General Information
Secondary Commodities: copper, zinc, silver, lead
Aliases: Harp
Deposit Type(s): Sediment hosted Mississippi Valley-Type Pb-Zn (MVT)
Location(s): 64.736670 N, -139.719720 W
NTS Mapsheet(s): 116B12
Location Comments: .5 Kilometres
Hand Samples Available at YGS: No
Capsule
Work History
Staked in Aug/74 as OZ cl 1-81 (Y89931) by Dynasty Explorations Limited, which conducted mapping and soil and rock geochem sampling later in the year.
In 1975, the OZ group was transferred to Cyprus Anvil Mining Corp, which drilled 3 holes totalling 379.5 m and completed grid soil sampling, mapping and hand trenching
Restaked as Harp cl 1-24 (YA64908) in Feb/82 by Enterprise Exploration Limited and transferred to U. Schmidt & E. Jensen, who prepared a topographic map in 1985. In Mar/91, the claims were transferred to U. Schmidt, who staked Harp cl 11-42 (YB40149). In Jul/95 the remaining surviving Harp claims (YA64908) were transferred to Jensen.
1 km to the north the following year Schmidt completed a property site map showing the location of claim posts, trenches and old drill hole locations. Schmidt also completed grid soil sampling, a radiometric survey and prospecting program. In Dec/96 the Corn claims were optioned to Atna Resources Ltd.
In Jun/96, High Sense Geophysics Ltd. under contract to Equity Engineering Limited flew a regional, helicopter borne, magnetic and radiometric survey over most of the Coal Creek Inlier, but no new claims were staked.
Capsule Geology
This occurrence is underlain by Middle Proterozoic Pinguicula Group siliceous carbonate rocks, Middle Proterozoic Wernecke breccias and mafic intrusive rocks (Hart River ?); and Lower Proterozoic Gillespie Lake orange weathering silty carbonates and shales (Thorkelson, 2000).
The area is noted to host two types of mineralization. The first reported as lead-zinc mineralization in stratabound sulphides occuring in a 1.5 to 15 m thick bed of black shale, argillite and chert containing bands and disseminated grains of galena and minor sphalerite with occasional barite. This type of mineralization is thought to reflect a sedimentary origin although best grades (up to 30% Pb + Zn with 102.9 g/t Ag) were found in brecciated zones related to faulting. The best assay from the 1975 drilling, which tested the central of three showings, was 2.2% Pb + Zn over 1.5 m. Also, dolomite breccias in adjacent rocks contain fracture fillings of calcite, barite and red-brown-yellow sphalerite with minor galena. These appear to be related to faulting.
The second type of mineralization reports lead-zinc-copper mineralization suspected to originate from the Wernecke Breccia unit. During Schmidt¿s 1996 program a ¿heart-shaped¿ breccia pipe was confirmed from local float with chalcopyrite mineralization and alteration similar to Wernecke breccias. Anomalous soils over the area assayed as high as 1181 ppm Pb, 1704 ppm Zn, 1.8m ppm Ag, and 127 ppm Cu.
The regional airborne geophysical survey outlined numerous northeast trending features which were interpreted to be faults..
References
CYPRUS ANVIL MINING CORPORATION LTD., Dec/75. Assessment Report #090041 by P. Dean.
DYNASTY EXPLORATIONS LIMITED, May/75. Assessment Report #061213 by P. Dean.
GORDEY, S.P., MAKEPEACE, A.J., Bedrock Geology, Yukon Territory, 1:1000 000 scale map. Geological Survey of Canada, Open File 3754 and Exploration and Geological Services Division, Yukon Indian and Northern Affairs Canada, Open File 2000-12.
ETHERIDGE HENLEY WILLIAMS & HIGH SENSE GEOPHYSICS LIMITED, Feb/97. Assessment Report #093600 by Allen Duffy et al.
MINERAL INDUSTRY REPORT 1974, p. 74-75; 1976, p. 85-86.
LANE, R.A., AND GODWIN, C.I., 1992. Geology of the Ogilvie Mountains Breccias, Coal Creek Inlier (NTS 116B/11,13,14), Yukon Territory. Exploration and Geological Services Division, DIAND, Open File 1992-1.
YUKON EXPLORATION 1985-86, p. 394.
SCHMIDT, U., Mar/85. Assessment Report #091631 by U. Schmidt.
SCHMIDT, U., Apr/97. Assessment Report #093657 by U. Schmidt.
SCHMIDT, U., May/97. Assessment Report #093688. by U. Schmidt.
THORKELSON, D., 2000. Geology and mineral occurrences of the Slats Creek, Fairchild Lake and ¿Dolores Creek¿ areas, Wernecke Mountains (106D/16, 106C/13, 106C/14), Yukon Territory, Bulletin 10.
Staked in Aug/74 as OZ cl 1-81 (Y89931) by Dynasty Explorations Limited, which conducted mapping and soil and rock geochem sampling later in the year.
In 1975, the OZ group was transferred to Cyprus Anvil Mining Corp, which drilled 3 holes totalling 379.5 m and completed grid soil sampling, mapping and hand trenching
Restaked as Harp cl 1-24 (YA64908) in Feb/82 by Enterprise Exploration Limited and transferred to U. Schmidt & E. Jensen, who prepared a topographic map in 1985. In Mar/91, the claims were transferred to U. Schmidt, who staked Harp cl 11-42 (YB40149). In Jul/95 the remaining surviving Harp claims (YA64908) were transferred to Jensen.
