	365		23	-0.5	-5	0.03	-1	-1	40
51000179	770,818.2	9,134,961.2	3,654.0	PSAD56_17S	24.00	26.00	2.00	CHANNEL				TR-11	0.005		0.39	-0.2		0.85	51		48	-0.5	-5	0.08	-1	-1	37
51000180	770,818.7	9,134,963.1	3,654.0	PSAD56_17S	26.00	28.50	2.50	CHANNEL				TR-11	-0.005		0.87	-0.2		0.84	41		78	-0.5	-5	0.09	-1	-1	49
51000181	770,781.0	9,134,942.0	3,648.0	PSAD56_17S	0.00	1.00	1.00	CHANNEL					3.334		2.59	14.5		0.24	11,200	1.12	146	-0.5	-5	0.05	-1	-1	168
51000182	770,780.0	9,134,946.0	3,648.0	PSAD56_17S	0.00	1.20	1.20	CHANNEL					9.073		4.58	7.4		0.27	25,000	2.50	107	-0.5	-5	0.07	-1	-1	131
51000183	770,775.0	9,134,948.0	3,648.0	PSAD56_17S	0.00	1.50	1.50	CHANNEL					0.384		2.56	0.3		0.62	1,609		110	-0.5	-5	0.14	-1	-1	17
51000184	770,721.0	9,134,964.0	3,649.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					1.799		7.98	3.2		0.38	3,086		749	-0.5	-5	0.08	-1	2	141
51000185	770,739.0	9,134,972.0	3,651.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.010		0.84	-0.2		1.01	99		63	2.9	-5	0.12	-1	33	18
51000186	770,581.0	9,135,043.0	3,672.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-12	0.006		1.11	-0.2		0.93	155		59	1.4	-5	0.22	-1	6	19
51000187	770,579.2	9,135,042.1	3,672.0	PSAD56_17S	2.00	4.00	2.00	CHANNEL				TR-12	0.069		0.89	2.4		0.47	415		35	-0.5	-5	0.09	-1	-1	14
51000188	770,577.4	9,135,041.2	3,672.0	PSAD56_17S	4.00	5.20	1.20	CHANNEL				TR-12	0.240		0.17	2.0		0.60	3,350		68	-0.5	-5	0.10	-1	-1	38
51000189	770,576.4	9,135,040.6	3,672.0	PSAD56_17S	5.20	7.40	2.20	CHANNEL				TR-12	1.686		0.35	10.7		0.44	5,794		46	-0.5	-5	0.11	-1	-1	91
51000190	770,572.6	9,135,038.7	3,672.0	PSAD56_17S	9.40	11.40	2.00	CHANNEL				TR-12	1.621		0.24	1.8		0.47	10,300	1.03	303	-0.5	-5	0.07	-1	-1	33
51000191	770,570.8	9,135,037.8	3,672.0	PSAD56_17S	11.40	13.40	2.00	CHANNEL				TR-12	0.035		0.70	-0.2		0.49	1,114		62	-0.5	-5	0.09	-1	-1	11
51000192	770,569.1	9,135,036.9	3,672.0	PSAD56_17S	13.40	15.40	2.00	CHANNEL				TR-12	0.020		0.23	0.3		0.57	241		85	-0.5	-5	0.11	-1	-1	13
51000193	770,567.3	9,135,036.0	3,672.0	PSAD56_17S	15.40	17.40	2.00	CHANNEL				TR-12	0.052		0.52	0.6		0.51	328		66	-0.5	-5	0.10	-1	-1	4
51000194	770,565.5	9,135,035.1	3,672.0	PSAD56_17S	17.40	19.40	2.00	CHANNEL				TR-12	0.048		0.53	-0.2		0.69	203		58	-0.5	-5	0.13	-1	-1	10
51000195	770,563.7	9,135,034.2	3,672.0	PSAD56_17S	19.40	21.40	2.00	CHANNEL				TR-12	0.044		0.38	-0.2		0.91	980		214	-0.5	-5	0.15	-1	5	8
51000196	770,561.9	9,135,033.3	3,672.0	PSAD56_17S	21.40	23.40	2.00	CHANNEL				TR-12	0.012		0.66	-0.2		0.91	51		60	-0.5	-5	0.18	-1	2	6
51000197	770,560.2	9,135,032.4	3,672.0	PSAD56_17S	23.40	25.40	2.00	CHANNEL				TR-12	0.009		0.25	-0.2		0.77	10		82	1.3	-5	0.13	-1	11	8
51000198	770,558.4	9,135,031.5	3,672.0	PSAD56_17S	25.40	27.40	2.00	CHANNEL				TR-12	0.026		0.34	-0.2		0.70	96		54	-0.5	-5	0.14	-1	-1	17
51000199	770,556.6	9,135,030.6	3,672.0	PSAD56_17S	27.40	29.40	2.00	CHANNEL				TR-12	0.010		0.72	-0.2		0.71	56		41	1.0	-5	0.10	-1	9	4
51000200	770,554.8	9,135,029.7	3,672.0	PSAD56_17S	29.40	31.40	2.00	CHANNEL				TR-12	0.115		0.81	-0.2		0.78	756		74	0.8	-5	0.10	-1	5	24
51000201	766,540.0	9,137,080.0	3,371.0	PSAD56_17S	0.00	1.50	1.50	CHANNEL					0.108		0.14	3.8		0.73	148		55	1.0	-5	0.02	-1	3	49
51000220	766,620.0	9,135,850.0	3,700.0	PSAD56_17S	0.00	0.75	0.75	CHANNEL					0.106		80.74	300.0	300	0.13	418		14	-0.5	14	-0.01	96	-1	267
51000221	766,619.0	9,135,850.0	3,700.0	PSAD56_17S	0.00	0.70	0.70	CHANNEL					0.181		345.00	978.0	978	0.21	535		5	-0.5	42	-0.01	51	-1	206
51000222	766,621.0	9,135,851.0	3,700.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.039		6.05	11.1		0.38	197		46	-0.5	-5	0.03	4	-1	58
51000223	766,621.0	9,135,853.0	3,699.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.009		0.23	-0.2		0.58	90		71	-0.5	-5	0.06	-1	-1	52
51000224	766,622.0	9,135,854.0	3,699.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					-0.005		0.87	0.6		0.84	98		92	0.9	-5	0.05	3	2	31
51000225	766,623.0	9,135,856.0	3,699.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.012		0.05	-0.2		0.60	97		74	-0.5	-5	0.01	1	-1	40
51000226	766,625.0	9,135,858.0	3,699.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					-0.005		0.12	-0.2		0.46	87		58	-0.5	-5	0.01	-1	-1	34
51000227	766,626.0	9,135,860.0	3,699.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					-0.005		0.16	-0.2		0.78	141		84	0.7	-5	0.02	-1	-1	31
51000228	766,627.0	9,135,861.0	3,700.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					-0.005		0.03	-0.2		0.58	186		150	2.1	6	0.01	55	13	34
51000229	766,619.0	9,135,849.0	3,700.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.020		1.17	2.0		0.42	131		45	-0.5	-5	0.03	-1	-1	67

SURILOMA PROJECT GEOCHEMICAL DATA BASE FEBRUARY 2013

5de 16 

SampleID	Easting	Northing	RL	Grid	IntervalFrom	IntervalTo	Interval	SampleSubType	ChkType	ParentID	StandardID	Comments	Auppm	Auppm2	Hgppm	Agppm	Agppm2	Al%	Asppm	As%	Bappm	Beppm	Bippm	Ca%	Cdppm	Coppm	Crppm
51000230	766,618.0	9,135,847.0	3,700.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.034		0.29	7.4		0.43	154		39	-0.5	17	0.02	1	-1	39
51000231	766,617.0	9,135,845.0	3,700.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.006		1.74	3.9		0.44	60		79	-0.5	-5	0.02	3	-1	37
51000232	766,616.0	9,135,844.0	3,701.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					-0.005		0.07	-0.2		0.41	44		155	0.5	-5	0.04	2	1	38
51000233	766,801.0	9,135,869.0	3,754.0	PSAD56_17S	0.00	1.50	1.50	CHANNEL					0.054		94.71	52.7		0.19	467		14	-0.5	6	-0.01	16	-1	203
51000234	766,802.0	9,135,871.0	3,754.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.012		3.49	15.7		0.39	414		85	-0.5	-5	-0.01	4	-1	56
51000235	766,802.0	9,135,873.0	3,754.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.016		2.41	4.4		0.39	396		60	-0.5	-5	-0.01	4	-1	37
51000236	766,803.0	9,135,875.0	3,754.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.014		0.86	0.7		0.40	140		80	-0.5	-5	-0.01	1	-1	64
51000237	766,804.0	9,135,876.0	3,754.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.016		0.50	-0.2		0.31	90		52	-0.5	-5	-0.01	-1	-1	41
51000238	766,805.0	9,135,878.0	3,754.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.008		0.27	-0.2		0.44	86		69	-0.5	-5	-0.01	-1	-1	38
51000239	766,805.0	9,135,880.0	3,754.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.019		1.35	0.6		0.35	88		51	-0.5	-5	-0.01	1	-1	44
51000240	766,801.0	9,135,868.0	3,754.0	PSAD56_17S	0.00	0.50	0.50	CHANNEL					0.244		102.00	200.0	200	0.31	260		14	-0.5	56	-0.01	28	-1	201
51000241	766,800.0	9,135,866.0	3,754.0	PSAD56_17S	0.00	1.50	1.50	CHANNEL					0.059		3.61	27.9		0.33	261		46	-0.5	-5	0.03	2	-1	54
51000242	766,394.0	9,135,528.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.031		0.15	-0.2		3.02	256		106	0.9	-5	0.17	6	26	31
51000243	766,393.0	9,135,527.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.053		0.20	-0.2		2.91	312		100	0.8	-5	0.35	3	27	33
51000244	766,392.0	9,135,526.0		PSAD56_17S	0.00	1.00	1.00	CHANNEL					0.058		0.11	1.2		2.58	348		92	0.6	-5	0.23	2	25	52
51000245	766,395.0	9,135,529.0	3,785.0	PSAD56_17S	0.00	1.10	1.10	CHANNEL					0.088		8.14	29.2		0.47	368		27	-0.5	7	0.05	3	2	87
51000246	766,395.0	9,135,529.0		PSAD56_17S	0.00	0.70	0.70	CHANNEL					0.034		0.48	-0.2		1.54	382		49	0.5	6	0.10	4	16	42
51000247	766,396.0	9,135,530.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.051		1.62	11.4		2.16	399		48	0.6	8	0.08	3	12	27
51000248	766,398.0	9,135,530.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.016		0.96	1.1		3.68	197		111	1.2	-5	0.11	6	29	22
51000249	766,398.0	9,135,532.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.084		14.42	98.8		0.58	512		29	-0.5	-5	0.04	4	-1	41
51000250	766,399.0	9,135,533.0		PSAD56_17S	0.00	1.05	1.05	CHANNEL					0.091		6.42	38.7		0.47	283		40	-0.5	-5	0.02	4	-1	102
51000251	766,401.0	9,135,535.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.018		0.48	2.9		3.73	346		131	0.8	-5	0.08	10	18	17
51000252	766,401.0	9,135,536.0		PSAD56_17S	0.00	1.40	1.40	CHANNEL					0.005		0.11	2.7		5.07	10		208	0.6	-5	0.07	14	33	19
51000253	766,403.0	9,135,538.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.010		0.08	1.7		2.60	60		134	1.3	-5	0.03	14	20	18
51000254	766,407.0	9,135,542.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.127		0.19	0.7		0.98	975		50	1.8	-5	0.02	6	9	18
51000255	766,946.0	9,135,451.0	3,875.0	PSAD56_17S	0.00	0.60	0.60	CHANNEL					0.220		2.54	18.9		0.46	714		44	-0.5	10	0.04	2	-1	96
51000256	766,946.0	9,135,449.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.059		0.10	1.6		1.41	1,678		67	0.5	-5	0.14	1	7	16
51000257	766,946.0	9,135,453.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.093		1.41	-0.2		0.63	1,334		56	-0.5	-5	0.05	1	-1	17
51000258	767,092.0	9,135,440.0		PSAD56_17S	0.00	0.55	0.55	CHANNEL					0.419		32.34	21.4		0.81	2,772		68	-0.5	8	0.03	9	-1	54
51000259	767,092.0	9,135,439.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.078		0.96	-0.2		0.78	1,085		34	-0.5	-5	0.04	4	-1	20
51000260	767,092.0	9,135,437.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.246		7.87	5.1		0.79	1,651		43	-0.5	7	0.03	4	1	113
51000261	767,092.0	9,135,435.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.435		4.14	11.5		0.61	946		34	-0.5	9	0.02	2	-1	54
51000262	767,091.0	9,135,433.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.115		1.68	1.1		0.86	1,056		49	-0.5	8	0.04	3	-1	21
51000263	767,092.0	9,135,441.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.069		0.63	8.0		1.01	652		73	-0.5	-5	0.07	12	31	12
51000264	767,092.0	9,135,443.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.032		0.36	78.4		1.32	297		342	1.6	6	0.17	80	62	25
51000265	767,210.0	9,135,425.0		PSAD56_17S	0.00	1.60	1.60	CHANNEL					0.492		12.20	117.0	117	0.88	767		43	-0.5	14	0.08	2	4	73
51000266	767,210.0	9,135,423.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.045		0.11	1.1		0.53	2,075		33	-0.5	-5	0.10	1	-1	38
51000267	767,210.0	9,135,421.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					-0.005		0.13	-0.2		1.15	138		52	0.6	6	0.09	6	3	56
51000268	767,209.0	9,135,419.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.007		0.05	-0.2		0.84	860		33	-0.5	-5	0.05	1	-1	42
51000269	767,209.0	9,135,417.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.007		0.05	-0.2		0.95	379		47	0.7	-5	0.21	-1	2	52
51000270	767,209.0	9,135,415.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.049		0.06	-0.2		0.84	1,101		39	-0.5	-5	0.06	-1	2	35
51000271	767,209.0	9,135,413.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.144		0.33	-0.2		0.47	1,350		44	-0.5	-5	0.08	7	2	53
51000272	767,208.0	9,135,411.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.057		0.08	-0.2		0.67	1,342		49	-0.5	-5	0.07	4	4	44
51000273	767,208.0	9,135,409.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.105		0.06	-0.2		0.76	1,757		127	0.5	-5	0.20	2	10	18
51000274	767,208.0	9,135,407.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.102		0.13	2.6		0.61	3,742		55	0.5	-5	0.10	3	13	12
51000275	767,210.0	9,135,426.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.055		0.72	7.2		0.51	276		30	-0.5	-5	0.09	1	-1	33
51000276	767,210.0	9,135,428.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.020		0.05	4.6		0.50	504		39	-0.5	-5	0.05	-1	-1	19
51000277	767,210.0	9,135,430.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.024		0.08	2.2		0.48	408		41	-0.5	-5	0.03	-1	-1	28
51000278	767,211.0	9,135,432.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.072		0.02	-0.2		0.41	114		38	-0.5	-5	0.03	-1	-1	32
51000279	767,211.0	9,135,434.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.006		0.02	-0.2		0.65	25		53	0.7	-5	0.04	13	10	26
51000280	767,211.0	9,135,436.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.011		0.02	1.3		0.66	55		61	0.7	-5	0.02	16	15	42
51000281	765,800.0	9,136,712.0	3,230.0	PSAD56_17S	0.00	0.60	0.60	CHANNEL					1.664		0.09	-0.2		1.12	18,700	1.87	51	-0.5	20	-0.01	6	3	30
51000282	765,798.0	9,136,710.0	3,228.0	PSAD56_17S	0.00	0.70	0.70	CHANNEL					4.485		0.04	1.4		0.20	726		7	-0.5	144	-0.01	-1	2	162
51000283	765,820.0	9,136,690.0	3,235.0	PSAD56_17S	0.00	1.50	1.50	SELECT					0.007		-0.02	-0.2		0.18	468		21	-0.5	-5	-0.01	-1	-1	153
51000284	765,800.0	9,136,680.0	3,238.0	PSAD56_17S	0.00	2.00	2.00	SELECT					0.230		0.07	0.6		0.39	2,524		19	-0.5	11	-0.01	-1	-1	81
51000285	765,798.0	9,136,681.0	3,237.0	PSAD56_17S	0.00	1.00	1.00	SELECT					1.216		0.06	1.4		0.12	10,200	1.02	48	-0.5	5	-0.01	1	-1	182
51000286	765,570.0	9,136,400.0		PSAD56_17S	0.00	5.00	5.00	SELECT					0.016		-0.02	2.2		2.78	201		35	0.6	-5	0.77	1	9	57
51000287	766,480.0	9,136,503.0	3,250.0	PSAD56_17S	0.00	4.00	4.00	SELECT					0.045		0.03	-0.2		0.52	918		11	-0.5	7	0.03	-1	-1	77
51000288	765,470.0	9,136,520.0	3,257.0	PSAD56_17S	0.00	2.00	2.00	SELECT					0.182		0.06	0.5		0.40	2,147		41	-0.5	17	0.02	-1	-1	110
51000289	765,470.0	9,136,590.0	3,217.0	PSAD56_17S	0.00	5.00	5.00	SELECT					0.088		0.36	-0.2		1.04	9,050		29	1.1	71	-0.01	2	-1	88
51000290	765,380.0	9,136,573.0	3,198.0	PSAD56_17S	0.00	4.00	4.00	SELECT					-0.005		0.02	0.8		0.26	382		32	-0.5	11	-0.01	-1	-1	123
51000291	765,342.0	9,136,583.0	3,257.0	PSAD56_17S	0.00	2.00	2.00	SELECT					0.011		0.06	1.8		0.44	389		28	-0.5	6	-0.01	-1	-1	49
51000292	766,611.0	9,137,077.0	3,418.0	PSAD56_17S				DUMP					0.507		0.14	48.6		0.53	1,781		55	-0.5	-5	-0.01	-1	-1	50
51000293	766,642.0	9,137,090.0	3,438.0	PSAD56_17S	0.00	1.50	1.50	CHANNEL					1.617		0.08	2.9		0.63	4,383		67	-0.5	15	-0.01	-1	-1	77
51000294	766,674.0	9,137,180.0	3,453.0	PSAD56_17S	0.00	1.50	1.50	SELECT					0.059		0.05	-0.2		0.73	61		21	0.6	-5	-0.01	-1	2	69
51000295	766,662.0	9,137,140.0	3,447.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.157		0.04	1.0		0.73	232		59	0.9	11	-0.01	-1	2	75
51000296									STD		Oreas 52c		0.349		0.05	0.8		1.71	20		157	-0.5	-5	1.36	-1	17	48
51000301	766,844.0	9,135,465.0	3,896.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				Anita T5	0.031		0.13	-0.2		1.10	370		53	0.8	-5	0.03	1	12	20
51000302	766,844.0	9,135,467.0	3,897.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				Anita T5	0.143		1.99	6.2		0.67	600		57	0.6	59	0.02	-1	5	23
51000303	766,844.0	9,135,469.0	3,897.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				Anita T5	0.031		0.05	0.8		1.11	237		60	0.9	-5	0.02	2	10	9
51000304	766,847.0	9,135,473.0	3,899.0	PSAD56_17S	0.00	1.50	1.50	CHANNEL				Anita T5	0.926		0.49	1.3		0.49	5,657		336	-0.5	-5	0.03	-1	-1	21
51000305	766,847.0	9,135,475.0	3,899.0	PSAD56_17S	0.00	1.50	1.50	CHANNEL				Anita T5	0.072		0.07	0.7		1.38	893		92	1.3	-5	0.04	1	8	6
51000306	767,263.0	9,135,740.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL				Giuliana T3	0.055		5.36	12.4		0.25	126		17	-0.5	10	0.04	27	1	53
51000307	767,263.0	9,135,742.0		PSAD56_17S	0.00	1.20	1.20	CHANNEL				Giuliana T3	0.185		132.00	174.0	174	0.10	353		9	-0.5	273	0.03	814	-1	112
51000308	767,263.0	9,135,744.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL				Giuliana T3	0.410		31.58	270.0	270	0.18	307		10	-0.5	858	0.02	418	-1	101
51000309	767,263.0	9,135,745.0		PSAD56_17S	0.00	1.20	1.20	CHANNEL				Giuliana T3	0.112		0.78	3.2		0.29	87		19	-0.5	-5	-0.01	20	-1	74
51000310	767,541.0	9,135,574.0	3,730.0	PSAD56_17S	0.00	1.50	1.50	CHANNEL				Giuliana Vein	0.338		11.85	51.6		0.12	537		165	-0.5	24	-0.01	7	-1	141
51000311	767,264.0	9,135,747.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL				Giuliana T3	0.042		0.78	1.9		0.24	524		225	-0.5	-5	0.01	5	-1	56
51000312	767,264.0	9,135,749.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL				Giuliana T3	0.008		0.27	3.6		0.42	165		76	0.7	-5	0.05	9	7	67
51000313	767,578.0	9,135,534.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL				Giuliana T4	0.032		1.23	13.4		0.25	327		97	-0.5	-5	0.09	5	2	104
51000314	767,579.0	9,135,537.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL				Giuliana T4	-0.005		0.16	6.5		0.32	950		104	0.8	-5	0.13	5	2	49
51000315	767,580.0	9,135,541.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL				Giuliana T4	0.018		0.40	5.8		0.38	245		189	-0.5	-5	0.13	3	-1	79
51000316	767,583.0	9,135,545.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL				Giuliana T4	0.091		2.27	3.0		0.34	482		59	0.7	-5	0.08	-1	3	86

