REPORT ON THE
2003 TO 2005
EXPLORATION PROGRAM
ON THE NEW POLARIS
MINE SITE
North Western British Columbia
NTS: 104 K 12
Latitude: 58º42’N Longitude: 133º37W
Atlin Mining Division
For:
Canarc Resource Corp.
800-850 West Hastings Street
Vancouver, BC V6C 1E1
By: John McClintock, P.Eng
800-850 West Hastings Street
Vancouver, BC V6C 1E1
October 1, 2006
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Item 2: Table of Contents
| Table of Contents | Page | 2 |
| List of Figures | Page | 3 |
| List of Tables | Page | 3 |
| Appendices | Page | 3 |
Item 3 | Summary | Page | 4 |
Item 4 | Introduction | Page | 5 |
Item 5 | Reliance on Other Experts | Page | 5 |
Item 6 | Property Description and Location | Page | 5 |
Item 7 | Accessibility, Climate, Local Resources, Infrastructure and Physiograph | Page | 10 |
Item 8 | History | Page | 11 |
Item 9 | Geological Setting | Page | 16 |
Item 10 | Deposit Types | Page | 19 |
Item 11 | Mineralization | Page | 20 |
Item 12 | Exploration | Page | 21 |
Item 13 | Diamond Drilling Program | Page | 21 |
Item 14 | Sample Method and Approach | Page | 36 |
Item 15 | Sample Preparation, Analyses and Security | Page | 37 |
Item 16 | Data Verification | Page | 42 |
Item 17 | Adjacent Properties | Page | 43 |
Item 18 | Mineral Processing and Metallurgical Testing | Page | 43 |
Item 19 | Mineral Resource and Reserve Estimate | Page | 45 |
Item 20 | Other Relevant Data and Information | Page | 45 |
Item 21 | Interpretation and Conclusions | Page | 45 |
Item 22 | Recommendations | Page | 45 |
Item 23 | References | Page | 46 |
Item 24 | Date | Page | 47 |
| Certificate of Author | Page | 47 |
| Consent of Author | Page | 49,50 |
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Illustrations
Figure | Title | Scale |
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1 | Property Location Map |
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2 3 | Claim Map Principle Vein Location Map |
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4 | Regional Geology Map |
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5 | Property Geology Map |
| Page | 18 |
6 | Three Dimensional View of Veins |
| Page | 21 |
7 | Collar Locations |
| Page | 31 |
8 | Inclined Section “C” Vein System |
| Page | 32 |
9 | Cross Section line 2000SW |
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10 | Cross Section line 2100SW |
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11 | Cross Section line 5500E |
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| Tables |
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No. | Title |
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1 | List of Claims |
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2 | Summary of Exploration Drilling to 2005 |
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3 | Diamond Drill Holes (1988 to 2005) |
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4 | Assay Composites C vein system |
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No. | Title |
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1 | Drill Sections |
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2 | Metallurgical Results |
| Page | 61 |
3 | Drill Hole Assay results |
| Page | 195 |
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Item 3: Summary
New Polaris (formerly Polaris-Taku) is an early Tertiary mesothermal gold mineralized body located in northwestern British Columbia about 100 kilometres south of Atlin, BC and 60 kilometres northeast of Juneau, Alaska. The nearest roads in the area terminated five miles due south of Atlin and 10 kilometres southeast of Juneau. Access at the present time is by aircraft. A short airstrip for light aircraft exists on the property. The gold property consists of 61 contiguous Crown-granted mineral claims and one modified grid claim covering 2,100 acres. All claims are 100% owned and held by New Polaris Gold Mines Ltd., a wholly owned subsidiary of Canarc Resource Corp. subject to a 15% net profit interest held by Rembrandt Gold Mines Ltd. Canarc can reduce this net profit interest to a 10% net profit.
The deposit is composed of three sets of veins (quartz-carbonate stringers in altered rock), the “A-B” veins northwest striking and southwest dipping, the “Y” veins north striking and dipping steeply east and finally the “C” veins eat-west striking and dipping to the south to southeast at 65º to vertical. The “C” veins appear to hook around to the north and south into the other two sets of veins so that their junctions from an arc. The gold is refractory an occurs dominantly in finally disseminated arsenopyrite grains that mineralize the altered wallrock and stockwork veins. The next most abundant mineral is pyrite, followed by minor stibnite and a trace of sphalerite. The zones of mineralization range from 15 to 250 metres in length and 0.3 to 14 metres in width. The gold values in the veins are remarkable in their continuity and uniformity.
Several consulting groups have estimated a mineral inventory for the property. Gary Giroux of Montgomery Consultants completed the last in 1995 in which he estimated 450,000 tons grading 0.365 oz/ton Au in a probable resource and 2,509,000 tons grading 0.365 oz/ton Au as a possible resource. Under the current guidelines of 43-101, this resource would be categorized as 450,000 tons grading 0.365 oz/ton Au as an indicated resource and 2,509,000 tons grading 0.365 oz/ton Au as an inferred resource. The Author has not done sufficient work to classify the historical estimate as a current mineral resource and the historical estimate should not be relied upon.
Canarc carried out initial phases of infill drilling in 2003 through 2005 with in the “C” vein system. The purpose of this drilling was to better define the continuity and grade of the vein systems prior to committing to a major infill drilling campaign.
The 2003 and 2004 drilling confirmed the continuity of both the “C” vein system and provides support and justification to complete the in-fill drilling of the “C” vein system. The objective of the proposed program is to define the grade and tonnes present in the upper portion of the “C” vein. To this end a program of 20,000 metres of drilling in approximately 65 holes is recommended the cost is estimated at $3.18 million.
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Item 4: Introduction
The Author was commissioned in September 2006 by Bradford J. Cooke, Chairman of Canarc Resource Corp to provide a report summarizing the results of the June 2002 to December 31, 2005 exploration on the New Polaris Property. The report will be used to file a revised Annual Information Report (AIF) as required by the provincial securities regulation. The author is familiar with the project having made site visits to the property in May, June, July and August 2006. In total, the Author has spent 7 days on site. During the time on the Polaris property, the Author inspected the underground workings and confirmed the nature of the mineralization. He examined drill core from the 2003 to 2005 drilling. He compared his observations with that of the drill logs and found no discrepancies. In addition, the author has reviews the drill hole database, drill hole information on sections and plans.
The data from this report is based upon the data and reports provided by Canarc Resource Corp. to the Author as well as observations made while at the New Polaris Property. The main sources are internal files and memos primarily assembled and authored by James Moors PGeo., a summary report on work carried out prior to 2002 by Godfrey Walton PGeo. and a reviewed of data on site as well as examining the sections, level plans and digital databases in Canarc Resource Corp.’s office.
The author has not verified the old resource estimated.
Item 5: Reliance on Other Experts
The metallurgical test work was carried out by RDi of Denver Colorado. RDi is reputable firm and the Author has full confidence in the quality of work, results, conclusions and recommendations.
Item 6: Property Description and Location
The New Polaris (formerly the Polaris-Taku mine) property consisting of a group of 61 contiguous crown grants and one modified grid claim totaling 2,956 acres located 60 miles south of Atlin, BC and 40 miles northeast of Juneau, Alaska. Located at approximately 133º37’W Longitude and 58º42’N Latitude, the deposit lies in close proximity to the “Tulesquah Chief” property of Redcorp on the eastern flank of the
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Tulsequah River Valley (Figure 1).
The claims are 100% owned and held by New Polaris Gold Mines Ltd., a wholly owned subsidiary of Canarc Resource Corp. subject to a 15% net profit interest held by Rembrandt Gold Mines Ltd. which Canarc has the right to reduce to 10%. The claims locations are shown on Figure 2 while Table 1 summarizes the claims shown on Figure 2.
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With the exception of the W.W.1 claim, the claims are crown granted and are kept in good standing through annual tax payments. The W.W.1 is a modified grid claim. The claim has sufficient work filed on it to keep it in good standing until February 4, 2015. The crown granted claims were legally surveyed in 1937. The mineralized areas are shown on Figure 4 and 6, which shows the geology of the property on the mineral showings. Notice of work for the program will be required before work on the property can start. The Polaris No. 1, Silver King No 1, Silver King No. 5, Black Diamond, Lloyd and Ant Fraction crown grants include the surface rights. Surface rights for the remainder of the property lie with the Crown.
Table 1 – List of Claims | ||||||
Claim Name | Lot No. | Folio No. |
| Claim Name | Lot No. | Folio No. |
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Polaris No. 1 | 6109 | 4472 |
| Snow | 3497 | 4545 |
Polaris No. 2 | 6140 | 4223 |
| Snow No. 2 | 3495 | 5088 |
Polaris No. 3 | 6141 | 4223 |
| Snow No. 3 | 3494 | 5495 |
Polaris No. 4 | 3498 | 4545 |
| Snow No. 4 | 3499 | 5495 |
Polaris No. 5 | 6143 | 5223 |
| Snow No. 5 | 6105 | 4472 |
Polaris No. 6 | 6144 | 5223 |
| Snow No. 8 | 6107 | 4472 |
Polaris No. 7 | 6145 | 5223 |
| Snow No. 7 | 3500 | 4472 |
Polaris No. 8 | 6146 | 5223 |
| Snow No. 6 | 6106 | 4472 |
Polaris No. 9 | 6147 | 5223 |
| Snow No. 9 | 6108 | 4472 |
Polaris No. 10 | 6148 | 5290 |
| Black Diamond | 3491 | 4472 |
Polaris No. 11 | 6149 | 5290 |
| Black Diamond No. 3 | 6030 | 4944 |
Polaris No. 12 Fr | 6150 | 5290 |
| Blue Bird No. 1 | 5708 | 4545 |
Polaris No. 13 Fr | 6151 | 5290 |
| Blue Bird No. 2 | 5707 | 4545 |
Polaris No. 14 | 6152 | 5290 |
| Lloyd | 6035 | 5010 |
Polaris No. 15 | 6153 | 5290 |
| Lloyd No. 2 | 6036 | 5010 |
Silver King No. 1 | 5489 | 4804 |
| Rand No. 1 | 6039 | 5010 |
Silver King No. 2 | 5490 | 4804 |
| Rand No. 2 | 6040 | 5010 |
Silver King No. 3 | 5493 | 4804 |
| Minto No. 2 | 6033 | 4944 |
Silver King No. 4 | 5494 | 4804 |
| Minto No. 3 | 6034 | 4944 |
Silver King No. 5 | 5491 | 4804 |
| Jumbo No. 5 | 6031 | 4944 |
Silver King No. 6 | 5492 | 4804 |
| Ready Bullion | 6032 | 4944 |
Silver King No. 7 | 5495 | 4804 |
| Roy | 6042 | 5088 |
Silver King No. 8 | 5717 | 4545 |
| Frances | 6041 | 5010 |
Silver Queen No. 1 | 6026 | 4545 |
| Eve Fraction | 6170 | 5494 |
Silver Queen No. 2 | 6027 | 4545 |
| Eve No. 1 Fraction | 6171 | 5495 |
Silver Queen No. 3 | 6028 | 4944 |
| P.T. Fraction | 3493 | 5495 |
Silver Queen No. 4 | 6029 | 4944 |
| Ant Fraction | 3492 | 5088 |
Silver Strand No. 1 | 6037 | 5010 |
| Atlin Fraction | 3496 | 5088 |
Silver Strand No. 2 | 6038 | 5010 |
| Powder Fraction | 6043 | 5088 |
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F.M. Fraction | 6044 | 5088 |
| Jay Fraction | 6045 | 5088 |
Par Fraction | 6154 | 5290 |
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W.W.1 Tenure No. 353540 Issue date February 4, 1997. Expiry date: February 4, 2015.
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The location of the known mineralization relative to the outside boundary of the property is shown on Figure 3.
Mining of the AB Vein system and to a lesser extent on the Y and C veins was carried out during the 1930s to early 1950s. Much of the former infrastructure has been reclaimed. A $200,000 reclamation bond is in place and it is the writer’s opinion that this
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adequately covers the cost of reclaiming the original mill site, and infrastructure. At this time there is no legal or regulatory requirement to remove or treat the tailings on the property. It is recommended that sampling of the tailings and water be carried out to determine if there acid water or contaminants draining from the tailings and mine workings as well as sampling of water down stream from the site to determine if drainage form the tailings and waste rock is affecting the water quality of Whitewater Creek or the Tulsequah River. If there is contamination of the waters down stream from the waste dumps and tailings a mitigation plan will be required. The cost of the mitigation will depend upon the level of contamination of the water down stream.
Prior to commencing exploration on the property a Notice of Work is required to be submitted to the Mining and Minerals Department of the BC Energy and Mines. Work can only commence once approval has been received.
Item 7: Accessibility, Climate, Local Resources, Infrastructure and Physiography
The New Polaris project area lies on the eastern flank of the steep, rugged, Coast Range Mountains. Relief is extreme with elevations ranging from the sea level to 2,600 metres.
Extensive recent glaciation was the dominant factor in topographic development. The Taku and Tulsequah Rivers are the most prominent topographic feature of broad valley bounded by steep mountains. Numerous tributary streams flow from valleys filled with glaciers. The majority of the glaciers are fingers branching from the extensive Muir ice cap, lying to the northwest of the Taku River. The Tulsequah glacier, which terminates in the Tulsequah valley about 16 kilometres north of the New Polaris mine site, is one of the largest glaciers in the immediate area. It forms a dam causing a large lake in a tributary valley that breaks through the ice barrier (Jakülhlaup) during the spring thaw every year, flooding the Tulsequah and Taku valleys below for three to five days.
Small aircraft provides access from Atlin or Juneau. Ocean-going barges have been used in the past to access the site when heavier equipment is required. Redfern has applied to complete a road to their project site, which could change the infrastructure to the site. The property can be operated year round, however access would be difficult during break up and freeze up.
The climate is one of heavy rainfalls during the last summer and fall months, and comparatively heavy snowfall, interspersed with rain during the winter. The annual precipitation is approximately 1.5 metres of which 0.7 metres occur as rainfall. The snow seldom accumulates to a depth greater than 1.5 metres on the level. Winter temperatures are not severe and rarely fall below –15ºC. Summer temperatures, in July, average 10ºC with daytime temperatures reaching the high 20’s on occasion. The vegetation is typical of northern temperature rain forest, consisting primarily of fir, hemlock, spruce and cedar forest on the hillsides and aspen and alder groves in the river valley.
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Item 8: History
From 1923 to 1925 the Big Bull and Tulsequah Chief properties were discovered along the east side of the Tulsequah River and opened up the Taku River district. In 1930, Noah A. Timmins Corporation optioned some of the claims that make up the New Polaris property and conducted trenching and diamond drilling in 1931. The trenching exposed a number of veins of which 10 showed promising grades. A short exploration adit (about 30 feet long) was also driven into the side of the hill and Timmins drilled 19 holes for a total of 5297 feet but was unable to correlate the intersections and elected to drop the option in September 1932.
The Alaska Juneau Gold Mining Company then optioned the property and conducted underground exploration from the “AJ” (Alaska Juneau) adit. Alaska Juneau drove a total of 625 feet of drifting and, although they intersected “ore grade” mineralization, they too had problems with correlation and dropped the property in the fall of 1934.
H. Townsend and M.H. Gidel of the Anaconda Corporation examined the property in 1934 carefully mapping the showings. They came to the conclusion that commercial ore bodies existed even though these showed irregularity due to faulting. Samples were sent to Geo G Griswold in Butte, Montana, who obtained gold recoveries from flotation tests in the order of 88%.
D.C. Sharpstone then secured an option on the property on behalf of Edward C. Congdon and Associates of Duluth, Minnesota. Congdon conducted 775 feet of underground exploration in the “AJ” tunnel and collared 85 feet into the Canyon adit. The Polaris-Taku Mining Company was then incorporated in 1936 to take over the property from Congdon. Polaris-Taku erected a 150-ton per day flotation mill in 1937 and mined underground continuously until it was closed down in April 1942 due to labour restrictions brought on the Second World War. Mining operations resumed in April 1946 and continued until 1951 when the mine was closed due to high operating costs, a fixed gold price and the sinking of a concentrate barge shipment during a storm in March 1951. Up to this date, 231,604 oz of gold was produced at a recovered grade of 0.3opt.
An Edwards Roaster and a cyanide plant to produce bullion were installed and tested in 1949 in order to improve recovery and reduce shipping cost of concentrates to the Tacoma smelter. The addition of the roasted helped improve milling economics, but its capacity was somewhat limited as it could treat only about 45% of the concentrates produced from the flotation plant. After closure, the mill was leased to Tulsequah Mines Ltd. (owned by Cominco) who modified it to process 600 TPD of massive sulphide polymetallic ore (containing gold, silver, copper, lead and zinc) from the Tulsequah Chief and Big Bull Mines. Tulsequah Mines Ltd. used the mill from 1953 to 1957.
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Numalake Mines acquired the property in 1953, changed their name to New Taku Mines Ltd and undertook rehabilitation work of the mine’s plant. A negative feasibility study in 1973 halted this work. New Taku changed its name to Rembrandt Gold Mines Ltd. in 1974. The property lay idle until Suntac Minerals Corp. optioned the property in 1988 and started surface exploration. Canarc merged with Suntac in 1992 and acquired a 100% interest from Rembrandt in 1994 subject to a 15% net profit interest, which Canarc can reduce to 10%. Canarc’s subsidiary, New Polaris Gold Mines Ltd. (formerly Golden Angus Mines Ltd.), currently operates the property.
Exploration restarted on the Polaris Taku property in 1988. During the period 1988 to the end of 2005, a total of 162,163 feet in 220 holes were drilled on the AB, C and Y vein systems. Individual annual footages are provided in Table 2.
Table 2
Summary of Exploration Drilling to 2006
Year | Zone | No. of Holes | Footage |
1988 | Y vein | 8 | 3373 |
1989 | Y vein | 19 | 13378 |
1990 | C vein | 10 | 9391 |
1991 | Y & C veins | 11 | 10934 |
1992 | Y& C veins | 23 | 20924 |
1993 | C vein | 8 | 4270 |
1994 | C & Y veins, North Zone | 30 | 17176 |
1995 | North Zone | 20 | 24934 |
1996 | Underground | 24 | 10514 |
1997 | Underground | 49 | 29098 |
1998 | No drilling | 0 | 0 |
1999 | No drilling | 0 | 0 |
2000 | No Drilling | 0 | 0 |
2001 | No drilling | 0 | 0 |
2002 | No drilling | 0 | 0 |
2003 | C & AB veins | 3 | 5021 |
2004 | C vein | 7 | 5417 |
2005 | C vein | 8 | 7733 |
Total |
| 220 | 162,163 |
A general distribution of this drilling can be seen in figure 6. Initial efforts were confined to the lower elevations of the property due to limited availability of road building equipment and were designed to test the "Y" Vein system either down dip or along strike
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from old workings. Discovery of the "C" Vein system in 1989 resulted in a refocusing of efforts towards defining this Zone. Drilling during 1994 and 1995 has been designed to test the North Zone and the downward continuity of the "C" Zone. Drilling on the North Zone cut low grade gold mineralization in a gently dipping shear zone. Drilling at 200 foot centres showed the mineralization to be of limited extent and bounded down dip by a post mineralization fault. No additional drilling of the North Zone is warranted.
Diamond drilling from underground workings in 1996 was focused from the AJ level and targeted both the AB and Y vein systems. This work showed that the AB system did not continue to depth and appears at its south east end to bend from a south east strike to an easterly strike direction and become part of the C vein system. As there appears to be little potential for significant additional mineralization on the AB vein system, little exploration of the AB vein has been carried out since 1997.
Diamond drilling from underground workings in 1997, was focused from the AJ, Polaris and 150 levels and targeted the AB, Y, and C vein systems. Due to the location of the workings relative to the orientation of the veins, many of the holes were drilled sub parallel to the dip and strike of the veins. For this reason, since 1997 drilling has been carried out from surface to allow holes to test the veins obliquely to strike and dip.
Drilling to the end of 1997 identified the C vein system as having the most potential for extensive gold mineralization with gold grades and thicknesses comparable to that mined in the 1930s to early 1950s. Mineralization was encountered in drill holes over a 250 metre by 300 metre area which remained open to depth. Although the mineralization appears to be continuous between drill holes, the spacing between vein pierce points was too great to give the confidence to calculate a resource. Drilling from 2003 to 2005 focused on closing the drill hole spacing in order to determine the continuity of the grade and thickness of the C vein system.
Drilling to the end of 1997 on the Y vein indicates they are relatively narrow and less continuous along strike than the C veins. Gold grades are comparable to the C vein and these veins have remaining potential for the discovery of additional gold mineralization at depth. Further drilling is required to prove the continuity, gold grades and thicknesses of the veins. The smaller size potential of the Y vein system makes it a second order priority for future drilling.
Since the closure of the Taku Polaris Mine in 1951, several resource calculations have been made with the goal of identifying the probable order of magnitude of "reserves" that may be defined over time. None of these calculations meet the definition requirements of NI 43 – 101 for a resource, have not been verified by the Author and should not be relied upon.
An estimate of Polaris-Taku reserves was made prior to closure in 1951 based on stringent precepts. "Reasonably Assured" ore was projected 25 feet in the plane of the vein above and below sampled drift sections of minable grade while "possible" ore was projected an additional 25 feet beyond these confines (Parliament 1949). These reserves
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were apparently based solely on underground sampling without using underground diamond drill intercepts (WGM 1992). The "remaining reserves" at the time of closure was 105,000 tons grading 0.42 oz/ton including 17% dilution.
Adtec Mining Consultants (1972) recalculated these "reserves" in contemplation of reopening the mine. These were recalculated to be 148,000 tons at 0.29 oz/ton. Based on similar definitions and existing mine drawings and assay plans, Adtec Consultants (1983) recalculated the remaining "reserves" within the mine workings. These were defined to be in the order of 223,000 tons at 0.32 opt gold (diluted) based on a 0.15 oz/t cut-off and a minimum mining width of 4 feet. These reserves were subdivided into 51,000 tons of "assured" and 72,000 tons of "reasonably assured" reserves.
Beacon Hill recalculated these reserves in 1988 for Suntac Minerals Corporation using a minimum mining width of 5 feet (instead of 4 feet) with similar results. Their reserve estimate was "limited to those areas where continuous sampling data was available along drifts, raises and stope backs, etc. and where it appears that minimal development work would be required to access the reserves". Beacon Hill estimated a total probable and possible reserve of 244,420 tons at 0.33 oz. opt gold with 132,210 tons at 0.33 opt gold classed as probable and 112,210 tons at 0.32 opt gold classed as possible.
In 1989, Beacon Hill added further probable and possible mining reserves from 27 new drill holes completed by Suntac. They estimated that the new drilling had increased the reserves by 380,000 tons at 0.39 oz. Au/SDT (probable) and 820,000 tons at 0.39 opt gold (possible) which, added to their previously calculated reserves, brought the overall reserve potential up to 1,450,000 tons at 0.38 opt gold (diluted) above the lowest worked level of the mine (600 level at elev. –462 feet Below Sea level ‘BSL’).
Montgomery Consultants were commissioned to conduct a Geostatistical Study of the Geological Resource for the Polaris-Taku Deposit in 1991. G.H. Giroux carried out this review and calculated a total resource of 2,225,000 tons grading 0.433 opt gold based on a geostatistical approach using a cut-off grade of 0.25 oz/ton. These reserves were divided into 333,000 tons at 0.437 opt gold (probable) and 1,892,000 tons at 0.432 opt gold (possible). The calculation discounted much of the reserves around the old workings and did not include dilution and minimum mining width provisions. These calculations were based on both old and new drilling and extended the resource base down to roughly 1200 feet BSL.
Watts, Griffis,and McQuat were contracted to review the previous reserves in August 1992. Their review incorporated the residual reserves within the mine workings, as calculated by Beacon Hill in 1989, into their overall estimate of a total (diluted) mineral resource of 1,600,000 tons at 0.46 opt gold. Their calculations were based upon a minimum mining width of 5 feet or 15 % dilution and a cut-off grade of 0.25 opt gold. The improvement in grade stems from the inclusion of new deeper holes that extend the known mineralization to a depth of 1200 feet BSL and exclusion of lower grade material previously included in the Montgomery estimate.
Giroux was further contracted to provide reserve updates throughout 1992 and in February 1995 he recalculated the resources for the newly drilled portions of the "C" Zone. Recent drilling has
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also confirmed the existence of a new "North" Zone which, although it appears to be low grade (0. 18 opt gold) has exhibited possible significant widths in the order of 22 feet. Giroux has included calculations for this zone, which for purposes of this review have been excluded due to grade. The results of his recalculation show that the "C" Vein discovered just prior to mine closure represents a significant new addition to the resource base. He has calculated a total of 85,700 tons grading 0.426 opt gold (probable) and 595,000 tons grading 0.425 opt gold (possible) for this zone below the 450 Level (elev. 313 ft BSL) and 1000 feet BSL.
Most of this resource lies above 800 feet BSL and within 200 feet of the existing shaft bottom. The total resources calculated by Giroux to date are summarized on Table 4.2. His calculations were in situ based on a 0.25 oz/ton cut-off and did not include dilution provisions as shown below.
In order to summarize the variety of calculations identified above; Godfrey Walton did the following: Beacon Hill calculation of residual reserves within and around the workings was totaled. To this total, the geostatistical resource calculations of Giroux were added after applying a general dilution factor of 25 % at zero grade to Giroux's figures for the " Y " Zone and 15% at zero grade for the "AB" and "C" Zones. The in-situ resource base is presently estimated as 582,910 tons at 0.359 opt gold (Probable), and 2,614,210 tons at 0.363 opt. gold (Possible) including appropriate dilution factors. The dilution factors were estimated based on vein characteristics. The "Y" Veins are described as being high grade, but narrow which makes them prone to high dilution from over-break during mining as well as over mining. The "AB" veins in-situ grade, as calculated by Giroux, already contains internal dil ution from a parallel dike. To this total, Walton added overall additional dilution of 15 % which he felt was appropriate as the "C" vein would not experience much dilution since it is generally thought to be fairly thick
In the Author’s opinion, the residual reserves in and around the workings included in the Beacon Hill calculation are unlikely to contribute significantly to any new mining operation. For the most part it is in remnants scattered amongst the old stopes and will be difficult to access and develop.
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Item 9: Geological Setting
The geology has been taken from regional report and a number of company reports listed in the bibliography.
Regional
The New Polaris Mine lies on the western edge of a large body of Upper Triassic Stuhini Group volcanic rocks, which has been intruded by a Jurassic-Cretaceous granodiorite body north of the mine. Older Triassic volcanic rocks and earlier sediments underline the Stuhini volcanic rocks. The granodiorite is part of the Coast Plutonic Complex (Figure 3).
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Figure 3 Regional Geology
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The structural trend in the area is northwest-southeast, paralleling major faults and folds to the east and intrusive alignment to the west. The Triassic volcanic rocks and older sedimentary rocks have been folded and sheared with the Stuhini Group rocks being deformed into broad to isoclinal, doubly plunging symmetrical folds with large amplitudes.