SURILOMA PROJECT GEOCHEMICAL DATA BASE FEBRUARY 2013

6de 16 

SampleID	Easting	Northing	RL	Grid	IntervalFrom	IntervalTo	Interval	SampleSubType	ChkType	ParentID	StandardID	Comments	Auppm	Auppm2	Hgppm	Agppm	Agppm2	Al%	Asppm	As%	Bappm	Beppm	Bippm	Ca%	Cdppm	Coppm	Crppm
51000317	767,575.0	9,135,530.0	3,701.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				Giuliana T4	0.116		6.92	26.5		0.27	408		71	-0.5	-5	0.09	3	-1	76
51000318	767,587.0	9,135,548.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL				Giuliana T4	0.024		0.19	1.0		0.45	237		46	-0.5	-5	0.13	-1	-1	76
51000319	767,590.0	9,135,551.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL				Giuliana T4	-0.005		0.07	0.4		0.89	42		56	-0.5	-5	0.12	-1	2	93
51000320	767,593.0	9,135,553.0		PSAD56_17S	0.00	2.00	2.00	CHANNEL				Giuliana T4	0.008		0.05	2.5		0.53	154		39	-0.5	-5	0.11	-1	-1	62
51000321	767,595.0	9,135,555.0	3,704.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				Giuliana T4	0.021		0.05	2.5		0.78	155		47	-0.5	-5	0.11	-1	-1	76
51000322									FDUP	51000310			0.209		7.79	30.4		0.14	454		174	-0.5	12	0.01	6	-1	142
51000323									STD		Oreas 22b		-0.005		-0.02	-0.2		0.01	-3		6	-0.5	-5	-0.01	-1	-1	24
51000329	766,720.0	9,137,128.0	3,472.0	PSAD56_17S	0.00	2.00	2.00	SELECT					0.051		0.18	-0.2		0.46	72		53	-0.5	-5	-0.01	-1	-1	78
51000330									FDUP				1.309		23.29	5.5		0.68	6,739		11	-0.5	71	-0.01	4	-1	40
51000331	766,712.0	9,137,123.0	3,474.0	PSAD56_17S	0.00	2.00	2.00	SELECT					0.062		0.16	-0.2		0.45	337		84	-0.5	-5	-0.01	-1	3	75
51000332	766,803.0	9,137,152.0		PSAD56_17S	0.00	1.00	1.00	SELECT					0.024		0.21	0.5		0.50	35		38	-0.5	-5	0.01	-1	1	119
51000333	766,803.0	9,137,148.0	3,465.0	PSAD56_17S	0.00	1.00	1.00	CHANNEL					0.280		0.43	3.2		0.72	241		40	0.8	9	0.01	-1	8	43
51000334	766,827.0	9,137,288.0	3,432.0	PSAD56_17S	0.00	1.00	1.00	CHANNEL					0.180		0.27	0.3		0.73	172		14	1.1	-5	-0.01	-1	2	26
51000335	766,693.0	9,137,297.0	3,423.0	PSAD56_17S	0.00	3.00	3.00	SELECT					0.120		0.19	0.8		0.81	250		23	-0.5	-5	-0.01	-1	5	44
51000336	766,890.0	9,137,324.0	3,420.0	PSAD56_17S	0.00	0.80	0.80	CHANNEL					0.187		0.34	1.0		0.74	313		28	-0.5	-5	-0.01	-1	2	54
51000337	766,080.0	9,137,070.0	3,045.0	PSAD56_17S	0.00	0.12	0.12	CHANNEL					10.190	10.190	1.49	269.0	269	0.20	63,000	6.30	25	-0.5	1,761	0.03	4	52	112
51000338	766,080.0	9,137,069.0	3,045.0	PSAD56_17S	0.00	1.00	1.00	SELECT					0.007		0.09	0.4		2.04	90		92	0.5	-5	0.04	-1	20	71
51000339	766,065.0	9,137,080.0	3,045.0	PSAD56_17S				DUMP					10.620	10.620	2.47	679.0	679	0.11	99,100	9.91	6	-0.5	220	-0.01	11	26	213
51000340									FDUP	51000331			0.070		0.04	0.2		0.43	365		78	-0.5	-5	-0.01	-1	3	95
51000341	766,190.0	9,136,977.0	3,208.0	PSAD56_17S	0.00	5.00	5.00	SELECT					0.035		0.11	2.8		0.32	192		35	-0.5	-5	-0.01	-1	3	149
51000342	766,045.0	9,136,658.0	3,291.0	PSAD56_17S	0.00	5.00	5.00	SELECT					0.036		0.05	2.6		0.34	269		16	-0.5	-5	-0.01	-1	2	163
51000343	766,090.0	9,136,650.0	3,330.0	PSAD56_17S	0.00	5.00	5.00	SELECT					0.189		0.04	3.4		0.42	661		8	-0.5	13	0.01	-1	3	166
51000344	766,360.0	9,137,198.0	3,224.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.058		0.04	1.0		1.09	59		31	-0.5	-5	0.02	-1	5	127
51000345	766,250.0	9,137,160.0	3,211.0	PSAD56_17S	0.00	4.00	4.00	SELECT					0.050		0.22	1.2		0.53	151		32	-0.5	-5	-0.01	-1	1	143
51000346	766,228.0	9,137,158.0		PSAD56_17S	0.00	4.00	4.00	SELECT					0.093		0.07	2.3		0.95	617		23	-0.5	-5	-0.01	-1	1	111
51000347	766,477.0	9,137,387.0	3,251.0	PSAD56_17S	0.00	0.80	0.80	CHANNEL					0.050		-0.02	-0.2		0.53	99		30	-0.5	-5	-0.01	-1	3	97
51000349	766,403.0	9,136,680.0	3,411.0	PSAD56_17S	0.00	4.00	4.00	SELECT					0.195		0.35	4.1		0.56	225		54	-0.5	-5	0.02	-1	2	36
51000350	766,050.0	9,136,960.0	3,160.0	PSAD56_17S	0.00	0.80	0.80	SELECT					0.017		0.07	-0.2		0.29	474		17	-0.5	-5	-0.01	11	6	94
51000351	766,115.0	9,136,914.0	3,173.0	PSAD56_17S	0.00	1.00	1.00	CHANNEL					0.016		0.08	-0.2		0.26	162		17	-0.5	-5	-0.01	-1	-1	92
51000360									FDUP	51000349			0.034		0.51	34.9		0.29	912		571	1.0	-5	0.03	41	9	100
51000370									STD		Oreas 22b		-0.005		-0.02	-0.2		0.01	13		5	-0.5	-5	-0.01	-1	-1	23
51000401									STD		OREAS 52c		0.345		0.05	0.7		1.69	20		154	-0.5	-5	1.34	-1	16	48
51000402	770,553.2	9,135,028.5	3,672.0	PSAD56_17S	31.40	33.40	2.00	CHANNEL				TR-12	0.158		0.15	0.4		0.58	3,035		79	1.0	-5	0.12	-1	6	91
51000403	770,551.5	9,135,027.4	3,672.0	PSAD56_17S	33.40	35.40	2.00	CHANNEL				TR-12	0.048		0.48	0.3		0.81	2,972		53	1.5	-5	0.13	-1	5	38
51000404	770,551.5	9,135,027.4	3,672.0	PSAD56_17S	35.40	37.40	2.00	CHANNEL				TR-12	0.056		0.56	-0.2		0.78	695		30	0.9	-5	0.17	-1	12	7
51000405	770,549.9	9,135,026.2	3,672.0	PSAD56_17S	37.40	39.40	2.00	CHANNEL				TR-12	0.938		2.48	1.1		0.58	3,573		695	-0.5	-5	0.14	-1	1	65
51000406									FDUP	51000405			0.800		2.64	0.8		0.42	4,154		224	-0.5	-5	0.15	-1	-1	21
51000407									FDUP	51000413			0.873		5.16	1.5		0.51	5,907		888	-0.5	-5	0.13	-1	-1	94
51000408	770,546.6	9,135,023.9	3,672.0	PSAD56_17S	41.40	43.40	2.00	CHANNEL				TR-12	1.740		1.97	1.6		0.55	11,200	1.12	100	-0.5	-5	0.15	-1	-1	58
51000409	770,545.0	9,135,022.8	3,672.0	PSAD56_17S	43.40	45.40	2.00	CHANNEL				TR-12	0.192		0.33	1.0		0.66	4,476		49	-0.5	-5	0.14	-1	-1	25
51000410	770,543.3	9,135,021.6	3,672.0	PSAD56_17S	45.40	47.40	2.00	CHANNEL				TR-12	0.685		0.53	0.6		0.66	3,826		53	1.2	-5	0.14	-1	2	30
51000411	770,541.7	9,135,020.5	3,672.0	PSAD56_17S	47.40	49.40	2.00	CHANNEL				TR-12	1.348		2.30	1.8		0.43	8,546		395	0.8	-5	0.15	1	3	46
51000412	770,540.1	9,135,019.3	3,672.0	PSAD56_17S	49.40	52.90	3.50	CHANNEL				TR-12	0.527		0.55	14.6		0.89	3,328		192	1.0	-5	0.12	2	82	58
51000413	770,548.3	9,135,025.1	3,672.0	PSAD56_17S	39.40	41.40	2.00	CHANNEL				TR-12	1.928		8.05	1.4		0.58	9,944		1812	-0.5	-5	0.14	-1	-1	56
51000414	770,560.0	9,135,018.0	3,672.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					8.106		11.66	35.9		0.39	33,000	3.30	1024	-0.5	-5	0.07	12	-1	171
51000415	770,660.0	9,134,992.0	3,656.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-13	1.348		9.50	3.7		0.75	2,829		1129	-0.5	-5	0.20	-1	-1	31
51000416	770,658.4	9,134,990.9	3,656.0	PSAD56_17S	2.00	4.00	2.00	CHANNEL				TR-13	0.988		3.01	0.9		0.57	2,311		347	-0.5	-5	0.18	-1	-1	49
51000417	770,656.7	9,134,989.7	3,656.0	PSAD56_17S	4.00	6.00	2.00	CHANNEL				TR-13	2.242		29.61	3.0		0.37	6,547		2219	-0.5	-5	0.12	-1	1	59
51000418	770,655.1	9,134,988.6	3,656.0	PSAD56_17S	6.00	8.00	2.00	CHANNEL				TR-13	0.080		3.37	-0.2		0.90	928		170	0.5	-5	0.25	1	-1	9
51000419	770,653.4	9,134,987.4	3,656.0	PSAD56_17S	8.00	10.00	2.00	CHANNEL				TR-13	0.022		1.77	-0.2		0.80	83		199	-0.5	-5	0.21	-1	-1	11
51000420	770,877.0	9,134,884.0	3,636.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-14	0.022		0.31	-0.2		1.67	179		113	1.9	-5	0.20	-1	40	27
51000421	770,877.7	9,134,885.9	3,636.0	PSAD56_17S	2.00	4.00	2.00	CHANNEL				TR-14	2.081		3.37	-0.2		0.73	3,382		38	-0.5	-5	0.11	-1	-1	41
51000422	770,878.3	9,134,887.8	3,635.0	PSAD56_17S	4.00	6.00	2.00	CHANNEL				TR-14	0.378		0.97	0.7		0.85	3,853		31	-0.5	-5	0.10	-1	-1	49
51000423	770,879.0	9,134,889.7	3,635.0	PSAD56_17S	6.00	8.00	2.00	CHANNEL				TR-14	4.999		1.36	1.1		0.76	11,600	1.16	194	-0.5	-5	0.06	-1	3	48
51000424	770,879.6	9,134,891.6	3,635.0	PSAD56_17S	8.00	10.00	2.00	CHANNEL				TR-14	0.054		0.68	-0.2		0.84	1,108		149	-0.5	-5	0.09	-1	-1	42
51000425	770,880.3	9,134,893.5	3,635.0	PSAD56_17S	10.00	12.00	2.00	CHANNEL				TR-14	0.221		3.82	-0.2		0.75	2,648		30	-0.5	-5	0.09	-1	-1	27
51000426	770,880.9	9,134,895.3	3,634.0	PSAD56_17S	12.00	14.00	2.00	CHANNEL				TR-14	0.182		2.15	-0.2		1.20	1,184		75	-0.5	-5	0.09	-1	5	31
51000427	770,881.6	9,134,897.2	3,634.0	PSAD56_17S	14.00	16.00	2.00	CHANNEL				TR-14	0.224		1.03	0.5		0.65	2,333		133	-0.5	-5	0.09	-1	2	29
51000428	770,882.2	9,134,899.1	3,634.0	PSAD56_17S	16.00	18.00	2.00	CHANNEL				TR-14	0.764		1.94	-0.2		0.93	3,831		75	0.5	-5	0.11	1	5	38
51000429	770,882.9	9,134,901.0	3,634.0	PSAD56_17S	18.00	20.00	2.00	CHANNEL				TR-14	2.500		1.86	0.8		0.53	9,574		57	-0.5	-5	0.05	-1	-1	80
51000430									FDUP	51000429			2.216		1.88	0.6		0.54	8,454		66	-0.5	-5	0.05	-1	-1	78
51000431	770,883.5	9,134,902.9	3,633.0	PSAD56_17S	20.00	22.00	2.00	CHANNEL				TR-14	2.741		2.20	1.4		0.69	12,700	1.27	115	-0.5	-5	0.08	-1	-1	45
51000432	770,884.2	9,134,904.8	3,633.0	PSAD56_17S	22.00	24.00	2.00	CHANNEL				TR-14	0.381		2.57	0.8		0.83	4,010		38	-0.5	-5	0.09	-1	-1	37
51000433	770,884.8	9,134,906.7	3,633.0	PSAD56_17S	24.00	26.00	2.00	CHANNEL				TR-14	1.417		3.36	0.9		0.64	5,572		104	-0.5	-5	0.05	-1	2	37
51000434									STD		OREAS 62d		10.970	10.970	0.26	8.8		0.75	21		54	-0.5	-5	8.47	-1	7	13
51000435	770,885.5	9,134,908.6	3,633.0	PSAD56_17S	26.00	28.00	2.00	CHANNEL				TR-14	0.716		2.30	0.8		0.87	3,810		85	-0.5	-5	0.08	-1	2	45
51000436	770,886.1	9,134,910.5	3,633.0	PSAD56_17S	28.00	30.00	2.00	CHANNEL				TR-14	0.191		0.96	0.9		1.12	3,108		136	0.7	-5	0.06	1	-1	28
51000437	770,886.8	9,134,912.4	3,633.0	PSAD56_17S	30.00	32.00	2.00	CHANNEL				TR-14	0.132		0.51	-0.2		2.40	1,209		68	1.3	-5	0.06	-1	13	34
51000438	770,887.4	9,134,914.3	3,633.0	PSAD56_17S	32.00	34.00	2.00	CHANNEL				TR-14	0.112		0.54	-0.2		0.93	2,049		63	0.5	-5	0.05	1	-1	18
51000439	770,888.1	9,134,916.1	3,633.0	PSAD56_17S	34.00	36.00	2.00	CHANNEL				TR-14	0.147		0.36	-0.2		0.81	1,366		84	-0.5	-5	0.04	-1	-1	32
51000440	770,888.7	9,134,918.0	3,633.0	PSAD56_17S	36.00	38.00	2.00	CHANNEL				TR-14	0.042		0.49	-0.2		1.21	3,122		54	1.0	-5	0.02	-1	7	20
51000441	770,889.4	9,134,919.9	3,633.0	PSAD56_17S	38.00	40.00	2.00	CHANNEL				TR-14	0.052		0.44	-0.2		1.09	3,484		45	1.1	-5	0.03	-1	10	21
51000442	770,890.0	9,134,921.8	3,633.0	PSAD56_17S	40.00	42.00	2.00	CHANNEL				TR-14	0.080		0.44	-0.2		0.93	2,409		79	0.9	-5	0.05	-1	11	40
51000443	770,890.7	9,134,923.7	3,633.0	PSAD56_17S	42.00	44.00	2.00	CHANNEL				TR-14	0.161		0.22	-0.2		2.22	3,869		63	1.3	-5	0.03	-1	9	15
51000444	770,891.3	9,134,925.6	3,633.0	PSAD56_17S	44.00	46.00	2.00	CHANNEL				TR-14	0.030		0.07	-0.2		1.54	2,204		42	0.7	-5	0.09	-1	4	17
51000445	770,892.0	9,134,927.5	3,633.0	PSAD56_17S	46.00	48.00	2.00	CHANNEL				TR-14	0.066		0.13	-0.2		1.80	3,526		58	1.1	-5	0.07	-1	8	4
51000446	770,892.6	9,134,929.4	3,633.0	PSAD56_17S	48.00	50.00	2.00	CHANNEL				TR-14	0.055		0.12	-0.2		2.71	3,546		104	1.1	-5	0.08	-1	30	10
51000447	770,893.3	9,134,931.3	3,633.0	PSAD56_17S	50.00	52.00	2.00	CHANNEL				TR-14	0.039		0.07	0.3		2.26	3,131		291	0.8	-5	0.09	-1	51	9
51000448									STD		OREAS 54Pa		2.999		0.12	4.6		1.14	7		26	-0.5	-5	1.32	-1	22	27
51000449	770,868.0	9,134,915.0	3,637.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					2.741		4.09	0.3		0.80	8,127		215	0.5	-5	0.10	-1	1	70
51000450	770,864.0	9,134,916.0	3,638.0	PSAD56_17S	0.00	3.00	3.00	CHANNEL					0.327		1.04	-0.2		0.70	1,661		42	-0.5	6	0.04	1	-1	27
51000452	769,006.0	9,135,911.0	3,340.0	PSAD56_17S	0.00	2.00	2.00	CHIPS					0.046		0.12	-0.2		0.51	228		95	-0.5	6	0.07	-1	-1	43
51000453	769,027.0	9,135,906.0	3,335.0	PSAD56_17S	0.00	1.00	1.00	CHANNEL					0.088		0.26	0.2		0.41	163		21	0.6	-5	1.85	-1	4	43

SURILOMA PROJECT GEOCHEMICAL DATA BASE FEBRUARY 2013

7de 16 

SampleID	Easting	Northing	RL	Grid	IntervalFrom	IntervalTo	Interval	SampleSubType	ChkType	ParentID	StandardID	Comments	Auppm	Auppm2	Hgppm	Agppm	Agppm2	Al%	Asppm	As%	Bappm	Beppm	Bippm	Ca%	Cdppm	Coppm	Crppm
51000454	769,031.0	9,135,950.0	3,339.0	PSAD56_17S				FLOAT					-0.005		-0.02	-0.2		0.16	-3		25	-0.5	-5	0.04	-1	2	441
51000455	770,906.0	9,134,824.0	3,636.0	PSAD56_17S	0.00	1.00	1.00	SUBCROP					0.067		0.72	125.0	125	0.90	550		45	0.9	-5	0.24	-1	10	52
51000456	771,021.0	9,134,814.0	3,615.0	PSAD56_17S	0.00	1.00	1.00	CHANNEL					0.686		0.92	0.5		0.63	2,098		183	0.8	-5	0.17	-1	7	45
51000457	771,013.0	9,134,790.0	3,618.0	PSAD56_17S	0.00	1.00	1.00	CHANNEL					0.032		1.13	0.6		1.11	418		156	4.5	-5	0.19	-1	31	15
51000458	769,546.0	9,134,762.0	3,774.0	PSAD56_17S	0.00	3.00	3.00	CHIPS					-0.005		0.06	0.6		0.70	25		207	-0.5	-5	0.02	-1	-1	30
51000459	768,313.0	9,135,069.0	3,743.0	PSAD56_17S	0.00	1.20	1.20	CHIPS					-0.005		0.05	-0.2		0.26	8		8	-0.5	-5	15.00	-1	2	10
51000460	767,693.0	9,135,444.0		PSAD56_17S	0.00	1.00	1.00	CHIPS					-0.005		-0.02	-0.2		1.16	4		33	-0.5	-5	15.00	-1	2	21
51000461	766,880.0	9,136,014.0	3,728.0	PSAD56_17S	0.00	1.00	1.00	CHIPS					-0.005		-0.02	-0.2		0.74	-3		64	-0.5	-5	13.97	-1	3	63
51000462	766,881.0	9,135,995.0	3,731.0	PSAD56_17S	0.00	2.00	2.00	CHIPS					-0.005		-0.02	-0.2		0.74	-3		50	-0.5	-5	0.18	-1	4	171
51000463	770,309.0	9,134,333.0	3,629.0	PSAD56_17S	0.00	0.30	0.30	CHANNEL					-0.005		-0.02	-0.2		0.10	-3		27	-0.5	-5	0.06	-1	-1	361
51000464	770,623.0	9,134,998.0	3,666.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-15	0.112		1.03	0.6		1.51	929		93	-0.5	-5	0.23	-1	2	41
51000465	770,621.2	9,134,997.1	3,666.0	PSAD56_17S	2.00	4.00	2.00	CHANNEL				TR-15	12.800	12.800	4.93	36.7		0.51	64,500	6.45	569	-0.5	-5	0.10	-1	4	188
51000466	770,619.4	9,134,996.2	3,666.0	PSAD56_17S	4.00	6.00	2.00	CHANNEL				TR-15	0.200		0.91	0.6		0.71	2,352		142	-0.5	-5	0.20	-1	1	42
51000467	770,617.6	9,134,995.4	3,666.0	PSAD56_17S	6.00	8.00	2.00	CHANNEL				TR-15	0.551		1.00	0.7		0.59	6,303		207	-0.5	-5	0.22	-1	2	51
51000468	770,615.8	9,134,994.5	3,666.0	PSAD56_17S	8.00	10.00	2.00	CHANNEL				TR-15	0.547		1.21	1.0		0.57	4,559		188	-0.5	-5	0.19	-1	1	42
51000469									STD		OREAS 22b		-0.005		-0.02	-0.2		0.01	13		5	-0.5	-5	-0.01	-1	-1	36
51000470	770,614.0	9,134,993.6	3,666.0	PSAD56_17S	10.00	12.00	2.00	CHANNEL				TR-15	0.128		0.95	-0.2		0.70	1,717		59	-0.5	-5	0.20	-1	3	33
51000471	770,612.2	9,134,992.7	3,666.0	PSAD56_17S	12.00	14.00	2.00	CHANNEL				TR-15	1.078		1.07	2.1		1.55	3,807		205	-0.5	-5	0.48	-1	11	57
51000472	770,610.4	9,134,991.9	3,666.0	PSAD56_17S	14.00	15.60	1.60	CHANNEL				TR-15	0.029		0.50	-0.2		1.36	555		83	-0.5	-5	0.27	-1	6	12
51000473									FDUP	51000472			0.030		0.49	-0.2		1.31	572		80	-0.5	-5	0.27	-1	7	13
51000474	770,609.0	9,134,991.2	3,666.0	PSAD56_17S	15.60	17.00	1.40	CHANNEL				TR-15	0.031		1.01	-0.2		0.77	1,504		86	-0.5	-5	0.21	-1	1	30
51000475	770,607.7	9,134,990.5	3,666.0	PSAD56_17S	17.00	19.00	2.00	CHANNEL				TR-15	2.189		0.69	1.4		2.10	4,386		248	0.5	-5	0.49	-1	14	30
51000476	770,605.9	9,134,989.7	3,666.0	PSAD56_17S	19.00	21.00	2.00	CHANNEL				TR-15	1.309		1.10	3.4		1.03	7,572		226	-0.5	-5	0.32	-1	7	31
51000477	770,604.1	9,134,988.8	3,666.0	PSAD56_17S	21.00	23.00	2.00	CHANNEL				TR-15	0.715		1.18	1.7		1.31	4,299		179	-0.5	-5	0.28	-1	12	25
51000478	770,602.3	9,134,987.9	3,666.0	PSAD56_17S	23.00	25.00	2.00	CHANNEL				TR-15	0.729		7.10	5.6		1.23	4,906		191	0.5	-5	0.10	1	6	32
51000479	770,600.5	9,134,987.0	3,666.0	PSAD56_17S	25.00	27.00	2.00	CHANNEL				TR-15	1.328		2.02	3.7		1.39	7,942		323	0.6	-5	0.17	-1	7	23
51000480	770,598.7	9,134,986.2	3,666.0	PSAD56_17S	27.00	29.00	2.00	CHANNEL				TR-15	1.432		7.83	8.7		1.06	6,689		374	-0.5	-5	0.17	2	4	25
51000481	770,596.9	9,134,985.3	3,666.0	PSAD56_17S	29.00	31.00	2.00	CHANNEL				TR-15	0.123		0.38	0.3		1.15	582		181	1.1	-5	0.23	-1	10	5
51000482	770,595.1	9,134,984.4	3,666.0	PSAD56_17S	31.00	33.00	2.00	CHANNEL				TR-15	0.036		0.16	-0.2		1.88	253		186	1.8	-5	0.14	-1	26	7
51000483	770,593.3	9,134,983.5	3,666.0	PSAD56_17S	33.00	35.00	2.00	CHANNEL				TR-15	0.028		0.40	-0.2		1.41	958		358	1.8	-5	0.71	-1	29	5
51000484	770,591.6	9,134,982.5	3,666.0	PSAD56_17S	35.00	37.00	2.00	CHANNEL				TR-15	0.432		1.01	1.4		1.37	3,207		328	0.8	-5	0.03	-1	25	8
51000485	770,589.9	9,134,981.5	3,666.0	PSAD56_17S	37.00	39.00	2.00	CHANNEL				TR-15	0.227		0.88	0.4		0.97	1,153		163	-0.5	-5	0.02	-1	19	6
51000486	770,588.2	9,134,980.4	3,666.0	PSAD56_17S	39.00	41.00	2.00	CHANNEL				TR-15	0.048		0.79	0.3		0.79	269		136	-0.5	-5	0.02	-1	4	5
51000487									STD		OREAS 52c		0.348		0.05	0.5		1.66	17		162	-0.5	-5	1.36	-1	15	47
51000488	770,586.5	9,134,979.4	3,666.0	PSAD56_17S	41.00	43.00	2.00	CHANNEL				TR-15	0.026		0.98	-0.2		0.69	224		81	-0.5	-5	0.03	-1	1	6
51000489	770,584.8	9,134,978.4	3,666.0	PSAD56_17S	43.00	45.00	2.00	CHANNEL				TR-15	0.023		0.09	-0.2		1.63	78		105	1.4	-5	0.55	-1	16	6
51000490	770,588.0	9,134,984.0	3,667.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL					0.044		1.35	0.8		0.79	783		324	-0.5	-5	0.03	-1	56	10
51000491	770,364.0	9,135,103.0	3,677.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-16	0.017		0.10	-0.2		1.96	1,293		61	2.1	-5	0.22	-1	19	17
51000492	770,362.3	9,135,102.2	3,677.0	PSAD56_17S	2.00	4.00	2.00	CHANNEL				TR-16	0.022		0.18	-0.2		1.32	3,812		62	3.1	-5	0.19	-1	17	20
51000493	770,360.4	9,135,101.6	3,677.0	PSAD56_17S	4.00	6.00	2.00	CHANNEL				TR-16	-0.005		0.60	-0.2		0.94	1,634		58	1.3	-5	0.22	-1	6	14
51000494	770,358.6	9,135,100.7	3,677.0	PSAD56_17S	6.00	8.00	2.00	CHANNEL				TR-16	-0.005		0.70	-0.2		0.65	244		35	0.8	-5	0.14	-1	3	62
51000495	770,357.3	9,135,098.6	3,677.0	PSAD56_17S	8.00	10.00	2.00	CHANNEL				TR-16	-0.005		2.36	-0.2		0.66	133		37	3.2	-5	0.23	-1	13	9
51000496	770,356.4	9,135,096.5	3,677.0	PSAD56_17S	10.00	13.00	3.00	CHANNEL				TR-16	-0.005		0.46	-0.2		0.89	265		85	1.5	-5	2.74	-1	12	7
51000497	770,296.0	9,135,084.0	3,683.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-17	0.025		0.58	-0.2		1.41	43		142	0.9	-5	0.30	-1	20	14
51000498	770,296.7	9,135,085.9	3,683.0	PSAD56_17S	2.00	4.00	2.00	CHANNEL				TR-17	0.882		2.60	1.0		0.58	4,622		94	-0.5	-5	0.14	1	1	47
51000499	770,297.4	9,135,087.8	3,682.0	PSAD56_17S	4.00	5.00	1.00	CHANNEL				TR-17	0.017		1.31	-0.2		1.19	90		50	1.3	-5	0.28	2	25	18
51000500									STD		OREAS 62d		10.890	10.890	0.25	7.3		0.76	17		53	-0.5	-5	7.90	-1	5	13
51000501	770,297.7	9,135,088.7	3,682.0	PSAD56_17S	5.00	7.00	2.00	CHANNEL				TR-17	0.006		0.31	0.2		2.04	-3		218	1.3	-5	0.47	-1	35	16
51000502	770,298.4	9,135,090.6	3,681.0	PSAD56_17S	7.00	9.00	2.00	CHANNEL				TR-17	0.005		0.02	-0.2		1.48	25		48	0.6	-5	0.50	-1	18	21
51000503	770,299.1	9,135,092.5	3,681.0	PSAD56_17S	9.00	11.00	2.00	CHANNEL				TR-17	-0.005		0.02	-0.2		1.31	14		48	-0.5	-5	0.43	-1	16	24
51000504	770,261.0	9,135,280.0	3,652.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-18	0.008		0.12	-0.2		0.71	17		71	0.8	-5	0.38	-1	5	21
51000505	770,259.7	9,135,278.5	3,652.0	PSAD56_17S	2.00	4.00	2.00	CHANNEL				TR-18	0.011		0.31	-0.2		0.85	42		167	1.2	-5	0.39	-1	10	9
51000506	770,258.4	9,135,276.9	3,653.0	PSAD56_17S	4.00	6.00	2.00	CHANNEL				TR-18	0.007		0.08	-0.2		0.58	97		44	-0.5	-5	0.25	-1	-1	23
51000507	770,257.1	9,135,275.4	3,653.0	PSAD56_17S	6.00	8.00	2.00	CHANNEL				TR-18	0.178		0.30	3.7		0.39	1,875		58	-0.5	-5	0.18	-1	-1	48
51000508	770,255.9	9,135,273.9	3,653.0	PSAD56_17S	8.00	10.00	2.00	CHANNEL				TR-18	1.446		3.67	658.0	658	0.25	1,916		67	-0.5	-5	0.11	18	-1	103
51000509									FDUP	51000508			1.216		3.51	543.0	543	0.29	1,626		46	-0.5	-5	0.11	17	-1	135
51000510	770,254.6	9,135,272.3	3,654.0	PSAD56_17S	10.00	12.00	2.00	CHANNEL				TR-18	0.118		0.59	2.2		0.33	1,287		19	-0.5	-5	0.14	-1	-1	68
51000511	770,253.3	9,135,270.8	3,654.0	PSAD56_17S	12.00	14.00	2.00	CHANNEL				TR-18	0.114		0.28	2.1		0.45	2,364		45	-0.5	-5	0.16	-1	-1	28
51000512	770,252.0	9,135,269.3	3,655.0	PSAD56_17S	14.00	16.00	2.00	CHANNEL				TR-18	0.890		1.12	0.6		0.48	8,862		48	0.7	-5	0.14	2	2	25
51000513	770,250.7	9,135,267.7	3,655.0	PSAD56_17S	16.00	18.00	2.00	CHANNEL				TR-18	0.008		0.38	0.5		1.03	263		201	1.9	-5	0.31	-1	24	6
51000514	770,249.4	9,135,266.2	3,656.0	PSAD56_17S	18.00	20.00	2.00	CHANNEL				TR-18	-0.005		0.25	-0.2		1.24	19		118	1.6	-5	0.51	-1	12	4
51000515	770,248.1	9,135,264.7	3,656.0	PSAD56_17S	20.00	22.50	2.50	CHANNEL				TR-18	0.082		0.16	-0.2		1.67	87		81	1.0	-5	0.43	-1	8	10
51000516	770,185.0	9,135,213.0	3,663.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-19	0.969		1.54	2.2		0.56	1,276		60	-0.5	-5	0.22	-1	-1	40
51000517	770,185.6	9,135,214.9	3,663.0	PSAD56_17S	2.00	4.00	2.00	CHANNEL				TR-19	0.544		0.76	9.9		0.77	1,169		93	-0.5	-5	0.23	1	3	51
51000518	770,186.2	9,135,216.8	3,664.0	PSAD56_17S	4.00	6.00	2.00	CHANNEL				TR-19	4.899		0.57	5.7		0.57	4,440		95	-0.5	-5	0.13	-1	2	99
51000519	770,186.9	9,135,218.7	3,664.0	PSAD56_17S	6.00	8.00	2.00	CHANNEL				TR-19	0.026		0.34	0.5		1.18	372		122	-0.5	-5	0.23	-1	-1	12
51000520	770,187.5	9,135,220.6	3,665.0	PSAD56_17S	8.00	10.00	2.00	CHANNEL				TR-19	0.968		1.02	0.9		1.02	675		66	0.6	-5	0.21	-1	-1	26
51000521	770,188.1	9,135,222.5	3,665.0	PSAD56_17S	10.00	12.00	2.00	CHANNEL				TR-19	0.038		0.45	-0.2		0.88	746		142	-0.5	-5	0.21	-1	-1	15
51000522	770,188.7	9,135,224.4	3,666.0	PSAD56_17S	12.00	14.00	2.00	CHANNEL				TR-19	0.013		0.49	-0.2		1.19	482		75	0.6	-5	0.26	-1	2	6
51000523	770,189.3	9,135,226.3	3,666.0	PSAD56_17S	14.00	16.00	2.00	CHANNEL				TR-19	0.535		0.19	0.4		0.48	1,869		81	-0.5	-5	0.17	-1	-1	19
51000524	770,189.9	9,135,228.2	3,667.0	PSAD56_17S	16.00	18.00	2.00	CHANNEL				TR-19	0.110		0.39	0.2		1.10	1,617		49	1.1	-5	0.18	-1	3	30
51000525	770,190.6	9,135,230.1	3,667.0	PSAD56_17S	18.00	20.00	2.00	CHANNEL				TR-19	0.420		0.23	0.4		0.80	2,823		76	0.9	-5	0.16	-1	4	39
51000526	770,867.0	9,134,841.0	3,641.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-20	-0.005		0.18	0.7		0.89	32		59	3.9	-5	0.22	3	45	26
51000527	770,866.0	9,134,839.3	3,641.0	PSAD56_17S	2.00	4.00	2.00	CHANNEL				TR-20	0.011		0.31	-0.2		0.67	199		51	0.6	-5	0.17	-1	5	23
51000528	770,865.0	9,134,837.5	3,642.0	PSAD56_17S	4.00	6.00	2.00	CHANNEL				TR-20	0.364		0.40	0.7		0.64	1,575		45	-0.5	-5	0.13	-1	3	58
51000529	770,864.0	9,134,835.8	3,642.0	PSAD56_17S	6.00	8.00	2.00	CHANNEL				TR-20	0.677		0.52	1.1		0.65	2,780		45	-0.5	-5	0.11	-1	1	73
51000530	770,863.0	9,134,834.1	3,643.0	PSAD56_17S	8.00	10.00	2.00	CHANNEL				TR-20	0.007		0.25	-0.2		0.65	207		31	-0.5	-5	0.12	-1	-1	37
51000531	770,862.0	9,134,832.3	3,643.0	PSAD56_17S	10.00	12.00	2.00	CHANNEL				TR-20	-0.005		0.55	-0.2		0.55	164		20	-0.5	-5	0.13	-1	-1	44
51000532	770,861.0	9,134,830.6	3,644.0	PSAD56_17S	12.00	14.00	2.00	CHANNEL				TR-20	-0.005		0.82	-0.2		0.70	53		19	0.7	-5	0.10	-1	-1	46
51000533	770,860.0	9,134,828.9	3,644.0	PSAD56_17S	14.00	16.00	2.00	CHANNEL				TR-20	-0.005		0.76	-0.2		0.71	10		40	1.3	-5	0.12	-1	7	33
51000534	770,859.0	9,134,827.1	3,645.0	PSAD56_17S	16.00	18.00	2.00	CHANNEL				TR-20	0.016		0.28	-0.2		1.07	111		39	1.1	-5	0.25	-1	8	20
51000535	770,397.0	9,135,209.0	3,673.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-21	0.021		-0.02	-0.2		2.53	27		94	0.8	-5	0.30	-1	13	12
51000536	770,396.2	9,135,207.2	3,673.0	PSAD56_17S	2.00	4.00	2.00	CHANNEL				TR-21	0.007		0.53	-0.2		0.69	75		43	-0.5	-5	0.17	-1	-1	18

SURILOMA PROJECT GEOCHEMICAL DATA BASE FEBRUARY 2013

8de 16 

SampleID	Easting	Northing	RL	Grid	IntervalFrom	IntervalTo	Interval	SampleSubType	ChkType	ParentID	StandardID	Comments	Auppm	Auppm2	Hgppm	Agppm	Agppm2	Al%	Asppm	As%	Bappm	Beppm	Bippm	Ca%	Cdppm	Coppm	Crppm
51000537	770,395.3	9,135,205.4	3,673.0	PSAD56_17S	4.00	6.00	2.00	CHANNEL				TR-21	0.178		0.53	0.9		0.46	206		36	-0.5	-5	0.12	-1	-1	46
51000538	770,394.5	9,135,203.6	3,673.0	PSAD56_17S	6.00	8.00	2.00	CHANNEL				TR-21	0.210		0.18	0.8		0.99	387		63	-0.5	-5	0.12	-1	-1	97
51000539	770,393.6	9,135,201.7	3,673.0	PSAD56_17S	8.00	10.00	2.00	CHANNEL				TR-21	-0.005		0.28	-0.2		1.00	15		142	0.7	-5	0.20	-1	12	15
51000540	770,392.8	9,135,199.9	3,673.0	PSAD56_17S	10.00	12.00	2.00	CHANNEL				TR-21	0.006		0.25	0.3		1.06	249		196	1.1	-5	0.18	-1	21	12
51000541									STD		OREAS 54Pa		2.886		0.10	4.0		1.15	-3		25	-0.5	9	1.31	-1	21	26
51000542	770,391.9	9,135,198.1	3,673.0	PSAD56_17S	12.00	14.00	2.00	CHANNEL				TR-21	0.047		0.16	0.2		0.86	1,358		57	-0.5	-5	0.19	-1	2	50
51000543	770,391.1	9,135,196.3	3,672.0	PSAD56_17S	14.00	16.00	2.00	CHANNEL				TR-21	2.178		0.44	27.5		0.59	7,831		737	0.6	-5	0.14	-1	1	134
51000544	770,390.2	9,135,194.5	3,672.0	PSAD56_17S	16.00	18.00	2.00	CHANNEL				TR-21	0.040		0.09	-0.2		0.79	550		29	0.6	-5	0.21	-1	8	9
51000545	770,389.4	9,135,192.7	3,672.0	PSAD56_17S	18.00	20.00	2.00	CHANNEL				TR-21	2.827		0.56	131.0	131	0.60	5,765		765	0.9	-5	0.15	-1	6	139
51000546	770,388.5	9,135,190.9	3,672.0	PSAD56_17S	20.00	22.00	2.00	CHANNEL				TR-21	0.009		0.12	0.4		0.77	596		587	1.3	-5	0.36	-1	18	13
51000547	770,387.7	9,135,189.1	3,672.0	PSAD56_17S	22.00	24.00	2.00	CHANNEL				TR-21	0.042		0.10	0.3		0.88	969		299	1.3	-5	0.37	-1	11	23
51000548	770,386.9	9,135,187.2	3,672.0	PSAD56_17S	24.00	26.00	2.00	CHANNEL				TR-21	0.862		0.15	0.9		0.67	4,255		184	0.9	-5	0.31	2	7	55
51000549	770,386.0	9,135,185.4	3,672.0	PSAD56_17S	26.00	27.50	1.50	CHANNEL				TR-21	0.028		0.26	0.4		1.32	704		258	1.7	-5	0.49	-1	20	7
51000550	770,250.0	9,135,141.0	3,679.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-22	0.015		0.64	-0.2		0.90	688		115	0.8	-5	0.22	-1	5	49
51000551	770,251.3	9,135,142.5	3,679.0	PSAD56_17S	2.00	4.00	2.00	CHANNEL				TR-22	0.479		0.63	2.4		0.61	12,300	1.23	56	-0.5	-5	0.29	-1	-1	111
51000552									STD		OREAS 22b		-0.005		-0.02	-0.2		0.01	-3		6	-0.5	-5	0.02	-1	2	26
51000553	770,252.6	9,135,144.1	3,678.0	PSAD56_17S	4.00	6.00	2.00	CHANNEL				TR-22	0.283		0.43	1.1		0.61	3,564		60	0.6	-5	0.31	-1	4	84
51000554	770,253.9	9,135,145.6	3,678.0	PSAD56_17S	6.00	8.00	2.00	CHANNEL				TR-22	0.010		0.82	-0.2		0.67	293		43	-0.5	-5	0.36	-1	-1	23
51000555	770,255.1	9,135,147.1	3,678.0	PSAD56_17S	8.00	10.00	2.00	CHANNEL				TR-22	1.237		0.79	1.4		0.29	2,484		210	-0.5	-5	0.18	-1	-1	155
51000556	770,256.4	9,135,148.7	3,677.0	PSAD56_17S	10.00	12.00	2.00	CHANNEL				TR-22	0.220		0.37	0.5		0.47	1,096		93	-0.5	-5	0.24	-1	1	176
51000557	770,257.7	9,135,150.2	3,677.0	PSAD56_17S	12.00	14.00	2.00	CHANNEL				TR-22	0.014		0.25	-0.2		0.58	483		61	-0.5	-5	0.39	-1	-1	27
51000558	770,259.0	9,135,151.7	3,677.0	PSAD56_17S	14.00	15.50	1.50	CHANNEL				TR-22	-0.005		0.58	-0.2		1.05	120		59	-0.5	6	0.56	1	2	21
51000559	770,260.0	9,135,152.9	3,676.0	PSAD56_17S	15.50	18.50	3.00	CHANNEL				TR-22	0.010		0.44	-0.2		1.31	419		47	-0.5	-5	0.40	-1	-1	25
51000560	770,955.0	9,134,868.0	3,624.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-23	1.036		0.78	1.1		0.91	5,055		788	5.4	-5	0.13	-1	3	96
51000561									FDUP	51000560			1.064		0.85	1.2		0.83	4,894		879	5.1	-5	0.13	-1	4	83
51000562	770,955.8	9,134,869.8	3,624.0	PSAD56_17S	2.00	4.00	2.00	CHANNEL				TR-23	0.209		0.43	0.5		0.79	2,936		614	1.5	-5	0.13	-1	-1	85
51000563	770,956.6	9,134,871.7	3,624.0	PSAD56_17S	4.00	6.00	2.00	CHANNEL				TR-23	0.083		1.38	0.3		1.25	3,093		415	1.8	-5	0.13	2	18	38
51000564	770,957.3	9,134,873.5	3,624.0	PSAD56_17S	6.00	8.00	2.00	CHANNEL				TR-23	0.055		0.49	-0.2		2.33	2,047		131	2.3	-5	0.17	-1	26	25
51000565	770,958.1	9,134,875.4	3,624.0	PSAD56_17S	8.00	10.00	2.00	CHANNEL				TR-23	0.246		0.46	0.4		1.80	1,596		340	1.4	-5	0.19	-1	48	22
51000566	770,958.9	9,134,877.2	3,624.0	PSAD56_17S	10.00	12.00	2.00	CHANNEL				TR-23	0.356		0.40	0.5		1.86	1,491		278	1.4	-5	0.17	-1	36	35
51000567	770,959.7	9,134,879.0	3,623.0	PSAD56_17S	12.00	14.00	2.00	CHANNEL				TR-23	0.222		0.28	0.2		2.17	1,355		226	1.2	-5	0.14	-1	24	33
51000568	770,960.5	9,134,880.9	3,623.0	PSAD56_17S	14.00	16.00	2.00	CHANNEL				TR-23	0.262		0.23	0.3		2.23	1,292		201	1.1	-5	0.15	-1	21	24
51000569	770,961.3	9,134,882.7	3,623.0	PSAD56_17S	16.00	18.00	2.00	CHANNEL				TR-23	0.249		0.28	0.2		2.77	1,240		188	1.0	-5	0.14	-1	22	27
51000570	770,962.0	9,134,884.6	3,623.0	PSAD56_17S	18.00	20.50	2.50	CHANNEL				TR-23	0.443		0.38	0.4		2.67	1,454		201	1.0	-5	0.16	-1	23	22
51000571	770,101.0	9,135,256.0	3,656.0	PSAD56_17S	0.00	2.00	2.00	CHANNEL				TR-24	0.005		0.27	0.2		0.92	543		102	1.7	-5	0.25	-1	25	6
51000572	770,101.8	9,135,257.8	3,656.0	PSAD56_17S	2.00	4.00	2.00	CHANNEL				TR-24	0.474		0.27	52.4		0.48	1,398		56	-0.5	-5	0.15	-1	2	28
51000573									STD		OREAS 22b		-0.005		-0.02	-0.2		0.01	-3		6	-0.5	-5	0.02	-1	1	26
51000574	770,102.6	9,135,259.7	3,655.0	PSAD56_17S	4.00	6.00	2.00	CHANNEL				TR-24	0.008		0.49	-0.2		0.87	378		36	-0.5	-5	0.17	-1	2	22
51000575	770,103.3	9,135,261.5	3,655.0	PSAD56_17S	6.00	8.00	2.00	CHANNEL				TR-24	0.069		0.26	0.5		0.55	480		47	-0.5	-5	0.14	-1	-1	27
51000576	770,104.1	9,135,263.4	3,654.0	PSAD56_17S	8.00	10.00	2.00	CHANNEL				TR-24	0.024		0.54	-0.2		0.62	340		28	-0.5	-5	0.13	-1	-1	13
51000577	770,104.9	9,135,265.2	3,654.0	PSAD56_17S	10.00	12.00	2.00	CHANNEL				TR-24	-0.005		1.52	-0.2		0.78	41		31	1.3	-5	0.13	-1	-1	13
51000578	770,105.7	9,135,267.0	3,653.0	PSAD56_17S	12.00	14.00	2.00	CHANNEL				TR-24	0.019		1.73	-0.2		0.90	117		57	-0.5	-5	0.14	-1	-1	11
51000579	770,106.5	9,135,268.9	3,653.0	PSAD56_17S	14.00	16.00	2.00	CHANNEL				TR-24	0.022		0.77	0.3		0.69	257		117	-0.5	-5	0.12	-1	2	7
51000580	770,107.3	9,135,270.7	3,652.0	PSAD56_17S	16.00	18.00	2.00	CHANNEL				TR-24	-0.005		0.52	-0.2		0.89	383		75	0.7	-5	0.16	-1	9	14
51000581	770,108.0	9,135,272.6	3,652.0	PSAD56_17S	18.00	19.00	1.00	CHANNEL				TR-24	-0.005		0.39	-0.2		2.16	49		132	2.0	-5	0.29	-1	25	5
51000582	770,115.0	9,135,259.0	3,655.0	PSAD56_17S	0.00	2.80	2.80	CHANNEL					2.051		0.53	3.3		0.42	3,571		42	-0.5	-5	0.15	-1	-1	65

SURILOMA PROJECT GEOCHEMICAL DATA BASE FEBRUARY 2013

9de 16 

SampleID	Cuppm	Cu%	Fe%	Gappm	K%	Lappm	Mg%	Mnppm	Moppm	Na%	Nbppm	Nippm	P%	Pbppm	Pb%	S%	Sbppm	Sb%	Scppm	Snppm	Srppm	Ti%	Tlppm	Vppm	Wppm	Yppm	Znppm	Zn%	Zrppm	BATCH
218367	198.0		1.32	-10	0.03	12.0	-0.01	73	4	-0.01	-1	7	0.05	262		0.02	155		1.5	-10	7.1	-0.01	-2	5	-10	2.5	37.1		0.8	ABR0134.R12
218368	101.0		8.04	11	0.29	13.6	0.01	65	2	-0.01	-1	2	0.11	134		0.21	320		20.7	-10	61.3	-0.01	5	38	-10	2.0	6.9		2.4	ABR0134.R12
218369	45.5		10.12	10	0.23	17.6	-0.01	119	3	-0.01	-1	3	0.14	156		0.21	353		22.8	-10	69.2	-0.01	6	49	-10	2.2	6.5		1.9	ABR0134.R12
218370	47.7		9.31	-10	0.07	20.4	-0.01	16	5	-0.01	-1	3	0.22	1,653		0.06	1,222		4.1	-10	72.9	-0.01	-2	67	-10	6.9	24.4		0.5	ABR0134.R12
218371	21.9		6.68	-10	0.13	41.6	-0.01	29	4	-0.01	-1	7	0.44	534		0.15	615		3.3	-10	516.0	-0.01	-2	55	-10	13.6	19.3		0.7	ABR0134.R12
218372	16.4		6.10	-10	0.25	12.0	-0.01	11	3	-0.01	-1	-1	0.17	21		0.01	483		10.4	-10	17.3	-0.01	-2	75	-10	3.2	6.7		2.5	ABR0134.R12
218373	18.6		3.00	-10	0.23	5.7	0.02	71	2	-0.01	1	4	0.15	25		0.22	131		12.8	-10	10.8	-0.01	9	18	-10	2.2	2.1		1.2	ABR0134.R12
218374	40.6		3.04	-10	0.05	5.0	-0.01	35	6	-0.01	2	9	0.04	700		0.07	1,039		2.2	-10	21.4	-0.01	-2	9	-10	1.0	125.0		1.4	ABR0134.R12
218375	16.7		6.28	-10	0.13	5.3	-0.01	43	31	-0.01	-1	3	0.09	31		0.16	667		4.0	-10	34.1	-0.01	8	31	-10	2.9	11.7		1.5	ABR0134.R12
218376	33.6		11.97	-10	0.29	9.6	-0.01	46	26	0.01	-1	2	0.09	32		0.48	381		5.9	-10	44.8	-0.01	8	60	-10	3.1	13.3		1.8	ABR0134.R12
218377	43.7		11.05	-10	0.18	12.2	-0.01	51	11	-0.01	-1	4	0.11	33		0.26	385		12.5	-10	24.6	-0.01	7	77	-10	4.2	12.3		2.3	ABR0134.R12
218378	18.9		7.14	-10	0.10	32.6	0.01	116	5	-0.01	-1	4	0.23	22		0.12	287		15.8	-10	306.0	-0.01	-2	22	-10	7.9	71.5		0.7	ABR0134.R12
218379	23.2		15.00	-10	0.09	9.1	-0.01	55	10	-0.01	-1	3	0.19	49		0.01	387		2.8	-10	3.4	-0.01	5	6	-10	9.5	172.0		1.4	ABR0134.R12
218383	6.3		0.77	-10	0.13	11.6	0.01	75	3	-0.01	-1	7	-0.01	7		0.02	33		1.2	-10	7.8	-0.01	5	4	-10	2.8	8.6		2.0	ABR0134.R12
218384	4.1		0.87	-10	0.03	28.6	0.02	472	2	-0.01	-1	6	0.01	7		0.03	-5		2.2	-10	22.7	-0.01	-2	10	-10	38.0	34.2		4.0	ABR0134.R12
218385	6.3		0.96	-10	0.06	13.1	-0.01	51	4	-0.01	1	4	0.02	56		0.02	52		1.2	-10	5.3	-0.01	-2	4	-10	3.2	16.9		1.3	ABR0134.R12
218386	8.1		0.65	-10	0.05	23.2	-0.01	53	3	-0.01	2	9	0.01	75		0.06	35		1.3	-10	14.5	-0.01	3	3	-10	4.5	10.0		1.7	ABR0134.R12
218387	6.5		0.29	-10	0.02	1.7	-0.01	26	3	-0.01	2	8	-0.01	1,061		0.02	1,817		-0.5	-10	1.3	-0.01	-2	-2	12	-0.5	70.6		-0.5	ABR0134.R12
218388	90.6		1.37	-10	0.08	3.8	-0.01	84	2	-0.01	2	9	-0.01	969		1.61	17,900	1.79	-0.5	-10	5.4	-0.01	-2	3	-10	0.7	264		-0.5	ABR0134.R12
218389	11.4		0.43	-10	0.08	2.4	0.02	178	4	-0.01	-1	11	-0.01	12		-0.01	78		-0.5	-10	3.0	-0.01	5	3	-10	0.9	5.5		0.6	ABR0134.R12
218390	36.8		1.95	-10	0.12	5.7	0.02	979	1	-0.01	-1	7	0.01	17		0.39	95		2.7	-10	9.2	-0.01	-2	6	-10	2.5	2.7		0.9	ABR0134.R12
218391	20.5		4.22	-10	0.38	12.8	0.04	147	1	-0.01	-1	3	0.02	26		0.13	79		5.0	-10	9.6	-0.01	-2	19	-10	2.9	7.9		2.4	ABR0134.R12
218392	19.6		2.45	-10	0.19	12.1	0.02	515	4	-0.01	-1	5	0.04	31		0.19	51		3.5	-10	11.5	-0.01	-2	8	-10	4.7	7.6		2.5	ABR0134.R12
218393	44.3		5.45	-10	0.38	15.2	0.01	46	1	-0.01	-1	4	0.07	266		1.76	127		2.8	-10	17.1	-0.01	-2	24	-10	2.2	109.0		2.1	ABR0134.R12
218394	291.0		3.03	-10	0.12	6.2	-0.01	280	5	-0.01	1	11	0.01	644		0.71	570		1.1	-10	10.3	-0.01	-2	6	-10	2.3	50.1		1.0	ABR0134.R12
218395	227.0		1.80	-10	0.14	11.8	0.01	97	5	-0.01	-1	8	0.02	1,839		0.17	4,302		1.1	-10	10.2	-0.01	-2	8	13	3.5	478.0		1.3	ABR0134.R12
218396	61.8		1.75	-10	0.08	10.3	-0.01	36	4	-0.01	-1	8	0.04	571		0.32	9,346		3.7	-10	47.5	-0.01	-2	8	-10	2.9	823.0		0.8	ABR0134.R12
218397	186.0		1.31	-10	0.06	3.4	-0.01	69	7	-0.01	4	20	-0.01	2,145		1.48	17,800	1.78	0.5	-10	1.8	-0.01	-2	4	13	-0.5	3660		-0.5	ABR0134.R12
218398	34.2		1.64	-10	0.08	4.7	-0.01	61	5	-0.01	-1	8	0.01	945		1.51	16,200	1.62	1.4	-10	6.4	-0.01	-2	4	-10	1.4	816		0.7	ABR0134.R12
218399	94.8		1.43	-10	0.07	3.2	-0.01	52	3	-0.01	-1	9	0.02	2,946		3.19	63,100	6.31	0.8	-10	9.4	-0.01	-2	3	-10	1.2	1630		0.6	ABR0134.R12
218400	61.5		1.16	-10	0.05	1.6	-0.01	63	6	-0.01	4	20	0.03	1,472		5.16	120,000	12.00	-0.5	-10	15.2	-0.01	-2	3	-10	0.7	4120		-0.5	ABR0134.R12
218971	3,370.0		4.82	-10	0.60	17.9	1.36	386	259	0.18	2	22	0.1	24		0.49	-5		6.5	-10	72.0	0.22	-2	111	-10	12.6	80.5		16.7	JUL0030.R12
218972	47.6		2.04	-10	0.18	4.8	0.49	556	6	0.03	-1	6	0.04	5		0.62	-5		3.6	44	104.0	0.01	5	30	-10	4.3	35.7		6.4	JUL0030.R12
218973	15,000.0	1.50	7.90	-10	0.13	7.8	1.06	320	2	0.06	-1	27	0.05	40		1.61	-5		5.1	-10	63.6	0.09	-2	98	12	7.1	145.0		9.0	JUL0030.R12
218974	10.2		0.56	-10	-0.01	0.8	-0.01	65	6	-0.01	-1	6	-0.01	6		-0.01	-5		-0.5	-10	-0.5	-0.01	-2	-2	-10	-0.5	8.3		-0.5	JUL0030.R12
218975	47.8		2.12	-10	0.19	4.9	0.51	578	5	0.03	-1	8	0.04	11		0.65	-5		3.7	-10	108.0	0.01	6	31	-10	4.6	37.2		6.6	JUL0030.R12
218976	8.4		0.52	-10	-0.01	0.8	-0.01	62	4	-0.01	-1	-1	-0.01	-2		-0.01	-5		-0.5	28	-0.5	-0.01	5	-2	-10	-0.5	7.5		-0.5	JUL0030.R12
218977	15,000.0	1.50	7.94	-10	0.13	7.8	1.06	320	4	0.06	-1	22	0.05	33		1.61	-5		5.1	-10	61.9	0.08	-2	98	-10	7.2	152.0		8.9	JUL0030.R12
218978	3,250.0		4.83	-10	0.60	17.8	1.33	381	255	0.17	-1	24	0.1	23		0.48	-5		6.4	16	68.7	0.22	-2	110	-10	12.5	74.7		16.2	JUL0030.R12
218979	47.2		2.08	-10	0.19	4.9	0.5	565	6	0.03	-1	8	0.04	15		0.63	-5		3.6	29	106.0	0.01	-2	31	-10	4.5	35.5		6.5	JUL0030.R12
218980	8.0		0.53	-10	-0.01	-0.5	-0.01	63	5	-0.01	-1	-1	-0.01	3		-0.01	-5		-0.5	18	-0.5	-0.01	-2	-2	14	-0.5	7.7		-0.5	JUL0030.R12
218981	14,900.0	1.49	8.11	-10	0.13	7.9	1.08	325	3	0.07	-1	24	0.05	36		1.64	-5		5.2	-10	64.7	0.09	-2	99	-10	7.3	145.0		9.3	JUL0030.R12
218982	50.3		2.15	-10	0.19	5.0	0.52	581	7	0.03	-1	10	0.04	25		0.65	-5		3.8	-10	109.0	0.01	8	31	-10	4.5	37.8		6.7	JUL0030.R12
218983	3,210.0		5.02	-10	0.59	17.4	1.33	377	250	0.17	2	24	0.1	20		0.48	-5		6.3	-10	69.7	0.22	-2	109	-10	12.4	76.7		16.3	JUL0030.R12
218984	8.0		0.55	-10	-0.01	0.8	-0.01	65	6	-0.01	-1	6	-0.01	-2		-0.01	-5		-0.5	-10	-0.5	-0.01	4	-2	-10	-0.5	7.5		-0.5	JUL0030.R12
218985	15,000.0	1.50	8.03	-10	0.14	8.0	1.1	329	3	0.07	-1	26	0.05	43		1.67	-5		5.2	-10	63.9	0.08	-2	100	-10	7.5	149.0		9.1	JUL0030.R12
218986	3,440.0		4.65	-10	0.60	17.9	1.36	383	256	0.18	3	22	0.1	21		0.48	-5		6.5	12	70.6	0.21	-2	109	-10	12.5	82.5		16.7	JUL0030.R12
218987	48.5		2.12	-10	0.19	5.2	0.52	578	7	0.03	-1	-1	0.04	34		0.65	-5		3.6	12	109.0	0.01	-2	31	-10	4.6	35.6		6.9	JUL0030.R12
218988	7.0		0.53	-10	-0.01	0.9	-0.01	63	3	-0.01	-1	-1	-0.01	7		-0.01	-5		-0.5	-10	-0.5	-0.01	-2	-2	-10	-0.5	7.4		0.6	JUL0030.R12
218989	3,250.0		4.74	-10	0.60	18.0	1.34	379	250	0.18	-1	23	0.1	16		0.48	-5		6.4	-10	70.0	0.21	-2	109	-10	12.3	77.8		16.4	JUL0030.R12
218990	15,100.0	1.51	7.77	-10	0.13	7.6	1.07	313	-1	0.06	-1	23	0.05	40		1.6	-5		4.9	12	61.4	0.08	-2	96	25	7.0	149.0		8.7	JUL0030.R12
218991	21.2		6.15	-10	0.25	15.0	0.04	26	2	0.02	-1	3	0.14	220		0.01	-5		14.5	-10	9.0	-0.01	-2	70	-10	4.8	59.6		1.3	JUL0261.R12
218992	43.7		12.23	-10	0.06	28.9	0.01	30	5	-0.01	-1	4	0.35	6,608		0.18	2,190		5.8	41	75.0	-0.01	-2	55	12	10.4	188.0		1.2	JUL0261.R12
218993	39.6		12.26	10	0.13	8.8	0.02	42	7	-0.01	-1	3	0.14	69		0.03	-5		10.6	-10	1.7	0.01	-2	329	16	11.1	77.3		1.4	JUL0261.R12
218994	63.0		5.41	-10	0.16	13.1	0.17	673	-1	0.02	-1	-1	0.07	67		0.02	19		2.4	-10	15.4	-0.01	-2	26	-10	3.6	91.3		0.7	JUL0261.R12
218995	47.4		3.55	-10	0.17	4.6	0.06	210	3	0.01	-1	2	0.05	189		0.01	8		1.4	-10	11.5	-0.01	-2	22	-10	3.5	64.1		0.6	JUL0261.R12
218996	155.0		6.75	35	0.12	1.1	-0.01	86	3	-0.01	-1	4	0.02	6,717		0.81	3,721		-0.5	-10	1.5	-0.01	-2	14	-10	0.7	5,320.0		-0.5	JUL0261.R12
218997	1,520.0		1.42	69	0.01	0.5	-0.01	153	2	-0.01	-1	7	-0.01	204,100	20.41	8.9	34,770	3.48	-0.5	-10	7.8	-0.01	-2	-2	55	-0.5	49200	4.92	-0.5	JUL0261.R12
218998	63.2		4.15	-10	0.23	4.9	-0.01	540	3	-0.01	-1	3	0.03	1,744		0.26	229		0.5	-10	2.8	-0.01	-2	4	-10	0.9	147.0		1.9	JUL0261.R12
219011	42.4		1.12	-10	0.21	10.8	0.01	71	3	-0.01	1	9	0.03	849		1.48	20,900	2.09	0.9	-10	30.4	-0.01	-2	7	-10	2	582		1.3	ABR0134.R12
219012	73.8		1.83	-10	0.07	1.7	-0.01	530	3	-0.01	-1	7	0.01	28		0.71	162		1.9	-10	13.7	-0.01	-2	3	-10	1.0	47.3		-0.5	ABR0134.R12
219013	8.1		0.42	-10	-0.01	0.7	-0.01	40	4	-0.01	4	11	-0.01	4		0.03	73		-0.5	-10	2.0	-0.01	-2	3	-10	1.0	9.3		-0.5	ABR0134.R12
219014	10.1		0.88	-10	-0.01	1.8	-0.01	1236	22	-0.01	2	24	-0.01	6		0.02	128		-0.5	-10	8.7	-0.01	-2	13	-10	1.0	7.8		0.8	ABR0134.R12
219015	431.0		5.77	-10	0.16	3.5	-0.01	40	7	-0.01	-1	9	0.04	929		0.77	345		1.1	-10	16.0	-0.01	-2	17	-10	1.5	58.3		1.0	ABR0134.R12
219016	23.0		4.82	-10	0.14	12.2	-0.01	32	16	-0.01	-1	3	0.1	18		0.11	237		9.9	-10	128.0	-0.01	-2	28	-10	4.7	19.2		1.1	ABR0134.R12
219017	21.7		2.53	-10	0.12	5.0	-0.01	37	1	-0.01	-1	4	0.03	20		0.04	128		1.9	-10	18.8	-0.01	-2	11	-10	2.2	3.2		2.1	ABR0134.R12
219018	32.6		1.54	-10	0.06	5.2	-0.01	29	3	-0.01	-1	6	0.04	109		0.17	955		1.8	-10	35.9	-0.01	-2	6	-10	2.7	7.7		1.0	ABR0134.R12
219019	11.7		2.54	-10	0.04	10.6	-0.01	44	2	-0.01	-1	2	0.05	22		0.14	103		2.7	-10	52.3	-0.01	-2	13	-10	5.3	10.0		2.5	ABR0134.R12
219020	53.2		3.00	-10	0.08	11.6	-0.01	42	8	-0.01	-1	6	0.15	271		0.19	3,301		4.4	-10	102.0	-0.01	-2	14	-10	5.4	6.8		1.2	ABR0134.R12
219021	11.6		1.59	-10	0.05	9.1	-0.01	61	2	-0.01	-1	5	0.07	34		0.22	264		2.5	-10	60.0	-0.01	-2	13	-10	3.7	11.4		1.0	ABR0134.R12
219022	8.6		3.56	-10	0.05	8.4	-0.01	60	1	-0.01	1	3	0.16	43		0.17	121		8.6	-10	39.2	-0.01	-2	25	-10	3.1	6.4		1.8	ABR0134.R12
219023	9.8		1.89	-10	0.07	11.4	-0.01	31	2	-0.01	1	5	0.08	20		0.02	127		3.6	-10	14.1	-0.01	-2	13	-10	3.5	3.3		1.9	ABR0134.R12
219024	8.9		1.11	-10	0.03	13.9	-0.01	73	2	-0.01	-1	4	0.06	12		0.05	47		4.7	-10	59.0	-0.01	-2	10	-10	7.1	6.1		1.4	ABR0134.R12
219025	666.0		2.50	-10	0.03	2.7	-0.01	49	9	-0.01	-1	6	0.07	8,140		1.51	10,400	1.04	1.6	16	44.7	-0.01	-2	5	38	1	8390		-0.5	MAY027.R12
219026	28.3		3.17	-10	0.06	6.5	0.01	55	-1	-0.01	-1	4	0.06	25		0.11	108		3.0	-10	34.9	-0.01	-2	15	-10	6.9	46.0		0.6	MAY027.R12
219027	20.7		3.94	-10	0.12	12.6	0.01	22	2	-0.01	-1	2	0.13	24		0.04	34		6.0	-10	16.4	-0.01	-2	34	-10	3.8	22.7		3.2	MAY027.R12
219028	53.1		1.20	-10	0.02	2.8	-0.01	35	2	-0.01	-1	6	0.03	1,892		0.6	1,128		1.5	-10	17.3	-0.01	-2	5	-10	1.0	31.3		-0.5	MAY027.R12
219029	24.9		1.20	-10	0.03	10.7	-0.01	73	1	-0.01	-1	6	0.03	18		0.03	12		2.6	-10	5.2	-0.01	-2	18	-10	6.7	25.7		2.8	MAY027.R12
219030	24.0		0.34	-10	0.07	5.4	0.01	1146	2	-0.01	-1	6	-0.01	290		0.04	175		1.6	-10	7.4	-0.01	-2	4	-10	1.4	141.0		0.8	MAY027.R12
219031	20.8		0.66	-10	0.03	4.0	-0.01	65	4	-0.01	-1	9	-0.01	399		0.04	1,204		0.6	-10	2.1	-0.01	-2	4	-10	1.0	57.1		-0.5	MAY027.R12
219032	6.0		3.43	-10	0.24	18.7	0.01	175	-1	-0.01	-1	8	0.11	21		3.69	18		4.6	-10	10.8	-0.01	-2	7	-10	14.3	135.0		0.8	MAY027.R12
219033	729.0		2.35	-10	0.10	5.4	-0.01	367	3	-0.01	-1	10	0.01	1,432		1.76	594		0.8	-10	2.2	-0.01	-2	3	-10	1.1	1,050.0		-0.5	MAY027.R12
219039	13.0		3.88	-10	0.12	16.0	-0.01	140	3	-0.01	-1	2	0.06	15		0.02	57		3.2	-10	14.0	-0.01	-2	19	-10	5.6	9.0		1.5	MAY027.R12