Property
Canarc has carried extensive mapping of the Polaris Taku property since the early 1990s. The work has been done by a number of employees and contractors and is shown in figure 5. The gold deposit is hosted within an assemblage of mafic (basalt and andesite units) volcanic rocks altered to greenschist metamorphic facies. The orientation of these units is inconclusive because there are no marker beds in the sequence. It is thought that the units are steeply dipping (70º to 80º) to the north based on the orientation of the limestone/basalt interface at the southern portion of the property.
Figure 4 property Geology
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A serpentinite unit is located to the northeast, which was identified in recent (996/97) drilling and underground mapping. This unit appears to form the eastern extent of the mineralization. The age relationship is unclear, but it is assumed that the serpentinite is a later stage feature possibly associated with tectonism in the area.
The ‘vein’ zones are structurally controlled shear zones and are typified by silicification and carbonitization cross cutting actual quartz-carbonate veins. These zones have sharp contacts with the wall rock and form anastamosing ribbons and dilations. These zones have been deformed several times, which makes original textures difficult to determine. The zones are generally tabular in geometry forming en-echelon sheets within the more competent host lithologies.
All of the strata within the property have been subjected a compression, rotation and subsequent extension. The plunge of folds appears to be variable though generally shallow. Small-scale isoclinal folds strike north-northwesterly and plunge moderately to the north. Numerous faults are found on the property, the more significant of which are discussed later.
The possible extension of the Llewellyn fault, termed the South Llewellyn fault, continues south from the Chief Cross fault along mine grid coordinate 4400 East. Slightly north of Whitewater Creek it is offset to the west by an east-west fault, the 101 fault, to continue in a more southeast orientation of the opposite side of Whitewater Creek. This northwest-southeast orientation structure was named the Limestone Fault due to its bedding parallel attitude within a discontinuous limestone/marble horizon. It marks the southwest boundary of the “mine wedge”; the wedge shaped package of rock within which all past production took place. The northern boundary of the “mine wedge” is further defined as mentioned above by the Whitewater Creek Schist Zone, a zone of schistose chlorite-amphibolite-serpentinite less than 300 feet thick. A complex network of brittle faults is also found within this zone.
Three major faults, Numbers 1 and 5, and an unnamed fault, lie within the mine wedge. The No.1 and No.5 faults strike northwest-southeast, dipping approximately 45º to the northeast, and are sub parallel to the unnamed fault, which dips steeply to the southwest. The No.1 fault has reverse displacement of up to 100 feet while the displacement of the No.5 fault is poorly defined. The southwest dipping, unnamed fault showed no displacement, as it apparently parallels the A-B vein system. The mined0out areas indicate the wedge shape, the predominant orientations and continuity of the zoned, and the overall plunge of the system to the southeast. An early interpretation of the structure showed that various veins appear to meet and form “junction arcs” where both thickness and grade improve.
Item 10: Deposit Types
The exploration target on the New Polaris project is orogenic load gold deposits also known as Mesothermal vein deposits. Numerous examples of this type of deposit are
20
known through out the work including the Cambell Red Lakedeposits in Ontario and the Bralorne deposit in British Columbia. Past exploration studies have demonstrated that the New Polaris vein systems have all of the attributes of the orogenic vein gold deposit including, but not limited to association with major structural break, quartz-carbonate vein association, low-sulphide assemblage of pyrite and arsenopyrite, chloritic and sericitically altered wall rocks and persistent gold mineralization over a vertical distance of nearly 1 km.
Prior mining and exploration have identified the vein systems so the 2003 to 2005 drill program was designed to test the vein systems between earlier drilled, widely spaced holes.
Item 11: Mineralization
Mineralization of the New Polaris deposit bears strong similarities to many Archean Lode gold deposits such as the arsenical gold camp of Red Lake, Ontario where the gold-bearing arsenopyrite is disseminated in the altered rock and in quartz-carbonate stringers.
The vein mineralization consists of arsenopyrite, pyrite, stibnite and gold in a gangue of quartz and carbonates. The sulphide content is up to 10% with arsenopyrite the most abundant and pyrite the next important. Stibnite is fairly abundant in some specimens but overall comprises less then one-tenth of 1% of the vein matter. Alteration minerals include fuchsite, silica, pyrite, sericite carbonate and albite.
In general, the zones of mineralization ranging from 15 to 250 metres in length with widths up to 14 metres appear to have been deposited only on the larger and stronger shears. Their walls pinch and swell showing considerable irregularity both vertically and horizontally. Gold values in the veins should remarkable continuity and uniformity, and are usually directly associated with the amount of arsenopyrite present. The prominent strike directions are north-south and northwest-southeast with weaker control of the vein systems, which is interpreted to be within a major shear zone. Up to 80% of the mine production was from “structural knots” or what is now known as “C” zones. In detail the “C” zones are arcuate structures. Figure 5 shows a 3D view of the “C” vein system.
21
Figure 5 3D Model C Vein
Item 12: Exploration
The exploration program being reported on in the report consisted of 67175.5 metres of core drilling in 23 holes and preliminary metallurgical sampling of vein material from the AB vein system. Results of this work are reported under item 13 and item 18.
Item 13: Diamond Drilling Program
Diamond drill programs have been carried out on the New Polaris Project since the project was reactivated in 1988 (Table 2). Initially, the drilling focused on the down dip and along strike extensions of the Y veins. This work showed that the Y veins, while good grade were narrow and less continuous than the AB vein system. It also showed that the Y vein system is comprised of about 12 separate veins all of which are narrow and of short strike length.
In 1990, drilling shifted to the area beneath the lowest most C vein stopes. This drilling found that the vein system continued to depth and that gold grades in the 0.3 to 0.45 opt
22
range over an average true thickness of 10 feet was present. From 1991 to 1993 most of the drill holes tested the C veins with a lesser number drilled on the Y vein system.
In 1994, the North Zone was discovered and was tested with a total of 30 drill holes during the 1994 and 1995 period. Although thicknesses of the North Zone are up to 22 feet, the grades are overall low (less than 0.2 opt). This combined with the limited extent due to structural termination of the zone by a fault resulted in a decision to terminate exploration of the North Zone.
Encouraging drill results from the C veins and to a lesser extent from the Y vein system lead to further drilling on these two vein systems. Drilling on the C vein showed the veins to be open to depth and to have gold grades that ranged from 0.2 to 0.6 opt over true thicknesses of 10 feet. The increased interest in the C vein systems was due to its greater continuity and thickness compared to the Y vein. The narrow width and lesser continuity of the Y vein system made it a secondary exploration target
In 1996 and 1997 the Y, C and AB veins were explored from underground. The plan was to closely test the upper portions of the Y, C and AB veins in order to allow calculation of a resource that might form the basis for resumption of mining. The results of the underground drilling program were mixed. The underground workings for the most part were driven along the vein structures with few cross cuts from which holes could be drilled to cut the down dip and along strike extension of the veins. As a result, except for those holes that tested the area immediately below the workings, most cut the veins at shallow angles. The very shallow angles that in places approach parallel to the vein make the use of these intersections inappropriate for a resource calculation (An example is hole 97-44 that cut 112 feet grading 0.42 opt). Despite the number of holes drilled during 1996 and 1997, the work did little to expanding the extent of the mineralization in the AB, C or Y vein systems. The work did confirm that the shoots in the lower most stopes on the Y and C veins were open to depth. The tables below summarize the locations of the 1988 to 2005 drilling. Composites of assay results are listed for the C vein system holes that intersected significant mineralization..
| Table 3: Diamond Drill Holes (1988 to 2005) |
| |||
HOLE-ID | Easting (m) | Northing (m) | Length (m) | Dip | Azimuth |
03-P01 | 1569.72 | 1021.08 | 365.46 | -70.0 | 345.0 |
03-P02 | 1513.33 | 1021.08 | 426.72 | -70.0 | 330.0 |
03-P03 | 1591.06 | 1255.78 | 768.71 | -60.0 | 260.0 |
04-1707E1 | 1706.88 | 873.25 | 259.08 | -75.4 | 358.8 |
04-1707E2 | 1707.44 | 873.25 | 280.11 | -83.0 | 359.0 |
04-1737E1 | 1737.63 | 873.16 | 287.43 | -83.0 | 359.0 |
04-1737E2 | 1737.33 | 845.82 | 289.26 | -83.0 | 320.0 |
04-300SW1 | 1842.61 | 902.79 | 224.03 | -66.1 | 320.0 |
04-300SW2 | 1841.57 | 901.60 | 246.89 | -75.0 | 320.0 |
23
04-300SW3 | 1842.70 | 902.73 | 248.41 | -83.0 | 320.0 |
04-330SW1 | 1785.71 | 922.54 | 213.06 | -81.7 | 323.8 |
04-330SW2 | 1789.62 | 904.06 | 237.44 | -83.8 | 324.0 |
04-360SW1 | 1777.39 | 884.53 | 237.44 | -75.0 | 318.5 |
04-360SW2 | 1777.39 | 884.53 | 243.84 | -83.0 | 318.0 |
05-1676E1 | 1676.40 | 872.49 | 210.92 | -71.0 | 359.0 |
05-1676E2 | 1676.40 | 872.49 | 240.49 | -78.0 | 359.0 |
05-1676E3 | 1676.40 | 872.49 | 94.49 | -83.0 | 359.0 |
05-300SW4 | 1875.64 | 860.29 | 289.86 | -77.5 | 322.0 |
05-300SW5 | 1877.20 | 858.36 | 315.16 | -85.0 | 318.0 |
05-300SW6 | 1911.06 | 816.86 | 347.17 | -84.5 | 320.0 |
05-330SW3 | 1835.64 | 860.95 | 277.98 | -77.0 | 320.0 |
05-330SW4 | 1835.69 | 860.88 | 298.40 | -83.0 | 320.0 |
05-330SW5 | 1853.22 | 839.92 | 315.16 | -83.0 | 320.0 |
L52 | 1465.17 | 1330.15 | 248.41 | -25.0 | 85.0 |
L55 | 1510.89 | 1361.54 | 274.32 | -17.0 | 40.0 |
L56 | 1498.70 | 1313.69 | 161.85 | -25.0 | 92.0 |
L57 | 1464.26 | 1330.45 | 215.49 | -25.0 | 51.0 |
L58 | 1473.40 | 1278.79 | 189.28 | -25.0 | 112.0 |
L59 | 1477.67 | 1279.25 | 343.20 | -25.0 | 95.0 |
L62 | 1463.04 | 1233.83 | 306.32 | -25.0 | 149.0 |
L84 | 1342.64 | 1237.79 | 229.21 | -2.5 | 247.5 |
P-9612 | 1289.97 | 1259.92 | 174.65 | -35.0 | 119.0 |
P8918A | 1819.79 | 889.97 | 367.89 | -70.0 | 315.0 |
P91C01 | 1888.57 | 762.30 | 322.17 | -65.0 | 338.0 |
P91C02 | 1888.57 | 762.30 | 331.62 | -77.0 | 338.0 |
P91C03 | 1937.98 | 805.62 | 320.04 | -75.0 | 339.0 |
P91C04 | 1937.98 | 805.62 | 324.92 | -87.0 | 339.0 |
P91C05 | 1827.28 | 942.78 | 199.19 | -73.0 | 339.0 |
P91C06 | 1672.83 | 818.27 | 263.96 | -71.0 | 339.0 |
P91C07 | 1907.53 | 704.18 | 320.65 | -75.0 | 335.0 |
P91Y01 | 1767.03 | 1369.25 | 330.10 | -66.0 | 270.0 |
P91Y02 | 1769.59 | 1336.46 | 305.10 | -64.0 | 266.0 |
P91Y03 | 1705.02 | 1095.33 | 274.93 | -49.0 | 268.0 |
P91Y04B | 1845.38 | 1336.03 | 444.09 | -68.0 | 274.0 |
P92C08 | 1810.12 | 984.99 | 199.03 | -71.0 | 342.0 |
P92C09 | 1889.24 | 964.20 | 210.31 | -72.0 | 340.0 |
P92C10 | 1917.31 | 894.37 | 243.84 | -76.5 | 340.0 |
P92C11 | 1978.82 | 925.86 | 251.16 | -71.5 | 337.0 |
P92C12 | 1870.25 | 819.00 | 282.55 | -71.5 | 337.0 |
P92C13 | 1635.16 | 860.39 | 223.72 | -70.0 | 345.0 |
P92C14 | 1614.98 | 823.90 | 262.13 | -70.0 | 343.0 |
P92C15 | 1702.92 | 823.57 | 258.17 | -71.5 | 338.0 |
P92C16 | 1816.00 | 780.29 | 254.20 | -71.5 | 338.0 |
P92C17 | 1730.41 | 865.11 | 264.26 | -76.0 | 339.0 |
P92C18 | 1606.63 | 792.60 | 350.22 | -70.0 | 337.0 |
P92C19 | 1694.87 | 761.73 | 381.30 | -70.0 | 350.0 |
P92C20 | 1549.57 | 832.74 | 267.31 | -70.0 | 350.0 |
24
P92C20A | 1549.57 | 832.74 | 273.71 | -70.0 | 350.0 |
P92C21 | 1534.49 | 871.36 | 213.97 | -71.0 | 358.0 |
P92C22 | 1624.58 | 743.71 | 413.61 | -71.0 | 336.0 |
P92C23 | 1518.98 | 873.06 | 274.62 | -72.0 | 337.0 |
P92C24 | 1798.02 | 918.21 | 149.66 | -61.0 | 331.0 |
P92Y05 | 1769.67 | 1335.82 | 346.56 | -70.0 | 259.0 |
P92Y08 | 1787.35 | 1367.03 | 326.96 | -67.0 | 274.0 |
P92Y09 | 1745.28 | 1336.55 | 248.11 | -61.0 | 269.0 |
P93C25 | 1737.36 | 911.35 | 102.41 | -65.5 | 340.0 |
P93C26 | 1858.98 | 1036.32 | 144.17 | -70.0 | 295.0 |
P93C27 | 1860.13 | 1034.89 | 166.73 | -85.0 | 295.0 |
P93C28 | 1882.41 | 1050.04 | 165.51 | -75.0 | 310.0 |
P93C29 | 1906.65 | 1088.81 | 179.83 | -75.0 | 280.0 |
P93C30 | 1928.77 | 1144.68 | 168.25 | -75.0 | 280.0 |
P93C31 | 1815.61 | 901.17 | 215.49 | -74.0 | 335.0 |
P94C32 | 1908.04 | 962.37 | 249.02 | -72.0 | 303.0 |
P94C33 | 1908.37 | 961.28 | 279.81 | -86.0 | 284.0 |
P94C34 | 1937.31 | 1015.90 | 258.17 | -72.0 | 287.0 |
P94C35 | 1937.31 | 1015.90 | 339.55 | -83.0 | 288.0 |
P94C36 | 1957.12 | 891.54 | 371.86 | -80.0 | 288.0 |
P94C37 | 1883.66 | 789.74 | 279.50 | -74.0 | 327.0 |
P94C38 | 1699.87 | 806.20 | 287.73 | -82.0 | 348.0 |
P94C39 | 1769.36 | 768.10 | 290.17 | -77.0 | 351.0 |
P94N01 | 1469.75 | 2124.76 | 84.73 | -55.0 | 85.0 |
P94N02 | 1469.75 | 2124.76 | 84.73 | -85.0 | 85.0 |
P94N03 | 1488.95 | 2194.26 | 60.35 | -55.0 | 85.0 |
P94N04 | 1488.95 | 2194.26 | 106.07 | -90.0 | 0.0 |
P94N05 | 1495.96 | 2258.26 | 118.26 | -56.0 | 85.0 |
P94N06 | 1495.96 | 2258.26 | 124.36 | -87.0 | 85.0 |
P94N07 | 1488.34 | 2332.63 | 224.94 | -55.0 | 85.0 |
P94N08 | 1488.34 | 2332.63 | 273.71 | -85.0 | 85.0 |
P94N09 | 1490.17 | 2438.10 | 264.57 | -50.0 | 70.0 |
P94N10 | 1481.33 | 2438.10 | 96.93 | -85.0 | 70.0 |
P94N11 | 1492.30 | 2499.36 | 75.59 | -50.0 | 70.0 |
P94N12 | 1492.30 | 2499.36 | 71.02 | -85.0 | 70.0 |
P94N13 | 1482.85 | 2384.76 | 66.45 | -50.0 | 70.0 |
P94N14 | 1482.85 | 2384.76 | 66.45 | -85.0 | 70.0 |
P94N15 | 1187.20 | 1822.70 | 51.21 | -60.0 | 70.0 |
P94N16 | 1187.20 | 1822.70 | 57.30 | -60.0 | 100.0 |
P94Y10 | 1663.90 | 1203.96 | 236.83 | -63.0 | 266.0 |
P94Y11 | 1813.56 | 1280.16 | 251.76 | -55.0 | 270.0 |
P94Y12 | 1813.56 | 1280.16 | 276.15 | -63.0 | 265.0 |
P94Y13 | 1929.69 | 1191.46 | 371.86 | -62.0 | 265.0 |
P94Y14 | 1929.69 | 1191.46 | 400.81 | -55.0 | 262.0 |
P95C40 | 1965.96 | 575.77 | 786.69 | -82.5 | 355.0 |
P95C41 | 2029.97 | 553.21 | 769.01 | -80.0 | 360.0 |
P95C42 | 1861.72 | 571.50 | 673.00 | -77.5 | 0.0 |
P95C43 | 1861.72 | 571.50 | 751.94 | -80.0 | 340.0 |
25
P95C44 | 1920.24 | 525.78 | 792.48 | -83.0 | 340.0 |
P95N17 | 1347.22 | 2122.93 | 264.57 | -69.5 | 85.0 |
P95N18 | 1370.69 | 2183.89 | 270.66 | -72.0 | 85.0 |
P95N19 | 1350.26 | 2243.33 | 315.47 | -68.0 | 85.0 |
P95N20 | 1348.74 | 2302.76 | 335.28 | -70.0 | 85.0 |
P95N21 | 1348.13 | 2329.59 | 215.80 | -70.0 | 70.0 |
P95N22 | 1353.92 | 2387.80 | 227.99 | -72.0 | 70.0 |
P95N23 | 1338.07 | 2449.07 | 261.52 | -68.0 | 70.0 |
P95N24 | 1336.24 | 2449.07 | 294.74 | -85.0 | 70.0 |
P95N25 | 1502.66 | 2804.16 | 255.42 | -55.0 | 100.0 |
P95N26 | 1325.88 | 2804.16 | 273.71 | -80.0 | 100.0 |
P95N27 | 1325.88 | 2804.16 | 334.67 | -80.0 | 80.0 |
P9705A | 1055.52 | 1545.03 | 231.34 | -21.0 | 52.0 |
PC25A | 1738.27 | 909.83 | 159.41 | -68.0 | 336.0 |
PC44A | 1920.24 | 525.78 | 749.81 | -83.0 | 340.0 |
PC8801 | 1554.16 | 1178.32 | 106.68 | -50.0 | 310.0 |
PC8802 | 1554.16 | 1178.32 | 38.71 | -90.0 | 0.0 |
PC8803 | 1496.69 | 1146.74 | 133.20 | -60.0 | 310.0 |
PC8804 | 1496.21 | 1141.91 | 119.48 | -60.0 | 280.0 |
PC8805 | 1614.15 | 1363.59 | 149.35 | -45.0 | 271.0 |
PC8806 | 1614.68 | 1363.74 | 189.28 | -60.0 | 270.0 |
PC8807 | 1614.14 | 1364.20 | 180.14 | -48.0 | 290.0 |
PC8808 | 1614.26 | 1365.03 | 110.95 | -48.0 | 310.0 |
PC8901 | 1573.08 | 1149.96 | 142.34 | -90.0 | 0.0 |
PC8902 | 1594.63 | 1088.77 | 128.32 | -86.0 | 275.0 |
PC8903 | 1593.56 | 1088.51 | 167.64 | -55.0 | 265.0 |
PC8904 | 1546.21 | 1068.50 | 50.90 | -52.0 | 90.0 |
PC8904A | 1546.21 | 1068.50 | 230.73 | -52.0 | 90.0 |
PC8905 | 1546.73 | 1039.04 | 167.94 | -60.0 | 90.0 |
PC8906 | 1705.42 | 1363.04 | 220.98 | -55.0 | 268.0 |
PC8907 | 1704.52 | 1363.20 | 236.83 | -70.0 | 290.0 |
PC8908 | 1704.52 | 1363.20 | 243.23 | -50.0 | 290.0 |
PC8909 | 1639.71 | 1341.13 | 185.32 | -45.0 | 270.0 |
PC8910 | 1639.14 | 1341.19 | 126.34 | -59.0 | 270.0 |
PC8911 | 1639.77 | 1342.07 | 187.45 | -53.0 | 310.0 |
PC8912 | 1726.56 | 1440.13 | 307.85 | -45.0 | 270.0 |
PC8913 | 1727.76 | 1440.48 | 244.75 | -60.0 | 270.0 |
PC8914 | 1726.95 | 1439.69 | 253.59 | -56.0 | 256.0 |
PC8915 | 1726.18 | 1163.72 | 413.31 | -65.0 | 270.0 |
PC8916 | 1762.08 | 1377.37 | 233.78 | -55.0 | 270.0 |
PC8917 | 1676.68 | 1157.69 | 171.30 | -45.0 | 270.0 |
PC8918 | 1819.79 | 889.97 | 191.11 | -70.0 | 315.0 |
PC8919 | 1777.26 | 1103.56 | 219.15 | -60.0 | 270.0 |
PC9001 | 1820.17 | 822.27 | 400.51 | -70.0 | 340.0 |
PC9002 | 1838.20 | 767.83 | 388.92 | -70.0 | 340.0 |
PC9003 | 1746.57 | 837.70 | 305.10 | -70.0 | 340.0 |
PC9004 | 1853.47 | 897.63 | 305.71 | -70.0 | 340.0 |
PC9004A | 1853.47 | 897.63 | 108.91 | -70.0 | 340.0 |
26
PC9005 | 1675.88 | 852.91 | 265.48 | -60.0 | 340.0 |
PC9006 | 1762.29 | 792.22 | 404.16 | -70.0 | 340.0 |
PC9007 | 1605.02 | 880.79 | 242.62 | -68.0 | 340.0 |
PC9008 | 1778.45 | 746.71 | 441.05 | -70.0 | 330.0 |
PT23A | 1317.96 | 1244.50 | 206.65 | -32.0 | 195.0 |
PT29A | 1317.96 | 1244.50 | 325.53 | -31.0 | 134.0 |
PT30A | 1317.96 | 1244.50 | 279.81 | -15.0 | 90.0 |
PT31A | 1334.41 | 1456.94 | 406.30 | 0.0 | 20.0 |
PT37B | 1595.05 | 1102.00 | 179.53 | -52.0 | 45.0 |
PT38A | 1595.32 | 1097.49 | 260.30 | -35.0 | 124.0 |
PT9601 | 1444.26 | 1379.06 | 106.07 | -36.0 | 79.0 |
PT9602 | 1441.21 | 1379.06 | 120.40 | -51.0 | 79.0 |
PT9603 | 1441.22 | 1378.72 | 102.11 | -36.0 | 96.0 |
PT9604 | 1441.22 | 1378.72 | 130.76 | -51.0 | 96.0 |
PT9605 | 1441.09 | 1379.36 | 101.80 | -49.0 | 68.0 |
PT9606 | 1441.33 | 1378.29 | 115.82 | -38.0 | 110.0 |
PT9607 | 1436.92 | 1380.33 | 43.59 | 21.5 | 291.0 |
PT9608 | 1436.92 | 1380.62 | 17.98 | 21.5 | 299.0 |
PT9609 | 1437.02 | 1380.72 | 119.48 | 21.5 | 304.0 |
PT9610 | 1437.02 | 1380.73 | 119.48 | -4.5 | 304.0 |
PT9611 | 1436.91 | 1380.62 | 125.88 | -22.0 | 299.0 |
PT9613 | 1289.76 | 1259.71 | 149.05 | -41.0 | 134.0 |
PT9614 | 1289.43 | 1258.88 | 121.01 | -52.0 | 164.0 |
PT9615 | 1289.76 | 1259.71 | 147.52 | -52.0 | 134.0 |
PT9616 | 1289.97 | 1259.92 | 176.78 | -46.0 | 119.0 |
PT9617 | 1288.85 | 1263.64 | 152.10 | 0.0 | 15.0 |
PT9618 | 1055.52 | 1545.03 | 146.00 | 18.0 | 88.0 |
PT9619 | 1055.52 | 1545.03 | 127.41 | 18.0 | 108.0 |
PT9620 | 1055.52 | 1545.03 | 173.74 | -10.0 | 118.0 |
PT9621 | 1055.52 | 1545.03 | 141.43 | -8.5 | 80.0 |
PT9622 | 1055.52 | 1545.03 | 152.10 | 22.0 | 108.0 |
PT9623 | 1055.52 | 1545.03 | 167.34 | -14.0 | 110.0 |
PT9624 | 1055.52 | 1545.03 | 272.19 | -10.0 | 52.0 |
PT9701 | 1055.52 | 1545.03 | 9.75 | -5.0 | 52.0 |
PT9702 | 1055.52 | 1545.03 | 287.73 | -7.0 | 52.0 |
PT9703 | 1055.52 | 1545.03 | 220.07 | -13.0 | 60.0 |
PT9704 | 1055.52 | 1545.03 | 205.44 | -10.0 | 60.0 |
PT9706 | 1055.52 | 1545.03 | 255.42 | -9.5 | 49.0 |
PT9707 | 1055.52 | 1545.03 | 240.18 | 10.0 | 52.0 |
PT9708 | 1049.12 | 1542.59 | 144.48 | 0.0 | 242.0 |
PT9709 | 1217.37 | 1301.04 | 69.80 | -22.0 | 0.0 |
PT9710 | 1217.98 | 1301.19 | 69.49 | -22.0 | 340.0 |
PT9711 | 1218.90 | 1301.04 | 163.37 | -15.5 | 78.0 |
PT9712 | 1218.90 | 1301.04 | 171.30 | 4.0 | 60.0 |
PT9713 | 1222.10 | 1299.97 | 281.33 | -15.0 | 90.0 |
PT9714 | 1219.20 | 1297.84 | 47.61 | -42.0 | 0.0 |
PT9715 | 1218.90 | 1301.04 | 59.74 | -46.0 | 330.0 |
PT9716 | 1217.07 | 1296.62 | 135.33 | -15.0 | 270.0 |
27
PT9717 | 1217.07 | 1296.62 | 154.84 | -30.0 | 270.0 |
PT9718 | 1217.07 | 1296.62 | 118.26 | -18.0 | 249.0 |
PT9719 | 1290.83 | 1417.62 | 112.47 | -5.0 | 90.0 |
PT9720 | 1290.83 | 1417.62 | 133.81 | -35.0 | 90.0 |
PT9721 | 1290.52 | 1417.62 | 153.92 | -44.0 | 71.0 |
PT9722 | 1289.30 | 1418.23 | 219.15 | -5.0 | 270.0 |
PT9723 | 1317.96 | 1244.50 | 17.98 | -32.0 | 195.0 |
PT9724 | 1317.96 | 1244.50 | 192.94 | -30.0 | 217.0 |
PT9725 | 1317.96 | 1244.50 | 244.14 | -47.0 | 218.0 |
PT9726 | 1317.96 | 1244.50 | 124.66 | -10.0 | 334.0 |
PT9727 | 1317.96 | 1244.50 | 110.34 | -12.0 | 351.0 |
PT9728 | 1317.96 | 1244.50 | 228.60 | -31.0 | 351.0 |
PT9731 | 1334.11 | 1456.94 | 19.20 | 0.0 | 20.0 |
PT9732 | 1594.99 | 1102.89 | 229.51 | -22.0 | 26.5 |
PT9733 | 1594.65 | 1102.28 | 272.49 | -52.0 | 23.5 |
PT9734 | 1595.23 | 1101.76 | 155.14 | -32.0 | 50.0 |
PT9735 | 1594.96 | 1102.83 | 198.73 | -10.0 | 26.0 |
PT9736 | 1594.87 | 1102.95 | 237.13 | -29.0 | 24.0 |
PT9738 | 1595.35 | 1097.49 | 14.33 | -35.0 | 124.0 |
PT9739 | 1594.96 | 1097.43 | 204.52 | -29.0 | 136.0 |
PT9740 | 1594.53 | 1097.25 | 180.75 | -34.0 | 146.0 |
PT9741 | 1594.93 | 1097.74 | 155.14 | -42.0 | 130.0 |
PT9742 | 1593.46 | 1096.88 | 247.65 | -37.0 | 188.0 |
PT9743 | 1592.92 | 1096.85 | 246.58 | -36.0 | 210.0 |
PT9744 | 1594.71 | 1097.40 | 290.17 | -38.0 | 134.0 |
PT9744A | 1594.71 | 1097.40 | 136.55 | -35.5 | 141.5 |
PT9745 | 1593.10 | 1096.85 | 219.46 | -26.0 | 193.0 |
PY06B | 1769.36 | 1406.96 | 295.05 | -60.0 | 273.0 |
PY07A | 1772.11 | 1406.96 | 387.10 | -67.0 | 275.0 |
Table 6 Assay Composites C Vein System |
| ||||
HOLE-ID | FROM | TO | LENGTH Metres | True Width | AU_COMP GPT |
04-1707E1 | 201.93 | 203.03 | 1.10 | C | 10.20 |
04-1707E1 | 209.46 | 213.42 | 3.96 | C | 5.10 |
04-1707E2 | 222.08 | 224.73 | 2.65 | C | 10.10 |
04-1707E2 | 246.64 | 248.72 | 2.07 | C | 11.80 |
04-1737E1 | 184.25 | 190.80 | 7.77 | C | 17.13 |
04-1737E1 | 200.25 | 207.57 | 7.32 | C | 4.00 |
04-1737E1 | 231.19 | 235.37 | 4.18 | C | 13.60 |
04-1737E2 | 233.66 | 233.96 | 0.30 | C | 30.90 |
04-1737E2 | 256.64 | 259.08 | 2.44 | C | 9.20 |
04-300SW1 | 180.75 | 181.72 | 0.98 | C | 11.20 |
04-300SW2 | 181.20 | 181.66 | 0.46 | C | 5.50 |
04-300SW2 | 206.53 | 208.94 | 2.41 | C | 14.80 |
04-300SW3 | 196.38 | 203.61 | 7.22 | C | 7.20 |
04-300SW3 | 223.88 | 230.73 | 6.86 | C | 14.50 |
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04-330SW1 | 167.18 | 168.80 | 1.62 | C | 4.00 |
04-330SW1 | 172.36 | 174.49 | 2.13 | C | 35.30 |
04-330SW2 | 168.86 | 171.60 | 2.74 | C | 5.40 |
04-330SW2 | 194.22 | 202.27 | 8.05 | C | 31.90 |
04-360SW1 | 162.76 | 163.67 | 0.91 | C | 5.10 |
04-360SW1 | 179.10 | 193.43 | 14.33 | C | 11.60 |
04-360SW2 | 191.20 | 195.38 | 4.18 | C | 25.70 |
04-360SW2 | 198.24 | 201.87 | 3.63 | C | 5.20 |
05-1676E1 | 185.62 | 191.20 | 5.58 | C | 12.10 |
05-1676E2 | 210.01 | 213.27 | 3.26 | C | 8.90 |
05-300SW4 | 200.13 | 200.86 | 0.73 | C | 13.40 |
05-300SW4 | 261.34 | 269.05 | 7.71 | C | 17.40 |
05-300SW5 | 215.80 | 218.30 | 2.50 | C | 14.10 |
05-300SW5 | 241.10 | 246.74 | 5.64 | C | 21.60 |
05-300SW6 | 233.54 | 240.79 | 7.25 | C | 16.70 |
05-300SW6 | 260.91 | 266.09 | 5.18 | C | 18.20 |
05-330SW3 | 213.94 | 223.11 | 9.17 | C | 9.90 |
05-330SW4 | 221.89 | 233.00 | 11.89 | C | 19.88 |
05-330SW5 | 230.89 | 246.28 | 15.39 | C | 8.57 |
P8918A | 194.43 | 199.49 | 5.06 | C | 37.70 |
P91C01 | 251.83 | 258.17 | 6.34 | C | 7.80 |
P91C01 | 274.93 | 281.48 | 6.55 | C | 20.20 |
P91C02 | 263.35 | 268.10 | 4.75 | C | 25.70 |
P91C03 | 226.47 | 229.64 | 4.20 | C | 11.46 |
P91C03 | 264.99 | 269.57 | 4.57 | C | 0.70 |
P91C04 | 282.55 | 288.74 | 6.19 | C | 4.80 |
P91C05 | 156.73 | 169.10 | 12.37 | C | 10.30 |
P91C06 | 228.66 | 231.31 | 2.65 | C | 22.40 |
P91C07 | 292.06 | 294.35 | 2.29 | C | 18.80 |
P92C08 | 124.05 | 127.35 | 3.29 | C | 8.90 |
P92C09 | 161.85 | 163.98 | 2.13 | C | 4.20 |
P92C12 | 216.26 | 218.08 | 1.83 | C | 4.20 |
P92C12 | 258.47 | 265.27 | 6.80 | C | 15.20 |
P92C13 | 190.56 | 192.39 | 1.83 | C | 15.00 |
P92C14 | 246.10 | 248.69 | 2.59 | C | 6.90 |
P92C15 | 231.77 | 233.17 | 1.40 | C | 4.80 |
P92C15 | 236.89 | 238.66 | 1.77 | C | 18.70 |
P92C16 | 229.36 | 231.65 | 2.29 | C | 4.20 |
P92C17 | 209.70 | 213.48 | 3.78 | C | 21.80 |
P92C18 | 281.18 | 283.98 | 2.80 | C | 9.20 |
P92C19 | 282.64 | 285.51 | 2.87 | C | 23.80 |
P92C20 | 243.35 | 245.97 | 2.62 | C | 8.90 |
P92C20A | 233.08 | 235.82 | 2.74 | C | 12.50 |
P92C21 | 172.15 | 178.06 | 5.91 | C | 18.70 |
P92C22 | 343.27 | 345.64 | 2.38 | C | 1.90 |
P92C23 | 184.13 | 186.14 | 2.01 | C | 1.60 |
P92C24 | 136.52 | 139.39 | 2.87 | C | 23.70 |
P93C26 | 108.02 | 110.95 | 2.93 | C | 26.60 |
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P93C27 | 148.89 | 151.49 | 2.59 | C | 12.50 |
P93C28 | 140.27 | 142.43 | 2.16 | C | 10.50 |
P93C31 | 184.80 | 186.99 | 2.19 | C | 8.00 |
P94C32 | 167.46 | 168.37 | 0.91 | C | 0.10 |
P94C32 | 213.33 | 215.95 | 2.62 | C | 0.10 |
P94C33 | 266.43 | 269.53 | 3.11 | C | 6.90 |
P94C34 | 176.72 | 180.14 | 3.41 | C | 7.20 |
P94C36 | 261.21 | 262.28 | 1.07 | C | 6.40 |
P94C37 | 255.24 | 261.27 | 6.04 | C | 22.20 |
P94C38 | 255.54 | 257.13 | 1.58 | C | 20.10 |
P94C38 | 274.53 | 279.23 | 4.69 | C | 22.90 |
P94C39 | 262.01 | 266.58 | 4.57 | C | 28.70 |
P95C40 | 493.01 | 498.93 | 5.92 | C | 8.47 |
P95C40 | 727.77 | 735.24 | 7.47 | C | 11.31 |
P95C42 | 456.47 | 457.54 | 1.10 | C | 13.13 |
P95C43 | 482.04 | 484.51 | 2.47 | C | 15.89 |
P95C44 | 586.50 | 589.57 | 3.07 | C | 18.76 |
P95C44 | 640.08 | 641.70 | 1.62 | C | 12.41 |
P95C44 | 692.38 | 694.15 | 1.77 | C | 28.06 |
PC25A | 137.31 | 141.00 | 3.69 | C | 5.60 |
PC44A | 586.40 | 591.22 | 4.78 | C | 16.00 |
PC44A | 726.40 | 730.60 | 4.18 | C | 6.00 |
PC9001 | 206.35 | 213.79 | 7.44 | C | 11.80 |
PC9002 | 277.31 | 279.96 | 2.65 | C | 29.30 |
PC9003 | 215.59 | 222.50 | 6.92 | C | 14.80 |
PC9003 | 227.17 | 232.87 | 5.70 | C | 31.20 |
PC9004 | 221.25 | 225.25 | 3.99 | C | 16.10 |
PC9005 | 189.43 | 190.96 | 1.52 | C | 18.90 |
PC9006 | 253.62 | 257.28 | 3.66 | C | 0.60 |
PC9007 | 160.90 | 162.31 | 1.40 | C | 15.20 |
PC9008 | 300.08 | 301.35 | 1.28 | C | 0.50 |
Poor market conditions after 1997 made financing of the New Polaris Project difficult. Drilling restarted on the property in 2003 with the objective of testing the extent of the C vein mineralization
Godfrey Walton, P. Geo., at the request of Bradford J. Cooke under took a review of the Polaris Project and recommended additional drilling in order to test the continuity of the “C” vein zone mineralization at depth below the lower most mine workings. To this end, limited drill programs were carried in 2003 to 2005. If successful, these programs would lead to the expanded drill program, to allow higher confidence level for the mineral estuation as recommended as a second phase by Walton.
The 2003 to 2005 exploration programs targeted the “C” vein extensions below the existing mine workings. Collar locations for the holes drilled during the 2003 to December 31, 2005 as well as relevant holes from earlier drilling are plotted on Figure 6. Because there are 220 drill holes on the property it is not possible to plot all of these holes in page size format and still be legible. A more complete plan map is presented in
30
Appendix III. this map is in PDF format and can be expanded to see detail using Adobe Acrobat 7 reader. An inclined section showing the pierce points of drill holes and grades of the 2003 to 2005 drilling is presented in figure 7. Cross sections of the C vein to assist the reader in understanding the attitude, grades and thickness of the C vein system are presented in figures 8 through 10.
The results of the 2003 to 2005 drilling of the C vein system confirmed the continuity of gold mineralization and the vein structure between the earlier drilled holes. As can be seen in the sections below, drill results show the “C” vein system to be an arc-like structure oriented east-west in the west swinging to a northeastern strike in the east. The change is strike occurs across the No.1 fault. To the east of the No.1 fault, the vein splays into 2 or more branches. The dip of the vein system is to the south and southeast and has an average dip of about 50º, although east of the No.1 fault the vein appears to flatten and thicken in a simoid-like feature. The exact nature of the apparent flattening of the vein’s dip is not clear and requires additional drilling to be resolved.
The thickness of the C veins varies from just over a foot to a maximum of 50 feet. The thicker parts of the vein occur to the east of the Number 1 Fault where the dip of the vein flattens due to an apparent folding of the vein.
Table 6 lists the core length of the vein material cut in the drill hole. Depending upon the angle of intersection, the true thickness ranges from 100% to about 70%. The average core length thickness of the intersections is approximately 13 feet and the average grade is 0.4 opt gold. The estimated average true thickness of the vein is 10 feet.
All of the holes in this period were drilled from surface and intersected a similar geologic sequence. From the collar, the holes penetrated from 50 to 260 feet of overburden followed by inter layered ash and lapilli tuff, volcanic wacke, and foliated andesite. The C vein system cross cuts the strike of the volcanic and volcaniclastic rocks at steep angles.
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32
Figure 7 Inclined Longitudinal Section
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Figure 8 Section 2000SW |
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Figure 9 Section 2100 SW |
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Figure 10 Section 5500E |
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Item 14: Sample Method and Approach
Sampling of the vein was done by a wire line diamond drills using NQ-size rods. Drill collar locations were surveyed in by total station surveying method. Drilling azimuth and dip were set using a brunton compass and clinometer. Routine down hole measurements of azimuth and dip were not done on the three holes drilled in 2003 and prior. In 2004, three different down hole survey systems were tried before settling on a Reflex system. The Reflex system was also used in 2005. The down hole surveying was operated by the Hytech’s drill crew. This information was entered into a GEMCOM program to plot the location of the collar and the pierce point of the veins.
Core recovery was very good and ranged from the low 90% to nearly 100% and is a fair sampling of the mineralization at the point where the drill hole pierced the vein.
The vein mineralization has well marked contacts with the wall rock. The transition from mineralized to non mineralized rock occurs over a few centimeters. The mineralization consists of at least 3 stages of quartz veining. The initial stage of quartz-ankerite introduced into the structure was accompanied by a pervasive hydrothermal alteration of the immediately surrounding wall rock. Arsenopyrite, pyrite and lesser stibinite were deposited with the alteration. Later stages of quartz-ankerite veining are barren and have the effect of diluting the gold grades in the structure. The sulphide minerals are very fine grained and disseminated in both the wall rock and early quartz and ankerite veins. Free gold is extremely rare and to the end of 2005 had not been recognized in core samples. The majority of the gold occurs in arsenopyrite and to a lesser extent in pyrite and stibnite. Because there is no visible gold and the host sulphides are very fine gra ined and disseminated there is little nugget effect and gold values even over short intervals rarely exceed 1 opt. Out of 4700 samples with greater than .03 opt gold collected from core and the underground workings, only 185 samples had a value greater than 1 opt, the highest being 3.69 opt. For this reason, no cutting of assays has not been done in calculating composites or are there many cases where a composite sample is carried by a single assay.
Determining intervals of core for sampling was done by the geologist during logging of the core. The mineralized vein structures were marked out. Selections of core intervals for sampling were based in the presences of veining and sulphide mineralization particularly arsenopyrite. Within the defined vein structure sample interval ranged from 1 foot to 5 feet. Divisions were based on intensity of mineralization and veining. Sampling of the core for 10s of feet either side of the mineralized vein structures was also done to the point where hydrothermal alteration disappeared. No sampling of core from the unaltered rock was done.
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The core was logged and stored in the camp. Access to be core was only available to the geologists and the core sampler. The core was brought from the drill set up to the logging facility by the geologist at the end of each shift. The core was geologically logged, recoveries calculated and samples marked out in intervals of 0.5 to 1 metre. The core was handed to the sample cutter who cut it with a diamond saw. Each sample was individually wrapped in plastic bags for shipment. The sample intervals were easily identified and correlate well with the drill logs.
Composite assay results for the C vein are provided in Table 4 and assay results for the holes drilled from 2003 through 2005 are listed in Appendix I.
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Item 15: Sample Preparation, Analyses and Security
Core splitting and packaging for shipment was done on site by employees of Canarc. Core was placed in plastic bags sealed with locking ties. Up to 6 samples were packaged in rice bags that were also sealed with locking ties. The rice bags were addressed and shipped to ASL Chemex’s laboratory at 212 Brooksbank North Vancouver. A sample shipment notice was sent separately to ASL to advise it of the quantity, samples numbers and analytical instructions included in the shipment. A paper copy of the same information was included with each shipment.
The samples were shipped from the property via fixed wing aircraft operated by Atlin Air. The sample shipment was received in Atlin by an expeditor from TME Expediting. The expeditor arranged for ground transportation from Atlin to Whitehorse where they were delivered to Air North for shipment to ASL Chemex. ASL Chemex was instructed to notify Canarc in the event that any of the sample bags were missing or if the bags had been opened en route. There were no incidents of tampering with samples.
ALS Chemex laboratories in North America are registered to ISO 9001:2000for the provision of assay and geochemical analytical services by QMI Quality Registrars. In addition, ALS Chemex's main North American laboratory in North Vancouver, BC, Canada, is accredited by the Standards Council of Canada (SCC) for specific tests listed in our Scope of Accreditation No. 579 which is available athttp://palcan.scc.ca/specs/pdf/677_e.pdf. This accreditation is based on international standards(ISO 17025) and involves extensive site audits and ongoing performance evaluations.
Samples received by ASL Chemex were dried, crushed, split, and a thirty gram sub sample taken for assay. Gold content was by fire assay with a gravimetric finish on samples containing greater than 1 gpt. Other elements including arsenic and antimony were analyzed by atomic absorption.
Three types of controls are employed to assure the quality of the assays. Blanks, standards and duplicates are inserted in with the samples sent to the assay laboratory.
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Blanks are simply a texturally and chemically uniform rock which contains no, or an insignificant amount of Au. Blanks are used to test for contamination during the assaying process. Standards are a rock material with a known amount of gold within. These are used to test the laboratory’s accuracy in determining the amount of gold in a given sample. Finally, duplicates are simply a second quantity of a real sample. These are submitted to test the reproducibility of the assay results. The way core is split has the most affect on the reproducibility a sample, especially in heterogeneously mineralized rocks. One of each, a standard, a blank and a duplicate, were submitted with roughly every 20 total samples (including the standard, etc.).
Blanks should return values less than or equal to three times the detection limit of Au for the assaying method reported by the lab (reported as 0.005 ppm or gpt). Chart 1 shows the results of 13 blank analyses. Measurements which fall within the grey shaded area are measurements which fall within three times the detection limit of the average measurement. These samples are considered to contain no contamination. One sample however, does fall outside the acceptable range. Rather than contamination, it is likely the result of a minor ‘nugget effect’ of gold within the blank material. Regardless, the 0.06 gpt measurement, whether it is from contamination or a minor nugget effect, is insignificant and would not affect a resource calculation.
Chart 1 Assay results of the blank used at New Polaris during the 2005 drilling program. Note that the x axis has no units, it is simply to separate the samples.
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Two standards were used and inserted in with the core samples to be assayed, PM 911 and PM 913. The results of both standards and the statistics of each are shown in Charts 2 and 3. For PM 911, 5 measurements fall outside the 95% confidence level, or within two times the accepted standard deviation above or below the accepted value of the standard. In general, the measurements for PM 911 are somewhat lower than the accepted values stated within the datasheet accompanying the standards. This is likely the result of a different lab technician and/or “drift” in the equipment used. The 5 batches of samples which contain the failed SRM samples will have to be re-assayed at some point. All measurements of PM 913 fall within the range.
Chart : Assay results for standard PM 911 from the 2005 drilling program. X axis is simply for separating samples.
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Chart : Assay results for standard PM 913 from the 2005 drilling program. X axis is simply for separating samples.
Results for the analysis of the duplicate assay results are shown in Charts 4 and 5. An gold content plot of samples verses their duplicates (Chart. 4) produces a linear regression line who’s slope is comparable to that of a y = x plot. This is indicating that there is not a systematic bias during either the core splitting process or the assaying itself.
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Figure : Au content of sample verses the duplicate.
Chart 5 shows the relative percent difference the duplicate assay is from the sample the duplicate was made from. In general, the gold assay results from most duplicates within are within 30% the value determined for the sample. This indicates that in general, the core splitting process was in general carried out properly. In other words, either heterogeneously mineralized core was split such that both had an even gold content, or the core was homogeneous. Duplicates which are significantly different could be caused by heterogeneously mineralized core. Close attention must be paid to the core splitting process to minimize this effect.
42
Chart : Relative difference percent difference between samples and duplicates. X axis is simply for separating samples.
In the author’s opinion the sample preparation, security and analytical procedures were adequate.
Item 16: Data Verification
The Author has spent a total of 7 days on the New Polaris project. While on the property, the author examined underground workings to confirm the nature of mineralization, dimensions and extent of the vein system. The writer also viewed a selection core from key holes drilled from the early 1990s to the end of 2005 and compared his observations with those documented in the drill logs. In both the case of the underground workings and the core, the Author found that his observations confirmed that recorded in logs and sections. The Author also confirmed that core had been properly cut and stored.
In addition to the site visit, the Author has reviewed assay sheets and compared these with the database. These were accurately transposed into the database. The core-logging sheets have been compared to the digital logs to check to accuracy. All sampling in the core was carefully laid out using geological parameters. The author discussed procedures with James Moors, P.Geo., who supervised the drilling program and was responsible for all of the work completed at the New Polaris property in the 2003 to 2005 period. The Author is satisfied with the data verification procedures used by Canarc on this project.
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The Author reviewed the quality control instituted. The core logging facility was clean and orderly. The system of check assaying is adequate. The only issue that the Author has with the system is the use of quartered core for the duplicate samples. The sample size difference between the quartered and half core may account in part for the high relative difference between the original sample and the duplicate. In future, resubmission of pulps on a blind basis should be carried to help separate variance cause by analysis from that due to sample size or bias cutting of the core.
The quality control systems in place prior to the 2003 program are poorly documented and seem to follow the norms of that time period. Of particular concerned is the manner in which the collar locations of drill holes were determined. Most of the holes were located using brunton compass and chaining. Also, the down hole surveying was not consistently done. As a result, the exact location of the vein intersections is not as certain as those from the 2003 to 2005 program. Some re drilling of prior holes is required especially where there are discrepancies with respect to the vein location between the recently drilled holes and those drilled in the 1990s.
Item 17: Adjacent Properties
There are no adjacent properties with similar types of vein mineralization.
Item 18: Mineral Processing and Metallurgical Testing
As part of the 2003 to 2005 exploration program a 200kg sample of vein mineralization was collected from a muck pile on the “AJ” mine working level. The mineralization sampled was a single bolder from the AB vein that had been exposed to air for over 40 years. For the following reason this sample may not be representative of the “C” and “Y” vein systems:
·
Although care was taken to remove the oxidized material from the surface of the boulder, there is no guarantee that the oxidation was not present along internal fractures.
·
The sample is of AB material and not from the “C” vein system that is the focus of the current work program.
·
The sample is from a single point in the vein and may not be representative of other parts of the vein systems.
Two metallurgical studies were carried out on the 200kg sample. The initial test by Resource Development Incorporated (RDi) had the primary objective of determining the deportation of gold in various minerals, reconfirm and/or optimize the flotation process conditions and produce a flotation concentrate containing maximum gold recovery and
44
minimum amount of carbonate for bio-oxidation studies. A copy of the RDI work can be found in Appendix II.
A second metallurgical study on the amenability of the concentrate to bio-oxidation was carried out by Mintek on the concentrate produced by RDI. This report is also available in Appendix II.
The RDi study highlighted the following:
·
The composited sample received by RDI assayed 19.41gpt, 2.835% As, 122ppm Sb, 1% S and less than 1.7gpt Ag.
·
The major minerals in the host rock were dolomite (32 to 35%), micalillite (32%), and quartz (23%).
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Only 9% of the gold was free milling and therefore the ore is refractory. Approximately 4.5% of the gold was associated with stibnite and 68% of the gold was associated with arsenopyrite and pyrite. About 20% of the gold is associated with quartz, possibly due to find grained arsenopyrite encapsulated in quartz.
·
Base-case flotation test using potassium anylxanthate (PAX) and methyl isobutt carbonal (MIBC) recovered 83.6% of the gold and 83.5% are arsenic in a concentrate assaying 73.63gpt gold. The concentrate weight recovery was 20.7%
·
Modified flotation test using Na2S in the grind and CuSO4in the flotation along with base-case reagents improved the flotation recovery and concentrate grade to 93.9% to 96.1% and ± 94gpt gold respectively.
·
Cleaner flotation tests indicate that significant amount of carbonates in the concentrate could be rejected in the first cleaner flotation (78.6%) while loosing only 3% of the gold. The carbonate content was reduced from 15% in the rougher concentrate to less and 1% in the first cleaner concentrate. The concentrate weight was also reduced from 18% to 15.27%.
·
A second cleaner did not reject sufficient gangue material, but reduced gold recovery by an additional 5%, therefore only one stage of cleaning is justified.
·
Gravity concentrate did not preferentially upgrade rougher concentrate or recover additional gold from the rougher tailings.
·
Leaching of rougher tailings resulted in 2% additional gold recovery. However it is not economically justified due to high NaCN consumption.
In summary, a flotation process consisting of roughers and one stage of cleaners can produce a concentrate assaying ± 110gpt gold and ± 15.7% arsenic with the weight and gold recoveries of 15.3% and 95.9% respectively. The concentrate will contain less than 1% carbonate.
The bio-oxidation study carried out by Mintek used a 12 kg sample of rougher concentrate obtained from RDi. This work showed that high levels of iron and arsenic extraction were achieved, however, there may be inhibitory substance associated with the concentrate. Further bio-oxidation studies were carried out by Oxidor Corporation who
45
concluded that bio-oxidation of the New Polaris concentrate appears facile and economically attractive. Gold recovery by bio-oxidation was later estimated by RDi to be 92%.
RDi also under took pressure oxidation tests on the sample. This test concluded that the average gold extraction was 98% in 24 hours with NaCN consumption ranging from 0.8 to 1.4 Kg/T. It cocluded that pressure oxidation was more attractive than bio-oxidation.
Item 19: Mineral Resource and Mineral Reserve Estimates
No independent NI 43-101 compliant resource estimate has been calculated for the New Polaris Deposit.
Item 20: Other Relevant Data and Information
No relevant data or information has knowingly been omitted by the author.
Item 21: Interpretation and Conclusions
The drilling programs conducted since 2002 have confirmed the continuity of the “C” vein system and improved the confidence that the mineralized vein systems are continuous between the earlier widely spaced holes. The “C” vein system appears to be the larger and most continuous of the vein systems found to date on the property.
The grades and thickness of the “C” is encouraging and are in the range of other gold producing mines of similar deposit type. However, more drilling is required to confirm the vein continuity and increase the confidence level to the point where a resource can be calculated. Additional geological information is required to better understand the structural complexity of the “C” veins, particularly to the northeast of the No.1 fault.
Metallurgical work confirmed the refractory nature of the mineralization and that up to 96% of the gold can be recovered into concentrate. Bio-oxidation and pressure also yielded positive results with 96 % and 93 % recoveries respectively. The reader is cautioned that the sample used in these tests came from a single boulder and may have contained oxidized material. For these reasons, the sample may not be representative of the mineralization in the “C” vein system.
Item 22: Recommendations
The drilling programs completed from 2003 to 2005 were successful in demonstrating the continuity and grade of the “C” vein system. Therefore, the phase one work program recommended by Walton is completed and his recommended second phase should be undertaken. To this end, it is recommended that 20,000m of infill drilling in the upper
46
portion of the “C” and vein system be carried out in 2006. The plan that would see about 60 holes drilled in order to reduce the drill hole spacing to approximately 30 metres.
The author is of the opinion that 30-metre spacing will allow a resource at the indicated and measured category to be calculated. This calculation will be determined if the grade and tonnage of the mineralization is sufficient to warrant proceeding to a next phase of preliminary economic evaluation of the resource.