SURILOMA PROJECT GEOCHEMICAL DATA BASE FEBRUARY 2013

10de 16 

SampleID	Cuppm	Cu%	Fe%	Gappm	K%	Lappm	Mg%	Mnppm	Moppm	Na%	Nbppm	Nippm	P%	Pbppm	Pb%	S%	Sbppm	Sb%	Scppm	Snppm	Srppm	Ti%	Tlppm	Vppm	Wppm	Yppm	Znppm	Zn%	Zrppm	BATCH
219040	14.0		3.92	-10	0.05	20.8	-0.01	33	9	-0.01	-1	5	0.2	22		-0.01	258		3.6	-10	139.0	-0.01	-2	15	-10	11.2	10.6		0.6	MAY027.R12
219041	13.0		3.71	-10	0.24	17.4	-0.01	15	4	-0.01	-1	-1	0.05	12		0.06	81		5.0	-10	17.2	-0.01	-2	16	-10	3.4	2.3		1.6	MAY027.R12
219042	35.3		2.65	-10	0.05	6.7	-0.01	37	11	-0.01	-1	6	0.13	78		0.18	369		1.6	-10	129.0	-0.01	-2	5	-10	4.7	5.8		-0.5	MAY027.R12
219043	12.1		5.42	-10	0.10	15.2	-0.01	28	4	-0.01	-1	2	0.11	13		0.1	69		2.6	-10	72.9	-0.01	-2	20	-10	4.4	4.7		1.4	MAY027.R12
219044	17.0		7.08	-10	0.22	17.4	-0.01	32	10	0.01	-1	2	0.16	21		0.3	172		4.4	-10	89.4	-0.01	-2	27	-10	5.9	7.7		1.0	MAY027.R12
219045	14.6		4.95	-10	0.19	16.9	-0.01	16	2	-0.01	-1	3	0.28	35		0.13	112		6.4	-10	36.8	-0.01	-2	34	-10	3.7	8.5		1.7	MAY027.R12
219046	43.8		8.80	-10	0.13	10.5	-0.01	18	-1	-0.01	-1	1	0.13	42		0.06	133		5.8	-10	26.1	-0.01	-2	34	-10	2.3	18.6		2.4	MAY027.R12
219047	27.6		5.63	-10	0.09	10.7	-0.01	30	2	-0.01	-1	3	0.08	185		0.07	269		5.9	-10	32.1	-0.01	-2	24	-10	2.3	18.6		2.1	MAY027.R12
219048	18.6		1.12	-10	0.03	5.8	-0.01	23	4	-0.01	-1	5	0.06	919		0.03	1,116		2.1	-10	42.9	-0.01	-2	5	-10	1.6	17.3		0.6	MAY027.R12
219049	21.4		5.71	-10	0.14	13.7	-0.01	34	1	-0.01	-1	2	0.11	59		0.16	182		9.8	-10	49.3	-0.01	-2	26	-10	2.1	3.4		1.3	MAY027.R12
219050	22.8		7.80	-10	0.36	14.3	-0.01	37	2	-0.01	-1	2	0.24	41		0.46	318		6.1	-10	98.5	-0.01	-2	27	-10	5.0	11.3		1.0	MAY027.R12
219051	13.5		4.54	-10	0.20	8.6	-0.01	23	1	-0.01	-1	4	0.14	31		0.21	182		4.1	-10	44.4	-0.01	-2	20	-10	3.0	4.4		1.0	MAY027.R12
219052	27.8		8.65	-10	0.17	7.2	0.01	15	-1	-0.01	-1	1	0.13	22		0.06	146		6.4	-10	5.4	-0.01	-2	33	-10	7.2	8.8		1.6	MAY027.R12
219053	8.3		3.08	-10	0.23	14.1	-0.01	46	1	-0.01	-1	2	0.19	21		0.06	166		6.0	-10	32.6	-0.01	-2	26	-10	3.6	3.1		1.6	MAY027.R12
219054	17.9		4.32	-10	0.13	11.2	-0.01	52	5	-0.01	-1	2	0.1	39		0.07	85		6.1	-10	9.8	-0.01	-2	19	-10	3.3	5.5		1.2	MAY027.R12
219055	31.9		5.20	-10	0.11	13.4	-0.01	29	-1	-0.01	-1	2	0.13	107		0.12	239		11.7	-10	55.2	-0.01	-2	22	-10	2.2	3.1		1.7	MAY027.R12
219056	15.5		5.47	-10	0.17	18.4	-0.01	25	-1	-0.01	-1	1	0.23	16		0.01	139		12.2	-10	41.2	-0.01	-2	35	-10	4.9	9.7		1.7	MAY027.R12
219057	15.2		6.07	-10	0.08	22.9	-0.01	62	1	-0.01	-1	4	0.29	16		0.01	136		11.1	-10	46.3	-0.01	-2	55	-10	5.1	32.4		2.0	MAY027.R12
219058	30.7		5.45	-10	0.33	9.6	0.03	74	-1	-0.01	-1	2	0.16	10		0.01	25		11.6	-10	8.0	-0.01	-2	49	-10	20.0	31.0		2.9	MAY027.R12
219059	79.8		1.99	-10	0.07	5.9	-0.01	50	2	-0.01	-1	6	0.03	2,930		0.54	2,810		1.3	-10	14.1	-0.01	-2	5	-10	1.1	2,440.0		-0.5	MAY027.R12
219060	135.0		2.59	-10	0.23	10.1	0.01	46	1	-0.01	-1	3	0.03	85		0.42	11,900	1.19	5.3	-10	8.7	-0.01	-2	8	-10	2.7	19.5		1.0	MAY027.R12
219061	51.3		2.92	-10	0.10	6.5	-0.01	88	2	-0.01	-1	7	0.03	742		1.19	4,866		2.9	-10	4.9	-0.01	-2	7	-10	1.4	1,270.0		0.7	MAY027.R12
219062	27.3		3.94	-10	0.30	6.3	0.01	42	2	-0.01	-1	3	0.02	49		0.5	606		4.8	-10	2.6	-0.01	-2	20	-10	1.3	55.3		1.1	MAY027.R12
219063	10.8		3.13	-10	0.17	12.1	0.03	19	-1	-0.01	-1	3	0.07	69		0.12	1,786		1.6	-10	27.9	-0.01	-2	16	-10	1.8	16.6		0.9	MAY027.R12
219064	29.2		8.05	-10	0.28	9.4	0.03	148	-1	-0.01	-1	-1	0.28	18		0.07	112		10.0	-10	17.1	-0.01	-2	48	-10	5.5	50.1		1.4	MAY027.R12
219065	18.8		4.08	-10	0.15	17.4	0.01	41	2	-0.01	-1	5	0.22	885		0.16	280		5.5	-10	153.0	-0.01	-2	17	-10	4.8	19.7		0.6	MAY027.R12
219066	20.2		10.93	-10	0.23	8.2	0.02	237	-1	-0.01	-1	1	0.23	12		0.03	32		7.0	-10	8.3	-0.01	-2	66	-10	11.1	174.0		2.1	MAY027.R12
219067	9.4		3.89	-10	0.37	12.4	0.03	32	-1	-0.01	-1	2	0.05	18		0.18	572		3.9	-10	15.1	-0.01	-2	27	-10	2.1	7.8		1.3	MAY027.R12
219068	319.0		1.25	-10	0.08	7.5	-0.01	39	2	-0.01	-1	5	0.07	4,076		1.06	12,300	1.23	1.3	-10	33.3	-0.01	-2	6	33	1.6	7520		-0.5	MAY027.R12
219069	28.0		5.61	-10	0.15	7.3	0.02	24	1	-0.01	-1	3	0.02	118		0.06	501		5.8	-10	5.4	-0.01	-2	23	-10	1.4	277.0		1.5	MAY027.R12
219070	20.8		4.97	-10	0.26	8.2	0.02	33	-1	-0.01	-1	3	0.05	140		0.15	1,867		5.4	-10	12.7	-0.01	-2	30	-10	1.4	20.2		1.1	MAY027.R12
219071	6,920.0		7.61	-10	0.09	8.6	0.16	510	3	0.03	-1	10	0.25	6,252		3.19	11,970	1.20	2.5	194	93.8	0.05	-2	44	-10	6	1340		3.4	MAY0286.R12
219072	36.4		5.03	-10	0.02	9.3	0.01	191	-1	-0.01	-1	6	0.09	31		0.08	179		5.5	-10	46.7	-0.01	-2	34	-10	8.5	49.9		1.2	MAY0286.R12
219073	16.7		11.25	-10	0.14	8.9	0.04	94	1	-0.01	2	3	0.25	63		0.06	47		3.8	11	12.2	-0.01	-2	51	-10	3.8	47.9		1.4	MAY0286.R12
219074	37.5		10.29	-10	0.05	30.4	0.01	37	-1	-0.01	4	10	0.35	11,100	1.11	0.24	2,761		3.9	127	88.9	-0.01	-2	27	-10	11.7	125.0		1.0	MAY0286.R12
219075	40.9		3.83	-10	-0.01	2.3	0.02	28	-1	-0.01	3	7	0.06	1,754		0.05	163		-0.5	-10	5.2	-0.01	-2	-2	-10	1.2	29.2		0.9	MAY0286.R12
219076	26.0		4.14	-10	0.11	17.7	0.36	158	-1	-0.01	2	-1	0.14	162		0.02	8		4.3	-10	13.4	0.03	-2	29	-10	8.4	74.9		1.3	MAY0286.R12
219077	52.4		5.66	-10	0.15	7.9	0.02	167	9	-0.01	-1	7	0.05	38		0.8	-5		1.8	11	4.2	-0.01	-2	14	-10	8.0	109.0		1.1	MAY0286.R12
219078	636.0		2.86	-10	0.14	0.8	-0.01	40	-1	-0.01	-1	-1	0.03	5,491		2.68	1,228		0.8	-10	2.5	-0.01	-2	7	-10	1.7	6,620.0		0.9	MAY0286.R12
219079	722.0		7.62	61	0.04	-0.5	-0.01	150	2	-0.01	-1	5	0.06	33,500	3.35	10	1,677		-0.5	33	3.8	-0.01	-2	50	-10	1.1	126,200.0	12.62	-0.5	MAY0286.R12
219080	370.0		6.31	14	0.12	6.8	-0.01	28	-1	-0.01	2	3	0.06	4,934		0.4	2,324		1.2	-10	7.9	-0.01	-2	43	-10	1.3	324.0		0.8	MAY0286.R12
219081	393.0		5.78	24	0.02	-0.5	-0.01	128	-1	-0.01	2	9	-0.01	8,872		1.43	8,269		-0.5	26	2.0	-0.01	-2	-2	-10	-0.5	10,500.0	1.05	-0.5	MAY0286.R12
219082	5,320.0		10.14	61	0.02	-0.5	-0.01	712	-1	-0.01	-1	5	0.03	45,600	4.56	10	6,494		-0.5	101	7.0	-0.01	-2	-2	19	2.4	100,500.0	10.05	-0.5	MAY0286.R12
219086	23.8		6.99	-10	0.10	7.5	0.02	830	-1	0.02	-1	-1	0.16	95		0.02	-5		10.2	16	3.7	-0.01	-2	65	-10	6.0	127.0		1.7	MAY0286.R12
219087	14.9		2.84	-10	0.23	17.1	0.05	3571	-1	-0.01	-1	-1	0.05	99		0.01	8		2.3	-10	26.4	-0.01	-2	22	-10	13.9	310.0		1.3	MAY0286.R12
219089	28.9		2.65	-10	0.16	10.8	0.03	129	2	-0.01	-1	4	0.04	430		0.28	2,451		3.0	-10	48.1	-0.01	-2	9	-10	4.2	139.0		1.0	JUL0261.R12
219090	52.2		1.80	-10	0.11	7.6	-0.01	96	2	-0.01	-1	7	0.05	466		0.59	10,400	1.04	2.4	-10	62.7	-0.01	-2	6	-10	1.9	276		0.6	JUL0261.R12
219091	26.5		1.04	-10	0.07	4.1	0.01	99	2	-0.01	-1	5	0.01	105		0.69	26,700	2.67	1.9	-10	37.4	-0.01	-2	4	-10	5.1	33.4		-0.5	JUL0261.R12
219092	20.0		2.74	-10	0.25	14.3	0.07	142	-1	-0.01	-1	1	0.05	38		0.06	38		4.1	-10	13.0	-0.01	-2	17	-10	5.0	50.9		3.0	JUL0261.R12
219093	29.9		4.01	-10	0.18	14.1	0.17	324	-1	0.01	-1	-1	0.09	135		0.18	32		3.6	-10	20.1	-0.01	-2	35	-10	3.0	36.5		1.2	JUL0261.R12
219094	9.5		2.94	-10	0.22	22.9	0.03	1377	11	-0.01	-1	3	0.04	150		-0.01	57		1.8	-10	13.0	-0.01	-2	5	-10	12.4	102.0		1.6	JUL0261.R12
219095	8.2		0.53	-10	-0.01	0.6	-0.01	78	6	-0.01	-1	3	-0.01	52		-0.01	6		-0.5	-10	-0.5	-0.01	-2	-2	-10	-0.5	23.9		-0.5	JUL0261.R12
219096	20.2		4.16	-10	0.12	-0.5	-0.01	57	2	-0.01	-1	-1	0.05	116		0.02	49		0.7	-10	2.0	-0.01	-2	11	-10	-0.5	140.0		0.6	JUL0261.R12
219097	19.8		2.88	-10	0.15	1.7	-0.01	23	1	-0.01	-1	2	0.05	266		0.07	52		0.8	-10	5.9	-0.01	-2	11	-10	0.7	169.0		0.6	JUL0261.R12
219098	4,260.0		15.00	12	0.02	-0.5	0.01	30	5	-0.01	-1	3	0.39	70,700	7.07	0.04	3,808		-0.5	14	3.7	-0.01	-2	492	29	2.5	2,180.0		-0.5	JUL0261.R12
219099	111.0		2.83	-10	0.16	15.2	0.01	76	2	-0.01	-1	3	0.04	63		0.02	8		0.8	-10	4.7	-0.01	-2	5	-10	3.1	97.6		0.7	JUL0261.R12
219100	14.5		1.02	-10	0.21	11.1	0.01	111	2	-0.01	-1	3	0.02	61		-0.01	-5		-0.5	-10	3.2	-0.01	-2	2	-10	4.7	42.5		1.1	JUL0261.R12
219147	23.8		2.02	-10	0.06	9.1	-0.01	23	2	0.02	-1	4	-0.01	12		0.01	-5		-0.5	-10	7.7	-0.01	-2	-2	-10	0.8	14.5		0.5	JUL0261.R12
219148	33.9		4.16	-10	0.06	4.8	-0.01	16	-1	-0.01	-1	3	0.03	22		0.02	-5		-0.5	-10	1.2	-0.01	-2	6	-10	0.8	28.5		0.7	JUL0261.R12
219335	40.6		5.16	-10	0.21	13.2	0.15	229	9	-0.01	-1	-1	0.15	23		0.03	11		5.3	-10	21.2	-0.01	-2	30	-10	11.8	54.1		1.7	JUN0505.R12
219336	7.0		3.07	-10	0.16	6.3	0.02	60	-1	-0.01	-1	-1	0.05	4		0.08	26		2.3	-10	8.6	-0.01	-2	19	-10	1.6	14.9		3.5	JUN0505.R12
219337	38.1		8.25	-10	0.23	27.0	0.03	10000	4	-0.01	-1	3	0.13	97		0.03	88		3.2	-10	24.1	-0.01	-2	20	-10	17.5	117.0		2.2	JUN0505.R12
219338	12.2		1.35	-10	0.09	4.8	0.01	71	2	-0.01	-1	4	0.02	216		0.05	24		0.7	-10	5.9	-0.01	-2	7	-10	0.9	201.0		-0.5	JUN0505.R12
219339	8.6		0.63	-10	0.06	23.7	-0.01	127	2	-0.01	-1	-1	0.01	25		0.17	32		1.2	-10	13.5	-0.01	-2	-2	-10	11.6	51.9		2.6	JUN0505.R12
219401	17.2		2.13	-10	0.35	11.2	0.01	33	1	0.01	-1	-1	0.04	16		0.32	89		5.4	-10	8.4	-0.01	-2	8	-10	2.3	13.9		0.9	JUL0261.R12
219402	9.3		3.52	-10	0.33	8.0	0.02	56	1	-0.01	-1	-1	0.07	18		0.23	252		4.4	-10	8.9	-0.01	-2	15	-10	2.1	20.1		1.0	JUL0261.R12
219403	12.7		4.01	-10	0.27	8.6	0.04	63	-1	-0.01	-1	-1	0.08	26		0.21	636		5.6	-10	12.3	-0.01	-2	20	-10	2.0	38.7		0.9	JUL0261.R12
219404	37.6		8.89	-10	0.23	10.5	0.04	458	1	-0.01	-1	-1	0.12	39		0.12	1,225		4.8	-10	8.3	-0.01	-2	24	-10	12.0	159.0		1.7	JUL0261.R12
219405	25.9		6.75	-10	0.22	8.4	0.03	688	-1	-0.01	-1	-1	0.1	33		0.03	722		4.9	-10	6.4	-0.01	-2	18	-10	3.5	60.1		1.2	JUL0261.R12
219406	10.2		3.46	-10	0.24	17.6	0.08	1109	2	-0.01	-1	-1	0.08	17		0.06	48		6.5	-10	12.5	-0.01	-2	40	-10	12.9	49.3		1.1	JUL0261.R12
219407	3.5		2.35	-10	0.29	18.6	0.03	113	4	-0.01	-1	1	0.08	19		0.04	45		4.7	-10	9.7	-0.01	-2	22	-10	9.8	15.4		2.1	JUL0261.R12
219408	7.7		3.43	-10	0.27	9.3	0.02	15	2	-0.01	-1	-1	0.04	15		0.02	14		2.9	-10	5.0	-0.01	-2	17	-10	4.2	10.8		2.2	JUL0261.R12
219409	4.9		4.36	-10	0.27	5.6	0.03	55	2	-0.01	-1	-1	0.03	21		0.02	55		2.5	-10	4.9	-0.01	-2	13	-10	2.5	28.1		1.8	JUL0261.R12
219410	11.2		2.90	-10	0.29	16.4	0.04	552	3	0.01	-1	1	0.06	41		0.19	41		2.2	-10	31.4	-0.01	-2	14	-10	4.5	107.0		1.9	JUL0261.R12
219411	7.0		5.13	-10	0.25	16.0	0.04	414	2	0.02	-1	-1	0.09	25		0.13	79		2.3	-10	37.0	-0.01	-2	23	-10	6.6	58.3		1.6	JUL0261.R12
219412	4.6		4.27	-10	0.33	23.9	0.06	738	-1	0.02	-1	-1	0.06	31		0.35	32		5.7	-10	37.7	-0.01	-2	30	-10	8.2	29.3		0.8	JUL0261.R12
219413	4.9		4.24	-10	0.28	5.8	0.02	83	2	-0.01	-1	-1	0.04	24		0.03	56		2.5	-10	6.7	-0.01	-2	12	-10	2.5	28.3		2.0	JUL0261.R12
219414	3,370.0		4.13	-10	0.52	18.6	1.25	378	263	0.14	-1	20	0.1	24		0.47	-5		6.1	-10	70.4	0.19	-2	104	11	11.5	77.6		12.5	JUL0261.R12
219415	9.1		3.77	-10	0.26	7.5	0.03	62	2	-0.01	-1	-1	0.04	17		0.07	22		2.8	-10	11.0	-0.01	-2	10	-10	2.8	28.2		1.7	JUL0261.R12
51000017	105.0		5.64	-10	0.16	6.8	0.01	823	7	0.01	-1	6	0.07	1,024		1.02	583		1.4	-10	9.7	-0.01	-2	14	-10	2.4	516.0		2.1	OCT0028.R12
51000018	8.2		6.68	-10	0.21	5.9	-0.01	24	7	-0.01	-1	3	0.04	593		0.12	473		-0.5	-10	3.3	-0.01	-2	6	-10	1.3	446.0		1.4	OCT0028.R12
51000019	13.8		2.73	-10	0.21	9.8	0.03	10000	1	-0.01	-1	4	0.04	80		0.02	26		1.3	-10	11.9	-0.01	-2	5	-10	6.7	558.0		3.9	OCT0028.R12
51000020	67.8		5.49	-10	0.26	1.5	-0.01	29	3	0.01	-1	6	0.02	734		4.72	133		0.8	-10	9.6	-0.01	-2	8	-10	1.0	108.0		-0.5	OCT0028.R12