Additional metallurgical testing is also recommended for the 2006 program. This testing of the reject material would use drill reject material from the 2006 drilling in order to provide a fresh representative samples. As well as confirmatory flotation testing, the 2006 metallurgical work should investigating improving the concentrate grade.
The estimated cost of the proposed next phase work is as follows:
Metallurgical Testing | $ 30,000 |
Mineral Estimation | $ 50,000 |
Surface Drilling | $ 3,100,000 |
Total | $ 3,180,000 |
Item 23: References
BC Ministry of Mines Annual Reports 1936 to 1953 |
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Beacon Hill Consultants Ltd. | 1989 Suntac Minerals Corporation – Polaris-Taku Atlin, BC. Conceptual Study by RJ Morris, MSc; BM Briggs, P.Eng.: and WR Stokes, P.Eng. | |||||||
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Montgomery Consultants Ltd. | 1991 Geostatistical Study of the Geological Resource contained within the Polaris-Taku Gold Deposit by GH Giroux, P.Eng. | |||||||
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| 1995 Update of Resource Estimate for Polaris-Taku “C” Vein System and NI Vein System by GH Giroux, P.Eng. | |||||||
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McKay D.L. 1996 | Technical and Economic Review of the Polaris-Taku Project | |||||||
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McKay D.L. 1997 | Update Report on the New Polaris Project | |||||||
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Canarc Resource Corp. | News Releases from Canarc Resource Corp. 1996 and 1997 | |||||||
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| New Polaris drill hole database | |||||||
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| New Polaris Gold Mines Ltd. – Technical Overview by David Watkinson, VP Mine Development, May 30, 1997 | |||||||
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Walton, G.J. 2002 | Report on the 1996 and 1997 Exploration program on the New Polaris Mine site, Northwestern British Columbia. | |||||||
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Watts Griffis, McOuat Ltd (1992) A report on the Polaris-Taku Gold project for Canarc Resource Corp.
Item 24: Date
The effective date of this report is May 1, 2006
“John A. McClintock”
John A. McClintock
CERTIFICATE OF AUTHOR
I, John A. McClintock do hereby certify that:
1.
I am currently employed as President by:
Canarc Resource Corp.
Suite 800-850 West Hastings Street
Vancouver, BC
V6C 1E1
48
2.
I graduated with a degree in BSc Hons from the University of British Columbia in 1973.
3.
I am a member in good standing of the Association of Professional Engineers of British Columbia (No. 12078)
4.
I have practiced my profession continuously for over 33 years and have examined and reported on numerous precious metal deposits throughout the world including northern British Columbia and Yukon..
5.
I have read the definition of a “qualified person” set out in National Instrument 43-101 (NI 43-101) and certify that by reason of my education, affiliation with a professional association (as defined in NI 43-101) and past relevant work experience, I fulfill the requirement to be a “qualified person” for the purposes of NI 43-101.
6.
I am responsible for the preparation of the technical report titled “Report on the 2003 to 2005 Exploration Program on the New Polaris Mine Site”, dated October 1, 2006 (the “Technical Report”). The information contained in this Technical Report was obtained from reports provided by Canarc Resource Corp., various public documents and my visits to the property. I have visited the property on several occasions since May 2006, and since that time have spent an accumulative 7 days on site examining under ground workings and drill core.
7.
I have had no prior involvement with the New Polaris Property.
8.
As of the date of this certificate, to the best of the writer’s knowledge, information and belief, this Technical Report contains all scientific and technical information that is required to be disclosed to make the Technical Report not misleading.
9.
I am not independent of Canarc Resource Corp. as defined by National Instrument 43-101 as I am an insider of that corporation.
10.
I have read National Instrument 43-101 and Form 43-101 F 1, and the technical report has been prepared in compliance with that instrument.
Dated this 1st day of October, 2006.
“John A. McClintock, P.Eng”
John A. McClintock, P.Eng.
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Appendix III Assay Results
Table :Assay Results For the 2003 to 2005 New Polaris Drill Programs | |||||||
Hole No. | From | To | Interval | Au (gpt) | Sample No. | AS (ppm) | SB (ppm) |
03-P01 | 0.00 | 22.56 | 22.56 | 0.00 | NE | 0 | 0 |
03-P01 | 22.56 | 23.01 | 0.46 | 0.07 | 20501 | 369 | 49 |
03-P01 | 23.01 | 24.08 | 1.07 | 2.40 | 20502 | 3570 | 74 |
03-P01 | 24.08 | 25.60 | 1.52 | 0.10 | 20503 | 683 | 70 |
03-P01 | 25.60 | 26.49 | 0.88 | 9.57 | 20504 | 9280 | 2680 |
03-P01 | 26.49 | 27.28 | 0.79 | 12.10 | 20505 | 22900 | 283 |
03-P01 | 27.28 | 27.89 | 0.61 | 0.45 | 20506 | 2030 | 40 |
03-P01 | 27.89 | 29.20 | 1.31 | 0.03 | 20507 | 527 | 25 |
03-P01 | 29.20 | 141.67 | 112.47 | 0.00 | NE | 0 | 0 |
03-P01 | 141.67 | 142.07 | 0.40 | 0.00 | 20508 | 44 | 18 |
03-P01 | 142.07 | 142.95 | 0.88 | 0.00 | 20509 | 59 | 13 |
03-P01 | 142.95 | 143.74 | 0.79 | 0.00 | 20510 | 53 | 17 |
03-P01 | 143.74 | 144.48 | 0.73 | 0.00 | 20511 | 38 | 23 |
03-P01 | 144.48 | 158.80 | 14.33 | 0.00 | NE | 0 | 0 |
03-P01 | 158.80 | 159.78 | 0.98 | 0.00 | 20512 | 5 | 9 |
03-P01 | 159.78 | 160.93 | 1.16 | 0.03 | 20513 | 5 | 5 |
03-P01 | 160.93 | 161.94 | 1.01 | 0.00 | 20514 | 5 | 5 |
03-P01 | 161.94 | 174.71 | 12.77 | 0.00 | NE | 0 | 0 |
03-P01 | 174.71 | 175.41 | 0.70 | 0.00 | 20515 | 27 | 12 |
03-P01 | 175.41 | 184.40 | 8.99 | 0.00 | NE | 0 | 0 |
03-P01 | 184.40 | 185.07 | 0.67 | 0.10 | 20516 | 2810 | 34 |
03-P01 | 185.07 | 185.99 | 0.91 | 0.00 | 20517 | 318 | 9 |
03-P01 | 185.99 | 243.54 | 57.55 | 0.00 | NE | 0 | 0 |
03-P01 | 243.54 | 244.42 | 0.88 | 0.00 | 20518 | 69 | 18 |
03-P01 | 244.42 | 245.06 | 0.64 | 0.00 | 20519 | 114 | 12 |
03-P01 | 245.06 | 245.67 | 0.61 | 0.00 | 20520 | 23 | 12 |
03-P01 | 245.67 | 252.65 | 6.98 | 0.00 | NE | 0 | 0 |
03-P01 | 252.65 | 254.20 | 1.55 | 0.00 | 20521 | 26 | 13 |
03-P01 | 254.20 | 255.00 | 0.79 | 0.00 | 20522 | 139 | 13 |
03-P01 | 255.00 | 255.79 | 0.79 | 0.00 | 20523 | 117 | 18 |
03-P01 | 255.79 | 256.85 | 1.07 | 0.00 | 20524 | 14 | 12 |
03-P01 | 256.85 | 257.46 | 0.61 | 0.00 | 20525 | 62 | 14 |
03-P01 | 257.46 | 331.41 | 73.94 | 0.00 | NE | 0 | 0 |
03-P01 | 331.41 | 332.02 | 0.61 | 0.00 | 20526 | 6 | 9 |
03-P01 | 332.02 | 365.46 | 33.44 | 0.00 | NE | 0 | 0 |
03-P02 | 0.00 | 22.86 | 22.86 | 0.00 | NE | 0 | 0 |
03-P02 | 22.86 | 24.02 | 1.16 | 0.00 | 20527 | 66 | 13 |
03-P02 | 24.02 | 32.92 | 8.90 | 0.00 | NE | 0 | 0 |
03-P02 | 32.92 | 33.56 | 0.64 | 0.00 | 20545 | 98 | 29 |
201
03-P02 | 33.56 | 36.09 | 2.53 | 0.00 | NE | 0 | 0 |
03-P02 | 36.09 | 36.58 | 0.49 | 1.06 | 20528 | 664 | 24 |
03-P02 | 36.58 | 38.65 | 2.07 | 0.00 | NE | 0 | 0 |
03-P02 | 38.65 | 39.26 | 0.61 | 0.17 | 20529 | 356 | 29 |
03-P02 | 39.26 | 45.42 | 6.16 | 0.00 | NE | 0 | 0 |
03-P02 | 45.42 | 46.70 | 1.28 | 0.14 | 20530 | 520 | 23 |
03-P02 | 46.70 | 51.82 | 5.12 | 0.00 | NE | 0 | 0 |
03-P02 | 51.82 | 52.64 | 0.82 | 0.00 | 20531 | 78 | 13 |
03-P02 | 52.64 | 53.19 | 0.55 | 0.00 | 20532 | 83 | 19 |
03-P02 | 53.19 | 54.65 | 1.46 | 0.00 | 20533 | 49 | 24 |
03-P02 | 54.65 | 103.78 | 49.13 | 0.00 | NE | 0 | 0 |
03-P02 | 103.78 | 104.70 | 0.91 | 0.00 | 20534 | 176 | 17 |
03-P02 | 104.70 | 105.86 | 1.16 | 1.20 | 20535 | 3480 | 30 |
03-P02 | 105.86 | 107.02 | 1.16 | 6.48 | 20536 | 11600 | 45 |
03-P02 | 107.02 | 107.90 | 0.88 | 0.55 | 20537 | 1960 | 23 |
03-P02 | 107.90 | 108.94 | 1.04 | 9.91 | 20538 | 18300 | 104 |
03-P02 | 108.94 | 109.58 | 0.64 | 0.03 | 20539 | 507 | 42 |
03-P02 | 109.58 | 110.15 | 0.58 | 8.19 | 20540 | 26400 | 146 |
03-P02 | 110.15 | 110.83 | 0.67 | 15.15 | 20541 | 8340 | 10000 |
03-P02 | 110.83 | 111.56 | 0.73 | 27.19 | 20542 | 24600 | 452 |
03-P02 | 111.56 | 112.32 | 0.76 | 0.10 | 20543 | 345 | 110 |
03-P02 | 112.32 | 113.84 | 1.52 | 0.03 | 20544 | 181 | 31 |
03-P02 | 113.84 | 115.70 | 1.86 | 0.00 | NE | 0 | 0 |
03-P02 | 115.70 | 116.77 | 1.07 | 0.00 | 20546 | 287 | 15 |
03-P02 | 116.77 | 135.70 | 18.93 | 0.00 | NE | 0 | 0 |
03-P02 | 135.70 | 136.55 | 0.85 | 0.07 | 20547 | 796 | 18 |
03-P02 | 136.55 | 138.07 | 1.52 | 9.46 | 20548 | 16200 | 19 |
03-P02 | 138.07 | 139.87 | 1.80 | 0.00 | 20549 | 156 | 9 |
03-P02 | 139.87 | 140.82 | 0.94 | 2.13 | 20550 | 1285 | 13 |
03-P02 | 140.82 | 141.88 | 1.07 | 0.00 | 20551 | 215 | 5 |
03-P02 | 141.88 | 192.48 | 50.60 | 0.00 | NE | 0 | 0 |
03-P02 | 192.48 | 194.08 | 1.62 | 0.00 | 20552 | 5 | 5 |
03-P02 | 194.10 | 202.69 | 8.63 | 0.00 | NE | 0 | 0 |
03-P02 | 202.69 | 203.85 | 1.16 | 0.00 | 20553 | 9 | 5 |
03-P02 | 203.85 | 226.77 | 22.92 | 0.00 | NE | 0 | 0 |
03-P02 | 226.77 | 227.87 | 1.10 | 0.00 | 20554 | 44 | 5 |
03-P02 | 227.87 | 228.63 | 0.76 | 0.00 | 20555 | 72 | 5 |
03-P02 | 228.63 | 230.03 | 1.40 | 0.00 | 20556 | 5 | 5 |
03-P02 | 230.03 | 230.95 | 0.91 | 0.00 | 20557 | 5 | 6 |
03-P02 | 230.95 | 232.20 | 1.25 | 0.00 | 20558 | 5 | 6 |
03-P02 | 232.20 | 233.11 | 0.91 | 0.00 | 20559 | 5 | 5 |
03-P02 | 233.11 | 234.60 | 1.49 | 0.00 | 20560 | 8 | 5 |
03-P02 | 234.60 | 245.55 | 10.94 | 0.00 | NE | 0 | 0 |
03-P02 | 245.55 | 247.04 | 1.49 | 0.00 | 20561 | 34 | 7 |
03-P02 | 247.04 | 254.60 | 7.56 | 0.00 | NE | 0 | 0 |
03-P02 | 254.60 | 255.30 | 0.70 | 0.00 | 20562 | 117 | 11 |
03-P02 | 255.30 | 275.60 | 20.30 | 0.00 | NE | 0 | 0 |
202
03-P02 | 275.60 | 276.67 | 1.07 | 0.00 | 20563 | 43 | 48 |
03-P02 | 276.67 | 277.86 | 1.19 | 0.00 | 20564 | 97 | 34 |
03-P02 | 277.86 | 341.07 | 63.22 | 0.00 | NE | 0 | 0 |
03-P02 | 341.07 | 341.86 | 0.79 | 0.03 | 20565 | 1445 | 85 |
03-P02 | 341.86 | 376.61 | 34.75 | 0.00 | NE | 0 | 0 |
03-P02 | 376.61 | 378.04 | 1.43 | 0.00 | 20566 | 15 | 7 |
03-P02 | 378.04 | 412.18 | 34.14 | 0.00 | NE | 0 | 0 |
03-P02 | 412.18 | 412.97 | 0.79 | 0.03 | 20567 | 13 | 5 |
03-P02 | 412.97 | 426.72 | 13.75 | 0.00 | NE | 0 | 0 |
03-P03 | 0.00 | 22.83 | 22.83 | 0.00 | NE | 0 | 0 |
03-P03 | 22.83 | 24.08 | 1.25 | 0.07 | 20568 | 1500 | 28 |
03-P03 | 24.08 | 25.18 | 1.10 | 38.81 | 20569 | 31000 | 68 |
03-P03 | 25.18 | 26.06 | 0.88 | 45.19 | 20570 | 34900 | 82 |
03-P03 | 26.06 | 27.13 | 1.07 | 21.50 | 20571 | 40200 | 68 |
03-P03 | 27.13 | 28.10 | 0.98 | 13.89 | 20572 | 18900 | 78 |
03-P03 | 28.10 | 29.32 | 1.22 | 0.21 | 20573 | 884 | 26 |
03-P03 | 29.32 | 30.18 | 0.85 | 0.72 | 20574 | 1870 | 35 |
03-P03 | 30.18 | 30.78 | 0.61 | 5.42 | 20575 | 7590 | 61 |
03-P03 | 30.78 | 31.39 | 0.61 | 8.67 | 20576 | 5460 | 94 |
03-P03 | 31.39 | 32.19 | 0.79 | 0.07 | 20577 | 270 | 23 |
03-P03 | 32.19 | 33.13 | 0.94 | 0.03 | 20578 | 208 | 18 |
03-P03 | 33.13 | 106.13 | 73.00 | 0.00 | NE | 0 | 0 |
03-P03 | 106.13 | 107.90 | 1.77 | 0.41 | 20579 | 1405 | 27 |
03-P03 | 107.90 | 112.59 | 4.69 | 0.00 | NE | 0 | 0 |
03-P03 | 112.59 | 113.72 | 1.13 | 0.00 | 20580 | 96 | 11 |
03-P03 | 113.72 | 114.45 | 0.73 | 0.00 | 20581 | 53 | 7 |
03-P03 | 114.45 | 115.89 | 1.43 | 0.86 | 20582 | 2990 | 46 |
03-P03 | 115.89 | 117.32 | 1.43 | 0.48 | 20583 | 1005 | 64 |
03-P03 | 117.32 | 184.92 | 67.60 | 0.00 | NE | 0 | 0 |
03-P03 | 184.92 | 185.93 | 1.01 | 0.00 | 20584 | 35 | 15 |
03-P03 | 185.93 | 187.15 | 1.22 | 0.00 | 20585 | 24 | 15 |
03-P03 | 187.15 | 188.03 | 0.88 | 0.00 | 20586 | 73 | 21 |
03-P03 | 188.03 | 204.98 | 16.95 | 0.00 |
| 0 | 0 |
03-P03 | 204.98 | 206.38 | 1.40 | 0.00 | 20587 | 117 | 17 |
03-P03 | 206.38 | 273.19 | 66.81 | 0.00 | NE | 0 | 0 |
03-P03 | 273.19 | 274.44 | 1.25 | 0.00 | 20588 | 245 | 53 |
03-P03 | 274.44 | 275.42 | 0.98 | 0.65 | 20589 | 1125 | 41 |
03-P03 | 275.42 | 300.23 | 24.81 | 0.00 | NE | 0 | 0 |
03-P03 | 300.23 | 300.81 | 0.58 | 0.00 | 20590 | 14 | 5 |
03-P03 | 300.81 | 324.19 | 23.38 | 0.00 | NE | 0 | 0 |
03-P03 | 324.19 | 325.34 | 1.16 | 0.00 | 20591 | 14 | 5 |
03-P03 | 325.34 | 363.96 | 38.62 | 0.00 | NE | 0 | 0 |
03-P03 | 363.96 | 364.88 | 0.91 | 0.00 | 20592 | 35 | 11 |
03-P03 | 364.88 | 365.76 | 0.88 | 0.00 | 20593 | 14 | 9 |
03-P03 | 365.76 | 370.06 | 4.30 | 0.00 | NE | 0 | 0 |
03-P03 | 370.06 | 371.25 | 1.19 | 0.00 | 20594 | 100 | 21 |
03-P03 | 371.25 | 372.04 | 0.79 | 0.93 | 20595 | 2550 | 70 |
203
03-P03 | 372.04 | 373.56 | 1.52 | 0.00 | 20596 | 68 | 28 |
03-P03 | 373.56 | 374.45 | 0.88 | 0.00 | 20597 | 97 | 17 |
03-P03 | 374.45 | 375.67 | 1.22 | 0.00 | 20598 | 33 | 20 |
03-P03 | 375.67 | 402.52 | 26.85 | 0.00 | NE | 0 | 0 |
03-P03 | 402.52 | 403.46 | 0.94 | 0.00 | 20599 | 11 | 10 |
03-P03 | 403.46 | 404.35 | 0.88 | 0.17 | 20600 | 317 | 21 |
03-P03 | 404.35 | 405.14 | 0.79 | 0.03 | 20601 | 375 | 22 |
03-P03 | 405.14 | 406.15 | 1.01 | 0.00 | 20602 | 122 | 23 |
03-P03 | 406.15 | 407.37 | 1.22 | 1.13 | 20603 | 3610 | 50 |
03-P03 | 407.37 | 408.28 | 0.91 | 0.00 | 20604 | 56 | 10 |
03-P03 | 408.28 | 428.21 | 19.93 | 0.00 | NE | 0 | 0 |
03-P03 | 428.21 | 429.19 | 0.98 | 0.00 | 20605 | 77 | 13 |
03-P03 | 429.19 | 430.19 | 1.01 | 0.00 | 20606 | 194 | 19 |
03-P03 | 430.19 | 430.80 | 0.61 | 0.03 | 20607 | 210 | 18 |
03-P03 | 430.80 | 431.72 | 0.91 | 0.00 | 20608 | 43 | 18 |
03-P03 | 431.72 | 443.48 | 11.77 | 0.00 | NE | 0 | 0 |
03-P03 | 443.48 | 444.52 | 1.04 | 0.00 | 20609 | 108 | 33 |
03-P03 | 444.52 | 461.65 | 17.13 | 0.00 | NE | 0 | 0 |
03-P03 | 461.65 | 462.26 | 0.61 | 0.00 | 20610 | 26 | 18 |
03-P03 | 462.26 | 462.90 | 0.64 | 3.91 | 20611 | 12600 | 131 |
03-P03 | 462.90 | 463.91 | 1.01 | 0.03 | 20612 | 80 | 21 |
03-P03 | 463.91 | 465.03 | 1.13 | 0.00 | 20613 | 97 | 45 |
03-P03 | 465.03 | 465.80 | 0.76 | 0.48 | 20614 | 2480 | 73 |
03-P03 | 465.80 | 466.92 | 1.13 | 7.06 | 20615 | 16500 | 181 |
03-P03 | 466.92 | 467.41 | 0.49 | 7.37 | 20616 | 18000 | 1075 |
03-P03 | 467.41 | 468.02 | 0.61 | 0.17 | 20617 | 3250 | 81 |
03-P03 | 468.02 | 468.93 | 0.91 | 0.03 | 20618 | 158 | 21 |
03-P03 | 468.93 | 469.67 | 0.73 | 0.03 | 20619 | 145 | 37 |
03-P03 | 469.67 | 470.09 | 0.43 | 0.10 | 20620 | 180 | 24 |
03-P03 | 470.09 | 471.40 | 1.31 | 0.03 | 20621 | 198 | 30 |
03-P03 | 471.40 | 472.29 | 0.88 | 0.00 | 20622 | 69 | 21 |
03-P03 | 472.29 | 473.81 | 1.52 | 0.27 | 20623 | 865 | 26 |
03-P03 | 473.81 | 475.09 | 1.28 | 0.24 | 20624 | 387 | 20 |
03-P03 | 475.09 | 523.65 | 48.55 | 0.00 | NE | 0 | 0 |
03-P03 | 523.65 | 524.26 | 0.61 | 0.00 | 20625 | 394 | 15 |
03-P03 | 524.26 | 524.71 | 0.46 | 8.30 | 20626 | 12800 | 50 |
03-P03 | 524.71 | 525.17 | 0.46 | 0.10 | 20627 | 1455 | 31 |
03-P03 | 525.17 | 525.63 | 0.46 | 10.18 | 20628 | 11300 | 52 |
03-P03 | 525.63 | 526.24 | 0.61 | 0.00 | 20629 | 114 | 20 |
03-P03 | 526.24 | 535.90 | 9.66 | 0.00 | NE | 0 | 0 |
03-P03 | 535.90 | 536.94 | 1.04 | 0.00 | 20630 | 128 | 17 |
03-P03 | 536.94 | 537.97 | 1.04 | 1.30 | 20631 | 6680 | 87 |
03-P03 | 537.97 | 539.01 | 1.04 | 0.03 | 20632 | 267 | 33 |
03-P03 | 539.01 | 539.89 | 0.88 | 3.87 | 20633 | 11100 | 103 |
03-P03 | 539.89 | 540.81 | 0.91 | 0.00 | 20634 | 87 | 17 |
03-P03 | 540.81 | 547.30 | 6.49 | 0.00 | NE | 0 | 0 |
03-P03 | 547.30 | 548.12 | 0.82 | 0.00 | 20635 | 100 | 14 |
204
03-P03 | 548.12 | 552.66 | 4.54 | 0.00 | NE | 0 | 0 |
03-P03 | 552.66 | 553.27 | 0.61 | 1.10 | 20636 | 2350 | 28 |
03-P03 | 553.27 | 554.40 | 1.13 | 0.07 | 20637 | 859 | 51 |
03-P03 | 554.40 | 555.59 | 1.19 | 0.03 | 20638 | 396 | 127 |
03-P03 | 555.59 | 565.43 | 9.85 | 0.00 | NE | 0 | 0 |
03-P03 | 565.43 | 566.04 | 0.61 | 7.47 | 20639 | 6580 | 2800 |
03-P03 | 566.04 | 573.94 | 7.89 | 0.00 | NE | 0 | 0 |
03-P03 | 573.94 | 574.97 | 1.04 | 0.00 | 20640 | 128 | 95 |
03-P03 | 574.97 | 575.80 | 0.82 | 1.61 | 20641 | 1650 | 10000 |
03-P03 | 575.80 | 577.08 | 1.28 | 5.59 | 20642 | 9520 | 1500 |
03-P03 | 577.08 | 578.60 | 1.52 | 0.93 | 20643 | 954 | 251 |
03-P03 | 578.60 | 579.64 | 1.04 | 0.82 | 20644 | 1315 | 400 |
03-P03 | 579.64 | 580.37 | 0.73 | 2.64 | 20645 | 3580 | 58 |
03-P03 | 580.37 | 606.77 | 26.40 | 0.00 | NE | 0 | 0 |
03-P03 | 606.77 | 607.37 | 0.61 | 3.50 | 20646 | 2880 | 53 |
03-P03 | 607.37 | 616.46 | 9.08 | 0.00 | NE | 0 | 0 |
03-P03 | 616.46 | 617.25 | 0.79 | 4.18 | 20647 | 3490 | 59 |
03-P03 | 617.25 | 625.63 | 8.38 | 0.00 | NE | 0 | 0 |
03-P03 | 625.63 | 626.55 | 0.91 | 0.07 | 20648 | 226 | 27 |
03-P03 | 626.55 | 670.44 | 43.89 | 0.00 | NE | 0 | 0 |
03-P03 | 670.44 | 671.41 | 0.98 | 0.03 | 20649 | 263 | 59 |
03-P03 | 671.41 | 672.11 | 0.70 | 4.56 | 20650 | 9750 | 106 |
03-P03 | 672.11 | 672.79 | 0.67 | 0.10 | 20651 | 350 | 56 |
03-P03 | 672.79 | 673.64 | 0.85 | 0.00 | 20652 | 84 | 40 |
03-P03 | 673.64 | 694.12 | 20.48 | 0.00 | NE | 0 | 0 |
03-P03 | 694.12 | 694.85 | 0.73 | 0.65 | 20653 | 805 | 51 |
03-P03 | 694.85 | 700.83 | 5.97 | 0.00 | NE | 0 | 0 |
03-P03 | 700.83 | 701.44 | 0.61 | 0.65 | 20654 | 1200 | 27 |
03-P03 | 701.44 | 726.73 | 25.30 | 0.00 | NE | 0 | 0 |
03-P03 | 726.73 | 727.89 | 1.16 | 0.00 | 20655 | 38 | 29 |
03-P03 | 727.89 | 729.02 | 1.13 | 0.00 | 20656 | 90 | 83 |
03-P03 | 729.02 | 729.94 | 0.91 | 2.85 | 20657 | 6180 | 1320 |
03-P03 | 729.94 | 730.79 | 0.85 | 1.68 | 20658 | 3500 | 120 |
03-P03 | 730.79 | 731.46 | 0.67 | 0.03 | 20659 | 216 | 72 |
03-P03 | 731.46 | 732.28 | 0.82 | 0.00 | 20660 | 47 | 49 |
03-P03 | 732.28 | 732.92 | 0.64 | 0.00 | 20661 | 31 | 32 |
03-P03 | 732.92 | 733.99 | 1.07 | 0.00 | 20662 | 97 | 41 |
03-P03 | 733.99 | 735.12 | 1.13 | 0.00 | 20663 | 288 | 53 |
03-P03 | 735.12 | 736.06 | 0.94 | 0.00 | 20664 | 139 | 40 |
03-P03 | 736.06 | 740.54 | 4.48 | 0.00 | NE | 0 | 0 |
03-P03 | 740.54 | 741.27 | 0.73 | 0.14 | 20665 | 360 | 44 |
03-P03 | 741.27 | 742.49 | 1.22 | 0.00 | 20666 | 279 | 51 |
03-P03 | 742.49 | 743.01 | 0.52 | 0.00 | 20667 | 137 | 81 |
03-P03 | 743.01 | 743.93 | 0.91 | 0.00 | 20668 | 126 | 37 |
03-P03 | 743.93 | 744.72 | 0.79 | 0.00 | 20669 | 76 | 44 |
03-P03 | 744.72 | 762.27 | 17.56 | 0.00 | NE | 0 | 0 |
03-P03 | 762.27 | 762.61 | 0.34 | 0.00 | 20670 | 382 | 76 |
205
03-P03 | 762.61 | 768.71 | 6.10 | 0.00 | NE | 0 | 0 |
04-1707E1 | 192.69 | 193.70 | 1.01 | 0.14 | 20988 | 0 | 0 |
04-1707E1 | 193.70 | 194.22 | 0.52 | 0.00 | 20989 | 0 | 0 |
04-1707E1 | 194.22 | 194.98 | 0.76 | 0.07 | 20990 | 0 | 0 |
04-1707E1 | 194.98 | 195.96 | 0.98 | 0.07 | 20991 | 0 | 0 |
04-1707E1 | 195.96 | 196.29 | 0.34 | 0.00 | 20992 | 0 | 0 |
04-1707E1 | 196.29 | 196.87 | 0.58 | 0.03 | 20993 | 0 | 0 |
04-1707E1 | 196.87 | 197.02 | 0.15 | 0.00 | 20994 | 0 | 0 |
04-1707E1 | 197.02 | 197.51 | 0.49 | 0.10 | 20995 | 0 | 0 |
04-1707E1 | 197.51 | 198.85 | 1.34 | 0.03 | 20996 | 0 | 0 |
04-1707E1 | 198.85 | 199.19 | 0.34 | 0.10 | 20997 | 0 | 0 |
04-1707E1 | 199.19 | 199.52 | 0.34 | 0.10 | 20998 | 0 | 0 |
04-1707E1 | 199.52 | 200.41 | 0.88 | 0.99 | 20999 | 0.13 | 0.04 |
04-1707E1 | 200.41 | 201.93 | 1.52 | 0.21 | 21000 | 0 | 0 |
04-1707E1 | 201.93 | 202.14 | 0.21 | 6.21 | 109001 | 0.04 | 0.19 |
04-1707E1 | 202.14 | 202.30 | 0.15 | 0.55 | 109002 | 0 | 0 |
04-1707E1 | 202.30 | 203.03 | 0.73 | 13.47 | 109003 | 0.04 | 1.95 |
04-1707E1 | 203.03 | 203.91 | 0.88 | 0.96 | 109004 | 0 | 0 |
04-1707E1 | 203.91 | 205.44 | 1.52 | 0.31 | 109005 | 0 | 0 |
04-1707E1 | 205.44 | 205.98 | 0.55 | 0.10 | 109006 | 0 | 0 |
04-1707E1 | 205.98 | 207.02 | 1.04 | 0.21 | 109007 | 0 | 0 |
04-1707E1 | 207.02 | 208.15 | 1.13 | 0.03 | 109008 | 0 | 0 |
04-1707E1 | 208.15 | 209.46 | 1.31 | 0.03 | 109009 | 0 | 0 |
04-1707E1 | 209.46 | 210.92 | 1.46 | 3.60 | 109010 | 0.01 | 0.44 |
04-1707E1 | 210.92 | 211.90 | 0.98 | 7.95 | 109011 | 0.11 | 0.45 |
04-1707E1 | 211.90 | 213.42 | 1.52 | 4.66 | 109012 | 0.03 | 1.14 |
04-1707E1 | 213.42 | 214.91 | 1.49 | 0.58 | 109013 | 0 | 0 |
04-1707E1 | 214.91 | 216.68 | 1.77 | 0.17 | 109014 | 0 | 0 |
04-1707E1 | 216.68 | 217.90 | 1.22 | 0.00 | 109015 | 0 | 0 |
04-1707E1 | 217.90 | 219.43 | 1.52 | 0.00 | 109016 | 0 | 0 |
04-1707E1 | 219.43 | 220.55 | 1.13 | 0.00 | 109017 | 0 | 0 |
04-1707E1 | 220.55 | 221.68 | 1.13 | 0.03 | 109018 | 0 | 0 |
04-1707E1 | 221.68 | 222.05 | 0.37 | 0.07 | 109019 | 0 | 0 |
04-1707E1 | 222.05 | 222.35 | 0.30 | 0.03 | 109020 | 0 | 0 |
04-1707E1 | 222.35 | 223.72 | 1.37 | 0.00 | 109021 | 0 | 0 |
04-1707E2 | 212.45 | 213.97 | 1.52 | 0.00 | 109023 | 0 | 0 |
04-1707E2 | 213.97 | 215.40 | 1.43 | 0.00 | 109024 | 0 | 0 |
04-1707E2 | 215.40 | 216.99 | 1.58 | 0.00 | 109025 | 0 | 0 |
04-1707E2 | 216.99 | 218.51 | 1.52 | 0.03 | 109026 | 0 | 0 |
04-1707E2 | 218.51 | 220.13 | 1.62 | 0.21 | 109027 | 0 | 0 |
04-1707E2 | 220.13 | 220.98 | 0.85 | 0.17 | 109028 | 0 | 0 |
04-1707E2 | 220.98 | 221.59 | 0.61 | 0.14 | 109029 | 0 | 0 |
04-1707E2 | 221.59 | 222.08 | 0.49 | 0.31 | 109030 | 0 | 0 |
04-1707E2 | 222.08 | 222.20 | 0.12 | 18.62 | 109031 | 1.31 | 0.03 |
04-1707E2 | 222.20 | 223.36 | 1.16 | 12.51 | 109032 | 1.14 | 0.05 |
04-1707E2 | 223.36 | 224.27 | 0.91 | 4.49 | 109033 | 0.95 | 0.01 |
04-1707E2 | 224.27 | 224.73 | 0.46 | 12.75 | 109034 | 1.75 | 0.01 |
206
04-1707E2 | 224.73 | 226.04 | 1.31 | 0.93 | 109035 | 0 | 0 |
04-1707E2 | 226.04 | 226.71 | 0.67 | 0.14 | 109036 | 0 | 0 |
04-1707E2 | 226.71 | 227.69 | 0.98 | 0.17 | 109037 | 0 | 0 |
04-1707E2 | 227.69 | 228.57 | 0.88 | 2.85 | 109038 | 0.91 | 0.01 |
04-1707E2 | 228.57 | 229.39 | 0.82 | 14.57 | 109039 | 1.16 | 0.27 |
04-1707E2 | 229.39 | 230.70 | 1.31 | 0.10 | 109040 | 0 | 0 |
04-1707E2 | 230.70 | 232.23 | 1.52 | 0.07 | 109041 | 0 | 0 |
04-1707E2 | 232.23 | 233.48 | 1.25 | 0.03 | 109042 | 0 | 0 |
04-1707E2 | 233.48 | 234.54 | 1.07 | 0.03 | 109043 | 0 | 0 |
04-1707E2 | 234.54 | 235.15 | 0.61 | 0.03 | 109044 | 0 | 0 |
04-1707E2 | 235.15 | 235.61 | 0.46 | 0.03 | 109045 | 0 | 0 |
04-1707E2 | 235.61 | 236.59 | 0.98 | 0.10 | 109046 | 0 | 0 |
04-1707E2 | 236.59 | 237.59 | 1.01 | 38.64 | 109047 | 3.03 | 0.01 |
04-1707E2 | 237.59 | 239.24 | 1.65 | 0.89 | 109048 | 0 | 0 |
04-1707E2 | 239.24 | 239.85 | 0.61 | 0.14 | 109049 | 0 | 0 |
04-1707E2 | 239.85 | 240.49 | 0.64 | 0.07 | 109050 | 0 | 0 |
04-1707E2 | 240.49 | 241.10 | 0.61 | 0.07 | 109051 | 0 | 0 |
04-1707E2 | 241.10 | 243.84 | 2.74 | 0.07 | 109052 | 0 | 0 |
04-1707E2 | 243.84 | 245.36 | 1.52 | 0.07 | 109053 | 0 | 0 |
04-1707E2 | 245.36 | 246.64 | 1.28 | 0.99 | 109054 | 0 | 0 |
04-1707E2 | 246.64 | 247.16 | 0.52 | 8.16 | 109055 | 0.06 | 0.01 |
04-1707E2 | 247.16 | 247.77 | 0.61 | 0.27 | 109056 | 0 | 0 |
04-1707E2 | 247.77 | 248.35 | 0.58 | 25.82 | 109057 | 0.1 | 0.01 |
04-1707E2 | 248.35 | 248.72 | 0.37 | 13.95 | 109058 | 0.05 | 0.01 |
04-1707E2 | 248.72 | 250.24 | 1.52 | 0.41 | 109059 | 0 | 0 |
04-1707E2 | 250.24 | 251.46 | 1.22 | 0.03 | 109060 | 0 | 0 |
04-1707E2 | 251.46 | 251.92 | 0.46 | 0.10 | 109061 | 0 | 0 |
04-1707E2 | 251.92 | 252.50 | 0.58 | 0.10 | 109062 | 0 | 0 |
04-1707E2 | 252.50 | 253.84 | 1.34 | 0.17 | 109063 | 0 | 0 |
04-1707E2 | 253.84 | 254.11 | 0.27 | 23.52 | 109064 | 0.71 | 1.21 |
04-1707E2 | 254.11 | 255.64 | 1.52 | 1.13 | 109065 | 0.14 | 0.59 |
04-1707E2 | 255.64 | 256.76 | 1.13 | 0.10 | 109066 | 0 | 0 |
04-1707E2 | 256.76 | 258.01 | 1.25 | 0.03 | 109067 | 0 | 0 |
04-1707E2 | 258.01 | 258.62 | 0.61 | 0.03 | 109068 | 0 | 0 |
04-1707E2 | 258.62 | 260.09 | 1.46 | 0.03 | 109069 | 0 | 0 |
04-1707E2 | 260.09 | 260.91 | 0.82 | 0.00 | 109070 | 0 | 0 |
04-1707E2 | 260.91 | 262.43 | 1.52 | 0.00 | 109071 | 0 | 0 |
04-1707E2 | 262.43 | 263.96 | 1.52 | 0.00 | 109072 | 0 | 0 |
04-1707E2 | 263.96 | 264.87 | 0.91 | 0.00 | 109073 | 0 | 0 |
04-1737E1 | 66.75 | 68.28 | 1.52 | 0.00 | 20848 | 0 | 0 |
04-1737E1 | 68.28 | 69.89 | 1.62 | 0.00 | 20849 | 0 | 0 |
04-1737E1 | 69.89 | 71.60 | 1.71 | 0.00 | 20850 | 0 | 0 |
04-1737E1 | 71.60 | 72.97 | 1.37 | 0.00 | 20851 | 0 | 0 |
04-1737E1 | 72.97 | 74.52 | 1.55 | 0.00 | 20852 | 0 | 0 |
04-1737E1 | 74.52 | 75.93 | 1.40 | 0.00 | 20853 | 0 | 0 |
04-1737E1 | 75.93 | 77.42 | 1.49 | 0.34 | 20854 | 0 | 0 |
04-1737E1 | 107.90 | 109.42 | 1.52 | 0.03 | 20856 | 0 | 0 |
207
04-1737E1 | 109.42 | 110.95 | 1.52 | 0.00 | 20857 | 0 | 0 |
04-1737E1 | 110.95 | 112.47 | 1.52 | 0.00 | 20858 | 0 | 0 |
04-1737E1 | 147.98 | 149.50 | 1.52 | 0.00 | 20859 | 0 | 0 |
04-1737E1 | 149.50 | 150.88 | 1.37 | 0.00 | 20860 | 0 | 0 |
04-1737E1 | 150.88 | 151.94 | 1.07 | 0.03 | 20861 | 0 | 0 |
04-1737E1 | 151.94 | 153.01 | 1.07 | 0.00 | 20862 | 0 | 0 |
04-1737E1 | 178.77 | 179.83 | 1.07 | 0.00 | 20864 | 0 | 0 |
04-1737E1 | 179.83 | 181.20 | 1.37 | 0.00 | 20865 | 0 | 0 |
04-1737E1 | 181.20 | 181.97 | 0.76 | 0.00 | 20866 | 0 | 0 |
04-1737E1 | 181.97 | 183.03 | 1.07 | 0.03 | 20867 | 0 | 0 |
04-1737E1 | 183.03 | 184.25 | 1.22 | 20.43 | 20868 | 1.83 | 0.07 |
04-1737E1 | 184.25 | 185.32 | 1.07 | 30.65 | 20869 | 2.99 | 0.02 |
04-1737E1 | 185.32 | 186.54 | 1.22 | 0.07 | 20870 | 0 | 0 |
04-1737E1 | 186.54 | 187.45 | 0.91 | 0.07 | 20871 | 0 | 0 |
04-1737E1 | 187.45 | 188.98 | 1.52 | 18.38 | 20873 | 1.24 | 0.01 |
04-1737E1 | 188.98 | 190.41 | 1.43 | 24.51 | 20874 | 1.71 | 0.22 |
04-1737E1 | 190.41 | 190.80 | 0.40 | 29.14 | 20875 | 1.43 | 0.24 |
04-1737E1 | 190.80 | 192.02 | 1.22 | 4.46 | 20876 | 0.75 | 0.01 |
04-1737E1 | 192.02 | 193.40 | 1.37 | 0.07 | 20877 | 0 | 0 |
04-1737E1 | 193.40 | 194.46 | 1.07 | 0.07 | 20878 | 0 | 0 |
04-1737E1 | 194.46 | 195.38 | 0.91 | 0.03 | 20879 | 0 | 0 |
04-1737E1 | 195.38 | 196.60 | 1.22 | 0.03 | 20880 | 0 | 0 |
04-1737E1 | 196.60 | 198.27 | 1.68 | 0.00 | 20881 | 0 | 0 |
04-1737E1 | 198.27 | 199.34 | 1.07 | 0.00 | 20882 | 0 | 0 |
04-1737E1 | 199.34 | 200.25 | 0.91 | 2.54 | 20883 | 0.4 | 0.01 |
04-1737E1 | 200.25 | 201.47 | 1.22 | 12.48 | 20884 | 1.68 | 0.01 |
04-1737E1 | 201.47 | 202.69 | 1.22 | 2.88 | 20885 | 1.24 | 0.01 |
04-1737E1 | 202.69 | 204.06 | 1.37 | 1.06 | 20886 | 0.47 | 0.01 |
04-1737E1 | 204.06 | 206.04 | 1.98 | 1.20 | 20887 | 0.32 | 0.01 |
04-1737E1 | 206.04 | 207.05 | 1.01 | 4.53 | 20888 | 0.23 | 0.01 |
04-1737E1 | 207.05 | 207.57 | 0.52 | 4.01 | 20889 | 0.01 | 0.01 |
04-1737E1 | 207.57 | 208.18 | 0.61 | 0.03 | 20891 | 0 | 0 |
04-1737E1 | 208.18 | 209.70 | 1.52 | 1.99 | 20892 | 0.19 | 0.01 |
04-1737E1 | 209.70 | 210.92 | 1.22 | 0.03 | 20893 | 0 | 0 |
04-1737E1 | 210.92 | 212.66 | 1.74 | 0.03 | 20894 | 0 | 0 |
04-1737E1 | 212.66 | 213.76 | 1.10 | 0.14 | 20895 | 0 | 0 |
04-1737E1 | 213.76 | 215.59 | 1.83 | 0.07 | 20896 | 0 | 0 |
04-1737E1 | 215.59 | 216.77 | 1.19 | 0.17 | 20897 | 0 | 0 |
04-1737E1 | 216.77 | 218.24 | 1.46 | 0.03 | 20898 | 0 | 0 |
04-1737E1 | 218.24 | 219.64 | 1.40 | 0.03 | 20899 | 0 | 0 |
04-1737E1 | 219.64 | 219.91 | 0.27 | 0.14 | 20900 | 0 | 0 |
04-1737E1 | 219.91 | 221.13 | 1.22 | 0.03 | 20901 | 0 | 0 |
04-1737E1 | 221.13 | 222.87 | 1.74 | 0.03 | 20902 | 0 | 0 |
04-1737E1 | 222.87 | 223.88 | 1.01 | 0.03 | 20903 | 0 | 0 |
04-1737E1 | 223.88 | 224.64 | 0.76 | 0.07 | 20904 | 0 | 0 |
04-1737E1 | 224.64 | 225.55 | 0.91 | 0.07 | 20905 | 0 | 0 |
04-1737E1 | 225.55 | 227.08 | 1.52 | 0.10 | 20906 | 0 | 0 |
208
04-1737E1 | 227.08 | 227.53 | 0.46 | 0.21 | 20907 | 0 | 0 |
04-1737E1 | 227.53 | 228.30 | 0.76 | 0.38 | 20908 | 0 | 0 |
04-1737E1 | 228.30 | 229.45 | 1.16 | 0.21 | 20909 | 0 | 0 |
04-1737E1 | 229.45 | 231.19 | 1.74 | 0.10 | 20910 | 0 | 0 |
04-1737E1 | 231.19 | 232.26 | 1.07 | 3.84 | 20911 | 0.57 | 0 |
04-1737E1 | 232.26 | 233.78 | 1.52 | 28.83 | 20912 | 4.7 | 0.01 |
04-1737E1 | 233.78 | 234.45 | 0.67 | 10.25 | 20913 | 3.1 | 0 |
04-1737E1 | 234.45 | 235.37 | 0.91 | 1.95 | 20914 | 1.41 | 0 |
04-1737E1 | 235.37 | 236.98 | 1.62 | 0.58 | 20915 | 0 | 0 |
04-1737E1 | 236.98 | 238.35 | 1.37 | 0.99 | 20916 | 0.27 | 0 |
04-1737E1 | 238.35 | 239.54 | 1.19 | 0.03 | 20917 | 0 | 0 |
04-1737E1 | 239.54 | 241.10 | 1.55 | 0.03 | 20918 | 0 | 0 |
04-1737E1 | 241.10 | 242.62 | 1.52 | 0.03 | 20919 | 0 | 0 |
04-1737E1 | 242.62 | 243.23 | 0.61 | 0.07 | 20920 | 0 | 0 |
04-1737E1 | 260.60 | 261.52 | 0.91 | 0.24 | 20922 | 0 | 0 |
04-1737E1 | 261.52 | 263.04 | 1.52 | 0.10 | 20923 | 0 | 0 |
04-1737E1 | 263.04 | 263.65 | 0.61 | 0.07 | 20924 | 0 | 0 |
04-1737E1 | 263.65 | 264.20 | 0.55 | 0.07 | 20925 | 0 | 0 |
04-1737E1 | 264.20 | 264.69 | 0.49 | 0.00 | 20926 | 0 | 0 |
04-1737E1 | 264.69 | 266.21 | 1.52 | 0.03 | 20927 | 0 | 0 |
04-1737E1 | 266.21 | 266.85 | 0.64 | 0.07 | 20928 | 0 | 0 |
04-1737E1 | 266.85 | 267.13 | 0.27 | 1.51 | 20929 | 0.83 | 0.01 |
04-1737E1 | 267.13 | 267.89 | 0.76 | 1.17 | 20930 | 0.55 | 0.01 |
04-1737E1 | 267.89 | 268.53 | 0.64 | 0.03 | 20931 | 0 | 0 |
04-1737E1 | 268.53 | 269.44 | 0.91 | 0.03 | 20932 | 0 | 0 |
04-1737E1 | 269.44 | 270.81 | 1.37 | 0.00 | 20933 | 0 | 0 |
04-1737E1 | 270.81 | 272.25 | 1.43 | 0.00 | 20934 | 0 | 0 |
04-1737E1 | 272.25 | 272.74 | 0.49 | 0.00 | 20935 | 0 | 0 |
04-1737E1 | 272.74 | 273.50 | 0.76 | 0.00 | 20936 | 0 | 0 |
04-1737E1 | 273.50 | 273.68 | 0.18 | 0.00 | 20937 | 0 | 0 |
04-1737E1 | 273.68 | 274.69 | 1.01 | 0.17 | 20938 | 0 | 0 |
04-1737E1 | 274.69 | 275.05 | 0.37 | 1.54 | 20939 | 0.5 | 0.01 |
04-1737E1 | 275.05 | 276.27 | 1.22 | 0.00 | 20940 | 0 | 0 |
04-1737E1 | 276.27 | 277.83 | 1.55 | 0.00 | 20941 | 0 | 0 |
04-1737E1 | 277.83 | 278.28 | 0.46 | 0.00 | 20942 | 0 | 0 |
04-1737E1 | 278.28 | 279.20 | 0.91 | 0.00 | 20943 | 0 | 0 |
04-1737E1 | 279.20 | 279.50 | 0.30 | 0.00 | 20944 | 0 | 0 |
04-1737E1 | 279.50 | 280.87 | 1.37 | 0.00 | 20945 | 0 | 0 |
04-1737E1 | 280.87 | 282.15 | 1.28 | 0.00 | 20946 | 0 | 0 |
04-1737E1 | 282.15 | 283.46 | 1.31 | 0.00 | 20947 | 0 | 0 |
04-1737E1 | 283.46 | 284.99 | 1.52 | 0.17 | 20948 | 0 | 0 |
04-1737E1 | 284.99 | 286.51 | 1.52 | 0.03 | 20949 | 0 | 0 |
04-1737E1 | 286.51 | 287.43 | 0.91 | 0.00 | 20950 | 0 | 0 |
04-1737E2 | 222.99 | 223.42 | 0.43 | 0.07 | 20952 | 0 | 0 |
04-1737E2 | 223.42 | 224.82 | 1.40 | 2.98 | 20953 | 0.4 | 0.02 |
04-1737E2 | 224.82 | 226.34 | 1.52 | 0.03 | 20954 | 0 | 0 |
04-1737E2 | 226.34 | 227.93 | 1.58 | 0.03 | 20955 | 0 | 0 |
209
04-1737E2 | 227.93 | 229.45 | 1.52 | 0.07 | 20956 | 0 | 0 |
04-1737E2 | 229.45 | 230.58 | 1.13 | 0.03 | 20957 | 0 | 0 |
04-1737E2 | 230.58 | 231.34 | 0.76 | 0.00 | 20958 | 0 | 0 |
04-1737E2 | 231.34 | 232.87 | 1.52 | 0.00 | 20959 | 0 | 0 |
04-1737E2 | 232.87 | 233.17 | 0.30 | 1.54 | 20960 | 0.42 | 0 |
04-1737E2 | 233.17 | 233.66 | 0.49 | 0.03 | 20961 | 0 | 0 |
04-1737E2 | 233.66 | 233.96 | 0.30 | 30.93 | 20962 | 2.65 | 0.01 |
04-1737E2 | 233.96 | 235.49 | 1.52 | 0.51 | 20963 | 0 | 0 |
04-1737E2 | 235.49 | 237.01 | 1.52 | 0.48 | 20964 | 0 | 0 |
04-1737E2 | 237.01 | 238.54 | 1.52 | 0.14 | 20965 | 0 | 0 |
04-1737E2 | 238.54 | 240.43 | 1.89 | 0.00 | 20966 | 0 | 0 |
04-1737E2 | 240.43 | 240.73 | 0.30 | 0.03 | 20967 | 0 | 0 |
04-1737E2 | 240.73 | 241.58 | 0.85 | 0.00 | 20968 | 0 | 0 |
04-1737E2 | 241.58 | 243.11 | 1.52 | 0.03 | 20969 | 0 | 0 |
04-1737E2 | 243.11 | 244.54 | 1.43 | 0.03 | 20970 | 0 | 0 |
04-1737E2 | 244.54 | 246.07 | 1.52 | 0.00 | 20971 | 0 | 0 |
04-1737E2 | 246.07 | 247.28 | 1.22 | 0.00 | 20972 | 0 | 0 |
04-1737E2 | 247.28 | 248.81 | 1.52 | 0.00 | 20973 | 0 | 0 |