SURILOMA PROJECT GEOCHEMICAL DATA BASE FEBRUARY 2013

11de 16 

SampleID	Cuppm	Cu%	Fe%	Gappm	K%	Lappm	Mg%	Mnppm	Moppm	Na%	Nbppm	Nippm	P%	Pbppm	Pb%	S%	Sbppm	Sb%	Scppm	Snppm	Srppm	Ti%	Tlppm	Vppm	Wppm	Yppm	Znppm	Zn%	Zrppm	BATCH
51000021	47.2		3.86	-10	0.11	5.1	0.01	10000	8	-0.01	-1	5	0.08	586		0.04	222		3.7	-10	9.8	-0.01	-2	13	-10	2.2	144.0		2.9	OCT0028.R12
51000022	135.0		5.69	-10	0.11	3.6	-0.01	246	11	-0.01	-1	5	0.05	1,499		0.2	360		1.2	-10	5.3	-0.01	-2	7	-10	2.2	500.0		1.0	OCT0028.R12
51000023	7.8		1.04	-10	0.21	13.0	0.09	901	-1	0.01	-1	2	0.04	80		0.07	7		1.1	-10	11.4	-0.01	-2	3	-10	5.8	104.0		2.2	OCT0028.R12
51000024	10,100.0		8.70	-10	0.08	3.3	-0.01	186	6	-0.01	-1	7	0.03	9,703		9.22	12,500	1.25	0.8	145	4	-0.01	-2	5	-10	2.2	6190		-0.5	OCT0028.R12
51000025	132.0		2.52	-10	0.25	13.9	0.02	250	1	-0.01	-1	1	0.02	294		0.04	78		0.5	-10	4.1	-0.01	-2	4	-10	4.1	133.0		1.6	OCT0028.R12
51000026	283.0		8.72	-10	0.11	-0.5	0.02	543	-1	-0.01	-1	4	0.03	1,388		1.2	289		-0.5	-10	4.4	-0.01	-2	135	-10	2.6	886.0		1.0	OCT0028.R12
51000027	87.4		4.54	-10	0.20	15.1	0.02	516	3	-0.01	-1	3	0.07	510		0.02	306		3.2	-10	6.6	-0.01	-2	16	-10	3.4	104.0		1.3	OCT0028.R12
51000028	240.0		2.67	-10	0.16	3.4	0.02	328	3	-0.01	-1	2	0.03	786		0.05	80		0.8	-10	8.5	-0.01	-2	6	-10	1.7	96.5		1.1	OCT0028.R12
51000029	316.0		4.12	-10	0.09	9.1	-0.01	657	4	-0.01	-1	5	0.13	6,117		0.32	623		2.7	77	20.3	-0.01	-2	26	-10	6.1	273.0		1.4	OCT0028.R12
51000030	952.0		10.33	-10	0.17	2.4	0.01	79	24	-0.01	-1	3	0.07	755		0.06	207		1.4	-10	9.9	-0.01	-2	32	-10	4.0	227.0		1.4	OCT0028.R12
51000031	590.0		13.32	-10	0.11	3.3	-0.01	166	23	-0.01	-1	4	0.12	378		0.04	295		1.1	-10	8.9	-0.01	-2	18	-10	4.6	117.0		1.0	OCT0028.R12
51000032	50.5		2.57	-10	0.14	-0.5	-0.01	30	13	-0.01	-1	2	0.02	36		0.03	9		-0.5	-10	3.7	-0.01	-2	4	-10	1.5	26.6		0.9	OCT0028.R12
51000033	1,370.0		6.07	-10	0.18	7.3	0.02	51	3	-0.01	-1	7	0.02	695		3.96	532		1.1	15	2.1	-0.01	-2	15	-10	1.7	898.0		0.8	OCT0028.R12
51000038	179.0		1.48	-10	0.07	4.2	0.01	4014	2	-0.01	-1	7	0.01	1,902		0.01	295		1.4	-10	5.8	-0.01	-2	124	-10	2.9	456.0		1.5	OCT0028.R12
51000039	149.0		1.33	17	0.15	1.5	0.02	1587	2	-0.01	-1	3	0.02	1,671		0.02	190		0.7	-10	12.9	-0.01	-2	38	-10	2.1	359.0		1.2	OCT0028.R12
51000040	29.3		3.53	-10	0.07	4.5	0.03	169	6	-0.01	-1	7	0.03	778		0.02	21		0.9	-10	3.4	-0.01	-2	29	-10	3.1	516.0		1.2	OCT0028.R12
51000041	10.6		0.82	-10	0.05	1.5	0.11	697	3	-0.01	1	14	0.03	13		0.03	-5		0.8	-10	8.2	-0.01	-2	10	-10	1.3	37.3		1.6	OCT0028.R12
51000042	107.0		1.52	-10	0.08	6.0	0.02	10000	3	-0.01	-1	6	0.02	2,806		0.12	356		1.6	-10	34.7	0.01	6	31	-10	5.4	2,210.0		4.7	OCT0028.R12
51000043	11.5		0.98	-10	0.05	1.3	0.01	2032	2	-0.01	-1	8	0.02	1,314		-0.01	168		-0.5	-10	3.0	-0.01	-2	4	-10	0.9	155.0		-0.5	OCT0028.R12
51000044	8.1		3.05	-10	0.26	7.6	0.03	10000	-1	-0.01	-1	5	0.04	42		0.02	30		2.6	-10	30.8	0.01	-2	5	-10	7.6	100.0		4.9	OCT0028.R12
51000045	244.0		4.28	-10	0.04	-0.5	-0.01	75	6	-0.01	-1	15	0.1	4,825		0.15	1,867		-0.5	-10	4.0	-0.01	-2	7	-10	-0.5	134.0		-0.5	OCT0377.R12
51000046	2,690.0		5.84	-10	0.17	7.1	-0.01	157	2	-0.01	-1	-1	0.13	3,601		1.05	3,506		1.2	93	26.8	-0.01	-2	18	-10	2.7	712.0		0.7	OCT0377.R12
51000047	302.0		8.40	-10	0.24	4.4	-0.01	680	-1	-0.01	-1	4	0.15	1,714		0.17	414		1.8	-10	25.8	-0.01	-2	8	-10	3.1	374.0		0.8	OCT0377.R12
51000048	10.6		0.59	-10	0.02	1.0	0.04	1183	2	-0.01	-1	16	0.03	14		0.02	10		-0.5	-10	3.7	-0.01	-2	3	-10	1.8	7.8		1.1	OCT0377.R12
51000049	9.3		0.69	-10	0.01	2.1	0.29	3323	2	-0.01	1	18	-0.01	5		0.02	9		0.6	-10	12.9	-0.01	-2	10	-10	3.1	9.5		1.0	OCT0377.R12
51000052	375.0		10.66	-10	0.06	-0.5	-0.01	199	-1	-0.01	-1	7	0.06	2,950		0.1	428		1.0	77	1.0	-0.01	-2	206	-10	-0.5	165.0		-0.5	OCT0377.R12
51000053	218.0		6.81	-10	0.15	8.9	-0.01	63	1	-0.01	-1	7	0.06	1,426		0.07	162		0.6	-10	1.3	-0.01	-2	13	-10	0.9	180.0		0.8	OCT0377.R12
51000054	80.6		3.40	-10	0.14	13.5	0.01	160	2	-0.01	-1	7	0.04	1,339		0.05	365		0.8	-10	2.5	-0.01	-2	8	-10	3.2	318.0		0.7	OCT0377.R12
51000055	5.9		1.06	-10	0.09	1.8	0.02	461	-1	-0.01	-1	6	0.02	16		-0.01	11		1.0	-10	2.1	-0.01	-2	5	-10	1.1	15.5		0.6	OCT0377.R12
51000056	75.3		5.70	-10	0.17	5.3	0.02	1005	-1	-0.01	-1	7	0.1	28		0.09	136		2.7	-10	8.8	-0.01	-2	33	-10	2.9	81.4		1.4	OCT0377.R12
51000057	10.5		1.92	-10	0.14	14.8	0.02	7129	-1	-0.01	-1	6	0.01	301		0.01	43		0.7	-10	59.9	-0.01	-2	2	-10	4.6	547.0		2.0	OCT0377.R12
51000059	45.8		4.73	-10	0.16	13.0	0.01	62	-1	-0.01	-1	6	0.07	2,395		0.05	277		1.1	-10	1.4	-0.01	-2	10	-10	1.0	502.0		-0.5	OCT0377.R12
51000060	15.0		7.05	-10	0.12	7.0	0.34	356	-1	-0.01	-1	2	0.05	122		0.02	19		2.6	15	9.5	-0.01	-2	61	-10	2.6	171.0		1.3	OCT0377.R12
51000063	35.8		2.24	-10	0.24	9.6	0.01	35	-1	-0.01	-1	5	0.05	485		0.01	54		0.5	-10	2.9	-0.01	-2	-2	-10	1.0	122.0		1.0	OCT0377.R12
51000064	2,080.0		15.00	-10	0.04	-0.5	0.02	285	-1	-0.01	-1	8	0.13	632		0.34	2,163		-0.5	55	1.6	-0.01	-2	55	38	0.8	611.0		-0.5	OCT0377.R12
51000065	640.0		15.00	-10	0.08	-0.5	-0.01	82	13	-0.01	-1	7	0.37	174		0.12	406		-0.5	-10	1.7	-0.01	-2	35	52	4.3	1,160.0		1.4	OCT0377.R12
51000066	78.3		3.02	-10	0.22	11.1	0.01	87	-1	-0.01	-1	4	0.03	414		0.02	21		1.2	-10	3.5	-0.01	-2	7	-10	1.5	61.4		1.1	OCT0377.R12
51000077	6,710.0		15.00	-10	0.05	-0.5	-0.01	2481	-1	-0.01	-1	6	0.15	946		10	865		2.0	53	4.1	0.01	-2	60	57	4.8	660.0		1.9	OCT0377.R12
51000078	12.6		5.83	-10	0.17	9.4	0.07	141	-1	0.04	-1	1	0.18	17		0.03	22		6.9	-10	16.0	-0.01	-2	38	-10	8.5	43.8		0.9	OCT0377.R12
51000079	34.8		6.30	-10	0.19	17.1	0.02	1657	4	-0.01	-1	4	0.14	26		0.1	34		1.7	-10	23.4	-0.01	-2	13	-10	11.1	70.6		1.0	OCT0377.R12
51000080	52.6		15.00	10	0.07	14.5	0.01	216	-1	-0.01	-1	8	0.12	2,079		0.09	27		4.0	-10	9.5	0.02	-2	59	-10	15.1	423.0		2.6	OCT0377.R12
51000081	166.0		9.53	-10	0.10	9.0	-0.01	44	-1	-0.01	-1	9	0.03	114		0.05	28		0.9	-10	0.8	-0.01	-2	8	-10	1.1	76.7		-0.5	OCT0377.R12
51000082	243.0		12.97	-10	0.07	-0.5	-0.01	45	13	-0.01	-1	13	0.1	217		0.15	55		0.6	-10	4.1	-0.01	-2	44	15	2.1	144.0		2.7	NOV0078.R12
51000083	123.0		2.64	-10	0.08	-0.5	0.01	691	4	-0.01	-1	15	0.07	5,420		1.76	597		1.4	-10	3.3	-0.01	-2	10	-10	0.6	13,000.0	1.3	-0.5	NOV0078.R12
51000084	69.2		5.18	-10	0.15	15.2	2.19	6029	-1	-0.01	-1	13	0.11	156		2.98	11		8.1	-10	30.6	-0.01	-2	64	-10	15.4	2,600.0		1.4	NOV0078.R12
51000085	508.0		3.14	-10	0.02	5.0	0.02	3956	3	-0.01	-1	23	0.12	6,098		0.05	296		0.9	25	4.8	-0.01	-2	20	-10	13.3	597.0		0.7	NOV0078.R12
51000086	162.0		11.81	-10	0.29	9.8	0.48	866	-1	-0.01	-1	4	0.16	3,107		0.17	59		4.0	-10	19.8	-0.01	-2	124	-10	2.8	612.0		2.5	NOV0078.R12
51000087	6,710.0		11.14	-10	0.06	-0.5	0.01	220	7	-0.01	-1	14	0.06	2,492		7.64	4,572		-0.5	71	1.4	-0.01	18	4	-10	0.7	1,540.0		-0.5	NOV0078.R12
51000088	20,200.0	2.02	13.23	-10	0.08	-0.5	-0.01	184	4	-0.01	-1	12	0.11	10,800	1.08	10	21,500	2.15	-0.5	445	7.5	-0.01	-2	8	-10	1.8	4360		-0.5	NOV0078.R12
51000089	133.0		4.34	-10	0.17	9.1	0.22	938	2	-0.01	-1	7	0.05	795		1.63	98		1.6	-10	6.8	-0.01	-2	15	-10	5.2	671.0		1.2	NOV0078.R12
51000090	117.0		2.21	-10	0.22	10.5	0.02	1179	1	-0.01	-1	6	0.03	169		0.05	112		0.8	-10	3.7	-0.01	-2	2	-10	1.4	109.0		1.0	NOV0078.R12
51000091	79.0		3.70	-10	0.30	14.7	0.02	85	2	-0.01	-1	3	0.07	155		0.02	34		1.3	-10	2.9	-0.01	-2	6	-10	2.0	86.4		1.4	NOV0078.R12
51000092	164.0		3.22	-10	0.17	6.8	0.02	233	5	-0.01	-1	8	0.04	153		0.05	84		0.9	-10	4.5	-0.01	-2	6	-10	2.1	54.6		1.4	NOV0078.R12
51000093	17.3		1.25	-10	0.18	13.8	0.33	429	-1	-0.01	-1	3	0.04	26		0.04	15		1.2	-10	8.5	-0.01	-2	5	-10	7.6	133.0		2.6	NOV0078.R12
51000094	466.0		15.00	108	0.10	-0.5	0.01	393	3	-0.01	-1	6	0.04	2,622		0.14	977		0.7	-10	2.2	-0.01	-2	55	16	2.7	1,620.0		1.5	NOV0078.R12
51000101	7.0		3.83	-10	0.31	11.7	0.05	119	-1	-0.01	-1	-1	0.12	9		0.19	40		4.0	-10	37.9	-0.01	-2	21	-10	6.1	24.2		0.7	NOV0121.R12
51000102	8.9		6.26	-10	0.31	8.3	0.06	1893	-1	-0.01	-1	-1	0.2	-2		0.08	27		8.0	-10	17.2	-0.01	-2	43	-10	11.2	87.9		1.4	NOV0121.R12
51000103	5.1		5.48	-10	0.40	9.9	0.05	1735	-1	-0.01	-1	-1	0.15	24		0.11	37		10.0	-10	14.6	-0.01	-2	53	-10	7.9	72.1		0.8	NOV0121.R12
51000104	19.3		3.71	-10	0.22	9.6	0.03	44	3	-0.01	-1	3	0.09	606		0.19	262		3.4	-10	52.2	-0.01	-2	15	-10	2.7	44.0		0.7	NOV0121.R12
51000105	41.8		7.75	-10	0.31	6.9	0.02	76	-1	-0.01	-1	2	0.12	62		0.19	138		7.3	-10	20.8	-0.01	-2	53	-10	2.3	25.2		0.7	NOV0121.R12
51000106	53.4		9.24	-10	0.23	6.6	0.02	54	-1	-0.01	-1	-1	0.14	195		0.09	288		7.0	-10	14.2	-0.01	-2	30	-10	2.5	90.8		0.9	NOV0121.R12
51000107	22.1		6.41	-10	0.17	11.7	0.01	74	-1	-0.01	-1	3	0.16	124		0.09	730		10.2	-10	22.0	-0.01	-2	19	-10	2.5	20.5		1.0	NOV0121.R12
51000108	8.5		5.20	-10	0.32	8.2	0.02	42	-1	-0.01	-1	-1	0.13	31		0.25	558		3.8	-10	23.7	-0.01	-2	21	-10	3.2	11.9		1.0	NOV0121.R12
51000109	6.9		3.38	-10	0.23	10.4	0.04	32	-1	-0.01	-1	-1	0.13	7		0.02	45		4.0	-10	10.4	-0.01	-2	16	-10	2.4	9.0		0.8	NOV0121.R12
51000110	1.8		1.86	-10	0.31	9.6	0.04	30	-1	-0.01	-1	3	0.12	3		0.19	284		8.2	-10	20.7	-0.01	-2	8	-10	4.4	4.6		0.9	NOV0121.R12
51000111	3.3		3.37	-10	0.32	14.7	0.03	43	-1	-0.01	-1	-1	0.13	-2		0.29	29		3.4	-10	19.6	-0.01	-2	17	-10	4.6	8.4		0.6	NOV0121.R12
51000112	9.2		5.16	-10	0.22	7.5	0.02	51	1	-0.01	-1	4	0.12	16		0.17	78		5.2	-10	21.1	-0.01	-2	15	-10	1.6	13.1		0.8	NOV0121.R12
51000113	12.2		5.66	-10	0.49	11.0	0.04	18	-1	-0.01	-1	-1	0.1	16		0.47	60		4.2	-10	31.2	-0.01	-2	25	-10	2.9	11.0		1.0	NOV0121.R12
51000114	12.4		3.77	-10	0.32	14.3	0.04	17	-1	-0.01	-1	-1	0.15	13		0.02	36		9.9	-10	10.4	-0.01	-2	33	-10	9.2	11.1		1.0	NOV0121.R12
51000115	6.9		2.94	-10	0.25	17.0	0.04	14	-1	-0.01	-1	-1	0.16	9		-0.01	31		9.7	-10	10.0	-0.01	-2	30	-10	12.2	10.1		0.7	NOV0121.R12
51000116	20.3		6.36	-10	0.23	12.2	0.04	25	-1	-0.01	-1	-1	0.13	10		0.09	81		6.5	-10	19.2	-0.01	-2	20	-10	6.6	14.7		0.6	NOV0121.R12
51000117	15.7		4.89	-10	0.28	15.9	0.04	29	-1	-0.01	-1	5	0.09	41		0.19	122		6.7	-10	42.4	-0.01	-2	19	-10	2.9	10.7		1.1	NOV0121.R12
51000118	42.6		12.29	-10	0.25	5.5	0.05	41	-1	-0.01	-1	-1	0.14	18		0.15	92		4.9	-10	30.1	-0.01	-2	42	-10	4.4	29.0		0.8	NOV0121.R12
51000119	11.9		3.84	-10	0.27	6.0	0.04	16	-1	-0.01	-1	-1	0.17	13		-0.01	33		8.0	-10	18.3	-0.01	-2	32	-10	5.1	17.9		1.9	NOV0121.R12
51000120	25.6		9.79	-10	0.29	1.9	0.06	302	-1	-0.01	-1	-1	0.18	9		0.04	36		5.9	-10	13.1	0.02	-2	59	-10	5.5	68.5		3.1	NOV0121.R12
51000121	17.6		8.59	-10	0.26	5.6	0.09	1143	-1	-0.01	-1	-1	0.23	13		-0.01	45		7.2	-10	15.8	0.02	-2	60	-10	8.6	80.5		2.6	NOV0121.R12
51000122	8.5		4.13	-10	0.24	19.2	0.27	835	-1	-0.01	-1	-1	0.15	-2		-0.01	24		6.4	-10	19.0	0.02	-2	61	-10	15.1	93.9		2.8	NOV0121.R12
51000123	13.3		5.68	-10	0.32	18.6	0.26	10000	-1	-0.01	-1	1	0.12	10		0.03	19		5.3	-10	18.7	0.04	-2	59	-10	21.2	335.0		6.0	NOV0121.R12
51000124	4.0		5.09	-10	0.34	27.7	0.56	10000	-1	-0.01	-1	6	0.12	-2		-0.01	17		5.7	-10	24.8	0.02	-2	40	-10	49.1	609.0		4.1	NOV0121.R12
51000125	3.5		4.60	-10	0.34	14.5	0.31	1616	-1	-0.01	-1	4	0.11	-2		-0.01	43		6.2	-10	9.8	0.02	-2	61	-10	12.6	158.0		2.9	NOV0121.R12
51000126	2.2		4.29	-10	0.16	14.8	0.41	2841	-1	-0.01	-1	4	0.13	12		0.07	47		5.3	-10	18.4	0.02	-2	60	-10	12.5	112.0		2.2	NOV0121.R12
51000127	57.7		9.49	-10	0.31	7.7	0.06	5719	-1	-0.01	-1	-1	0.14	30		0.07	87		11.0	-10	12.7	-0.01	-2	52	-10	10.6	184.0		1.8	NOV0121.R12
51000128	8.8		2.84	-10	0.33	5.2	0.03	36	-1	-0.01	-1	-1	0.1	-2		0.08	64		12.9	-10	8.8	-0.01	-2	24	-10	4.5	21.3		0.6	NOV0121.R12