04-1737E2 | 248.81 | 250.27 | 1.46 | 0.00 | 20974 | 0 | 0 |
04-1737E2 | 250.27 | 251.76 | 1.49 | 0.00 | 20975 | 0 | 0 |
04-1737E2 | 251.76 | 253.14 | 1.37 | 0.27 | 20976 | 0 | 0 |
04-1737E2 | 253.14 | 254.42 | 1.28 | 0.00 | 20977 | 0 | 0 |
04-1737E2 | 254.42 | 255.27 | 0.85 | 0.00 | 20978 | 0 | 0 |
04-1737E2 | 255.27 | 255.88 | 0.61 | 0.00 | 20979 | 0 | 0 |
04-1737E2 | 255.88 | 256.64 | 0.76 | 0.03 | 20980 | 0 | 0 |
04-1737E2 | 256.64 | 256.92 | 0.27 | 8.91 | 20981 | 0.49 | 0 |
04-1737E2 | 256.92 | 257.83 | 0.91 | 2.23 | 20982 | 0.97 | 0.01 |
04-1737E2 | 257.83 | 259.08 | 1.25 | 14.37 | 20983 | 0.96 | 0.01 |
04-1737E2 | 259.08 | 260.60 | 1.52 | 0.03 | 20984 | 0 | 0 |
04-1737E2 | 260.60 | 262.13 | 1.52 | 0.03 | 20985 | 0 | 0 |
04-1737E2 | 262.13 | 263.65 | 1.52 | 0.00 | 20986 | 0 | 0 |
04-300SW1 | 178.64 | 179.62 | 0.98 | 0.89 | 109177 | 0 | 0 |
04-300SW1 | 179.62 | 180.75 | 1.13 | 1.23 | 109178 | 0.05 | 0.06 |
04-300SW1 | 180.75 | 181.72 | 0.98 | 11.21 | 109179 | 1.18 | 0.05 |
04-300SW1 | 181.72 | 183.18 | 1.46 | 0.03 | 109180 | 0 | 0 |
04-300SW2 | 80.35 | 80.62 | 0.27 | 0.24 | 109074 | 0 | 0 |
04-300SW2 | 80.62 | 82.30 | 1.68 | 0.03 | 109075 | 0 | 0 |
04-300SW2 | 82.30 | 83.21 | 0.91 | 0.69 | 109076 | 0 | 0 |
04-300SW2 | 107.72 | 108.72 | 1.01 | 0.45 | 109077 | 0 | 0 |
04-300SW2 | 108.72 | 110.28 | 1.55 | 0.00 | 109078 | 0 | 0 |
04-300SW2 | 110.28 | 111.40 | 1.13 | 3.98 | 109079 | 2.1 | 0.01 |
04-300SW2 | 111.40 | 112.26 | 0.85 | 4.56 | 109080 | 2.61 | 0.01 |
04-300SW2 | 112.26 | 113.39 | 1.13 | 0.00 | 109081 | 0 | 0 |
04-300SW2 | 113.39 | 114.00 | 0.61 | 0.03 | 109082 | 0 | 0 |
04-300SW2 | 180.20 | 181.20 | 1.01 | 0.03 | 109083 | 0 | 0 |
04-300SW2 | 181.20 | 181.66 | 0.46 | 5.49 | 109084 | 1.09 | 0.07 |
04-300SW2 | 181.66 | 182.58 | 0.91 | 0.21 | 109085 | 0 | 0 |
210
04-300SW2 | 182.58 | 183.49 | 0.91 | 0.03 | 109086 | 0 | 0 |
04-300SW2 | 183.49 | 185.01 | 1.52 | 0.00 | 109087 | 0 | 0 |
04-300SW2 | 185.01 | 186.48 | 1.46 | 0.00 | 109088 | 0 | 0 |
04-300SW2 | 186.48 | 187.70 | 1.22 | 0.00 | 109089 | 0 | 0 |
04-300SW2 | 187.70 | 188.88 | 1.19 | 0.00 | 109090 | 0 | 0 |
04-300SW2 | 188.88 | 190.41 | 1.52 | 0.00 | 109091 | 0 | 0 |
04-300SW2 | 190.41 | 190.90 | 0.49 | 0.00 | 109092 | 0 | 0 |
04-300SW2 | 190.90 | 191.17 | 0.27 | 0.03 | 109093 | 0 | 0 |
04-300SW2 | 191.17 | 192.91 | 1.74 | 0.03 | 109094 | 0 | 0 |
04-300SW2 | 192.91 | 193.09 | 0.18 | 0.03 | 109095 | 0 | 0 |
04-300SW2 | 193.09 | 194.61 | 1.52 | 0.03 | 109096 | 0 | 0 |
04-300SW2 | 194.61 | 195.16 | 0.55 | 0.10 | 109097 | 0 | 0 |
04-300SW2 | 195.16 | 196.75 | 1.58 | 0.14 | 109098 | 0 | 0 |
04-300SW2 | 196.75 | 197.66 | 0.91 | 0.03 | 109099 | 0 | 0 |
04-300SW2 | 197.66 | 199.80 | 2.13 | 0.03 | 109100 | 0 | 0 |
04-300SW2 | 199.80 | 201.02 | 1.22 | 0.31 | 109101 | 0 | 0 |
04-300SW2 | 201.02 | 202.54 | 1.52 | 0.00 | 109102 | 0 | 0 |
04-300SW2 | 202.54 | 203.91 | 1.37 | 0.00 | 109103 | 0 | 0 |
04-300SW2 | 203.91 | 205.44 | 1.52 | 0.00 | 109104 | 0 | 0 |
04-300SW2 | 205.44 | 206.53 | 1.10 | 0.10 | 109105 | 0 | 0 |
04-300SW2 | 206.53 | 206.96 | 0.43 | 10.11 | 109106 | 1.3 | 0.02 |
04-300SW2 | 206.96 | 207.84 | 0.88 | 0.03 | 109107 | 0 | 0 |
04-300SW2 | 207.84 | 208.94 | 1.10 | 28.63 | 109108 | 2.01 | 0.03 |
04-300SW2 | 208.94 | 210.59 | 1.65 | 0.55 | 109109 | 0 | 0 |
04-300SW2 | 210.59 | 212.11 | 1.52 | 0.03 | 109110 | 0 | 0 |
04-300SW3 | 77.63 | 78.94 | 1.31 | 0.00 | 109113 | 0 | 0 |
04-300SW3 | 78.94 | 80.47 | 1.52 | 0.00 | 109114 | 0 | 0 |
04-300SW3 | 80.47 | 80.92 | 0.46 | 0.03 | 109115 | 0 | 0 |
04-300SW3 | 80.92 | 81.53 | 0.61 | 0.03 | 109116 | 0 | 0 |
04-300SW3 | 81.53 | 83.06 | 1.52 | 0.00 | 109117 | 0 | 0 |
04-300SW3 | 83.06 | 84.43 | 1.37 | 0.00 | 109118 | 0 | 0 |
04-300SW3 | 122.99 | 124.21 | 1.22 | 0.14 | 109119 | 0 | 0 |
04-300SW3 | 124.21 | 125.64 | 1.43 | 0.03 | 109120 | 0 | 0 |
04-300SW3 | 125.64 | 126.25 | 0.61 | 2.13 | 109121 | 1.19 | 0.01 |
04-300SW3 | 131.52 | 133.05 | 1.52 | 1.37 | 109122 | 0.83 | 0.01 |
04-300SW3 | 133.05 | 134.02 | 0.98 | 0.00 | 109123 | 0 | 0 |
04-300SW3 | 134.02 | 135.82 | 1.80 | 0.00 | 109124 | 0 | 0 |
04-300SW3 | 135.82 | 136.37 | 0.55 | 0.17 | 109125 | 0 | 0 |
04-300SW3 | 136.37 | 137.65 | 1.28 | 10.66 | 109126 | 1.99 | 0.01 |
04-300SW3 | 137.65 | 138.87 | 1.22 | 0.41 | 109127 | 0 | 0 |
04-300SW3 | 138.87 | 140.24 | 1.37 | 0.03 | 109128 | 0 | 0 |
04-300SW3 | 140.24 | 140.60 | 0.37 | 0.00 | 109129 | 0 | 0 |
04-300SW3 | 140.60 | 142.16 | 1.55 | 0.00 | 109130 | 0 | 0 |
04-300SW3 | 142.16 | 143.80 | 1.65 | 0.00 | 109131 | 0 | 0 |
04-300SW3 | 143.80 | 144.29 | 0.49 | 0.03 | 109132 | 0 | 0 |
04-300SW3 | 144.29 | 145.08 | 0.79 | 0.03 | 109133 | 0 | 0 |
04-300SW3 | 145.08 | 145.39 | 0.30 | 0.34 | 109134 | 0 | 0 |
211
04-300SW3 | 145.39 | 146.00 | 0.61 | 0.00 | 109135 | 0 | 0 |
04-300SW3 | 194.71 | 196.38 | 1.68 | 0.10 | 109136 | 0 | 0 |
04-300SW3 | 196.38 | 196.87 | 0.49 | 13.27 | 109137 | 1.3 | 0.03 |
04-300SW3 | 196.87 | 197.48 | 0.61 | 1.75 | 109138 | 0.58 | 0.02 |
04-300SW3 | 197.48 | 199.03 | 1.55 | 10.32 | 109139 | 2.67 | 0.02 |
04-300SW3 | 199.03 | 199.80 | 0.76 | 0.10 | 109140 | 0 | 0 |
04-300SW3 | 199.80 | 201.11 | 1.31 | 2.13 | 109141 | 1.13 | 0.01 |
04-300SW3 | 201.11 | 201.63 | 0.52 | 2.88 | 109142 | 1.2 | 0.01 |
04-300SW3 | 201.63 | 202.57 | 0.94 | 7.30 | 109143 | 2.42 | 0.02 |
04-300SW3 | 202.57 | 203.61 | 1.04 | 16.97 | 109144 | 3.41 | 0.02 |
04-300SW3 | 203.61 | 204.58 | 0.98 | 0.07 | 109145 | 0 | 0 |
04-300SW3 | 204.58 | 205.44 | 0.85 | 0.55 | 109146 | 0 | 0 |
04-300SW3 | 205.44 | 206.75 | 1.31 | 0.00 | 109147 | 0 | 0 |
04-300SW3 | 206.75 | 208.18 | 1.43 | 0.00 | 109148 | 0 | 0 |
04-300SW3 | 208.18 | 209.55 | 1.37 | 0.00 | 109149 | 0 | 0 |
04-300SW3 | 209.55 | 211.23 | 1.68 | 0.00 | 109150 | 0 | 0 |
04-300SW3 | 211.23 | 212.54 | 1.31 | 0.00 | 109151 | 0 | 0 |
04-300SW3 | 212.54 | 213.36 | 0.82 | 0.00 | 109152 | 0 | 0 |
04-300SW3 | 213.36 | 214.73 | 1.37 | 0.00 | 109153 | 0 | 0 |
04-300SW3 | 214.73 | 215.31 | 0.58 | 0.00 | 109154 | 0 | 0 |
04-300SW3 | 215.31 | 216.71 | 1.40 | 0.00 | 109155 | 0 | 0 |
04-300SW3 | 216.71 | 217.93 | 1.22 | 0.03 | 109156 | 0 | 0 |
04-300SW3 | 217.93 | 219.52 | 1.58 | 0.03 | 109157 | 0 | 0 |
04-300SW3 | 219.52 | 221.19 | 1.68 | 0.00 | 109158 | 0 | 0 |
04-300SW3 | 221.19 | 222.81 | 1.62 | 0.03 | 109159 | 0 | 0 |
04-300SW3 | 222.81 | 223.42 | 0.61 | 0.31 | 109160 | 0 | 0 |
04-300SW3 | 223.42 | 223.88 | 0.46 | 0.34 | 109161 | 0 | 0 |
04-300SW3 | 223.88 | 224.58 | 0.70 | 4.83 | 109162 | 1.85 | 0.02 |
04-300SW3 | 224.58 | 225.86 | 1.28 | 0.00 | 109163 | 0 | 0 |
04-300SW3 | 225.86 | 227.26 | 1.40 | 22.42 | 109164 | 3.27 | 0.13 |
04-300SW3 | 227.26 | 227.96 | 0.70 | 1.99 | 109165 | 0.84 | 0.03 |
04-300SW3 | 227.96 | 228.84 | 0.88 | 22.22 | 109166 | 1.95 | 1.36 |
04-300SW3 | 228.84 | 230.00 | 1.16 | 34.15 | 109167 | 2.98 | 0.02 |
04-300SW3 | 230.00 | 230.73 | 0.73 | 5.83 | 109168 | 1.17 | 0.01 |
04-300SW3 | 230.73 | 232.26 | 1.52 | 0.10 | 109169 | 0 | 0 |
04-300SW3 | 232.26 | 233.84 | 1.58 | 0.00 | 109170 | 0 | 0 |
04-300SW3 | 233.84 | 235.00 | 1.16 | 0.00 | 109171 | 0 | 0 |
04-300SW3 | 235.00 | 236.22 | 1.22 | 0.00 | 109172 | 0 | 0 |
04-300SW3 | 236.22 | 236.71 | 0.49 | 0.14 | 109173 | 0 | 0 |
04-300SW3 | 236.71 | 237.44 | 0.73 | 0.00 | 109174 | 0 | 0 |
04-300SW3 | 237.44 | 238.96 | 1.52 | 0.00 | 109175 | 0 | 0 |
04-330SW1 | 91.74 | 93.27 | 1.52 | 0.00 | 20701 | 0 | 0 |
04-330SW1 | 93.27 | 94.79 | 1.52 | 0.00 | 20702 | 0 | 0 |
04-330SW1 | 94.79 | 96.32 | 1.52 | 0.00 | 20703 | 0 | 0 |
04-330SW1 | 163.07 | 164.21 | 1.14 | 0.00 | 20704 | 0 | 0 |
04-330SW1 | 164.21 | 165.35 | 1.14 | 0.07 | 20705 | 0 | 0 |
04-330SW1 | 165.35 | 165.89 | 0.53 | 0.03 | 20706 | 0 | 0 |
212
04-330SW1 | 165.89 | 166.60 | 0.72 | 0.03 | 20707 | 0 | 0 |
04-330SW1 | 166.60 | 166.73 | 0.12 | 0.07 | 20708 | 0 | 0 |
04-330SW1 | 166.73 | 167.18 | 0.46 | 0.00 | 20709 | 0 | 0 |
04-330SW1 | 167.18 | 168.25 | 1.07 | 1.06 | 20710 | 0.23 | 0.01 |
04-330SW1 | 168.25 | 168.78 | 0.53 | 10.01 | 20711 | 1.05 | 0.02 |
04-330SW1 | 168.78 | 170.54 | 1.75 | 0.93 | 20712 | 0 | 0 |
04-330SW1 | 170.54 | 172.21 | 1.68 | 0.38 | 20713 | 0 | 0 |
04-330SW1 | 172.21 | 172.36 | 0.15 | 1.27 | 20714 | 0.06 | 0.05 |
04-330SW1 | 172.36 | 172.82 | 0.46 | 30.03 | 20715 | 2.73 | 0.83 |
04-330SW1 | 172.82 | 173.74 | 0.91 | 35.45 | 20716 | 3.14 | 1.28 |
04-330SW1 | 173.74 | 174.19 | 0.46 | 9.94 | 20717 | 2.75 | 0.33 |
04-330SW1 | 174.19 | 174.50 | 0.30 | 80.61 | 20718 | 4.41 | 2.23 |
04-330SW1 | 174.50 | 175.11 | 0.61 | 2.13 | 20719 | 1.03 | 0.02 |
04-330SW1 | 175.11 | 175.56 | 0.46 | 0.14 | 20720 | 0 | 0 |
04-330SW1 | 175.56 | 176.02 | 0.46 | 0.03 | 20721 | 0 | 0 |
04-330SW1 | 176.02 | 177.09 | 1.07 | 0.10 | 20722 | 0 | 0 |
04-330SW2 | 167.34 | 168.86 | 1.52 | 0.00 | 20723 | 0 | 0 |
04-330SW2 | 168.86 | 170.93 | 2.07 | 2.85 | 20724 | 0.27 | 0.01 |
04-330SW2 | 170.93 | 171.60 | 0.67 | 13.68 | 20725 | 2.15 | 0.01 |
04-330SW2 | 171.60 | 173.13 | 1.52 | 0.03 | 20726 | 0 | 0 |
04-330SW2 | 173.13 | 173.81 | 0.69 | 0.00 | 20727 | 0 | 0 |
04-330SW2 | 173.81 | 175.26 | 1.45 | 0.00 | 20728 | 0 | 0 |
04-330SW2 | 175.26 | 176.78 | 1.52 | 0.00 | 20729 | 0 | 0 |
04-330SW2 | 176.78 | 178.31 | 1.52 | 0.00 | 20730 | 0 | 0 |
04-330SW2 | 178.31 | 179.83 | 1.52 | 0.00 | 20731 | 0 | 0 |
04-330SW2 | 179.83 | 181.36 | 1.52 | 0.00 | 20732 | 0 | 0 |
04-330SW2 | 181.36 | 181.84 | 0.49 | 0.00 | 20733 | 0 | 0 |
04-330SW2 | 181.84 | 183.42 | 1.57 | 0.00 | 20734 | 0 | 0 |
04-330SW2 | 183.42 | 183.79 | 0.38 | 0.03 | 20735 | 0 | 0 |
04-330SW2 | 183.79 | 184.56 | 0.76 | 0.03 | 20736 | 0 | 0 |
04-330SW2 | 184.56 | 186.08 | 1.52 | 0.24 | 20737 | 0 | 0 |
04-330SW2 | 186.08 | 187.18 | 1.10 | 0.00 | 20738 | 0 | 0 |
04-330SW2 | 187.18 | 187.67 | 0.49 | 0.38 | 20739 | 0 | 0 |
04-330SW2 | 187.67 | 188.98 | 1.31 | 0.27 | 20740 | 0 | 0 |
04-330SW2 | 188.98 | 190.58 | 1.60 | 0.10 | 20741 | 0 | 0 |
04-330SW2 | 190.58 | 190.80 | 0.23 | 0.03 | 20742 | 0 | 0 |
04-330SW2 | 190.80 | 191.96 | 1.16 | 0.17 | 20743 | 0 | 0 |
04-330SW2 | 191.96 | 192.57 | 0.61 | 2.33 | 20744 | 1.83 | 0.26 |
04-330SW2 | 192.57 | 193.09 | 0.52 | 0.65 | 20746 | 0 | 0 |
04-330SW2 | 193.09 | 194.22 | 1.13 | 0.24 | 20747 | 0 | 0 |
04-330SW2 | 194.22 | 195.56 | 1.34 | 16.22 | 20748 | 1.89 | 0.08 |
04-330SW2 | 195.56 | 197.08 | 1.52 | 44.37 | 20749 | 2.39 | 1.48 |
04-330SW2 | 197.08 | 198.42 | 1.34 | 39.74 | 20750 | 2.26 | 0.38 |
04-330SW2 | 198.42 | 199.40 | 0.98 | 0.55 | 20751 | 0 | 0 |
04-330SW2 | 199.40 | 200.62 | 1.22 | 45.67 | 20752 | 1.49 | 0.15 |
04-330SW2 | 200.62 | 202.27 | 1.65 | 35.35 | 20753 | 2.45 | 0.01 |
04-330SW2 | 202.27 | 203.30 | 1.04 | 0.17 | 20754 | 0 | 0 |
213
04-330SW2 | 203.30 | 203.76 | 0.46 | 1.61 | 20755 | 0.71 | 0.01 |
04-330SW2 | 203.76 | 205.59 | 1.83 | 0.03 | 20756 | 0 | 0 |
04-330SW2 | 205.59 | 206.35 | 0.76 | 0.03 | 20757 | 0 | 0 |
04-330SW2 | 206.35 | 207.39 | 1.04 | 0.00 | 20758 | 0 | 0 |
04-360SW1 | 157.95 | 159.47 | 1.52 | 0.00 | 20797 | 0 | 0 |
04-360SW1 | 159.47 | 161.00 | 1.52 | 0.00 | 20798 | 0 | 0 |
04-360SW1 | 161.00 | 162.21 | 1.22 | 0.00 | 20799 | 0 | 0 |
04-360SW1 | 162.21 | 162.76 | 0.55 | 0.03 | 20800 | 0 | 0 |
04-360SW1 | 162.76 | 163.68 | 0.91 | 5.18 | 20801 | 0.07 | 0.01 |
04-360SW1 | 163.68 | 164.56 | 0.88 | 0.10 | 20802 | 0 | 0 |
04-360SW1 | 164.56 | 165.66 | 1.10 | 0.00 | 20803 | 0 | 0 |
04-360SW1 | 165.66 | 167.34 | 1.68 | 0.00 | 20804 | 0 | 0 |
04-360SW1 | 167.34 | 168.55 | 1.22 | 0.00 | 20805 | 0 | 0 |
04-360SW1 | 168.55 | 170.08 | 1.52 | 0.00 | 20806 | 0 | 0 |
04-360SW1 | 170.08 | 170.87 | 0.79 | 0.00 | 20807 | 0 | 0 |
04-360SW1 | 170.87 | 171.60 | 0.73 | 0.03 | 20808 | 0 | 0 |
04-360SW1 | 171.60 | 173.00 | 1.40 | 0.00 | 20809 | 0 | 0 |
04-360SW1 | 173.00 | 174.96 | 1.95 | 0.00 | 20810 | 0 | 0 |
04-360SW1 | 174.96 | 175.75 | 0.79 | 0.00 | 20811 | 0 | 0 |
04-360SW1 | 175.75 | 177.24 | 1.49 | 0.00 | 20812 | 0 | 0 |
04-360SW1 | 177.24 | 177.88 | 0.64 | 0.03 | 20813 | 0 | 0 |
04-360SW1 | 177.88 | 179.10 | 1.22 | 0.03 | 20814 | 0 | 0 |
04-360SW1 | 179.10 | 180.05 | 0.94 | 31.34 | 20815 | 2.36 | 7.99 |
04-360SW1 | 180.05 | 181.57 | 1.52 | 4.80 | 20816 | 1.17 | 0.02 |
04-360SW1 | 181.57 | 182.39 | 0.82 | 9.29 | 20817 | 2.84 | 0.13 |
04-360SW1 | 182.39 | 183.95 | 1.55 | 28.53 | 20818 | 2.49 | 0.46 |
04-360SW1 | 183.95 | 184.47 | 0.52 | 13.95 | 20819 | 2.26 | 0.02 |
04-360SW1 | 184.47 | 185.93 | 1.46 | 5.11 | 20820 | 0.94 | 0.02 |
04-360SW1 | 185.93 | 187.38 | 1.45 | 1.51 | 20821 | 0.11 | 0.01 |
04-360SW1 | 187.38 | 188.90 | 1.52 | 1.65 | 20822 | 0.09 | 0.01 |
04-360SW1 | 188.90 | 189.74 | 0.84 | 14.23 | 20823 | 0.33 | 0.01 |
04-360SW1 | 189.74 | 190.50 | 0.76 | 0.31 | 20824 | 0 | 0 |
04-360SW1 | 190.50 | 191.69 | 1.19 | 12.75 | 20825 | 1.12 | 0.11 |
04-360SW1 | 191.69 | 192.69 | 1.01 | 18.38 | 20826 | 2.61 | 0.02 |
04-360SW1 | 192.69 | 193.43 | 0.73 | 17.62 | 20827 | 3.71 | 0.02 |
04-360SW1 | 193.43 | 194.95 | 1.52 | 0.75 | 20828 | 0 | 0 |
04-360SW1 | 194.95 | 195.99 | 1.04 | 0.10 | 20829 | 0 | 0 |
04-360SW1 | 195.99 | 197.51 | 1.52 | 0.00 | 20830 | 0 | 0 |
04-360SW1 | 197.51 | 198.73 | 1.22 | 0.00 | 20831 | 0 | 0 |
04-360SW1 | 198.73 | 199.40 | 0.67 | 0.00 | 20832 | 0 | 0 |
04-360SW1 | 199.40 | 200.86 | 1.46 | 0.03 | 20833 | 0 | 0 |
04-360SW1 | 200.86 | 201.17 | 0.30 | 0.03 | 20834 | 0 | 0 |
04-360SW1 | 201.17 | 202.39 | 1.22 | 0.00 | 20835 | 0 | 0 |
04-360SW1 | 202.39 | 202.84 | 0.46 | 0.00 | 20836 | 0 | 0 |
04-360SW1 | 202.84 | 204.22 | 1.37 | 0.07 | 20837 | 0 | 0 |
04-360SW1 | 204.22 | 205.40 | 1.19 | 0.00 | 20838 | 0 | 0 |
04-360SW1 | 225.25 | 227.08 | 1.83 | 0.03 | 20839 | 0 | 0 |
214
04-360SW1 | 227.08 | 228.60 | 1.52 | 0.00 | 20840 | 0 | 0 |
04-360SW1 | 228.60 | 230.12 | 1.52 | 0.00 | 20841 | 0 | 0 |
04-360SW1 | 230.12 | 231.34 | 1.22 | 0.00 | 20842 | 0 | 0 |
04-360SW1 | 231.34 | 232.87 | 1.52 | 0.00 | 20843 | 0 | 0 |
04-360SW1 | 232.87 | 234.18 | 1.31 | 0.00 | 20844 | 0 | 0 |
04-360SW1 | 234.18 | 235.70 | 1.52 | 0.00 | 20845 | 0 | 0 |
04-360SW1 | 235.70 | 237.44 | 1.74 | 0.00 | 20846 | 0 | 0 |
04-360SW2 | 137.77 | 139.29 | 1.52 | 0.00 | 20759 | 0 | 0 |
04-360SW2 | 139.29 | 140.54 | 1.25 | 0.00 | 20760 | 0 | 0 |
04-360SW2 | 140.54 | 142.04 | 1.49 | 0.03 | 20761 | 0 | 0 |
04-360SW2 | 142.04 | 143.87 | 1.83 | 0.03 | 20762 | 0 | 0 |
04-360SW2 | 143.87 | 145.39 | 1.52 | 0.00 | 20763 | 0 | 0 |
04-360SW2 | 145.39 | 146.67 | 1.28 | 0.00 | 20764 | 0 | 0 |
04-360SW2 | 146.67 | 147.83 | 1.16 | 0.00 | 20765 | 0 | 0 |
04-360SW2 | 147.83 | 149.35 | 1.52 | 0.07 | 20766 | 0 | 0 |
04-360SW2 | 157.58 | 159.04 | 1.46 | 0.10 | 20767 | 0 | 0 |
04-360SW2 | 159.04 | 160.48 | 1.43 | 0.27 | 20768 | 0 | 0 |
04-360SW2 | 160.48 | 161.39 | 0.91 | 0.07 | 20769 | 0 | 0 |
04-360SW2 | 161.39 | 162.76 | 1.37 | 0.03 | 20770 | 0 | 0 |
04-360SW2 | 185.11 | 186.75 | 1.65 | 0.24 | 20772 | 0 | 0 |
04-360SW2 | 186.75 | 188.15 | 1.40 | 0.07 | 20773 | 0 | 0 |
04-360SW2 | 188.15 | 189.68 | 1.52 | 0.00 | 20774 | 0 | 0 |
04-360SW2 | 189.68 | 191.20 | 1.52 | 1.37 | 20775 | 0.13 | 0.02 |
04-360SW2 | 191.20 | 192.42 | 1.22 | 62.26 | 20776 | 0.35 | 0.02 |
04-360SW2 | 192.42 | 193.91 | 1.49 | 0.10 | 20777 | 0 | 0 |
04-360SW2 | 193.91 | 195.38 | 1.46 | 21.33 | 20778 | 0.03 | 0.01 |
04-360SW2 | 195.38 | 197.24 | 1.86 | 0.03 | 20779 | 0 | 0 |
04-360SW2 | 197.24 | 198.24 | 1.01 | 0.03 | 20780 | 0 | 0 |
04-360SW2 | 198.24 | 199.52 | 1.28 | 2.47 | 20781 | 0.08 | 0.01 |
04-360SW2 | 199.52 | 201.02 | 1.49 | 9.50 | 20782 | 1.03 | 0.05 |
04-360SW2 | 201.02 | 201.87 | 0.85 | 1.71 | 20783 | 0.88 | 0.12 |
04-360SW2 | 201.87 | 203.39 | 1.52 | 0.10 | 20784 | 0 | 0 |
04-360SW2 | 203.39 | 203.52 | 0.12 | 0.17 | 20785 | 0 | 0 |
05-1676E1 | 121.92 | 122.53 | 0.61 | 0.03 | 109252 | 0 | 0 |
05-1676E1 | 122.53 | 123.44 | 0.91 | 0.27 | 109253 | 0 | 0 |
05-1676E1 | 123.44 | 124.66 | 1.22 | 0.00 | 109254 | 0 | 0 |
05-1676E1 | 124.66 | 126.19 | 1.52 | 0.00 | 109255 | 0 | 0 |
05-1676E1 | 126.19 | 127.04 | 0.85 | 0.00 | 109257 | 0 | 0 |
05-1676E1 | 167.03 | 168.55 | 1.52 | 0.00 | 109258 | 0 | 0 |
05-1676E1 | 168.55 | 170.08 | 1.52 | 0.00 | 109259 | 0 | 0 |
05-1676E1 | 170.08 | 171.60 | 1.52 | 0.03 | 109260 | 0 | 0 |
05-1676E1 | 171.60 | 173.13 | 1.52 | 0.00 | 109261 | 0 | 0 |
05-1676E1 | 173.13 | 173.89 | 0.76 | 0.00 | 109263 | 0 | 0 |
05-1676E1 | 173.89 | 174.80 | 0.91 | 0.03 | 109264 | 0 | 0 |
05-1676E1 | 174.80 | 176.33 | 1.52 | 0.00 | 109265 | 0 | 0 |
05-1676E1 | 176.33 | 178.00 | 1.68 | 0.03 | 109266 | 0 | 0 |
05-1676E1 | 178.00 | 178.61 | 0.61 | 0.03 | 109267 | 0 | 0 |
215
05-1676E1 | 178.61 | 180.14 | 1.52 | 0.03 | 109269 | 0 | 0 |
05-1676E1 | 180.14 | 181.05 | 0.91 | 0.00 | 109270 | 0 | 0 |
05-1676E1 | 181.05 | 181.97 | 0.91 | 0.00 | 109271 | 0 | 0 |
05-1676E1 | 181.97 | 183.03 | 1.07 | 0.07 | 109272 | 0 | 0 |
05-1676E1 | 183.03 | 184.40 | 1.37 | 0.62 | 109273 | 0 | 0 |
05-1676E1 | 184.40 | 185.32 | 0.91 | 0.93 | 109275 | 0 | 0 |
05-1676E1 | 185.32 | 185.62 | 0.30 | 0.45 | 109276 | 0 | 0 |
05-1676E1 | 185.62 | 187.15 | 1.52 | 4.08 | 109277 | 0 | 0 |
05-1676E1 | 187.15 | 187.88 | 0.73 | 14.43 | 109278 | 0 | 0 |
05-1676E1 | 187.88 | 188.21 | 0.34 | 3.22 | 109279 | 0 | 0 |
05-1676E1 | 188.21 | 188.52 | 0.30 | 22.01 | 109280 | 0 | 0 |
05-1676E1 | 188.52 | 189.37 | 0.85 | 33.02 | 109281 | 0 | 0 |
05-1676E1 | 189.37 | 189.68 | 0.30 | 10.25 | 109283 | 0 | 0 |
05-1676E1 | 189.68 | 191.20 | 1.52 | 7.58 | 109284 | 0 | 0 |
05-1676E1 | 191.20 | 192.73 | 1.52 | 0.21 | 109285 | 0 | 0 |
05-1676E1 | 192.73 | 194.25 | 1.52 | 0.10 | 109286 | 0 | 0 |
05-1676E1 | 194.25 | 195.56 | 1.31 | 0.07 | 109287 | 0 | 0 |
05-1676E1 | 195.56 | 195.68 | 0.12 | 0.24 | 109288 | 0 | 0 |
05-1676E1 | 195.68 | 195.86 | 0.18 | 0.10 | 109289 | 0 | 0 |
05-1676E1 | 195.86 | 195.99 | 0.12 | 0.07 | 109290 | 0 | 0 |
05-1676E1 | 195.99 | 197.21 | 1.22 | 0.00 | 109291 | 0 | 0 |
05-1676E1 | 197.21 | 198.27 | 1.07 | 0.03 | 109293 | 0 | 0 |
05-1676E1 | 198.27 | 199.95 | 1.68 | 0.00 | 109294 | 0 | 0 |
05-1676E1 | 199.95 | 201.69 | 1.74 | 0.00 | 109295 | 0 | 0 |
05-1676E1 | 201.69 | 203.00 | 1.31 | 0.00 | 109296 | 0 | 0 |
05-1676E2 | 113.60 | 115.03 | 1.43 | 0.00 | 109299 | 0 | 0 |
05-1676E2 | 115.03 | 116.43 | 1.40 | 0.00 | 109300 | 0 | 0 |
05-1676E2 | 116.43 | 117.96 | 1.52 | 0.00 | 109301 | 0 | 0 |
05-1676E2 | 117.96 | 119.48 | 1.52 | 0.00 | 109302 | 0 | 0 |
05-1676E2 | 119.48 | 121.01 | 1.52 | 0.00 | 109303 | 0 | 0 |
05-1676E2 | 121.01 | 121.62 | 0.61 | 0.00 | 109304 | 0 | 0 |
05-1676E2 | 185.29 | 186.81 | 1.52 | 0.00 | 109306 | 0 | 0 |
05-1676E2 | 186.81 | 188.34 | 1.52 | 0.00 | 109307 | 0 | 0 |
05-1676E2 | 188.34 | 189.56 | 1.22 | 0.00 | 109308 | 0 | 0 |
05-1676E2 | 189.56 | 190.99 | 1.43 | 0.07 | 109309 | 0 | 0 |
05-1676E2 | 190.99 | 192.51 | 1.52 | 0.00 | 109310 | 0 | 0 |
05-1676E2 | 192.51 | 194.04 | 1.52 | 0.00 | 109312 | 0 | 0 |
05-1676E2 | 194.04 | 195.56 | 1.52 | 0.03 | 109313 | 0 | 0 |
05-1676E2 | 195.56 | 196.41 | 0.85 | 0.03 | 109314 | 0 | 0 |
05-1676E2 | 196.41 | 197.94 | 1.52 | 0.03 | 109316 | 0 | 0 |
05-1676E2 | 197.94 | 199.55 | 1.62 | 0.10 | 109317 | 0 | 0 |
05-1676E2 | 199.55 | 200.35 | 0.79 | 0.10 | 109318 | 0 | 0 |
05-1676E2 | 200.35 | 202.05 | 1.71 | 0.14 | 109319 | 0 | 0 |
05-1676E2 | 202.05 | 202.39 | 0.34 | 0.07 | 109320 | 0 | 0 |
05-1676E2 | 202.39 | 202.84 | 0.46 | 0.14 | 109322 | 0 | 0 |
05-1676E2 | 202.84 | 203.15 | 0.30 | 0.10 | 109323 | 0 | 0 |
05-1676E2 | 203.15 | 204.34 | 1.19 | 0.72 | 109324 | 0 | 0 |
216
05-1676E2 | 204.34 | 204.52 | 0.18 | 6.48 | 109325 | 0 | 0 |
05-1676E2 | 204.52 | 205.28 | 0.76 | 0.31 | 109327 | 0 | 0 |
05-1676E2 | 205.28 | 205.56 | 0.27 | 6.93 | 109328 | 0 | 0 |
05-1676E2 | 205.56 | 207.69 | 2.13 | 1.92 | 109329 | 0 | 0 |
05-1676E2 | 207.69 | 207.87 | 0.18 | 0.27 | 109330 | 0 | 0 |
05-1676E2 | 207.87 | 208.48 | 0.61 | 0.14 | 109332 | 0 | 0 |
05-1676E2 | 208.48 | 210.01 | 1.52 | 0.07 | 109333 | 0 | 0 |
05-1676E2 | 210.01 | 210.77 | 0.76 | 20.71 | 109334 | 0 | 0 |
05-1676E2 | 210.77 | 212.29 | 1.52 | 6.14 | 109336 | 0 | 0 |
05-1676E2 | 212.29 | 213.27 | 0.98 | 3.84 | 109337 | 0 | 0 |
05-1676E2 | 213.27 | 214.18 | 0.91 | 0.48 | 109338 | 0 | 0 |
05-1676E2 | 214.18 | 215.71 | 1.52 | 0.07 | 109339 | 0 | 0 |
05-1676E2 | 215.71 | 217.02 | 1.31 | 0.03 | 109342 | 0 | 0 |
05-1676E2 | 217.02 | 218.54 | 1.52 | 0.00 | 109343 | 0 | 0 |
05-1676E2 | 218.54 | 219.76 | 1.22 | 0.03 | 109344 | 0 | 0 |
05-1676E2 | 219.76 | 220.37 | 0.61 | 0.03 | 109345 | 0 | 0 |
05-1676E2 | 220.37 | 221.89 | 1.52 | 0.03 | 109346 | 0 | 0 |
05-1676E2 | 221.89 | 223.11 | 1.22 | 0.00 | 109347 | 0 | 0 |
05-1676E2 | 223.11 | 224.61 | 1.49 | 0.00 | 109348 | 0 | 0 |
05-1676E2 | 224.61 | 226.13 | 1.52 | 0.00 | 109350 | 0 | 0 |
05-1676E2 | 226.13 | 227.66 | 1.52 | 0.00 | 109351 | 0 | 0 |
05-300SW4 | 186.32 | 188.28 | 1.95 | 0.00 | 109352 | 0 | 0 |
05-300SW4 | 188.28 | 189.80 | 1.52 | 0.00 | 109353 | 0 | 0 |
05-300SW4 | 189.80 | 191.11 | 1.31 | 0.00 | 109354 | 0 | 0 |
05-300SW4 | 191.11 | 192.42 | 1.31 | 0.00 | 109355 | 0 | 0 |
05-300SW4 | 192.42 | 193.03 | 0.61 | 0.03 | 109357 | 0 | 0 |
05-300SW4 | 193.03 | 194.01 | 0.98 | 0.03 | 109358 | 0 | 0 |
05-300SW4 | 194.01 | 194.77 | 0.76 | 0.03 | 109359 | 0 | 0 |
05-300SW4 | 194.77 | 195.16 | 0.40 | 0.21 | 109360 | 0 | 0 |
05-300SW4 | 195.16 | 195.99 | 0.82 | 2.88 | 109361 | 0 | 0 |
05-300SW4 | 195.99 | 197.21 | 1.22 | 0.03 | 109362 | 0 | 0 |
05-300SW4 | 197.21 | 198.73 | 1.52 | 0.03 | 109363 | 0 | 0 |
05-300SW4 | 198.73 | 200.13 | 1.40 | 0.00 | 109364 | 0 | 0 |
05-300SW4 | 200.13 | 200.86 | 0.73 | 13.41 | 109365 | 0 | 0 |
05-300SW4 | 200.86 | 203.00 | 2.13 | 0.24 | 109367 | 0 | 0 |
05-300SW4 | 203.00 | 204.22 | 1.22 | 0.03 | 109368 | 0 | 0 |
05-300SW4 | 204.22 | 204.83 | 0.61 | 4.01 | 109369 | 0 | 0 |
05-300SW4 | 204.83 | 205.89 | 1.07 | 0.27 | 109370 | 0 | 0 |
05-300SW4 | 205.89 | 206.96 | 1.07 | 3.39 | 109371 | 0 | 0 |
05-300SW4 | 206.96 | 208.33 | 1.37 | 0.03 | 109373 | 0 | 0 |
05-300SW4 | 208.33 | 209.55 | 1.22 | 0.31 | 109374 | 0 | 0 |
05-300SW4 | 209.55 | 210.92 | 1.37 | 1.41 | 109375 | 0 | 0 |
05-300SW4 | 210.92 | 212.14 | 1.22 | 1.61 | 109376 | 0 | 0 |
05-300SW4 | 212.14 | 212.84 | 0.70 | 0.03 | 109378 | 0 | 0 |
05-300SW4 | 212.84 | 213.36 | 0.52 | 8.09 | 109379 | 0 | 0 |
05-300SW4 | 213.36 | 214.12 | 0.76 | 0.07 | 109380 | 0 | 0 |
05-300SW4 | 214.12 | 214.58 | 0.46 | 0.27 | 109381 | 0 | 0 |
217
05-300SW4 | 214.58 | 215.49 | 0.91 | 0.03 | 109382 | 0 | 0 |
05-300SW4 | 215.49 | 216.26 | 0.76 | 0.00 | 109384 | 0 | 0 |
05-300SW4 | 216.26 | 216.71 | 0.46 | 0.00 | 109385 | 0 | 0 |
05-300SW4 | 216.71 | 217.93 | 1.22 | 0.00 | 109386 | 0 | 0 |
05-300SW4 | 217.93 | 218.18 | 0.24 | 0.03 | 109387 | 0 | 0 |
05-300SW4 | 218.18 | 219.46 | 1.28 | 0.00 | 109388 | 0 | 0 |
05-300SW4 | 219.46 | 220.80 | 1.34 | 0.00 | 109389 | 0 | 0 |
05-300SW4 | 220.80 | 221.38 | 0.58 | 0.31 | 109390 | 0 | 0 |
05-300SW4 | 221.38 | 222.20 | 0.82 | 0.03 | 109392 | 0 | 0 |
05-300SW4 | 222.20 | 223.72 | 1.52 | 0.00 | 109393 | 0 | 0 |
05-300SW4 | 223.72 | 225.25 | 1.52 | 0.00 | 109394 | 0 | 0 |
05-300SW4 | 225.25 | 226.77 | 1.52 | 0.14 | 109395 | 0 | 0 |
05-300SW4 | 226.77 | 228.30 | 1.52 | 0.00 | 109396 | 0 | 0 |
05-300SW4 | 228.30 | 228.78 | 0.49 | 0.00 | 109397 | 0 | 0 |
05-300SW4 | 228.78 | 229.39 | 0.61 | 0.03 | 109398 | 0 | 0 |
05-300SW4 | 229.39 | 230.92 | 1.52 | 0.00 | 109399 | 0 | 0 |
05-300SW4 | 230.92 | 231.22 | 0.30 | 0.00 | 109401 | 0 | 0 |
05-300SW4 | 231.22 | 232.04 | 0.82 | 0.03 | 109402 | 0 | 0 |
05-300SW4 | 232.04 | 233.57 | 1.52 | 0.00 | 109403 | 0 | 0 |
05-300SW4 | 233.57 | 234.39 | 0.82 | 0.00 | 109404 | 0 | 0 |
05-300SW4 | 234.39 | 235.31 | 0.91 | 0.00 | 109405 | 0 | 0 |
05-300SW4 | 235.31 | 236.83 | 1.52 | 0.00 | 109407 | 0 | 0 |
05-300SW4 | 236.83 | 237.13 | 0.30 | 0.10 | 109408 | 0 | 0 |
05-300SW4 | 237.13 | 238.90 | 1.77 | 0.00 | 109409 | 0 | 0 |
05-300SW4 | 238.90 | 239.09 | 0.18 | 0.00 | 109410 | 0 | 0 |
05-300SW4 | 239.09 | 240.49 | 1.40 | 0.00 | 109412 | 0 | 0 |
05-300SW4 | 240.49 | 240.94 | 0.46 | 0.00 | 109413 | 0 | 0 |
05-300SW4 | 240.94 | 242.01 | 1.07 | 0.00 | 109414 | 0 | 0 |
05-300SW4 | 242.01 | 242.93 | 0.91 | 0.00 | 109415 | 0 | 0 |
05-300SW4 | 242.93 | 243.54 | 0.61 | 0.00 | 109417 | 0 | 0 |
05-300SW4 | 243.54 | 245.06 | 1.52 | 0.00 | 109418 | 0 | 0 |
05-300SW4 | 245.06 | 245.67 | 0.61 | 0.00 | 109419 | 0 | 0 |
05-300SW4 | 245.67 | 246.13 | 0.46 | 0.00 | 109420 | 0 | 0 |
05-300SW4 | 246.13 | 246.89 | 0.76 | 0.00 | 109422 | 0 | 0 |
05-300SW4 | 246.89 | 247.38 | 0.49 | 0.00 | 109423 | 0 | 0 |
05-300SW4 | 247.38 | 248.47 | 1.10 | 0.03 | 109424 | 0 | 0 |
05-300SW4 | 248.47 | 248.96 | 0.49 | 0.03 | 109425 | 0 | 0 |
05-300SW4 | 248.96 | 249.54 | 0.58 | 0.00 | 109426 | 0 | 0 |
05-300SW4 | 249.54 | 250.06 | 0.52 | 0.03 | 109428 | 0 | 0 |
05-300SW4 | 250.06 | 250.97 | 0.91 | 0.00 | 109429 | 0 | 0 |
05-300SW4 | 250.97 | 251.40 | 0.43 | 0.00 | 109430 | 0 | 0 |
05-300SW4 | 251.40 | 252.22 | 0.82 | 0.00 | 109431 | 0 | 0 |
05-300SW4 | 252.22 | 252.62 | 0.40 | 0.00 | 109432 | 0 | 0 |
05-300SW4 | 252.62 | 253.84 | 1.22 | 0.03 | 109434 | 0 | 0 |
05-300SW4 | 253.84 | 254.33 | 0.49 | 0.03 | 109435 | 0 | 0 |
05-300SW4 | 254.33 | 254.63 | 0.30 | 0.17 | 109436 | 0 | 0 |
05-300SW4 | 254.63 | 255.24 | 0.61 | 1.30 | 109437 | 0 | 0 |
218
05-300SW4 | 255.24 | 255.85 | 0.61 | 0.03 | 109438 | 0 | 0 |
05-300SW4 | 255.73 | 256.34 | 0.61 | 0.58 | 109440 | 0 | 0 |
05-300SW4 | 256.34 | 256.95 | 0.61 | 3.33 | 109441 | 0 | 0 |
05-300SW4 | 256.95 | 257.56 | 0.61 | 3.26 | 109442 | 0 | 0 |
05-300SW4 | 257.56 | 258.17 | 0.61 | 0.03 | 109443 | 0 | 0 |
05-300SW4 | 258.17 | 258.78 | 0.61 | 7.75 | 109444 | 0 | 0 |
05-300SW4 | 258.78 | 259.23 | 0.46 | 0.48 | 109445 | 0 | 0 |
05-300SW4 | 259.23 | 259.99 | 0.76 | 4.11 | 109446 | 0 | 0 |
05-300SW4 | 259.99 | 260.82 | 0.82 | 0.75 | 109448 | 0 | 0 |
05-300SW4 | 260.82 | 261.34 | 0.52 | 0.21 | 109449 | 0 | 0 |
05-300SW4 | 261.34 | 261.82 | 0.49 | 10.90 | 109451 | 0 | 0 |
05-300SW4 | 261.82 | 263.35 | 1.52 | 42.21 | 109452 | 0 | 0 |
05-300SW4 | 263.35 | 263.65 | 0.30 | 52.80 | 109453 | 0 | 0 |
05-300SW4 | 263.65 | 264.41 | 0.76 | 1.92 | 109454 | 0 | 0 |
05-300SW4 | 264.41 | 265.02 | 0.61 | 0.24 | 109455 | 0 | 0 |
05-300SW4 | 265.02 | 265.72 | 0.70 | 11.55 | 109457 | 0 | 0 |
05-300SW4 | 265.72 | 267.25 | 1.52 | 11.25 | 109458 | 0 | 0 |
05-300SW4 | 267.25 | 267.92 | 0.67 | 9.57 | 109459 | 0 | 0 |
05-300SW4 | 267.92 | 269.05 | 1.13 | 13.54 | 109460 | 0 | 0 |
05-300SW4 | 269.05 | 269.75 | 0.70 | 0.86 | 109461 | 0 | 0 |
05-300SW4 | 269.75 | 270.97 | 1.22 | 0.10 | 109463 | 0 | 0 |
05-300SW4 | 270.97 | 271.64 | 0.67 | 0.03 | 109464 | 0 | 0 |
05-300SW4 | 271.64 | 273.04 | 1.40 | 0.03 | 109465 | 0 | 0 |
05-300SW4 | 273.04 | 273.28 | 0.24 | 0.00 | 109466 | 0 | 0 |
05-300SW4 | 273.28 | 273.89 | 0.61 | 0.00 | 109467 | 0 | 0 |
05-300SW4 | 273.89 | 275.11 | 1.22 | 0.00 | 109468 | 0 | 0 |
05-300SW4 | 275.11 | 276.58 | 1.46 | 0.03 | 109469 | 0 | 0 |
05-300SW4 | 276.58 | 276.82 | 0.24 | 0.03 | 109471 | 0 | 0 |
05-300SW4 | 276.82 | 277.12 | 0.30 | 0.03 | 109472 | 0 | 0 |
05-300SW4 | 277.12 | 277.34 | 0.21 | 0.03 | 109473 | 0 | 0 |
05-300SW4 | 277.34 | 277.98 | 0.64 | 0.00 | 109474 | 0 | 0 |
05-300SW4 | 277.98 | 278.74 | 0.76 | 0.00 | 109475 | 0 | 0 |
05-300SW4 | 278.74 | 280.11 | 1.37 | 0.00 | 109476 | 0 | 0 |
05-300SW4 | 280.11 | 281.00 | 0.88 | 0.00 | 109477 | 0 | 0 |
05-300SW5 | 205.44 | 206.75 | 1.31 | 0.00 | 109479 | 0 | 0 |
05-300SW5 | 206.75 | 207.11 | 0.37 | 0.03 | 109480 | 0 | 0 |
05-300SW5 | 207.11 | 208.64 | 1.52 | 0.03 | 109481 | 0 | 0 |
05-300SW5 | 208.64 | 210.01 | 1.37 | 0.03 | 109482 | 0 | 0 |
05-300SW5 | 210.01 | 211.53 | 1.52 | 0.00 | 109483 | 0 | 0 |
05-300SW5 | 211.53 | 212.45 | 0.91 | 0.00 | 109484 | 0 | 0 |
05-300SW5 | 212.45 | 212.90 | 0.46 | 0.00 | 109486 | 0 | 0 |
05-300SW5 | 212.90 | 213.21 | 0.30 | 0.03 | 109487 | 0 | 0 |
05-300SW5 | 213.21 | 214.12 | 0.91 | 0.03 | 109488 | 0 | 0 |
05-300SW5 | 214.12 | 214.34 | 0.21 | 0.03 | 109489 | 0 | 0 |
05-300SW5 | 214.34 | 215.80 | 1.46 | 0.10 | 109490 | 0 | 0 |
05-300SW5 | 215.80 | 216.71 | 0.91 | 16.66 | 109492 | 0 | 0 |
05-300SW5 | 216.71 | 217.78 | 1.07 | 7.03 | 109493 | 0 | 0 |
219
05-300SW5 | 217.78 | 218.30 | 0.52 | 24.10 | 109494 | 0 | 0 |
05-300SW5 | 218.30 | 219.15 | 0.85 | 0.45 | 109495 | 0 | 0 |
05-300SW5 | 219.15 | 219.91 | 0.76 | 0.48 | 109496 | 0 | 0 |
05-300SW5 | 219.91 | 220.68 | 0.76 | 0.07 | 109498 | 0 | 0 |
05-300SW5 | 220.68 | 221.28 | 0.61 | 0.00 | 109499 | 0 | 0 |
05-300SW5 | 221.28 | 221.44 | 0.15 | 0.00 | 109500 | 0 | 0 |
05-300SW5 | 221.44 | 222.50 | 1.07 | 0.00 | 109501 | 0 | 0 |
05-300SW5 | 222.50 | 224.03 | 1.52 | 0.00 | 109502 | 0 | 0 |
05-300SW5 | 224.03 | 224.64 | 0.61 | 0.00 | 109504 | 0 | 0 |
05-300SW5 | 224.64 | 226.16 | 1.52 | 0.00 | 109505 | 0 | 0 |
05-300SW5 | 226.16 | 227.69 | 1.52 | 0.00 | 109506 | 0 | 0 |
05-300SW5 | 227.69 | 229.21 | 1.52 | 0.00 | 109507 | 0 | 0 |
05-300SW5 | 229.21 | 230.73 | 1.52 | 0.00 | 109508 | 0 | 0 |
05-300SW5 | 230.73 | 232.26 | 1.52 | 0.00 | 109509 | 0 | 0 |
05-300SW5 | 232.26 | 233.78 | 1.52 | 0.03 | 109511 | 0 | 0 |
05-300SW5 | 233.78 | 235.31 | 1.52 | 0.03 | 109512 | 0 | 0 |
05-300SW5 | 235.31 | 236.46 | 1.16 | 0.03 | 109513 | 0 | 0 |
05-300SW5 | 236.46 | 236.77 | 0.30 | 3.19 | 109514 | 0 | 0 |
05-300SW5 | 236.77 | 238.05 | 1.28 | 0.03 | 109515 | 0 | 0 |
05-300SW5 | 238.05 | 239.33 | 1.28 | 0.03 | 109516 | 0 | 0 |
05-300SW5 | 239.33 | 239.63 | 0.30 | 0.03 | 109517 | 0 | 0 |
05-300SW5 | 239.63 | 240.49 | 0.85 | 0.00 | 109518 | 0 | 0 |
05-300SW5 | 240.49 | 241.10 | 0.61 | 2.30 | 109520 | 0 | 0 |
05-300SW5 | 241.10 | 241.71 | 0.61 | 5.62 | 109521 | 0 | 0 |
05-300SW5 | 241.71 | 242.41 | 0.70 | 18.75 | 109522 | 0 | 0 |
05-300SW5 | 242.41 | 243.02 | 0.61 | 26.91 | 109523 | 0 | 0 |
05-300SW5 | 243.02 | 243.99 | 0.98 | 18.89 | 109524 | 0 | 0 |
05-300SW5 | 243.99 | 245.06 | 1.07 | 45.81 | 109525 | 0 | 0 |
05-300SW5 | 245.06 | 245.67 | 0.61 | 18.03 | 109526 | 0 | 0 |
05-300SW5 | 245.67 | 246.74 | 1.07 | 9.94 | 109528 | 0 | 0 |
05-300SW5 | 246.74 | 247.80 | 1.07 | 0.07 | 109529 | 0 | 0 |
05-300SW5 | 247.80 | 248.87 | 1.07 | 0.07 | 109530 | 0 | 0 |
05-300SW5 | 248.87 | 249.78 | 0.91 | 0.10 | 109532 | 0 | 0 |
05-300SW5 | 249.78 | 250.85 | 1.07 | 0.69 | 109533 | 0 | 0 |
05-300SW5 | 250.85 | 251.31 | 0.46 | 0.10 | 109534 | 0 | 0 |
05-300SW5 | 251.31 | 251.73 | 0.43 | 0.03 | 109535 | 0 | 0 |
05-300SW5 | 251.73 | 252.37 | 0.64 | 0.03 | 109536 | 0 | 0 |
05-300SW5 | 252.37 | 252.74 | 0.37 | 0.07 | 109538 | 0 | 0 |
05-300SW5 | 252.74 | 254.14 | 1.40 | 0.00 | 109539 | 0 | 0 |
05-300SW5 | 254.14 | 254.81 | 0.67 | 0.00 | 109540 | 0 | 0 |
05-300SW5 | 254.81 | 256.34 | 1.52 | 0.00 | 109541 | 0 | 0 |
05-300SW5 | 256.34 | 257.71 | 1.37 | 0.00 | 109543 | 0 | 0 |
05-300SW5 | 257.71 | 258.78 | 1.07 | 0.00 | 109544 | 0 | 0 |
05-300SW5 | 258.78 | 260.09 | 1.31 | 0.03 | 109545 | 0 | 0 |
05-300SW6 | 215.34 | 216.41 | 1.07 | 0.00 | 109546 | 0 | 0 |
05-300SW6 | 216.41 | 217.17 | 0.76 | 0.00 | 109547 | 0 | 0 |