SURILOMA PROJECT GEOCHEMICAL DATA BASE FEBRUARY 2013

12de 16 

SampleID	Cuppm	Cu%	Fe%	Gappm	K%	Lappm	Mg%	Mnppm	Moppm	Na%	Nbppm	Nippm	P%	Pbppm	Pb%	S%	Sbppm	Sb%	Scppm	Snppm	Srppm	Ti%	Tlppm	Vppm	Wppm	Yppm	Znppm	Zn%	Zrppm	BATCH
51000129	36.0		7.23	-10	0.09	4.1	0.01	47	-1	-0.01	-1	5	0.13	809		0.17	1,083		4.7	-10	15.2	-0.01	-2	32	-10	3.1	409.0		-0.5	NOV0121.R12
51000130	51.3		4.36	-10	0.24	7.3	0.03	924	-1	-0.01	-1	-1	0.13	-2		0.04	44		11.9	-10	8.4	-0.01	-2	19	-10	6.5	38.6		1.2	NOV0121.R12
51000131	28.5		6.17	-10	0.26	7.1	0.03	838	-1	-0.01	-1	4	0.12	9		0.09	306		11.9	-10	9.4	-0.01	-2	27	-10	8.6	61.4		0.9	NOV0121.R12
51000132	48.7		7.46	-10	0.25	5.2	0.03	1032	-1	-0.01	-1	-1	0.17	10		0.05	105		11.2	-10	9.3	-0.01	-2	28	-10	3.5	38.4		1.1	NOV0121.R12
51000133	15.2		3.87	-10	0.35	12.3	0.03	67	-1	-0.01	-1	-1	0.1	10		0.05	215		6.4	-10	14.3	-0.01	-2	23	-10	10.7	31.2		1.3	NOV0121.R12
51000134	26.4		7.56	-10	0.31	4.8	0.03	336	-1	-0.01	-1	-1	0.08	11		0.06	53		7.1	-10	8.1	-0.01	-2	28	-10	8.9	67.6		1.2	NOV0121.R12
51000135	7.9		3.55	-10	0.23	19.6	0.27	958	-1	-0.01	-1	-1	0.16	6		0.03	26		7.6	-10	22.2	-0.01	-2	36	-10	15.7	43.7		1.7	NOV0121.R12
51000136	3,400.0		4.74	-10	0.56	19.2	1.21	398	277	0.17	-1	24	0.11	14		0.46	-5		6.8	-10	83.2	0.21	-2	111	-10	13.6	71.4		18.3	NOV0121.R12
51000137	25.2		3.52	-10	0.22	6.3	0.03	65	3	-0.01	-1	-1	0.03	37		0.1	2,273		2.2	-10	30.1	-0.01	-2	10	-10	3.7	36.8		1.5	NOV0121.R12
51000138	35.0		9.05	-10	0.21	12.3	0.02	209	-1	-0.01	-1	2	0.14	85		0.15	216		8.8	-10	24.2	-0.01	-2	50	-10	6.2	24.3		1.9	NOV0121.R12
51000139	20.1		5.46	-10	0.14	9.3	-0.01	63	-1	-0.01	-1	-1	0.13	119		0.07	583		6.2	-10	20.9	-0.01	-2	27	-10	3.9	16.3		1.6	NOV0121.R12
51000140	17.2		5.52	-10	0.32	8.1	0.01	65	-1	-0.01	-1	-1	0.11	17		0.15	125		8.7	-10	15.2	-0.01	-2	29	-10	2.9	14.7		2.1	NOV0121.R12
51000141	31.8		10.62	-10	0.22	4.8	0.01	50	-1	-0.01	-1	2	0.14	19		0.15	108		8.8	-10	13.2	-0.01	-2	33	-10	3.0	25.4		1.9	NOV0121.R12
51000142	15.6		5.71	-10	0.15	6.6	0.01	49	2	-0.01	-1	3	0.13	207		0.17	187		3.4	-10	17.6	-0.01	-2	18	-10	2.9	19.1		-0.5	NOV0121.R12
51000143	11.0		5.44	-10	0.16	8.3	0.01	63	-1	-0.01	-1	-1	0.09	61		0.14	149		4.2	-10	13.4	-0.01	-2	15	-10	3.1	16.9		1.2	NOV0121.R12
51000144	11.3		4.36	-10	0.16	14.7	0.02	101	2	-0.01	-1	5	0.09	21		0.11	67		4.1	-10	20.3	-0.01	-2	17	-10	3.6	13.1		1.5	NOV0121.R12
51000145	30.1		5.24	-10	0.19	9.0	0.01	79	1	-0.01	-1	-1	0.09	41		0.11	104		4.5	-10	9.6	-0.01	-2	23	-10	2.1	14.6		1.3	NOV0121.R12
51000146	21.3		3.90	-10	0.12	9.3	0.01	35	1	-0.01	-1	4	0.1	546		0.1	390		7.0	-10	11.1	-0.01	-2	19	-10	2.9	128.0		0.7	NOV0121.R12
51000147	15.9		5.14	-10	0.21	10.5	0.02	67	-1	-0.01	-1	2	0.09	61		0.13	118		6.2	-10	13.9	-0.01	-2	23	-10	3.5	22.1		1.0	NOV0121.R12
51000148	27.9		6.12	-10	0.23	7.1	0.02	30	-1	-0.01	-1	-1	0.07	16		0.08	69		7.2	-10	10.4	-0.01	-2	27	-10	2.4	20.3		2.1	NOV0121.R12
51000149	9.1		0.55	-10	-0.01	0.7	-0.01	74	6	-0.01	-1	3	-0.01	-2		-0.01	-5		-0.5	-10	-0.5	-0.01	-2	-2	-10	-0.5	9.3		1.2	NOV0121.R12
51000150	17.5		4.41	-10	0.16	10.1	0.02	54	1	-0.01	-1	-1	0.06	64		0.12	87		7.8	-10	13.0	-0.01	-2	13	-10	3.1	16.9		0.7	NOV0121.R12
51000151	38.8		3.77	-10	0.23	11.8	0.02	376	-1	-0.01	-1	-1	0.08	17		0.01	48		11.3	-10	20.7	-0.01	-2	19	-10	4.8	24.4		1.8	NOV0121.R12
51000152	21.5		6.73	-10	0.29	16.2	0.03	10000	-1	-0.01	-1	6	0.11	14		-0.01	55		11.6	-10	11.2	-0.01	-2	36	-10	23.4	177.0		4.5	NOV0121.R12
51000153	5.3		6.55	-10	0.28	22.1	0.03	6101	-1	-0.01	-1	7	0.15	23		0.05	27		12.7	-10	11.8	-0.01	-2	39	-10	26.7	73.2		3.3	NOV0121.R12
51000154	13.8		4.13	-10	0.34	15.0	0.04	6427	1	-0.01	-1	5	0.07	12		-0.01	18		11.3	-10	6.4	-0.01	-2	37	-10	14.1	41.0		4.6	NOV0121.R12
51000155	18.6		3.78	-10	0.26	14.5	0.04	3225	-1	-0.01	-1	4	0.07	8		-0.01	20		10.3	-10	7.1	-0.01	-2	43	-10	10.9	36.0		4.1	NOV0121.R12
51000156	12.3		3.55	-10	0.25	23.7	0.06	1840	-1	-0.01	-1	5	0.09	-2		-0.01	29		9.9	-10	9.5	0.02	-2	49	-10	20.7	35.8		3.9	NOV0121.R12
51000157	15.5		3.54	-10	0.33	10.5	0.06	1739	-1	-0.01	-1	4	0.05	-2		-0.01	6		9.6	-10	3.2	0.01	-2	56	-10	7.3	39.0		4.2	NOV0121.R12
51000158	20.8		8.54	-10	0.24	17.7	0.02	10000	-1	-0.01	-1	6	0.11	21		0.04	51		9.3	-10	8.7	0.01	-2	34	-10	21.6	166.0		3.0	NOV0121.R12
51000159	9.2		3.20	-10	0.21	9.9	-0.01	70	-1	-0.01	-1	2	0.07	14		0.1	38		6.9	-10	7.7	-0.01	-2	17	-10	2.9	7.2		1.5	NOV0121.R12
51000160	22.4		7.14	-10	0.24	4.3	0.01	36	-1	-0.01	-1	-1	0.07	13		0.12	128		4.5	-10	6.7	-0.01	-2	23	-10	1.4	11.6		0.7	NOV0121.R12
51000161	50.1		6.58	-10	0.24	2.7	0.02	15	-1	-0.01	-1	-1	0.06	15		0.06	88		6.5	-10	4.0	-0.01	-2	21	-10	1.6	13.5		1.2	NOV0121.R12
51000162	51.7		5.79	-10	0.25	4.6	0.01	22	-1	-0.01	-1	-1	0.05	12		0.2	129		6.6	-10	7.4	-0.01	-2	18	-10	1.5	13.3		-0.5	NOV0121.R12
51000163	30.3		9.42	-10	0.46	6.4	-0.01	58	1	-0.01	-1	-1	0.08	38		0.62	380		5.8	-10	19.2	-0.01	-2	31	-10	2.0	16.3		0.6	NOV0121.R12
51000164	22.4		8.03	-10	0.32	5.7	-0.01	25	3	-0.01	-1	-1	0.14	29		0.39	544		4.5	-10	65.0	-0.01	-2	32	-10	2.7	16.9		-0.5	NOV0121.R12
51000165	24.2		4.48	-10	0.16	8.9	-0.01	19	2	-0.01	-1	-1	0.13	56		0.19	306		4.9	-10	116.0	-0.01	-2	19	-10	3.3	16.7		0.7	NOV0121.R12
51000166	8.5		6.02	-10	0.51	7.1	-0.01	25	2	-0.01	-1	5	0.08	39		0.61	330		5.3	-10	32.3	-0.01	-2	21	-10	1.6	11.8		0.9	NOV0121.R12
51000167	9.0		3.61	-10	0.22	8.1	-0.01	21	2	-0.01	-1	2	0.09	46		0.29	220		5.0	-10	56.0	-0.01	-2	11	-10	2.3	10.5		-0.5	NOV0121.R12
51000168	8.2		3.56	-10	0.16	19.9	-0.01	42	-1	-0.01	-1	5	0.24	105		0.18	189		5.4	-10	242.0	-0.01	-2	16	-10	7.0	20.7		0.8	NOV0121.R12
51000169	26.5		7.84	-10	0.30	15.9	0.01	25	-1	-0.01	-1	-1	0.25	62		0.13	320		5.8	-10	173.0	-0.01	-2	44	-10	6.5	24.2		2.0	NOV0121.R12
51000170	13.0		10.84	-10	0.21	14.0	-0.01	27	2	-0.01	-1	-1	0.29	33		0.08	524		6.6	-10	88.5	-0.01	-2	77	-10	6.6	25.2		1.2	NOV0121.R12
51000171	15.7		13.61	-10	0.19	10.6	-0.01	23	1	-0.01	-1	-1	0.27	21		0.07	560		5.9	-10	75.2	-0.01	-2	90	-10	5.9	29.0		1.6	NOV0121.R12
51000172	21.1		2.84	-10	0.21	5.6	0.01	15	2	-0.01	-1	2	0.05	10		0.01	54		10.3	-10	10.0	-0.01	-2	27	-10	3.0	6.7		1.3	NOV0121.R12
51000173	21.7		8.86	-10	0.10	8.9	-0.01	46	-1	-0.01	-1	-1	0.22	22		0.03	177		9.1	-10	29.5	-0.01	-2	50	-10	4.0	34.6		1.8	NOV0121.R12
51000174	32.1		7.03	-10	0.16	11.7	-0.01	14	-1	-0.01	-1	-1	0.18	19		0.06	87		17.0	-10	54.0	-0.01	-2	36	-10	4.4	16.5		1.4	NOV0121.R12
51000175	23.1		4.43	-10	0.15	6.9	-0.01	13	-1	-0.01	-1	-1	0.13	10		0.02	74		13.8	-10	21.1	-0.01	-2	41	-10	3.2	12.8		2.0	NOV0121.R12
51000176	37.5		2.54	-10	0.25	8.5	0.02	5	-1	-0.01	-1	-1	0.05	-2		0.03	55		9.4	-10	5.1	-0.01	-2	29	-10	4.5	4.8		1.9	NOV0121.R12
51000177	15.4		6.72	-10	0.20	4.5	0.02	8	-1	-0.01	-1	2	0.32	-2		0.02	79		18.0	-10	4.5	-0.01	-2	110	-10	5.9	10.3		1.9	NOV0121.R12
51000178	10.7		3.48	-10	0.22	8.2	0.02	9	-1	-0.01	1	5	0.15	22		0.01	37		10.3	-10	7.8	-0.01	-2	50	-10	5.1	7.6		1.5	NOV0121.R12
51000179	2.7		1.68	-10	0.27	18.5	0.04	32	-1	-0.01	-1	5	0.06	37		-0.01	13		4.2	-10	9.2	-0.01	-2	28	-10	15.0	8.8		1.6	NOV0121.R12
51000180	3.2		1.69	-10	0.31	20.7	0.04	25	1	-0.01	-1	3	0.08	38		0.03	16		4.5	-10	16.3	-0.01	-2	29	-10	11.9	7.6		1.9	NOV0121.R12
51000181	16.2		1.87	-10	0.09	3.2	0.01	66	-1	-0.01	1	7	0.03	173		0.04	212		2.3	-10	34.4	-0.01	-2	8	-10	1.4	8.3		-0.5	NOV0121.R12
51000182	11.7		3.46	-10	0.11	7.5	0.02	66	2	-0.01	-1	5	0.09	70		0.03	209		6.2	-10	45.7	-0.01	-2	9	-10	2.7	7.7		-0.5	NOV0121.R12
51000183	3.8		2.95	-10	0.39	10.6	0.05	10	-1	-0.01	-1	2	0.08	17		0.34	90		10.0	-10	27.9	-0.01	-2	21	-10	5.6	6.3		0.7	NOV0121.R12
51000184	5.1		1.89	-10	0.14	8.4	0.02	160	2	-0.01	1	6	0.05	26		0.14	85		3.3	-10	20.2	-0.01	-2	14	-10	3.7	9.7		1.2	NOV0121.R12
51000185	63.7		10.28	-10	0.24	5.0	0.11	4405	-1	-0.01	-1	7	0.11	12		0.02	51		9.2	-10	9.6	-0.01	-2	61	-10	13.3	136.0		2.3	NOV0121.R12
51000186	18.4		3.58	-10	0.36	31.1	0.08	540	1	-0.01	-1	4	0.14	14		0.19	32		22.3	-10	45.1	-0.01	-2	37	-10	17.6	58.4		-0.5	NOV0355.R12
51000187	8.7		2.78	-10	0.32	16.8	0.04	20	2	-0.01	-1	-1	0.08	6		0.32	194		7.9	-10	28.0	-0.01	-2	28	-10	3.2	2.6		-0.5	NOV0355.R12
51000188	-0.5		2.70	-10	0.60	8.6	0.04	38	-1	-0.01	-1	-1	0.11	12		0.57	192		4.1	-10	21.4	-0.01	-2	31	-10	2.7	4.5		1.2	NOV0355.R12
51000189	3.6		1.39	-10	0.22	8.9	0.04	35	-1	-0.01	-1	2	0.02	40		0.1	168		1.5	-10	15.8	-0.01	-2	8	-10	1.6	53.7		1.6	NOV0355.R12
51000190	1.2		2.26	-10	0.32	10.1	0.03	29	-1	-0.01	-1	-1	0.07	14		0.23	550		3.5	-10	9.0	-0.01	-2	13	-10	1.8	11.7		1.5	NOV0355.R12
51000191	3.2		1.20	-10	0.22	8.5	0.04	25	-1	-0.01	-1	-1	0.05	8		0.03	1,574		2.3	-10	6.5	-0.01	-2	16	-10	2.4	10.4		-0.5	NOV0355.R12
51000192	-0.5		0.83	-10	0.30	13.7	0.05	23	1	-0.01	-1	-1	0.09	5		0.12	156		2.1	-10	10.5	-0.01	-2	10	-10	2.8	6.0		1.1	NOV0355.R12
51000193	1.4		2.41	-10	0.21	11.8	0.04	29	-1	-0.01	-1	-1	0.08	5		0.12	281		3.0	-10	10.5	-0.01	-2	20	-10	2.6	6.3		-0.5	NOV0355.R12
51000194	-0.5		0.99	-10	0.26	13.7	0.07	18	-1	-0.01	-1	-1	0.09	13		0.05	148		4.9	-10	12.6	-0.01	-2	16	-10	6.6	2.2		1.5	NOV0355.R12
51000195	14.8		8.15	-10	0.24	9.1	0.08	738	-1	-0.01	-1	-1	0.12	14		0.06	417		3.1	-10	15.1	-0.01	-2	28	-10	4.0	33.1		-0.5	NOV0355.R12
51000196	-0.5		3.24	-10	0.27	14.3	0.12	138	1	-0.01	-1	-1	0.19	8		0.05	102		5.5	-10	14.7	-0.01	-2	37	-10	7.6	20.0		1.2	NOV0355.R12
51000197	5.6		3.49	-10	0.24	10.7	0.09	1310	-1	-0.01	-1	-1	0.09	7		0.02	30		9.1	-10	8.7	-0.01	-2	31	-10	9.4	73.4		0.6	NOV0355.R12
51000198	1.5		0.98	-10	0.27	8.8	0.09	58	-1	-0.01	-1	-1	0.06	9		0.03	44		5.4	-10	10.2	-0.01	-2	18	-10	3.5	10.5		-0.5	NOV0355.R12
51000199	10.7		3.66	-10	0.21	10.9	0.06	1304	-1	-0.01	-1	-1	0.08	7		0.04	96		5.6	-10	7.2	-0.01	-2	20	-10	8.5	37.9		0.7	NOV0355.R12
51000200	3.7		3.58	-10	0.30	12.6	0.07	665	-1	-0.01	-1	-1	0.12	10		0.06	105		4.9	-10	8.5	-0.01	-2	25	-10	8.7	29.7		1.4	NOV0355.R12
51000201	40.0		10.45	-10	0.24	13.6	0.03	97	3	-0.01	-1	4	0.21	172		0.04	31		2.2	-10	9.2	-0.01	-2	25	-10	5.9	127.0		0.6	NOV0078.R12
51000220	590.0		7.27	16	0.03	1.1	-0.01	68	3	-0.01	-1	11	0.03	6,576		0.76	5,494		0.7	24	0.9	-0.01	-2	10	-10	1.3	3,290.0		-0.5	NOV0186.R12
51000221	358.0		10.05	126	0.04	2.8	-0.01	99	2	-0.01	-1	8	0.03	4,419		0.2	3,721		0.9	70	1.0	-0.01	-2	12	12	2.3	1,630.0		1.1	NOV0186.R12
51000222	246.0		5.52	-10	0.15	9.7	0.01	112	5	-0.01	-1	2	0.02	943		0.11	326		0.7	-10	6.0	-0.01	-2	7	-10	2.9	286.0		1.3	NOV0186.R12
51000223	15.9		1.69	-10	0.18	15.7	0.03	387	2	-0.01	-1	3	0.02	89		-0.01	22		1.1	-10	12.2	-0.01	-2	4	-10	6.0	122.0		0.7	NOV0186.R12
51000224	15.2		2.07	-10	0.19	14.6	0.05	1580	1	-0.01	-1	-1	0.02	34		0.01	18		1.1	-10	10.5	-0.01	-2	5	-10	5.8	210.0		2.1	NOV0186.R12
51000225	13.3		1.43	-10	0.18	15.0	0.01	73	4	-0.01	-1	-1	0.02	21		-0.01	-5		1.1	-10	4.7	-0.01	-2	4	-10	3.1	122.0		2.1	NOV0186.R12
51000226	11.6		1.60	-10	0.15	12.8	-0.01	97	2	-0.01	-1	-1	0.02	26		-0.01	23		1.0	-10	4.5	-0.01	-2	4	-10	2.4	83.6		1.4	NOV0186.R12
51000227	13.2		1.49	-10	0.20	16.0	0.04	534	-1	-0.01	-1	2	0.02	19		-0.01	9		1.1	-10	6.6	-0.01	-2	4	-10	4.3	150.0		1.7	NOV0186.R12
51000228	17.7		1.70	-10	0.20	17.0	0.08	10000	-1	-0.01	-1	6	0.02	70		-0.01	30		1.0	-10	15.6	-0.01	-2	5	-10	11.0	1,130.0		3.7	NOV0186.R12
51000229	28.4		2.22	-10	0.17	16.6	0.02	189	-1	-0.01	-1	4	0.07	2,843		0.04	20		0.8	-10	5.3	-0.01	-2	7	-10	3.7	95.2		1.6	NOV0186.R12

SURILOMA PROJECT GEOCHEMICAL DATA BASE FEBRUARY 2013

13de 16 

SampleID	Cuppm	Cu%	Fe%	Gappm	K%	Lappm	Mg%	Mnppm	Moppm	Na%	Nbppm	Nippm	P%	Pbppm	Pb%	S%	Sbppm	Sb%	Scppm	Snppm	Srppm	Ti%	Tlppm	Vppm	Wppm	Yppm	Znppm	Zn%	Zrppm	BATCH
51000230	13.3		2.96	-10	0.17	14.1	0.01	73	2	-0.01	-1	2	0.04	1,651		0.03	11		0.8	-10	2.4	-0.01	-2	15	-10	1.9	152.0		1.7	NOV0186.R12
51000231	17.7		1.30	-10	0.20	16.8	0.02	1692	2	-0.01	-1	2	0.03	753		0.02	28		0.7	-10	8.4	-0.01	-2	5	-10	2.8	260.0		2.3	NOV0186.R12
51000232	7.0		1.17	-10	0.22	16.5	0.03	2270	1	-0.01	-1	-1	0.02	46		-0.01	-5		0.8	-10	14.8	-0.01	-2	6	-10	5.4	151.0		2.2	NOV0186.R12
51000233	89.0		7.50	19	0.13	4.0	-0.01	66	5	-0.01	-1	7	0.04	5,229		0.24	2,949		-0.5	-10	0.7	-0.01	-2	15	-10	1.0	464.0		0.9	NOV0186.R12
51000234	22.4		1.69	-10	0.30	15.4	0.02	2575	-1	-0.01	-1	-1	0.03	2,168		0.12	207		0.7	-10	10.2	-0.01	-2	5	-10	2.1	499.0		2.4	NOV0186.R12
51000235	12.2		1.20	-10	0.28	13.2	0.02	2560	-1	-0.01	-1	2	0.03	804		0.06	121		-0.5	-10	7.1	-0.01	-2	9	-10	2.5	308.0		2.2	NOV0186.R12
51000236	7.4		1.22	-10	0.26	12.3	0.02	1291	3	-0.01	-1	2	0.03	259		0.01	27		0.6	-10	3.6	-0.01	-2	5	-10	2.3	143.0		4.1	NOV0186.R12
51000237	13.4		1.34	-10	0.20	11.3	0.01	94	3	-0.01	-1	4	0.02	127		0.02	15		-0.5	-10	1.7	-0.01	-2	7	-10	1.5	53.8		2.9	NOV0186.R12
51000238	14.4		1.74	-10	0.27	13.9	0.02	1249	2	-0.01	-1	2	0.04	60		0.01	29		0.6	-10	4.0	-0.01	-2	5	-10	2.9	81.9		3.9	NOV0186.R12
51000239	12.6		1.73	-10	0.21	13.1	0.01	651	3	-0.01	-1	-1	0.03	432		0.04	29		0.5	-10	4.4	-0.01	-2	3	-10	2.6	322.0		2.3	NOV0186.R12
51000240	226.0		15.00	-10	0.12	3.1	-0.01	357	4	-0.01	-1	7	0.09	5,514		0.52	289		1.1	12	0.8	-0.01	-2	23	-10	1.6	2,450.0		2.6	NOV0186.R12
51000241	61.6		4.00	-10	0.33	14.6	0.01	40	4	-0.01	-1	5	0.03	4,193		0.41	142		0.7	-10	2.9	-0.01	-2	5	-10	1.9	168.0		1.5	NOV0186.R12
51000242	22.4		6.22	-10	0.12	12.1	1.49	3414	-1	-0.01	-1	14	0.13	104		-0.01	7		10.7	-10	21.6	-0.01	-2	103	-10	17.2	853.0		2.6	NOV0186.R12
51000243	15.6		5.99	-10	0.07	15.0	1.19	2808	-1	0.01	-1	11	0.13	53		-0.01	-5		10.2	-10	49.0	0.01	-2	113	-10	18.4	415.0		2.5	NOV0186.R12
51000244	13.9		6.12	-10	0.09	9.5	0.81	2149	-1	0.02	-1	11	0.12	57		0.08	9		9.0	-10	40.9	0.01	-2	93	-10	12.3	205.0		3.3	NOV0186.R12
51000245	537.0		6.92	-10	0.15	10.5	0.04	117	12	-0.01	-1	-1	0.09	1,579		0.06	941		1.5	11	8.5	-0.01	-2	30	-10	4.4	300.0		0.7	NOV0186.R12
51000246	185.0		6.12	-10	0.19	14.3	0.62	1594	1	-0.01	-1	6	0.15	618		-0.01	62		7.5	-10	15.8	-0.01	-2	70	-10	13.4	356.0		2.5	NOV0186.R12
51000247	382.0		6.76	-10	0.17	15.0	0.55	987	-1	-0.01	-1	6	0.12	1,215		0.02	69		10.5	-10	22.4	-0.01	-2	126	-10	12.0	497.0		1.7	NOV0186.R12
51000248	188.0		6.11	-10	0.21	19.7	1.91	2335	-1	-0.01	-1	18	0.11	597		-0.01	21		11.7	-10	20.8	0.01	-2	123	-10	19.5	1,230.0		2.8	NOV0186.R12
51000249	372.0		5.97	-10	0.19	10.9	0.04	80	-1	-0.01	-1	-1	0.08	2,007		0.07	496		2.5	-10	10.1	-0.01	-2	26	-10	2.8	258.0		1.5	NOV0186.R12
51000250	286.0		4.49	-10	0.19	11.7	0.02	88	5	-0.01	-1	6	0.03	698		0.05	207		1.5	-10	9.6	-0.01	-2	11	-10	1.9	468.0		-0.5	NOV0186.R12
51000251	188.0		5.93	-10	0.12	13.8	1.31	2789	-1	-0.01	-1	10	0.07	1,020		0.02	21		10.1	-10	43.4	0.02	-2	126	-10	12.4	1,410.0		2.7	NOV0186.R12
51000252	186.0		5.96	-10	0.15	14.6	3.03	4767	-1	-0.01	-1	15	0.05	25		-0.01	-5		12.8	-10	32.6	0.05	-2	148	-10	22.2	2,900.0		4.6	NOV0186.R12
51000253	45.7		4.67	-10	0.27	15.8	1.36	4087	-1	-0.01	-1	12	0.05	45		-0.01	18		7.7	-10	16.4	-0.01	-2	56	-10	10.8	1,230.0		4.6	NOV0186.R12
51000254	43.0		4.33	-10	0.27	14.6	0.07	1220	-1	-0.01	-1	-1	0.07	357		0.02	33		5.7	-10	4.5	-0.01	-2	32	-10	10.0	493.0		1.2	NOV0186.R12
51000255	423.0		5.61	-10	0.17	8.6	0.03	93	17	-0.01	-1	4	0.24	10,600	1.06	0.26	474		3.3	-10	14.9	-0.01	-2	21	-10	1.4	120.0		0.9	NOV0186.R12
51000256	64.0		5.30	-10	0.29	6.4	0.42	934	2	-0.01	-1	-1	0.08	200		0.02	40		4.7	-10	15.5	-0.01	-2	29	-10	2.8	153.0		1.5	NOV0186.R12
51000257	100.0		5.63	-10	0.22	9.3	0.03	636	-1	-0.01	-1	2	0.09	1,042		0.03	76		4.2	-10	10.4	-0.01	-2	16	-10	2.9	129.0		0.8	NOV0186.R12
51000258	427.0		11.64	-10	0.26	12.6	0.02	112	5	-0.01	-1	4	0.13	3,663		0.13	191		4.3	-10	33.2	-0.01	-2	64	-10	7.5	447.0		1.2	NOV0186.R12
51000259	123.0		7.97	-10	0.25	5.0	0.03	54	2	-0.01	-1	3	0.11	66		0.02	108		8.0	-10	6.0	-0.01	-2	60	-10	5.9	65.4		1.3	NOV0186.R12
51000260	206.0		7.24	-10	0.21	7.2	0.02	340	9	-0.01	-1	3	0.11	1,618		0.05	220		3.7	-10	14.2	-0.01	-2	45	-10	4.6	185.0		-0.5	NOV0186.R12
51000261	438.0		5.13	-10	0.19	11.8	0.01	99	5	-0.01	-1	3	0.07	1,059		0.02	153		2.3	-10	16.2	-0.01	-2	13	-10	4.3	119.0		0.8	NOV0186.R12
51000262	79.3		6.78	-10	0.31	10.6	0.03	114	-1	-0.01	-1	-1	0.14	1,044		0.02	86		8.1	-10	12.9	-0.01	-2	41	-10	6.8	93.9		1.3	NOV0186.R12
51000263	301.0		5.52	-10	0.19	9.2	0.12	3596	2	-0.01	-1	6	0.06	285		0.01	29		5.0	-10	16.1	-0.01	-2	37	-10	12.2	427.0		2.9	NOV0186.R12
51000264	538.0		7.10	-10	0.32	25.5	0.26	10000	2	-0.01	-1	18	0.14	55		-0.01	68		6.1	-10	73.0	0.03	-2	64	-10	43.6	2,970.0		8.0	NOV0186.R12
51000265	262.0		1.71	-10	0.14	11.5	0.02	1484	4	-0.01	-1	3	0.28	11,700	1.17	0.12	99		3.5	25	21.9	-0.01	-2	33	-10	6.5	226.0		1.0	NOV0186.R12
51000266	139.0		4.77	-10	0.20	9.1	0.04	75	6	-0.01	-1	2	0.03	403		0.07	18		1.1	-10	12.9	-0.01	-2	7	-10	4.1	81.3		0.7	NOV0186.R12
51000267	3.4		1.29	-10	0.16	11.7	0.44	4019	1	-0.01	-1	2	0.02	58		-0.01	-5		1.6	-10	12.2	-0.01	-2	7	-10	5.6	695.0		2.3	NOV0186.R12
51000268	3.8		1.38	-10	0.12	14.9	0.31	1980	1	-0.01	-1	2	0.03	19		-0.01	-5		1.3	-10	4.1	-0.01	-2	5	-10	5.8	154.0		1.9	NOV0186.R12
51000269	2.6		1.35	-10	0.14	22.5	0.31	3029	-1	-0.01	-1	6	0.03	17		-0.01	-5		1.5	-10	6.6	-0.01	-2	5	-10	19.5	198.0		2.9	NOV0186.R12
51000270	-0.5		1.35	-10	0.12	14.9	0.25	3876	-1	-0.01	-1	3	0.03	9		-0.01	-5		1.4	-10	7.6	-0.01	-2	5	-10	12.1	148.0		2.2	NOV0186.R12
51000271	9.1		1.60	-10	0.18	13.0	0.03	7001	3	-0.01	-1	3	0.02	287		-0.01	8		1.3	-10	31.9	-0.01	-2	5	-10	5.0	599.0		2.9	NOV0186.R12
51000272	4.8		1.69	-10	0.12	17.3	0.17	7661	-1	-0.01	-1	-1	0.03	97		-0.01	7		1.8	-10	16.0	-0.01	-2	4	-10	13.2	586.0		3.1	NOV0186.R12
51000273	4.3		1.93	-10	0.15	12.0	0.24	6351	1	-0.01	-1	5	0.06	270		0.01	10		2.4	-10	40.9	-0.01	-2	8	-10	10.0	379.0		3.1	NOV0186.R12
51000274	23.6		5.77	-10	0.17	6.3	0.07	9505	2	-0.01	-1	-1	0.09	637		0.02	27		5.2	-10	32.4	-0.01	-2	26	-10	5.4	744.0		2.8	NOV0186.R12
51000275	131.0		1.75	-10	0.18	12.9	0.02	87	7	-0.01	-1	3	0.04	1,091		0.01	112		0.8	-10	11.3	-0.01	-2	11	-10	2.0	47.4		2.1	NOV0186.R12
51000276	80.8		1.43	-10	0.19	18.6	0.02	41	7	-0.01	-1	-1	0.02	474		-0.01	28		-0.5	-10	8.3	-0.01	-2	3	-10	3.5	25.4		2.1	NOV0186.R12
51000277	34.7		0.90	-10	0.18	12.9	0.02	47	2	-0.01	-1	3	0.01	43		-0.01	-5		-0.5	-10	4.5	-0.01	-2	3	-10	2.7	30.2		2.1	NOV0186.R12
51000278	34.5		0.94	-10	0.15	11.9	0.02	23	3	-0.01	2	2	0.02	80		-0.01	7		-0.5	-10	5.2	-0.01	-2	7	-10	3.6	40.9		2.1	NOV0186.R12
51000279	105.0		0.96	-10	0.19	16.5	0.12	3831	5	-0.01	-1	3	0.02	18		-0.01	-5		0.6	-10	8.4	-0.01	-2	4	-10	8.9	158.0		2.5	NOV0186.R12
51000280	88.8		1.04	-10	0.14	14.7	0.25	5667	3	-0.01	-1	3	0.02	28		-0.01	-5		0.5	-10	7.1	-0.01	-2	5	-10	9.0	264.0		2.0	NOV0186.R12
51000281	49.9		15.00	-10	0.04	-0.5	-0.01	12	-1	-0.01	-1	-1	0.07	98		0.2	74		4.9	-10	1.3	-0.01	-2	118	-10	2.0	42.0		-0.5	NOV0354.R12
51000282	11.7		15.00	-10	0.05	-0.5	-0.01	26	2	-0.01	-1	7	0.02	72		0.04	51		0.7	17	-0.5	-0.01	-2	5	220	0.6	11.7		-0.5	NOV0354.R12
51000283	12.8		4.77	-10	0.10	4.1	-0.01	82	2	-0.01	-1	4	0.03	75		0.02	21		-0.5	-10	0.6	-0.01	-2	16	-10	1.0	8.4		-0.5	NOV0354.R12
51000284	34.5		14.77	-10	0.08	2.4	-0.01	29	2	-0.01	-1	2	0.09	54		0.05	44		1.5	-10	0.9	-0.01	-2	15	70	1.2	47.8		-0.5	NOV0354.R12
51000285	13.8		5.51	-10	0.03	3.2	-0.01	179	3	-0.01	1	10	0.02	103		0.38	40		1.0	-10	0.7	-0.01	-2	3	87	0.8	102.0		-0.5	NOV0354.R12
51000286	51.2		4.85	-10	0.14	4.2	1.48	449	1	0.16	-1	4	0.08	170		4.01	20		2.4	-10	50.3	-0.01	-2	30	-10	5.1	213.0		-0.5	NOV0354.R12
51000287	455.0		13.17	15	0.11	2.8	-0.01	68	2	-0.01	-1	2	0.07	42		0.07	185		2.2	-10	2.6	-0.01	-2	85	586	0.9	17.5		1.2	NOV0354.R12
51000288	151.0		10.63	-10	0.17	5.5	-0.01	29	5	-0.01	-1	5	0.03	49		0.08	208		2.7	-10	2.3	-0.01	-2	26	-10	1.3	8.4		-0.5	NOV0354.R12
51000289	512.0		15.00	-10	0.08	16.7	-0.01	16	2	-0.01	-1	6	0.19	189		0.02	540		19.3	-10	15.1	-0.01	-2	119	20	9.8	29.4		1.9	NOV0354.R12
51000290	78.3		6.67	-10	0.17	4.6	-0.01	14	3	-0.01	-1	4	0.03	17		0.06	-5		-0.5	-10	3.3	-0.01	-2	20	-10	0.7	2.6		-0.5	NOV0354.R12
51000291	135.0		12.78	-10	0.19	4.1	0.01	10	9	-0.01	-1	3	0.07	37		0.07	65		1.6	-10	3.3	-0.01	-2	47	-10	0.6	2.5		0.6	NOV0354.R12
51000292	108.0		9.00	-10	0.16	12.3	0.01	13	-1	-0.01	-1	-1	0.11	3,317		0.87	37		3.4	-10	18.5	-0.01	-2	30	-10	4.5	57.7		1.3	NOV0354.R12
51000293	70.8		8.48	-10	0.18	7.1	0.01	48	2	-0.01	-1	4	0.2	5,646		0.05	308		4.8	-10	7.3	-0.01	-2	26	-10	5.8	149.0		-0.5	NOV0354.R12
51000294	19.8		9.50	-10	0.08	-0.5	0.01	35	-1	-0.01	-1	-1	0.11	105		0.03	17		7.9	-10	2.4	-0.01	-2	172	-10	1.2	98.2		-0.5	NOV0354.R12
51000295	53.3		11.37	-10	0.13	9.1	-0.01	145	3	-0.01	-1	5	0.29	2,047		0.04	45		14.4	-10	16.5	-0.01	-2	133	-10	5.1	235.0		-0.5	NOV0354.R12
51000296	3,380.0		4.12	-10	0.54	18.6	1.21	382	268	0.14	-1	22	0.11	22		0.45	-5		6.6	-10	71.9	0.20	-2	108	-10	12.9	72.1		15.7	NOV0354.R12
51000301	166.0		3.77	-10	0.24	7.8	0.05	922	8	-0.01	-1	-1	0.12	51		-0.01	25		5.0	-10	7.7	0.02	-2	36	-10	28.9	142.0		5.0	NOV0354.R12
51000302	172.0		5.50	-10	0.19	20.6	0.01	276	4	-0.01	-1	-1	0.16	748		0.04	462		5.6	-10	13.6	-0.01	-2	26	-10	23.4	66.7		-0.5	NOV0354.R12
51000303	131.0		4.46	-10	0.21	19.1	0.19	1461	1	-0.01	-1	5	0.11	146		-0.01	32		3.0	-10	14.0	-0.01	-2	27	-10	34.6	216.0		1.5	NOV0354.R12
51000304	101.0		4.96	-10	0.26	23.1	0.02	262	2	-0.01	-1	-1	0.08	1,473		0.04	78		2.7	-10	23.0	-0.01	-2	14	-10	20.4	96.1		-0.5	NOV0354.R12
51000305	26.5		4.79	-10	0.28	17.7	0.21	2253	1	-0.01	-1	-1	0.13	178		-0.01	18		5.0	-10	12.4	-0.01	-2	35	-10	19.7	391.0		1.4	NOV0354.R12
51000306	44.7		1.30	-10	0.18	6.4	0.02	70	2	-0.01	-1	1	0.02	1,487		1.22	205		0.6	-10	3.2	-0.01	-2	9	-10	3.0	3,300.0		-0.5	NOV0354.R12
51000307	357.0		5.01	27	0.07	-0.5	-0.01	342	5	-0.01	-1	5	0.04	20,500	2.05	0	2,137		-0.5	-10	4.4	-0.01	-2	26	-10	1.4	10,630.0	10.63	-0.5	NOV0354.R12
51000308	740.0		3.55	18	0.11	0.6	-0.01	81	3	-0.01	-1	5	0.03	21,400	2.14	5.68	1,221		-0.5	-10	2.9	-0.01	-2	15	-10	1.4	34,800.0	3.48	-0.5	NOV0354.R12
51000309	12.1		1.03	-10	0.17	7.4	-0.01	21	2	-0.01	-1	3	-0.01	2,507		1.21	16		-0.5	-10	3.5	-0.01	-2	3	-10	0.9	453.0		-0.5	NOV0354.R12
51000310	222.0		7.29	-10	0.05	-0.5	-0.01	1032	3	-0.01	-1	4	0.06	1,317		0.07	354		-0.5	11	2.8	-0.01	-2	74	-10	0.6	1,150.0		-0.5	NOV0354.R12
51000311	9.1		2.52	-10	0.17	9.8	-0.01	2290	-1	-0.01	-1	-1	0.06	238		0.06	104		1.0	-10	15.0	-0.01	-2	10	-10	3.1	536.0		1.1	NOV0354.R12
51000312	13.9		1.58	-10	0.23	17.5	0.03	3872	2	-0.01	-1	3	0.05	282		0.03	94		1.2	-10	13.7	-0.01	-2	7	-10	8.6	929.0		2.1	NOV0354.R12
51000313	144.0		2.08	-10	0.14	5.5	0.02	5215	2	-0.01	-1	3	0.02	795		0.03	106		0.9	-10	41.4	-0.01	-2	26	-10	1.6	458.0		1.1	NOV0354.R12
51000314	194.0		2.82	-10	0.14	9.0	0.02	1561	-1	-0.01	-1	-1	0.03	46		0.02	34		1.5	-10	25.2	-0.01	-2	8	-10	3.5	296.0		1.6	NOV0354.R12
51000315	91.6		1.68	-10	0.17	6.3	0.03	2212	2	-0.01	-1	3	0.02	238		-0.01	85		1.7	-10	37.8	-0.01	-2	16	-10	2.5	257.0		1.2	NOV0354.R12
51000316	194.0		4.52	-10	0.14	7.1	0.01	359	-1	-0.01	-1	3	0.06	683		0.05	305		1.3	-10	14.2	-0.01	-2	23	-10	2.2	280.0		1.4	NOV0354.R12

SURILOMA PROJECT GEOCHEMICAL DATA BASE FEBRUARY 2013

14de 16 

SampleID	Cuppm	Cu%	Fe%	Gappm	K%	Lappm	Mg%	Mnppm	Moppm	Na%	Nbppm	Nippm	P%	Pbppm	Pb%	S%	Sbppm	Sb%	Scppm	Snppm	Srppm	Ti%	Tlppm	Vppm	Wppm	Yppm	Znppm	Zn%	Zrppm	BATCH
51000317	132.0		2.78	-10	0.13	7.1	0.02	2142	2	-0.01	-1	2	0.04	1,653		0.08	171		0.7	-10	16.6	-0.01	-2	25	-10	1.6	519.0		-0.5	NOV0354.R12
51000318	69.6		1.96	-10	0.16	4.2	0.03	121	2	-0.01	-1	3	0.03	119		-0.01	22		1.1	-10	7.2	-0.01	-2	11	-10	2.1	50.3		2.3	NOV0354.R12
51000319	91.4		1.47	-10	0.19	10.7	0.14	319	-1	-0.01	-1	4	0.03	51		-0.01	-5		1.7	-10	10.1	-0.01	-2	9	-10	2.6	84.3		2.2	NOV0354.R12
51000320	66.7		1.27	-10	0.18	7.4	0.04	92	-1	-0.01	-1	-1	0.03	34		-0.01	-5		4.1	-10	7.2	-0.01	-2	5	-10	2.6	51.8		1.8	NOV0354.R12
51000321	72.1		1.33	-10	0.19	9.4	0.06	89	-1	-0.01	-1	5	0.04	18		-0.01	6		4.2	-10	8.5	-0.01	-2	6	-10	3.8	41.6		1.4	NOV0354.R12
51000322	142.0		6.54	-10	0.07	-0.5	-0.01	754	3	-0.01	-1	5	0.05	791		0.05	186		-0.5	-10	2.9	-0.01	-2	52	-10	0.7	793.0		-0.5	NOV0354.R12
51000323	6.8		0.51	-10	-0.01	-0.5	-0.01	73	5	-0.01	-1	3	-0.01	-2		-0.01	-5		-0.5	-10	-0.5	-0.01	-2	-2	-10	-0.5	9.6		-0.5	NOV0354.R12
51000329	18.6		8.68	-10	0.21	-0.5	0.01	18	-1	-0.01	-1	-1	0.1	355		0.03	29		1.6	-10	1.4	-0.01	-2	17	11	0.7	56.9		0.9	DIC0042.R12
51000330	669.0		15.00	-10	0.12	-0.5	-0.01	56	4	-0.01	-1	-1	0.16	942		0.11	3,039		2.2	22	1.5	-0.01	-2	20	33	2.1	950.0		2.6	DIC0042.R12
51000331	29.8		11.07	-10	0.22	-0.5	0.01	21	-1	-0.01	-1	-1	0.15	436		0.05	23		1.2	-10	2.8	-0.01	-2	17	-10	0.8	72.7		0.9	DIC0042.R12
51000332	23.2		4.08	-10	0.18	10.6	0.04	64	3	0.01	-1	5	0.02	53		-0.01	24		1.0	-10	4.5	-0.01	-2	10	-10	1.1	89.7		1.1	DIC0042.R12
51000333	229.0		15.00	-10	0.13	-0.5	0.01	543	-1	-0.01	-1	3	0.18	116		0.04	76		1.7	12	6.2	-0.01	-2	14	24	2.1	213.0		1.1	DIC0042.R12
51000334	69.0		15.00	-10	0.07	-0.5	0.03	64	-1	-0.01	-1	-1	0.52	592		0.03	75		7.2	17	2.3	-0.01	-2	77	25	2.8	364.0		1.7	DIC0042.R12
51000335	52.3		15.00	-10	0.16	-0.5	0.02	250	-1	-0.01	-1	-1	0.33	225		0.02	21		2.1	-10	3.1	-0.01	-2	23	13	4.1	210.0		3.1	DIC0042.R12
51000336	52.6		15.00	-10	0.13	-0.5	0.01	15	-1	-0.01	-1	-1	0.07	71		0.06	20		2.8	-10	2.1	-0.01	-2	18	15	0.8	117.0		1.9	DIC0042.R12
51000337	1,660.0		15.00	-10	0.08	-0.5	-0.01	1112	3	-0.01	-1	41	0.07	1,253		10	2,042		0.5	19	17.8	-0.01	-2	8	295	2.3	188.0		-0.5	DIC0042.R12
51000338	24.9		5.26	-10	0.28	19.6	0.31	639	-1	0.03	-1	55	0.02	16		0.37	11		2.3	-10	13.1	0.06	-2	58	-10	3.1	56.1		1.5	DIC0042.R12
51000339	3,840.0		15.00	-10	0.06	-0.5	-0.01	81	-1	-0.01	-1	28	0.02	3,466		10	4,330		0.8	31	2.9	-0.01	-2	5	1335	0.6	546.0		-0.5	DIC0042.R12
51000340	27.3		11.06	-10	0.20	-0.5	0.01	21	-1	-0.01	-1	7	0.14	411		0.05	18		1.1	13	2.6	-0.01	-2	16	-10	0.7	67.5		0.9	DIC0042.R12
51000341	21.6		4.58	-10	0.15	23.2	-0.01	20	2	0.01	-1	5	0.02	95		0.04	62		-0.5	-10	4.8	-0.01	-2	6	-10	2.6	21.2		0.6	DIC0042.R12
51000342	65.2		7.05	-10	0.10	5.3	-0.01	49	3	-0.01	-1	5	0.03	339		0.02	24		1.2	21	1.6	-0.01	-2	12	-10	1.0	53.3		1.1	DIC0042.R12
51000343	153.0		14.02	-10	0.10	5.3	-0.01	31	1	-0.01	-1	3	0.06	360		0.09	17		1.2	17	0.9	-0.01	-2	15	-10	1.7	127.0		0.9	DIC0042.R12
51000344	42.4		7.46	-10	0.18	6.0	0.08	76	2	-0.01	-1	3	0.14	82		0.43	20		2.0	-10	4.3	-0.01	-2	16	-10	2.6	33.4		1.0	DIC0042.R12
51000345	82.8		4.05	-10	0.18	14.5	0.07	31	16	-0.01	-1	6	0.03	188		0.01	110		1.1	13	1.4	-0.01	-2	13	-10	1.6	26.9		0.7	DIC0042.R12
51000346	88.2		5.69	-10	0.14	13.0	0.33	62	22	-0.01	-1	-1	0.04	622		0.03	60		2.4	30	2.3	-0.01	-2	26	-10	1.8	59.8		0.6	DIC0042.R12
51000347	50.7		8.66	-10	0.12	-0.5	0.02	31	3	0.01	-1	-1	0.04	25		0.04	28		0.5	-10	1.3	-0.01	-2	13	-10	-0.5	26.2		0.9	DIC0042.R12
51000349	36.7		10.41	-10	0.18	12.5	-0.01	51	-1	-0.01	-1	-1	0.13	1,210		0.1	40		1.6	-10	12.6	-0.01	-2	11	-10	-0.5	222.0		-0.5	ENE0102.R14
51000350	58.7		10.50	-10	0.10	12.6	-0.01	19	-1	-0.01	-1	7	0.07	29		0.07	26		-0.5	-10	2.9	-0.01	-2	6	-10	0.8	53.0		-0.5	ENE0102.R15
51000351	40.6		6.08	-10	0.12	8.9	-0.01	19	2	-0.01	-1	2	0.05	41		0.05	39		-0.5	-10	3.6	-0.01	-2	5	-10	-0.5	26.5		-0.5	ENE0102.R16
51000360	42.4		2.08	-10	0.20	11.2	-0.01	10000	4	-0.01	-1	3	0.03	3,503		-0.01	126		1.3	-10	63.2	0.02	23	4	-10	4.6	1,190.0		5.2	ENE0102.R25
51000370	9.1		0.59	-10	-0.01	-0.5	-0.01	74	4	-0.01	-1	2	-0.01	-2		-0.01	-5		-0.5	-10	-0.5	-0.01	-2	-2	-10	-0.5	7.7		-0.5	ENE0102.R35
51000401	3,370.0		4.16	-10	0.52	18.4	1.19	376	268	0.14	-1	21	0.11	18		0.45	-5		6.4	-10	71.9	0.19	-2	105	-10	12.6	71.1		15.5	NOV0355.R12
51000402	10.9		4.15	-10	0.27	19.4	0.05	848	2	-0.01	-1	2	0.23	6		0.15	90		6.8	-10	15.1	-0.01	-2	20	-10	10.0	26.0		1.0	NOV0355.R12
51000403	6.2		4.75	-10	0.32	13.9	0.07	426	1	-0.01	-1	1	0.13	10		0.24	101		7.4	-10	23.7	-0.01	-2	31	-10	7.2	27.4		0.7	NOV0355.R12
51000404	26.7		4.21	-10	0.23	9.6	0.09	1496	-1	-0.01	-1	-1	0.07	6		0.04	56		9.9	-10	5.5	-0.01	-2	24	-10	6.8	57.1		0.7	NOV0355.R12
51000405	2.2		1.54	-10	0.18	10.2	0.07	58	1	-0.01	-1	3	0.03	9		0.08	85		5.0	-10	13.4	-0.01	-2	15	-10	4.1	18.1		-0.5	NOV0355.R12
51000406	0.6		1.57	-10	0.14	11.0	0.07	32	1	-0.01	-1	-1	0.04	14		0.06	80		5.8	-10	12.5	-0.01	-2	11	-10	4.2	10.7		0.6	NOV0355.R12
51000407	9.5		2.06	-10	0.15	8.6	0.06	61	1	-0.01	-1	4	0.04	14		0.23	93		3.2	-10	17.3	-0.01	-2	20	-10	4.3	14.4		-0.5	NOV0355.R12
51000408	6.6		1.93	-10	0.15	14.0	0.07	56	-1	-0.01	-1	2	0.07	21		0.05	93		7.4	-10	25.7	-0.01	-2	11	-10	4.7	11.9		-0.5	NOV0355.R12
51000409	2.6		2.33	-10	0.26	11.8	0.06	55	2	-0.01	-1	-1	0.06	20		0.11	65		15.2	-10	14.5	-0.01	-2	18	-10	6.9	17.4		0.8	NOV0355.R12
51000410	7.9		2.87	-10	0.18	15.1	0.07	502	-1	-0.01	-1	-1	0.04	27		0.07	96		5.9	-10	12.3	-0.01	-2	25	-10	18.5	82.9		0.5	NOV0355.R12
51000411	8.9		2.82	-10	0.08	14.9	0.06	363	1	-0.01	-1	3	0.05	59		0.17	126		3.8	-10	21.0	-0.01	-2	23	-10	14.9	237.0		-0.5	NOV0355.R12
51000412	23.6		7.04	-10	0.21	10.8	0.14	10000	2	-0.01	-1	3	0.09	99		0.19	4,189		6.5	-10	11.3	0.02	-2	42	-10	7.0	578.0		3.5	NOV0355.R12
51000413	6.6		2.78	-10	0.16	11.6	0.07	79	-1	-0.01	-1	2	0.05	19		0.11	141		4.5	-10	41.2	-0.01	-2	20	-10	6.7	29.4		1.2	NOV0355.R12
51000414	29.2		4.29	-10	0.08	7.6	0.02	98	3	-0.01	-1	10	0.06	1,159		0.69	1,279		2.1	-10	38.7	-0.01	-2	11	-10	2.8	1,850.0		0.7	NOV0355.R12
51000415	6.4		2.64	-10	0.26	12.6	0.14	111	1	-0.01	-1	-1	0.03	74		0.24	110		10.7	-10	30.1	-0.01	-2	15	-10	4.1	9.0		1.4	NOV0355.R12
51000416	2.6		1.78	-10	0.30	11.2	0.08	39	2	-0.01	-1	2	0.06	46		0.24	73		4.2	-10	41.0	-0.01	-2	14	-10	3.0	3.9		1.4	NOV0355.R12
51000417	11.9		2.64	-10	0.15	8.8	0.04	50	1	-0.01	-1	3	0.04	23		0.08	167		5.5	-10	30.9	-0.01	-2	12	-10	5.0	18.8		1.6	NOV0355.R12
51000418	52.4		14.00	-10	0.28	6.9	0.11	268	1	-0.01	-1	-1	0.19	22		0.04	100		5.1	-10	18.1	-0.01	-2	43	-10	12.5	42.2		1.5	NOV0355.R12
51000419	4.2		3.19	-10	0.33	17.8	0.1	214	-1	-0.01	-1	-1	0.11	9		0.16	52		2.9	-10	17.8	-0.01	-2	33	-10	8.8	13.1		1.4	NOV0355.R12
51000420	40.8		9.87	-10	0.22	11.0	0.17	3071	-1	-0.01	-1	9	0.18	15		-0.01	27		8.4	-10	28.8	0.01	-2	88	-10	12.7	123.0		3.9	NOV0355.R12
51000421	10.8		5.69	-10	0.14	9.1	0.04	141	3	-0.01	-1	-1	0.06	20		0.04	185		3.7	-10	19.4	-0.01	-2	26	-10	4.6	11.9		1.6	NOV0355.R12
51000422	14.7		6.37	-10	0.15	7.0	0.02	121	4	-0.01	-1	2	0.08	18		0.05	100		11.4	-10	22.1	-0.01	-2	33	-10	6.5	5.5		1.6	NOV0355.R12
51000423	39.4		6.34	-10	0.27	9.5	0.02	178	3	0.01	-1	2	0.1	21		0.27	217		14.0	-10	23.9	-0.01	-2	33	-10	3.6	5.6		1.6	NOV0355.R12
51000424	15.5		3.13	-10	0.32	15.3	0.03	50	4	-0.01	-1	-1	0.1	9		0.23	43		15.1	-10	26.5	-0.01	-2	45	-10	6.0	3.7		-0.5	NOV0355.R12
51000425	59.3		7.70	-10	0.22	4.4	0.03	51	7	-0.01	-1	-1	0.09	14		0.05	202		8.4	-10	12.7	-0.01	-2	41	-10	3.1	9.8		0.7	NOV0355.R12
51000426	28.0		4.97	-10	0.22	9.9	0.05	196	2	-0.01	-1	2	0.09	11		0.06	80		11.0	-10	18.4	-0.01	-2	80	-10	7.7	12.2		1.1	NOV0355.R12
51000427	62.8		9.14	-10	0.19	8.8	0.02	94	3	-0.01	-1	-1	0.12	20		0.22	104		11.5	-10	16.6	-0.01	-2	56	-10	7.2	16.1		-0.5	NOV0355.R12
51000428	73.1		11.29	-10	0.25	7.4	0.03	123	7	-0.01	-1	-1	0.13	15		0.14	190		13.1	-10	16.8	-0.01	-2	71	-10	7.1	13.1		1.1	NOV0355.R12
51000429	23.5		4.96	-10	0.09	5.9	0.02	75	13	-0.01	-1	2	0.06	21		0.08	230		6.9	-10	12.7	-0.01	-2	33	-10	3.4	6.0		-0.5	NOV0355.R12
51000430	24.7		5.31	-10	0.09	6.0	0.01	66	11	-0.01	-1	3	0.06	21		0.08	201		7.2	-10	12.4	-0.01	-2	34	-10	3.7	6.4		0.9	NOV0355.R12
51000431	37.9		9.19	-10	0.22	16.2	0.02	58	4	-0.01	-1	-1	0.13	22		0.28	261		18.3	-10	51.2	-0.01	-2	54	-10	5.5	8.1		1.5	NOV0355.R12
51000432	66.4		10.75	-10	0.17	4.8	0.03	106	14	-0.01	-1	2	0.12	18		0.08	134		9.5	-10	19.9	-0.01	-2	49	-10	4.0	17.3		1.5	NOV0355.R12
51000433	34.8		9.42	-10	0.14	14.6	0.01	104	19	-0.01	-1	-1	0.19	10		0.15	194		11.5	-10	79.9	-0.01	-2	56	-10	7.7	20.8		1.5	NOV0355.R12
51000434	48.9		1.61	-10	0.18	5.6	0.46	555	6	0.03	-1	5	0.04	21		0.6	-5		3.9	-10	108.0	0.01	-2	28	-10	5.0	42.7		6.0	NOV0355.R12
51000435	54.5		6.89	-10	0.17	8.2	0.02	164	4	-0.01	-1	-1	0.1	17		0.05	106		11.5	-10	24.7	-0.01	-2	31	-10	4.2	33.0		1.0	NOV0355.R12
51000436	37.8		8.93	-10	0.27	8.2	0.03	81	13	-0.01	-1	-1	0.16	16		0.09	100		14.8	-10	20.6	-0.01	-2	72	-10	6.7	20.0		3.2	NOV0355.R12
51000437	30.0		7.36	-10	0.13	6.6	0.18	522	2	-0.01	-1	5	0.16	14		-0.01	42		12.7	-10	12.8	0.01	-2	109	-10	4.1	50.9		4.1	NOV0355.R12
51000438	24.9		6.41	-10	0.17	8.0	0.02	57	10	-0.01	-1	4	0.13	18		0.05	73		7.3	-10	8.1	-0.01	-2	30	-10	4.8	18.2		2.6	NOV0355.R12
51000439	4.2		3.16	-10	0.15	19.7	0.02	35	5	-0.01	-1	-1	0.08	21		0.11	70		5.1	-10	12.3	-0.01	-2	19	-10	4.5	9.5		1.3	NOV0355.R12
51000440	4.1		6.20	-10	0.18	14.6	0.02	368	7	-0.01	-1	2	0.16	29		0.02	338		4.1	-10	8.7	-0.01	-2	78	-10	8.4	18.0		1.2	NOV0355.R12
51000441	5.2		6.29	-10	0.16	10.9	0.02	525	6	-0.01	-1	2	0.18	27		0.01	297		5.7	-10	7.4	-0.01	-2	71	-10	9.2	22.9		1.5	NOV0355.R12
51000442	5.9		5.74	-10	0.16	16.5	0.02	448	10	-0.01	-1	2	0.12	19		0.03	106		3.3	-10	17.7	-0.01	-2	25	-10	7.5	29.7		1.0	NOV0355.R12
51000443	12.5		8.13	-10	0.17	10.7	0.08	703	4	-0.01	-1	3	0.19	13		0.01	269		4.4	-10	10.4	0.01	-2	93	-10	11.5	48.4		2.1	NOV0355.R12
51000444	7.7		4.52	-10	0.24	8.5	0.06	182	3	-0.01	-1	-1	0.08	11		-0.01	254		3.8	-10	10.3	0.01	-2	63	-10	13.4	28.9		2.6	NOV0355.R12
51000445	10.1		6.20	-10	0.14	13.9	0.06	583	4	-0.01	-1	3	0.14	15		-0.01	465		4.9	-10	14.2	0.01	-2	90	-10	12.4	38.8		2.0	NOV0355.R12
51000446	10.5		5.67	-10	0.15	17.6	0.09	1959	2	-0.01	-1	3	0.14	19		-0.01	309		5.7	-10	22.0	0.02	-2	68	-10	21.0	38.1		3.0	NOV0355.R12
51000447	8.0		5.22	-10	0.16	12.2	0.05	6322	2	-0.01	-1	2	0.1	12		-0.01	188		4.6	-10	15.4	0.02	-2	45	-10	22.9	43.3		3.4	NOV0355.R12
51000448	15,200.0	1.52	7.06	-10	0.13	7.3	1.01	334	4	0.05	-1	20	0.1	33		1.49	-5		5.4	11	53.4	0.08	-2	95	-10	7.7	119.0		7.7	NOV0355.R12
51000449	51.6		6.04	-10	0.10	18.0	0.01	55	4	-0.01	-1	3	0.29	18		0.02	320		12.0	-10	82.3	-0.01	-2	32	-10	7.5	25.8		0.6	NOV0355.R12
51000450	28.4		5.32	-10	0.19	5.1	0.01	39	1	-0.01	-1	-1	0.09	9		0.07	107		4.9	-10	7.6	-0.01	-2	52	-10	3.1	7.9		1.9	NOV0355.R12
51000452	-0.5		4.81	-10	0.27	23.2	0.03	120	1	-0.01	-1	-1	0.09	17		0.06	9		2.1	-10	18.8	-0.01	-2	4	16	5.7	23.1		1.9	DIC0362.R13
51000453	1.2		4.56	-10	0.29	10.7	0.21	2890	-1	-0.01	-1	-1	0.06	16		4.72	20		2.9	-10	12.8	-0.01	-2	-2	17	13.7	133.0		1.4	DIC0362.R14