05-300SW6 | 217.17 | 217.93 | 0.76 | 0.00 | 109549 | 0 | 0 |
220
05-300SW6 | 217.93 | 219.46 | 1.52 | 0.00 | 109550 | 0 | 0 |
05-300SW6 | 219.46 | 220.98 | 1.52 | 0.00 | 109551 | 0 | 0 |
05-300SW6 | 220.98 | 221.44 | 0.46 | 0.00 | 109552 | 0 | 0 |
05-300SW6 | 221.44 | 222.20 | 0.76 | 0.00 | 109553 | 0 | 0 |
05-300SW6 | 222.20 | 223.11 | 0.91 | 0.00 | 109554 | 0 | 0 |
05-300SW6 | 223.11 | 224.64 | 1.52 | 0.00 | 109555 | 0 | 0 |
05-300SW6 | 224.64 | 225.86 | 1.22 | 0.00 | 109557 | 0 | 0 |
05-300SW6 | 225.86 | 227.38 | 1.52 | 0.00 | 109558 | 0 | 0 |
05-300SW6 | 227.38 | 228.90 | 1.52 | 0.00 | 109559 | 0 | 0 |
05-300SW6 | 228.90 | 230.43 | 1.52 | 0.00 | 109560 | 0 | 0 |
05-300SW6 | 230.43 | 231.95 | 1.52 | 0.00 | 109561 | 0 | 0 |
05-300SW6 | 231.95 | 233.54 | 1.58 | 0.00 | 109562 | 0 | 0 |
05-300SW6 | 233.54 | 234.70 | 1.16 | 11.69 | 109563 | 0 | 0 |
05-300SW6 | 234.70 | 236.22 | 1.52 | 14.61 | 109564 | 0 | 0 |
05-300SW6 | 236.22 | 236.68 | 0.46 | 22.49 | 109565 | 0 | 0 |
05-300SW6 | 236.68 | 237.13 | 0.46 | 12.99 | 109566 | 0 | 0 |
05-300SW6 | 237.13 | 237.59 | 0.46 | 23.31 | 109567 | 0 | 0 |
05-300SW6 | 237.59 | 238.66 | 1.07 | 33.02 | 109568 | 0 | 0 |
05-300SW6 | 238.81 | 239.57 | 0.76 | 8.67 | 109570 | 0 | 0 |
05-300SW6 | 239.57 | 240.79 | 1.22 | 13.65 | 109571 | 0 | 0 |
05-300SW6 | 240.79 | 242.32 | 1.52 | 0.51 | 109572 | 0 | 0 |
05-300SW6 | 242.32 | 243.84 | 1.52 | 0.82 | 109573 | 0 | 0 |
05-300SW6 | 243.84 | 245.36 | 1.52 | 0.14 | 109574 | 0 | 0 |
05-300SW6 | 245.36 | 246.89 | 1.52 | 0.27 | 109575 | 0 | 0 |
05-300SW6 | 246.89 | 248.41 | 1.52 | 0.82 | 109577 | 0 | 0 |
05-300SW6 | 248.41 | 249.33 | 0.91 | 0.00 | 109578 | 0 | 0 |
05-300SW6 | 249.33 | 250.09 | 0.76 | 5.62 | 109579 | 0 | 0 |
05-300SW6 | 250.09 | 250.39 | 0.30 | 0.00 | 109580 | 0 | 0 |
05-300SW6 | 250.39 | 251.76 | 1.37 | 0.24 | 109581 | 0 | 0 |
05-300SW6 | 251.76 | 252.98 | 1.22 | 0.03 | 109582 | 0 | 0 |
05-300SW6 | 252.98 | 253.59 | 0.61 | 0.34 | 109583 | 0 | 0 |
05-300SW6 | 253.59 | 255.12 | 1.52 | 0.00 | 109584 | 0 | 0 |
05-300SW6 | 255.12 | 256.64 | 1.52 | 0.03 | 109586 | 0 | 0 |
05-300SW6 | 256.64 | 258.17 | 1.52 | 0.03 | 109587 | 0 | 0 |
05-300SW6 | 258.17 | 259.54 | 1.37 | 0.03 | 109588 | 0 | 0 |
05-300SW6 | 259.54 | 260.91 | 1.37 | 0.03 | 109589 | 0 | 0 |
05-300SW6 | 260.91 | 261.82 | 0.91 | 5.18 | 109590 | 0 | 0 |
05-300SW6 | 261.82 | 262.43 | 0.61 | 40.11 | 109591 | 0 | 0 |
05-300SW6 | 262.43 | 263.04 | 0.61 | 24.31 | 109593 | 0 | 0 |
05-300SW6 | 263.04 | 263.65 | 0.61 | 23.90 | 109594 | 0 | 0 |
05-300SW6 | 263.65 | 264.05 | 0.40 | 30.69 | 109595 | 0 | 0 |
05-300SW6 | 264.05 | 264.87 | 0.82 | 12.55 | 109596 | 0 | 0 |
05-300SW6 | 264.87 | 266.09 | 1.22 | 10.70 | 109597 | 0 | 0 |
05-300SW6 | 266.09 | 267.46 | 1.37 | 0.38 | 109599 | 0 | 0 |
05-300SW6 | 267.46 | 267.92 | 0.46 | 0.38 | 109600 | 0 | 0 |
05-300SW6 | 267.92 | 269.44 | 1.52 | 0.03 | 109601 | 0 | 0 |
05-300SW6 | 269.44 | 270.36 | 0.91 | 0.03 | 109602 | 0 | 0 |
221
05-300SW6 | 327.05 | 327.36 | 0.30 | 0.14 | 109604 | 0 | 0 |
05-300SW6 | 327.36 | 328.57 | 1.22 | 0.00 | 109605 | 0 | 0 |
05-300SW6 | 328.57 | 329.43 | 0.85 | 0.51 | 109606 | 0 | 0 |
05-300SW6 | 329.43 | 330.10 | 0.67 | 0.03 | 109607 | 0 | 0 |
05-300SW6 | 330.10 | 331.47 | 1.37 | 0.14 | 109608 | 0 | 0 |
05-300SW6 | 331.47 | 332.84 | 1.37 | 0.62 | 109610 | 0 | 0 |
05-300SW6 | 332.84 | 334.37 | 1.52 | 0.51 | 109611 | 0 | 0 |
05-300SW6 | 334.37 | 335.28 | 0.91 | 0.07 | 109612 | 0 | 0 |
05-300SW6 | 335.28 | 336.80 | 1.52 | 0.03 | 109613 | 0 | 0 |
05-300SW6 | 336.80 | 338.33 | 1.52 | 0.07 | 109614 | 0 | 0 |
05-300SW6 | 338.33 | 339.85 | 1.52 | 0.00 | 109615 | 0 | 0 |
05-300SW6 | 339.85 | 340.16 | 0.30 | 0.03 | 109616 | 0 | 0 |
05-300SW6 | 340.16 | 341.38 | 1.22 | 0.00 | 109617 | 0 | 0 |
05-300SW6 | 341.38 | 342.75 | 1.37 | 0.03 | 109618 | 0 | 0 |
05-300SW6 | 342.75 | 344.12 | 1.37 | 0.00 | 109619 | 0 | 0 |
05-300SW6 | 344.12 | 345.49 | 1.37 | 0.00 | 109620 | 0 | 0 |
05-300SW6 | 345.49 | 346.56 | 1.07 | 0.00 | 109621 | 0 | 0 |
05-300SW6 | 346.56 | 347.17 | 0.61 | 0.00 | 109622 | 0 | 0 |
05-330SW3 | 204.22 | 205.13 | 0.91 | 0.14 | 109788 | 0 | 0 |
05-330SW3 | 205.13 | 206.20 | 1.07 | 6.93 | 109789 | 0 | 0 |
05-330SW3 | 206.20 | 206.47 | 0.27 | 2.37 | 109790 | 0 | 0 |
05-330SW3 | 206.47 | 207.48 | 1.01 | 7.17 | 109791 | 0 | 0 |
05-330SW3 | 207.48 | 207.87 | 0.40 | 19.10 | 109792 | 0 | 0 |
05-330SW3 | 207.87 | 209.06 | 1.19 | 7.41 | 109793 | 0 | 0 |
05-330SW3 | 209.06 | 209.67 | 0.61 | 0.14 | 109794 | 0 | 0 |
05-330SW3 | 209.67 | 210.59 | 0.91 | 0.07 | 109796 | 0 | 0 |
05-330SW3 | 210.59 | 212.11 | 1.52 | 0.07 | 109797 | 0 | 0 |
05-330SW3 | 212.11 | 213.06 | 0.94 | 0.03 | 109798 | 0 | 0 |
05-330SW3 | 213.06 | 213.94 | 0.88 | 0.14 | 109799 | 0 | 0 |
05-330SW3 | 213.94 | 214.43 | 0.49 | 10.11 | 109801 | 0 | 0 |
05-330SW3 | 214.43 | 214.82 | 0.40 | 18.45 | 109802 | 0 | 0 |
05-330SW3 | 214.82 | 215.65 | 0.82 | 16.94 | 109803 | 0 | 0 |
05-330SW3 | 215.65 | 216.10 | 0.46 | 18.34 | 109804 | 0 | 0 |
05-330SW3 | 216.10 | 216.41 | 0.30 | 8.50 | 109806 | 0 | 0 |
05-330SW3 | 216.41 | 217.93 | 1.52 | 7.30 | 109807 | 0 | 0 |
05-330SW3 | 217.93 | 219.15 | 1.22 | 7.44 | 109808 | 0 | 0 |
05-330SW3 | 219.15 | 220.68 | 1.52 | 7.27 | 109809 | 0 | 0 |
05-330SW3 | 220.68 | 222.11 | 1.43 | 10.80 | 109810 | 0 | 0 |
05-330SW3 | 222.11 | 223.11 | 1.01 | 6.65 | 109812 | 0 | 0 |
05-330SW3 | 223.11 | 223.42 | 0.30 | 0.07 | 109813 | 0 | 0 |
05-330SW3 | 223.42 | 223.88 | 0.46 | 2.13 | 109814 | 0 | 0 |
05-330SW3 | 223.88 | 224.94 | 1.07 | 1.06 | 109815 | 0 | 0 |
05-330SW3 | 224.94 | 225.70 | 0.76 | 0.14 | 109816 | 0 | 0 |
05-330SW3 | 225.70 | 226.31 | 0.61 | 0.03 | 109818 | 0 | 0 |
05-330SW3 | 226.31 | 227.38 | 1.07 | 0.00 | 109819 | 0 | 0 |
05-330SW3 | 227.38 | 227.99 | 0.61 | 0.03 | 109820 | 0 | 0 |
05-330SW3 | 227.99 | 229.67 | 1.68 | 0.00 | 109821 | 0 | 0 |
222
05-330SW3 | 229.67 | 230.12 | 0.46 | 0.00 | 109822 | 0 | 0 |
05-330SW3 | 230.12 | 230.73 | 0.61 | 1.10 | 109823 | 0 | 0 |
05-330SW3 | 230.73 | 232.56 | 1.83 | 0.03 | 109824 | 0 | 0 |
05-330SW3 | 232.56 | 233.63 | 1.07 | 0.45 | 109825 | 0 | 0 |
05-330SW3 | 251.76 | 252.68 | 0.91 | 0.00 | 109827 | 0 | 0 |
05-330SW3 | 252.68 | 253.59 | 0.91 | 0.10 | 109828 | 0 | 0 |
05-330SW3 | 270.05 | 270.66 | 0.61 | 1.85 | 109829 | 0 | 0 |
05-330SW3 | 270.66 | 270.97 | 0.30 | 0.10 | 109830 | 0 | 0 |
05-330SW3 | 270.97 | 271.58 | 0.61 | 0.00 | 109831 | 0 | 0 |
05-330SW3 | 271.58 | 272.03 | 0.46 | 0.27 | 109832 | 0 | 0 |
05-330SW3 | 272.03 | 273.10 | 1.07 | 0.00 | 109834 | 0 | 0 |
05-330SW3 | 273.10 | 274.62 | 1.52 | 0.07 | 109835 | 0 | 0 |
05-330SW3 | 274.62 | 275.54 | 0.91 | 0.00 | 109836 | 0 | 0 |
05-330SW3 | 275.54 | 276.76 | 1.22 | 0.34 | 109837 | 0 | 0 |
05-330SW3 | 276.76 | 277.37 | 0.61 | 0.31 | 109838 | 0 | 0 |
05-330SW3 | 277.37 | 277.98 | 0.61 | 0.03 | 109839 | 0 | 0 |
05-330SW4 | 138.38 | 138.68 | 0.30 | 4.53 | 109676 | 0 | 0 |
05-330SW4 | 138.68 | 139.42 | 0.73 | 1.47 | 109677 | 0 | 0 |
05-330SW4 | 139.42 | 140.51 | 1.10 | 0.03 | 109678 | 0 | 0 |
05-330SW4 | 140.51 | 140.82 | 0.30 | 0.51 | 109679 | 0 | 0 |
05-330SW4 | 140.82 | 141.73 | 0.91 | 0.86 | 109680 | 0 | 0 |
05-330SW4 | 141.73 | 142.04 | 0.30 | 0.00 | 109681 | 0 | 0 |
05-330SW4 | 197.82 | 199.34 | 1.52 | 0.00 | 109682 | 0 | 0 |
05-330SW4 | 199.34 | 200.16 | 0.82 | 0.00 | 109683 | 0 | 0 |
05-330SW4 | 200.16 | 200.86 | 0.70 | 0.03 | 109684 | 0 | 0 |
05-330SW4 | 200.86 | 201.78 | 0.91 | 0.00 | 109686 | 0 | 0 |
05-330SW4 | 201.78 | 202.27 | 0.49 | 0.03 | 109687 | 0 | 0 |
05-330SW4 | 202.27 | 203.00 | 0.73 | 0.03 | 109688 | 0 | 0 |
05-330SW4 | 203.00 | 203.76 | 0.76 | 0.99 | 109689 | 0 | 0 |
05-330SW4 | 203.76 | 204.37 | 0.61 | 0.38 | 109690 | 0 | 0 |
05-330SW4 | 204.37 | 205.74 | 1.37 | 8.16 | 109691 | 0 | 0 |
05-330SW4 | 205.74 | 206.96 | 1.22 | 0.45 | 109692 | 0 | 0 |
05-330SW4 | 206.96 | 208.64 | 1.68 | 0.55 | 109694 | 0 | 0 |
05-330SW4 | 208.64 | 209.09 | 0.46 | 0.10 | 109695 | 0 | 0 |
05-330SW4 | 209.09 | 209.70 | 0.61 | 0.03 | 109696 | 0 | 0 |
05-330SW4 | 209.70 | 210.46 | 0.76 | 1.89 | 109697 | 0 | 0 |
05-330SW4 | 210.46 | 211.35 | 0.88 | 0.03 | 109698 | 0 | 0 |
05-330SW4 | 211.35 | 212.26 | 0.91 | 0.24 | 109699 | 0 | 0 |
05-330SW4 | 212.26 | 213.06 | 0.79 | 2.54 | 109700 | 0 | 0 |
05-330SW4 | 213.06 | 214.58 | 1.52 | 0.31 | 109701 | 0 | 0 |
05-330SW4 | 214.58 | 215.28 | 0.70 | 13.41 | 109702 | 0 | 0 |
05-330SW4 | 215.28 | 215.89 | 0.61 | 2.06 | 109703 | 0 | 0 |
05-330SW4 | 215.89 | 216.07 | 0.18 | 0.21 | 109704 | 0 | 0 |
05-330SW4 | 216.07 | 217.63 | 1.55 | 27.60 | 109705 | 0 | 0 |
05-330SW4 | 217.63 | 218.85 | 1.22 | 0.45 | 109706 | 0 | 0 |
05-330SW4 | 218.85 | 219.15 | 0.30 | 0.00 | 109708 | 0 | 0 |
05-330SW4 | 219.15 | 219.76 | 0.61 | 0.03 | 109709 | 0 | 0 |
223
05-330SW4 | 219.76 | 220.68 | 0.91 | 1.06 | 109710 | 0 | 0 |
05-330SW4 | 220.68 | 221.22 | 0.55 | 0.10 | 109711 | 0 | 0 |
05-330SW4 | 221.22 | 221.89 | 0.67 | 0.72 | 109713 | 0 | 0 |
05-330SW4 | 221.89 | 223.36 | 1.46 | 6.17 | 109714 | 0 | 0 |
05-330SW4 | 223.36 | 224.67 | 1.31 | 25.71 | 109715 | 0 | 0 |
05-330SW4 | 224.67 | 225.06 | 0.40 | 48.62 | 109716 | 0 | 0 |
05-330SW4 | 225.06 | 226.28 | 1.22 | 8.78 | 109717 | 0 | 0 |
05-330SW4 | 226.28 | 227.26 | 0.98 | 27.29 | 109718 | 0 | 0 |
05-330SW4 | 227.26 | 228.39 | 1.13 | 36.00 | 109720 | 0 | 0 |
05-330SW4 | 228.39 | 228.57 | 0.18 | 58.11 | 109721 | 0 | 0 |
05-330SW4 | 228.57 | 228.87 | 0.30 | 6.82 | 109722 | 0 | 0 |
05-330SW4 | 228.87 | 229.36 | 0.49 | 47.01 | 109723 | 0 | 0 |
05-330SW4 | 229.36 | 229.73 | 0.37 | 22.22 | 109724 | 0 | 0 |
05-330SW4 | 229.73 | 230.64 | 0.91 | 25.61 | 109725 | 0 | 0 |
05-330SW4 | 230.64 | 231.95 | 1.31 | 8.98 | 109726 | 0 | 0 |
05-330SW4 | 231.95 | 232.56 | 0.61 | 1.58 | 109727 | 0 | 0 |
05-330SW4 | 232.56 | 233.78 | 1.22 | 11.86 | 109728 | 0 | 0 |
05-330SW4 | 233.78 | 234.39 | 0.61 | 0.07 | 109730 | 0 | 0 |
05-330SW4 | 234.39 | 235.92 | 1.52 | 0.07 | 109731 | 0 | 0 |
05-330SW4 | 235.92 | 237.44 | 1.52 | 0.00 | 109732 | 0 | 0 |
05-330SW4 | 237.44 | 238.96 | 1.52 | 0.00 | 109733 | 0 | 0 |
05-330SW4 | 238.96 | 240.49 | 1.52 | 0.00 | 109734 | 0 | 0 |
05-330SW4 | 240.49 | 242.01 | 1.52 | 0.00 | 109735 | 0 | 0 |
05-330SW4 | 242.01 | 243.54 | 1.52 | 0.00 | 109736 | 0 | 0 |
05-330SW4 | 243.54 | 244.14 | 0.61 | 0.00 | 109737 | 0 | 0 |
05-330SW4 | 244.14 | 244.60 | 0.46 | 0.00 | 109738 | 0 | 0 |
05-330SW4 | 244.60 | 245.67 | 1.07 | 0.00 | 109739 | 0 | 0 |
05-330SW4 | 245.67 | 245.97 | 0.30 | 0.00 | 109740 | 0 | 0 |
05-330SW4 | 245.97 | 246.43 | 0.46 | 0.00 | 109741 | 0 | 0 |
05-330SW4 | 246.43 | 247.65 | 1.22 | 0.00 | 109743 | 0 | 0 |
05-330SW4 | 247.65 | 249.72 | 2.07 | 0.17 | 109744 | 0 | 0 |
05-330SW4 | 249.72 | 250.55 | 0.82 | 0.21 | 109745 | 0 | 0 |
05-330SW4 | 250.55 | 252.07 | 1.52 | 0.03 | 109746 | 0 | 0 |
05-330SW4 | 252.07 | 253.59 | 0.00 | 0.24 | 109748 | 0 | 0 |
05-330SW4 | 253.59 | 255.27 | 1.68 | 0.00 | 109749 | 0 | 0 |
05-330SW4 | 255.27 | 256.34 | 1.07 | 0.00 | 109750 | 0 | 0 |
05-330SW4 | 256.34 | 257.65 | 1.31 | 0.07 | 109751 | 0 | 0 |
05-330SW4 | 257.65 | 258.47 | 0.82 | 0.03 | 109753 | 0 | 0 |
05-330SW4 | 258.47 | 259.23 | 0.76 | 0.00 | 109754 | 0 | 0 |
05-330SW4 | 259.23 | 260.30 | 1.07 | 0.03 | 109755 | 0 | 0 |
05-330SW4 | 260.30 | 261.82 | 1.52 | 0.00 | 109756 | 0 | 0 |
05-330SW4 | 261.82 | 263.35 | 1.52 | 0.00 | 109757 | 0 | 0 |
05-330SW4 | 263.35 | 264.23 | 0.88 | 0.00 | 109758 | 0 | 0 |
05-330SW4 | 264.23 | 265.18 | 0.94 | 0.00 | 109759 | 0 | 0 |
05-330SW4 | 265.18 | 265.79 | 0.61 | 0.00 | 109760 | 0 | 0 |
05-330SW4 | 265.79 | 267.61 | 1.83 | 0.00 | 109761 | 0 | 0 |
05-330SW4 | 267.61 | 268.22 | 0.61 | 0.00 | 109762 | 0 | 0 |
224
05-330SW4 | 268.22 | 269.75 | 1.52 | 0.00 | 109763 | 0 | 0 |
05-330SW4 | 269.75 | 270.81 | 1.07 | 0.00 | 109764 | 0 | 0 |
05-330SW4 | 270.81 | 271.88 | 1.07 | 0.00 | 109765 | 0 | 0 |
05-330SW4 | 271.88 | 273.19 | 1.31 | 0.55 | 109766 | 0 | 0 |
05-330SW4 | 273.19 | 274.02 | 0.82 | 0.00 | 109768 | 0 | 0 |
05-330SW4 | 274.02 | 275.54 | 1.52 | 0.00 | 109769 | 0 | 0 |
05-330SW4 | 275.54 | 276.64 | 1.10 | 0.00 | 109770 | 0 | 0 |
05-330SW4 | 276.64 | 278.16 | 1.52 | 0.00 | 109771 | 0 | 0 |
05-330SW4 | 278.16 | 279.68 | 1.52 | 0.00 | 109772 | 0 | 0 |
05-330SW4 | 279.68 | 281.21 | 1.52 | 0.00 | 109773 | 0 | 0 |
05-330SW4 | 281.21 | 282.85 | 1.65 | 0.00 | 109775 | 0 | 0 |
05-330SW4 | 282.85 | 283.77 | 0.91 | 0.03 | 109776 | 0 | 0 |
05-330SW4 | 283.77 | 285.87 | 2.10 | 0.27 | 109777 | 0 | 0 |
05-330SW4 | 285.87 | 286.82 | 0.94 | 0.00 | 109779 | 0 | 0 |
05-330SW4 | 286.82 | 288.34 | 1.52 | 0.00 | 109780 | 0 | 0 |
05-330SW4 | 288.34 | 289.86 | 1.52 | 0.00 | 109781 | 0 | 0 |
05-330SW4 | 289.86 | 291.08 | 1.22 | 0.00 | 109782 | 0 | 0 |
05-330SW4 | 291.08 | 292.61 | 1.52 | 0.00 | 109783 | 0 | 0 |
05-330SW4 | 292.61 | 293.83 | 1.22 | 0.00 | 109784 | 0 | 0 |
05-330SW4 | 293.83 | 295.35 | 1.52 | 0.00 | 109786 | 0 | 0 |
05-330SW5 | 133.14 | 133.81 | 0.67 | 0.00 | 109626 | 0 | 0 |
05-330SW5 | 133.81 | 135.21 | 1.40 | 0.00 | 109627 | 0 | 0 |
05-330SW5 | 135.21 | 135.70 | 0.49 | 0.00 | 109628 | 0 | 0 |
05-330SW5 | 135.70 | 136.86 | 1.16 | 0.03 | 109629 | 0 | 0 |
05-330SW5 | 226.10 | 226.77 | 0.67 | 0.00 | 109631 | 0 | 0 |
05-330SW5 | 226.77 | 227.84 | 1.07 | 0.00 | 109632 | 0 | 0 |
05-330SW5 | 227.84 | 229.21 | 1.37 | 0.00 | 109633 | 0 | 0 |
05-330SW5 | 229.21 | 230.12 | 0.91 | 0.00 | 109634 | 0 | 0 |
05-330SW5 | 230.12 | 230.89 | 0.76 | 0.65 | 109636 | 0 | 0 |
05-330SW5 | 230.89 | 231.22 | 0.34 | 3.98 | 109637 | 0 | 0 |
05-330SW5 | 231.22 | 232.11 | 0.88 | 0.03 | 109638 | 0 | 0 |
05-330SW5 | 232.11 | 233.17 | 1.07 | 8.67 | 109639 | 0 | 0 |
05-330SW5 | 233.17 | 234.39 | 1.22 | 10.94 | 109640 | 0 | 0 |
05-330SW5 | 234.39 | 235.61 | 1.22 | 10.80 | 109641 | 0 | 0 |
05-330SW5 | 235.61 | 236.07 | 0.46 | 5.55 | 109642 | 0 | 0 |
05-330SW5 | 236.07 | 236.52 | 0.46 | 12.34 | 109643 | 0 | 0 |
05-330SW5 | 236.52 | 237.44 | 0.91 | 12.10 | 109644 | 0 | 0 |
05-330SW5 | 237.44 | 238.66 | 1.22 | 1.61 | 109645 | 0 | 0 |
05-330SW5 | 238.66 | 239.45 | 0.79 | 4.18 | 109647 | 0 | 0 |
05-330SW5 | 239.45 | 240.27 | 0.82 | 0.07 | 109648 | 0 | 0 |
05-330SW5 | 240.27 | 240.49 | 0.21 | 0.03 | 109649 | 0 | 0 |
05-330SW5 | 240.49 | 241.07 | 0.58 | 4.70 | 109650 | 0 | 0 |
05-330SW5 | 241.07 | 241.40 | 0.34 | 2.85 | 109652 | 0 | 0 |
05-330SW5 | 241.40 | 241.68 | 0.27 | 7.75 | 109653 | 0 | 0 |
05-330SW5 | 241.68 | 242.01 | 0.34 | 0.58 | 109654 | 0 | 0 |
05-330SW5 | 242.01 | 242.47 | 0.46 | 2.43 | 109655 | 0 | 0 |
05-330SW5 | 242.47 | 243.17 | 0.70 | 1.82 | 109657 | 0 | 0 |
225
05-330SW5 | 243.17 | 243.54 | 0.37 | 6.99 | 109658 | 0 | 0 |
05-330SW5 | 243.54 | 244.91 | 1.37 | 30.62 | 109659 | 0 | 0 |
05-330SW5 | 244.91 | 246.28 | 1.37 | 13.61 | 109660 | 0 | 0 |
05-330SW5 | 246.28 | 247.50 | 1.22 | 0.14 | 109662 | 0 | 0 |
05-330SW5 | 247.50 | 248.38 | 0.88 | 0.07 | 109663 | 0 | 0 |
05-330SW5 | 248.38 | 248.72 | 0.34 | 0.10 | 109664 | 0 | 0 |
05-330SW5 | 248.72 | 249.63 | 0.91 | 0.03 | 109665 | 0 | 0 |
05-330SW5 | 270.97 | 271.58 | 0.61 | 0.00 | 109667 | 0 | 0 |
05-330SW5 | 271.58 | 272.80 | 1.22 | 0.03 | 109668 | 0 | 0 |
05-330SW5 | 272.80 | 273.41 | 0.61 | 0.03 | 109669 | 0 | 0 |
05-330SW5 | 273.41 | 274.02 | 0.61 | 0.00 | 109670 | 0 | 0 |
05-330SW5 | 274.02 | 275.54 | 1.52 | 0.00 | 109671 | 0 | 0 |
05-330SW5 | 275.54 | 277.06 | 1.52 | 0.10 | 109672 | 0 | 0 |
05-330SW5 | 277.06 | 277.37 | 0.30 | 0.31 | 109673 | 0 | 0 |
05-330SW5 | 277.37 | 278.89 | 1.52 | 0.03 | 109674 | 0 | 0 |