SURILOMA PROJECT GEOCHEMICAL DATA BASE FEBRUARY 2013

15de 16 

SampleID	Cuppm	Cu%	Fe%	Gappm	K%	Lappm	Mg%	Mnppm	Moppm	Na%	Nbppm	Nippm	P%	Pbppm	Pb%	S%	Sbppm	Sb%	Scppm	Snppm	Srppm	Ti%	Tlppm	Vppm	Wppm	Yppm	Znppm	Zn%	Zrppm	BATCH
51000454	4.0		0.76	-10	0.05	1.1	0.04	229	2	-0.01	4	16	-0.01	-2		0.03	-5		-0.5	-10	3.3	-0.01	-2	-2	11	2.3	8.4		1.4	DIC0362.R15
51000455	8.7		2.21	-10	0.26	24.1	0.09	2456	-1	0.01	-1	6	0.05	398		0.09	441		6.4	-10	16.3	-0.01	-2	19	18	21.2	44.7		2.1	DIC0362.R16
51000456	6.3		7.90	-10	0.11	7.2	0.04	2635	1	-0.01	-1	5	0.11	15		0.02	503		3.8	-10	13.0	-0.01	-2	15	19	11.7	91.4		2.1	DIC0362.R17
51000457	19.1		15.00	-10	0.29	15.6	0.06	3989	1	-0.01	-1	4	0.41	17		0.06	102		12.7	-10	122.0	-0.01	-2	39	29	21.2	202.0		2.0	DIC0362.R18
51000458	1.2		1.42	-10	0.06	12.2	0.01	345	1	-0.01	-1	2	0.03	27		-0.01	8		2.6	-10	3.6	-0.01	-2	12	11	3.6	37.3		2.5	DIC0362.R19
51000459	4.9		1.01	-10	-0.01	4.2	1.84	2181	1	-0.01	-1	-1	0.02	25		0.02	-5		1.7	-10	82.3	-0.01	-2	13	19	4.2	29.5		-0.5	DIC0362.R20
51000460	15.9		0.89	-10	0.01	5.8	1.25	3076	-1	-0.01	-1	2	0.03	6		-0.01	-5		2.2	-10	43.1	-0.01	-2	15	11	5.2	22.0		1.2	DIC0362.R21
51000461	4.8		1.16	-10	0.18	10.1	0.67	1728	-1	-0.01	-1	4	0.03	3		-0.01	-5		2.6	10	45.7	0.01	-2	11	-10	12.4	26.1		2.6	DIC0362.R22
51000462	3.1		1.22	-10	0.13	9.2	0.56	491	2	-0.01	-1	9	-0.01	3		-0.01	-5		1.5	-10	5.1	-0.01	-2	7	-10	5.1	35.7		1.6	DIC0362.R23
51000463	5.9		0.56	-10	0.04	-0.5	0.02	116	2	-0.01	-1	15	-0.01	5		-0.01	-5		-0.5	-10	2.5	-0.01	-2	2	-10	-0.5	6.7		-0.5	DIC0362.R24
51000464	4.7		2.70	-10	0.34	8.1	0.22	81	-1	-0.01	-1	3	0.04	18		0.07	77		6.5	-10	26.7	-0.01	-2	29	-10	5.3	12.9		2.4	DIC0362.R25
51000465	70.3		7.16	-10	0.19	11.6	0.07	251	2	-0.01	-1	9	0.1	401		0.25	894		9.5	-10	38.6	0.01	-2	23	-10	4.1	32.8		3.6	DIC0362.R26
51000466	15.1		3.74	-10	0.27	18.0	0.11	67	-1	-0.01	-1	2	0.12	30		0.18	106		9.9	-10	40.4	-0.01	-2	24	-10	3.5	12.8		1.7	DIC0362.R27
51000467	4.3		4.28	-10	0.38	22.9	0.1	66	-1	-0.01	-1	3	0.23	38		0.52	126		19.3	-10	89.6	-0.01	-2	22	-10	3.9	8.2		2.3	DIC0362.R28
51000468	8.6		4.66	-10	0.41	20.8	0.09	41	-1	-0.01	-1	1	0.16	16		0.47	139		10.4	-10	70.5	-0.01	-2	26	-10	4.0	7.5		2.2	DIC0362.R29
51000469	6.7		0.54	-10	-0.01	-0.5	-0.01	71	5	-0.01	-1	10	-0.01	-2		-0.01	-5		-0.5	-10	0.6	-0.01	-2	-2	-10	-0.5	9.5		-0.5	DIC0362.R30
51000470	13.1		2.75	-10	0.31	15.5	0.11	86	-1	-0.01	-1	2	0.18	17		0.05	107		9.2	-10	20.4	-0.01	-2	53	-10	10.5	16.9		1.9	DIC0362.R31
51000471	15.2		3.20	-10	0.29	20.3	0.51	581	-1	0.02	-1	8	0.09	82		0.05	175		7.5	-10	35.3	0.06	-2	66	-10	24.0	65.9		9.9	DIC0362.R32
51000472	14.7		3.20	-10	0.23	25.4	0.31	122	-1	-0.01	-1	5	0.14	9		-0.01	74		8.9	-10	34.2	0.04	-2	78	-10	29.7	35.5		2.6	DIC0362.R33
51000473	14.8		3.29	-10	0.23	27.7	0.3	124	-1	-0.01	-1	5	0.14	9		-0.01	71		9.1	-10	34.1	0.04	-2	80	-10	31.4	36.7		2.3	DIC0362.R34
51000474	5.1		3.01	-10	0.24	15.3	0.12	57	-1	-0.01	-1	3	0.24	9		0.06	165		8.8	-10	26.0	0.01	-2	64	-10	8.8	23.5		0.7	DIC0362.R35
51000475	14.1		4.76	-10	0.20	21.7	0.92	740	-1	0.01	-1	9	0.13	36		0.13	126		9.0	-10	42.0	0.18	-2	93	-10	9.4	74.9		3.9	DIC0362.R36
51000476	10.3		4.06	-10	0.19	17.4	0.37	425	-1	-0.01	-1	4	0.12	150		0.2	289		6.5	-10	54.7	0.05	-2	49	-10	5.3	85.5		2.5	DIC0362.R37
51000477	9.0		3.78	-10	0.19	14.5	0.37	586	-1	-0.01	-1	4	0.11	84		0.14	240		5.9	-10	37.7	0.04	-2	49	-10	6.6	109.0		2.4	DIC0362.R38
51000478	22.6		3.59	-10	0.20	13.3	0.21	424	-1	-0.01	-1	3	0.13	206		0.17	322		7.1	-10	36.8	0.02	-2	39	-10	4.6	307.0		1.6	DIC0362.R39
51000479	12.0		3.81	-10	0.25	15.9	0.23	535	-1	-0.01	-1	3	0.12	208		0.3	393		8.5	-10	48.3	0.01	-2	33	-10	6.6	232.0		2.3	DIC0362.R40
51000480	11.9		3.73	-10	0.25	14.3	0.15	324	-1	-0.01	-1	1	0.12	363		0.28	319		7.8	-10	46.8	-0.01	-2	29	-10	4.4	378.0		1.3	DIC0362.R41
51000481	5.8		3.59	-10	0.24	15.5	0.16	1707	-1	-0.01	-1	2	0.05	14		0.03	71		7.8	-10	13.2	0.01	-2	60	-10	12.5	100.0		1.0	DIC0362.R42
51000482	8.9		4.52	-10	0.22	23.0	0.67	4073	-1	-0.01	-1	-1	0.09	10		0.03	59		9.7	-10	6.2	0.02	-2	73	-10	28.3	292.0		2.5	DIC0362.R43
51000483	14.7		6.74	-10	0.18	15.8	0.46	2530	-1	-0.01	-1	3	0.16	13		0.06	64		7.2	-10	10.8	-0.01	-2	65	-10	19.0	281.0		2.3	DIC0362.R44
51000484	17.6		4.07	-10	0.23	12.2	0.11	2262	-1	-0.01	-1	-1	0.07	41		0.17	212		10.0	-10	12.5	-0.01	-2	36	-10	5.3	94.9		1.1	DIC0362.R45
51000485	8.8		3.38	-10	0.20	9.6	0.07	2089	-1	-0.01	-1	-1	0.05	32		0.1	122		10.3	-10	6.6	-0.01	-2	28	-10	3.6	82.0		0.7	DIC0362.R46
51000486	11.7		2.95	-10	0.34	10.8	0.03	464	-1	-0.01	-1	-1	0.05	14		0.2	76		5.4	-10	9.1	-0.01	-2	18	-10	3.1	50.9		1.2	DIC0362.R47
51000487	3,370.0		4.51	-10	0.52	17.5	1.21	394	262	0.14	-1	21	0.11	15		0.47	-5		6.7	-10	72.9	0.21	-2	111	-10	13.4	72.4		16.4	DIC0362.R48
51000488	19.4		1.61	-10	0.29	14.8	0.03	132	2	-0.01	-1	-1	0.1	9		0.13	32		4.0	-10	5.3	-0.01	-2	21	-10	5.7	15.0		2.3	DIC0362.R49
51000489	5.8		3.95	-10	0.22	26.9	0.94	1738	-1	-0.01	-1	3	0.12	10		0.01	18		4.7	-10	13.2	0.02	-2	61	-10	26.8	142.0		2.7	DIC0362.R50
51000490	13.4		4.90	-10	0.25	3.7	0.07	7963	-1	-0.01	-1	-1	0.1	7		0.14	79		4.5	-10	7.2	-0.01	-2	50	-10	4.0	95.6		2.7	DIC0362.R51
51000491	9.9		9.80	-10	0.16	9.0	0.43	1193	-1	0.01	-1	5	0.09	24		0.02	19		4.7	-10	19.6	0.09	-2	91	-10	7.7	132.0		8.9	FEB0067.R13
51000492	12.7		15.00	-10	0.22	7.2	0.15	1206	-1	-0.01	-1	7	0.19	21		0.03	60		6.1	-10	15.8	0.05	-2	71	-10	6.3	196.0		6.3	FEB0067.R13
51000493	7.6		12.85	-10	0.33	4.5	0.06	981	-1	-0.01	-1	-1	0.18	16		0.02	38		4.2	19	12.5	-0.01	-2	46	-10	7.2	147.0		1.8	FEB0067.R13
51000494	10.6		7.01	-10	0.26	5.7	0.04	540	-1	-0.01	-1	5	0.09	13		0.04	21		3.4	-10	10.6	-0.01	-2	26	-10	5.4	72.3		2.0	FEB0067.R13
51000495	9.8		6.04	-10	0.26	11.2	0.06	3357	-1	-0.01	-1	5	0.16	-2		0.01	19		8.8	-10	11.0	-0.01	-2	62	-10	14.8	145.0		1.1	FEB0067.R13
51000496	15.5		4.91	-10	0.23	15.5	0.16	2616	-1	-0.01	-1	2	0.1	16		-0.01	31		5.1	-10	25.2	0.03	-2	79	-10	13.3	83.0		2.5	FEB0067.R13
51000497	25.0		6.22	-10	0.26	16.3	0.34	1336	-1	-0.01	-1	6	0.09	11		0.05	30		5.2	-10	40.6	-0.01	-2	46	-10	18.5	87.7		2.9	FEB0067.R13
51000498	25.1		5.90	-10	0.37	16.3	0.05	155	4	0.01	-1	4	0.14	12		0.59	214		11.8	12	125.0	-0.01	-2	26	-10	5.9	42.5		1.1	FEB0067.R13
51000499	37.1		3.67	-10	0.25	12.4	0.16	2090	2	-0.01	-1	7	0.09	4		-0.01	42		5.4	-10	22.9	-0.01	-2	46	-10	12.8	54.2		2.7	FEB0067.R13
51000500	42.5		1.64	-10	0.18	5.4	0.46	515	6	0.02	-1	10	0.04	30		0.63	-5		3.6	-10	110.0	0.01	-2	30	-10	4.1	33.5		5.0	FEB0067.R13
51000501	15.2		5.13	-10	0.21	20.1	0.73	6926	1	-0.01	-1	11	0.09	7		-0.01	17		5.1	-10	29.0	0.03	-2	101	-10	20.5	104.0		3.0	FEB0067.R13
51000502	10.0		4.40	-10	0.19	13.5	0.83	872	-1	0.01	-1	7	0.09	11		-0.01	-5		4.6	-10	17.3	0.03	-2	100	-10	12.1	63.9		3.6	FEB0067.R13
51000503	8.6		4.58	-10	0.16	13.1	0.5	977	-1	0.01	-1	5	0.09	8		-0.01	-5		4.3	-10	16.5	0.03	-2	100	-10	11.3	51.1		2.6	FEB0067.R13
51000504	6.1		2.03	-10	0.24	19.6	0.06	2304	-1	-0.01	-1	3	0.06	7		-0.01	15		2.4	-10	10.6	-0.01	-2	14	-10	13.1	46.8		2.2	FEB0067.R13
51000505	6.8		2.80	-10	0.26	27.5	0.07	4756	1	-0.01	-1	4	0.06	11		0.02	28		2.6	-10	17.6	-0.01	-2	9	-10	22.3	132.0		1.7	FEB0067.R13
51000506	6.4		1.00	-10	0.29	16.1	0.05	48	-1	-0.01	-1	-1	0.09	9		0.03	10		2.2	-10	10.0	-0.01	-2	7	-10	8.6	9.7		1.0	FEB0067.R13
51000507	7.4		4.11	-10	0.24	11.1	0.03	83	-1	-0.01	-1	5	0.15	28		0.23	47		2.9	-10	28.4	-0.01	-2	8	-10	2.9	38.9		1.3	FEB0067.R13
51000508	89.8		2.10	-10	0.10	10.3	0.02	81	2	-0.01	-1	5	0.04	2,842		0.19	2,143		1.6	-10	12.9	-0.01	-2	6	20	2.9	1,790.0		0.7	FEB0067.R13
51000509	86.5		2.11	-10	0.10	9.9	0.02	88	-1	-0.01	-1	6	0.04	2,437		0.14	1,719		1.5	-10	14.0	-0.01	-2	7	-10	2.8	1,210.0		0.6	FEB0067.R13
51000510	11.0		3.62	-10	0.13	7.2	0.02	90	-1	-0.01	-1	6	0.04	16		0.06	35		3.7	-10	13.6	-0.01	-2	12	-10	2.4	26.7		0.6	FEB0067.R13
51000511	6.5		4.28	-10	0.22	14.0	0.04	87	2	-0.01	-1	1	0.14	18		0.15	56		6.4	-10	31.9	-0.01	-2	18	-10	4.2	30.3		0.9	FEB0067.R13
51000512	16.2		12.00	-10	0.16	9.2	0.03	244	-1	-0.01	-1	4	0.08	24		0.11	122		6.1	-10	24.8	-0.01	-2	34	-10	4.0	32.2		1.1	FEB0067.R13
51000513	8.4		6.29	-10	0.22	14.3	0.07	6842	-1	-0.01	-1	2	0.08	6		-0.01	87		12.2	-10	15.3	-0.01	-2	22	-10	12.1	139.0		1.3	FEB0067.R13
51000514	8.4		4.72	-10	0.22	23.6	0.1	4103	-1	-0.01	-1	5	0.09	14		-0.01	22		10.5	-10	18.0	-0.01	-2	45	-10	26.0	57.6		1.3	FEB0067.R13
51000515	7.4		3.70	-10	0.23	13.3	0.53	1109	-1	-0.01	-1	-1	0.09	12		-0.01	16		5.3	-10	14.5	-0.01	-2	46	-10	11.3	59.1		1.4	FEB0067.R13
51000516	8.5		2.98	-10	0.25	13.1	0.05	83	2	-0.01	-1	7	0.04	16		0.25	344		6.0	-10	69.0	-0.01	-2	15	-10	4.0	13.3		1.3	FEB0067.R13
51000517	5.3		2.41	-10	0.19	21.5	0.07	81	1	-0.01	-1	6	0.04	85		0.12	145		5.2	-10	91.9	-0.01	-2	15	-10	5.9	11.4		1.3	FEB0067.R13
51000518	52.8		3.52	-10	0.16	14.6	0.05	137	-1	-0.01	-1	4	0.05	27		0.12	79		7.0	-10	68.7	-0.01	-2	18	-10	3.6	12.5		0.8	FEB0067.R13
51000519	10.5		4.19	-10	0.28	13.4	0.07	96	-1	-0.01	-1	2	0.07	14		0.18	71		8.5	-10	39.5	-0.01	-2	33	-10	5.2	12.4		0.8	FEB0067.R13
51000520	33.9		6.63	-10	0.21	9.7	0.06	52	-1	-0.01	-1	4	0.16	10		0.06	80		7.2	-10	31.2	-0.01	-2	42	-10	6.2	21.8		1.0	FEB0067.R13
51000521	4.6		3.33	-10	0.35	16.1	0.06	51	-1	-0.01	-1	3	0.14	15		0.23	63		4.9	-10	55.9	-0.01	-2	18	-10	6.2	9.7		0.7	FEB0067.R13
51000522	4.2		3.45	-10	0.29	13.9	0.08	124	-1	-0.01	-1	-1	0.09	4		0.05	68		5.6	-10	66.1	-0.01	-2	28	-10	6.3	20.7		0.8	FEB0067.R13
51000523	2.3		3.84	-10	0.30	21.6	0.05	51	1	0.01	-1	-1	0.1	14		0.36	144		6.9	-10	49.1	-0.01	-2	25	-10	5.0	13.3		1.0	FEB0067.R13
51000524	7.4		4.78	-10	0.34	14.7	0.07	468	1	-0.01	-1	-1	0.14	14		0.09	232		6.8	-10	45.3	-0.01	-2	37	-10	9.2	31.1		0.9	FEB0067.R13
51000525	6.7		5.93	-10	0.22	15.0	0.05	877	-1	0.01	-1	-1	0.14	14		0.22	131		3.7	-10	52.3	-0.01	-2	24	-10	7.4	29.1		1.0	FEB0067.R13
51000526	21.4		8.13	-10	0.21	32.5	0.12	10000	-1	-0.01	-1	21	0.08	18		0.02	13		5.0	-10	61.0	0.02	-2	24	-10	50.8	412.0		4.0	FEB0067.R13
51000527	5.6		2.81	-10	0.21	19.6	0.05	1223	1	-0.01	-1	2	0.07	12		0.04	22		3.6	-10	30.8	-0.01	-2	10	-10	10.1	33.5		1.3	FEB0067.R13
51000528	10.2		3.96	-10	0.19	15.7	0.04	63	2	-0.01	-1	3	0.05	12		0.1	72		4.8	11	46.5	-0.01	-2	12	-10	5.6	11.3		1.1	FEB0067.R13
51000529	5.5		2.13	-10	0.22	20.1	0.05	32	1	-0.01	-1	2	0.08	21		0.09	39		5.5	-10	42.2	-0.01	-2	8	-10	5.6	5.8		0.9	FEB0067.R13
51000530	3.6		1.02	-10	0.23	20.1	0.05	17	1	-0.01	-1	3	0.08	16		0.04	9		4.3	-10	14.8	-0.01	-2	8	-10	8.8	2.9		1.0	FEB0067.R13
51000531	4.4		1.25	-10	0.19	18.2	0.05	21	2	-0.01	1	2	0.07	16		0.02	8		3.9	-10	15.5	-0.01	-2	12	-10	7.6	4.4		1.1	FEB0067.R13
51000532	5.5		2.81	-10	0.19	13.1	0.05	72	-1	-0.01	-1	-1	0.05	6		0.02	8		3.1	21	10.8	-0.01	-2	16	-10	6.2	26.3		1.1	FEB0067.R13
51000533	5.4		3.47	-10	0.21	14.9	0.05	4661	-1	-0.01	-1	-1	0.05	11		0.02	8		3.4	-10	14.5	-0.01	-2	17	-10	9.1	50.8		1.7	FEB0067.R13
51000534	5.9		3.88	-10	0.17	24.2	0.19	2005	-1	-0.01	-1	5	0.05	16		-0.01	13		6.2	-10	27.7	0.01	-2	40	-10	20.1	50.5		1.5	FEB0067.R13
51000535	5.8		4.29	-10	0.36	18.3	0.9	980	-1	0.02	-1	3	0.12	12		-0.01	372		3.8	-10	13.9	0.02	-2	40	-10	11.9	82.1		4.4	FEB0067.R13
51000536	5.2		2.42	-10	0.30	19.1	0.05	164	-1	-0.01	-1	-1	0.05	-2		0.1	35		2.5	-10	27.7	-0.01	-2	24	-10	9.6	19.3		1.5	FEB0067.R13

SURILOMA PROJECT GEOCHEMICAL DATA BASE FEBRUARY 2013

16de 16 

SampleID	Cuppm	Cu%	Fe%	Gappm	K%	Lappm	Mg%	Mnppm	Moppm	Na%	Nbppm	Nippm	P%	Pbppm	Pb%	S%	Sbppm	Sb%	Scppm	Snppm	Srppm	Ti%	Tlppm	Vppm	Wppm	Yppm	Znppm	Zn%	Zrppm	BATCH
51000537	8.5		4.65	-10	0.26	9.2	0.02	34	2	-0.01	-1	4	0.05	17		0.09	60		1.9	-10	19.7	-0.01	-2	27	-10	4.2	13.2		1.3	FEB0067.R13
51000538	8.3		2.60	-10	0.42	17.6	0.04	118	2	-0.01	-1	6	0.05	13		0.12	38		4.2	-10	20.6	-0.01	-2	20	-10	8.8	11.3		1.0	FEB0067.R13
51000539	5.6		2.66	-10	0.41	19.7	0.06	2776	-1	-0.01	-1	-1	0.07	7		0.03	16		7.7	11	21.0	-0.01	-2	25	-10	14.2	32.1		1.9	FEB0067.R13
51000540	8.0		4.34	-10	0.35	13.8	0.04	6488	-1	-0.01	-1	-1	0.08	6		0.01	57		4.4	-10	18.3	-0.01	-2	18	-10	14.1	53.8		2.5	FEB0067.R13
51000541	15,700.0	1.57	7.52	-10	0.14	7.1	1.02	348	4	0.05	-1	24	0.08	33		1.44	-5		5.3	-10	65.2	0.08	-2	100	-10	7.1	126.0		8.3	FEB0067.R13
51000542	14.3		3.69	-10	0.31	16.1	0.05	106	1	-0.01	-1	-1	0.05	-2		0.05	78		5.4	-10	17.9	-0.01	-2	19	-10	7.4	14.4		0.7	FEB0067.R13
51000543	27.9		4.81	-10	0.19	16.4	0.03	354	-1	-0.01	-1	4	0.06	194		0.1	316		3.9	-10	20.7	-0.01	-2	18	-10	10.1	63.8		1.4	FEB0067.R13
51000544	8.9		3.49	-10	0.24	14.7	0.05	339	-1	-0.01	-1	-1	0.07	-2		0.02	251		5.5	-10	15.0	-0.01	-2	16	-10	7.6	34.6		1.0	FEB0067.R13
51000545	24.8		5.12	-10	0.17	14.8	0.03	455	-1	-0.01	-1	6	0.09	711		0.08	544		4.1	-10	25.4	-0.01	-2	15	-10	9.1	72.7		1.5	FEB0067.R13
51000546	7.7		4.91	-10	0.20	20.6	0.07	5697	2	-0.01	-1	2	0.09	17		-0.01	77		7.3	11	29.1	-0.01	-2	15	-10	14.1	78.4		2.0	FEB0067.R13
51000547	10.6		4.72	-10	0.27	16.9	0.06	6281	-1	-0.01	2	-1	0.06	14		-0.01	57		5.9	-10	24.6	-0.01	-2	15	-10	10.2	93.7		2.0	FEB0067.R13
51000548	8.8		4.68	-10	0.24	18.3	0.04	664	-1	-0.01	-1	-1	0.09	19		0.03	72		3.4	-10	22.5	-0.01	-2	13	-10	11.2	61.8		1.7	FEB0067.R13
51000549	7.5		4.49	-10	0.27	15.3	0.09	5345	-1	-0.01	2	-1	0.06	14		0.01	59		8.7	-10	31.2	-0.01	-2	34	-10	14.6	86.0		2.3	FEB0067.R13
51000550	15.5		6.86	-10	0.30	7.2	0.05	1506	3	-0.01	-1	-1	0.1	16		0.11	49		3.9	-10	27.5	-0.01	-2	47	-10	8.1	40.0		3.1	FEB0067.R13
51000551	18.9		4.40	-10	0.30	12.2	0.04	249	-1	-0.01	1	4	0.04	-2		0.12	144		3.2	-10	40.4	-0.01	-2	12	-10	7.4	22.0		1.7	FEB0067.R13
51000552	6.6		0.58	-10	-0.01	0.6	-0.01	72	6	-0.01	1	3	-0.01	-2		-0.01	-5		-0.5	25	-0.5	-0.01	-2	-2	-10	-0.5	8.9		0.6	FEB0067.R13
51000553	19.7		4.36	-10	0.27	14.3	0.05	350	2	-0.01	-1	2	0.04	14		0.1	68		3.3	11	28.7	-0.01	-2	16	-10	8.4	24.4		1.5	FEB0067.R13
51000554	7.2		2.14	-10	0.33	11.6	0.06	93	2	-0.01	-1	-1	0.02	13		0.05	40		2.9	-10	19.6	-0.01	-2	16	-10	3.4	13.3		2.1	FEB0067.R13
51000555	8.5		2.89	-10	0.15	8.8	0.03	79	2	-0.01	-1	6	0.05	9		0.17	59		2.6	-10	27.5	-0.01	-2	9	-10	3.7	15.1		1.0	FEB0067.R13
51000556	13.3		4.30	-10	0.22	6.5	0.04	49	1	-0.01	2	8	0.05	-2		0.08	29		2.5	-10	17.9	-0.01	-2	17	-10	3.3	13.2		1.4	FEB0067.R13
51000557	8.4		4.52	-10	0.32	15.1	0.06	18	-1	-0.01	-1	-1	0.05	-2		0.19	25		3.1	-10	31.0	-0.01	-2	20	-10	3.7	8.1		1.4	FEB0067.R13
51000558	4.0		2.90	-10	0.34	16.4	0.1	16	-1	-0.01	2	5	0.06	13		0.11	20		5.3	-10	34.4	-0.01	-2	40	-10	8.6	8.4		2.5	FEB0067.R13
51000559	9.1		6.86	-10	0.20	11.5	0.29	104	-1	-0.01	-1	-1	0.13	7		0.01	28		5.0	-10	21.9	0.02	-2	85	-10	9.7	29.6		2.8	FEB0067.R13
51000560	20.4		13.69	-10	0.23	18.0	0.03	255	27	-0.01	-1	-1	0.27	27		0.29	334		3.7	-10	208.0	-0.01	-2	64	-10	17.3	165.0		1.0	FEB0067.R13
51000561	17.2		12.88	-10	0.23	18.6	0.03	252	25	0.01	1	6	0.27	23		0.3	310		3.7	-10	222.0	-0.01	-2	63	-10	17.0	151.0		1.0	FEB0067.R13
51000562	11.2		7.35	-10	0.26	18.5	0.04	151	27	0.01	-1	5	0.14	14		0.45	172		4.8	11	114.0	-0.01	-2	46	-10	7.4	51.2		1.3	FEB0067.R13
51000563	13.2		9.55	-10	0.35	16.5	0.05	1089	8	-0.01	-1	-1	0.23	12		0.22	108		12.5	-10	64.3	-0.01	-2	49	-10	6.8	44.2		1.2	FEB0067.R13
51000564	17.2		10.07	-10	0.37	6.1	0.12	1641	5	-0.01	-1	5	0.24	22		-0.01	91		14.4	-10	20.9	0.01	-2	100	-10	10.0	55.3		2.5	FEB0067.R13
51000565	20.4		7.77	-10	0.16	14.0	0.11	6417	6	-0.01	-1	2	0.17	18		0.05	66		9.7	-10	28.7	0.03	-2	86	-10	13.9	83.9		2.2	FEB0067.R13
51000566	21.5		8.21	-10	0.17	13.3	0.11	5402	7	-0.01	2	4	0.18	22		0.05	71		10.3	-10	28.0	0.04	-2	90	-10	9.0	86.7		3.1	FEB0067.R13
51000567	19.8		7.24	-10	0.17	12.6	0.18	3583	7	-0.01	1	6	0.17	12		0.05	71		7.7	-10	27.2	0.04	-2	85	-10	8.3	88.4		2.4	FEB0067.R13
51000568	19.1		6.79	-10	0.15	13.3	0.22	2768	6	-0.01	-1	6	0.2	15		0.05	63		7.7	-10	30.5	0.05	-2	85	-10	9.3	81.3		2.0	FEB0067.R13
51000569	20.0		6.43	-10	0.17	12.5	0.25	2465	5	-0.01	2	2	0.21	21		0.05	64		8.2	-10	31.7	0.05	-2	88	-10	8.2	81.8		2.5	FEB0067.R13
51000570	19.4		6.35	-10	0.16	12.5	0.31	2256	4	-0.01	-1	5	0.21	21		0.07	74		8.8	-10	32.1	0.06	-2	88	-10	9.2	90.7		2.1	FEB0067.R13
51000571	13.9		4.81	-10	0.20	14.4	0.12	6338	-1	-0.01	-1	-1	0.1	-2		0.03	191		3.9	-10	41.5	0.01	-2	27	-10	9.3	106.0		1.6	FEB0067.R13
51000572	15.2		3.99	-10	0.17	17.4	0.04	201	-1	-0.01	-1	-1	0.11	328		0.06	421		3.1	-10	76.2	-0.01	-2	10	-10	5.0	26.1		1.0	FEB0067.R13
51000573	6.4		0.57	-10	-0.01	0.6	-0.01	73	6	-0.01	-1	5	-0.01	8		-0.01	-5		-0.5	-10	-0.5	-0.01	-2	-2	-10	-0.5	8.7		0.5	FEB0067.R13
51000574	4.0		3.40	-10	0.39	13.8	0.07	26	-1	-0.01	2	4	0.08	16		0.1	60		5.3	-10	29.1	-0.01	-2	19	-10	4.2	9.2		1.1	FEB0067.R13
51000575	1.1		2.10	-10	0.39	16.1	0.05	41	-1	-0.01	1	-1	0.07	12		0.28	95		6.3	-10	32.2	-0.01	-2	12	-10	3.3	6.2		0.8	FEB0067.R13
51000576	9.0		3.85	-10	0.31	8.2	0.05	34	-1	-0.01	-1	-1	0.06	13		0.12	100		8.0	-10	15.7	-0.01	-2	27	-10	3.5	10.6		1.0	FEB0067.R13
51000577	23.0		4.79	-10	0.30	11.9	0.06	53	-1	-0.01	-1	-1	0.12	10		0.08	55		5.0	-10	20.4	-0.01	-2	44	-10	8.1	35.1		3.3	FEB0067.R13
51000578	8.9		8.33	-10	0.33	13.4	0.06	28	-1	-0.01	-1	-1	0.15	17		0.16	100		3.6	-10	40.8	-0.01	-2	45	-10	5.2	19.7		0.6	FEB0067.R13
51000579	2.7		4.14	-10	0.36	17.2	0.05	14	-1	-0.01	-1	-1	0.1	11		0.34	61		3.2	-10	49.9	-0.01	-2	28	-10	3.3	6.9		-0.5	FEB0067.R13
51000580	8.1		5.42	-10	0.31	19.5	0.11	1764	-1	-0.01	-1	-1	0.13	16		0.15	45		3.7	-10	60.8	-0.01	-2	39	-10	2.6	32.8		1.6	FEB0067.R13
51000581	17.5		4.35	-10	0.23	27.7	0.35	5133	-1	-0.01	1	5	0.06	16		0.05	25		8.7	-10	31.5	0.01	-2	73	-10	30.4	106.0		1.3	FEB0067.R13
51000582	4.6		5.26	-10	0.22	15.2	0.04	114	2	-0.01	-1	-1	0.07	47		0.17	679		2.7	-10	42.8	-0.01	-2	19	-10	5.6	32.4		1.2	FEB0067.R13