1 km to the north the following year Schmidt completed a property site map showing the location of claim posts, trenches and old drill hole locations. Schmidt also completed grid soil sampling, a radiometric survey and prospecting program. In Dec/96 the Corn claims were optioned to Atna Resources Ltd.
In Jun/96, High Sense Geophysics Ltd. under contract to Equity Engineering Limited flew a regional, helicopter borne, magnetic and radiometric survey over most of the Coal Creek Inlier, but no new claims were staked.
Capsule Geology
This occurrence is underlain by Middle Proterozoic Pinguicula Group siliceous carbonate rocks, Middle Proterozoic Wernecke breccias and mafic intrusive rocks (Hart River ?); and Lower Proterozoic Gillespie Lake orange weathering silty carbonates and shales (Thorkelson, 2000).
The area is noted to host two types of mineralization. The first reported as lead-zinc mineralization in stratabound sulphides occuring in a 1.5 to 15 m thick bed of black shale, argillite and chert containing bands and disseminated grains of galena and minor sphalerite with occasional barite. This type of mineralization is thought to reflect a sedimentary origin although best grades (up to 30% Pb + Zn with 102.9 g/t Ag) were found in brecciated zones related to faulting. The best assay from the 1975 drilling, which tested the central of three showings, was 2.2% Pb + Zn over 1.5 m. Also, dolomite breccias in adjacent rocks contain fracture fillings of calcite, barite and red-brown-yellow sphalerite with minor galena. These appear to be related to faulting.
The second type of mineralization reports lead-zinc-copper mineralization suspected to originate from the Wernecke Breccia unit. During Schmidt¿s 1996 program a ¿heart-shaped¿ breccia pipe was confirmed from local float with chalcopyrite mineralization and alteration similar to Wernecke breccias. Anomalous soils over the area assayed as high as 1181 ppm Pb, 1704 ppm Zn, 1.8m ppm Ag, and 127 ppm Cu.
The regional airborne geophysical survey outlined numerous northeast trending features which were interpreted to be faults..
References
CYPRUS ANVIL MINING CORPORATION LTD., Dec/75. Assessment Report #090041 by P. Dean.
DYNASTY EXPLORATIONS LIMITED, May/75. Assessment Report #061213 by P. Dean.
GORDEY, S.P., MAKEPEACE, A.J., Bedrock Geology, Yukon Territory, 1:1000 000 scale map. Geological Survey of Canada, Open File 3754 and Exploration and Geological Services Division, Yukon Indian and Northern Affairs Canada, Open File 2000-12.
ETHERIDGE HENLEY WILLIAMS & HIGH SENSE GEOPHYSICS LIMITED, Feb/97. Assessment Report #093600 by Allen Duffy et al.
MINERAL INDUSTRY REPORT 1974, p. 74-75; 1976, p. 85-86.
LANE, R.A., AND GODWIN, C.I., 1992. Geology of the Ogilvie Mountains Breccias, Coal Creek Inlier (NTS 116B/11,13,14), Yukon Territory. Exploration and Geological Services Division, DIAND, Open File 1992-1.
YUKON EXPLORATION 1985-86, p. 394.
SCHMIDT, U., Mar/85. Assessment Report #091631 by U. Schmidt.
SCHMIDT, U., Apr/97. Assessment Report #093657 by U. Schmidt.
SCHMIDT, U., May/97. Assessment Report #093688. by U. Schmidt.
THORKELSON, D., 2000. Geology and mineral occurrences of the Slats Creek, Fairchild Lake and ¿Dolores Creek¿ areas, Wernecke Mountains (106D/16, 106C/13, 106C/14), Yukon Territory, Bulletin 10.
Location Map
Last Updated: Sep 14, 2018
Work History
Year | Work Type | Comment |
---|---|---|
1996 | Airborne Geophysics: Magnetic | Also radiometric survey . |
1996 | Geochemistry: Soil | |
1996 | Ground Geophysics: Radiometric Survey | |
1996 | Other: Prospecting | |
1996 | Pre-existing Data: Data Compilation | Created property map showing all claim posts, trenches and showing. |
1985 | Airphotography: Interpretation | Used airphotos to construct 1:50 000 topographic base map. |
1975 | Drilling: Diamond | Three holes, 379.5 m. |
1975 | Geochemistry: Soil | |
1975 | Geology: Bedrock Mapping | |
1975 | Trenching: Hand | |
1974 | Geochemistry: Rock | |
1974 | Geology: Bedrock Mapping |
Regional Geology - Terrane
Group: Ancestral North America
Affinity: W Laurentia
Name: North America - basinal strata
Realm: Laurentia
Regional Geology - Bedrock
Supergroup: Wernecke
Group/Suite: Gillespie Lake
Formation:
Member:
Terrane: Laurentia
Period Max: Statherian
Age Max: 1700 MA
Period Min: Statherian
Age Min: 1600 MA
Rock Major: dolomite
Rock Minor: shale
Reference: Thompson et al. (1994) - GSC OF 2849
Geological Unit (1M): lPG
Geological Unit (250K): lPG
Assessment Reports that overlap occurrence
Report Number | Year | Title | Worktypes | Holes Drilled | Meters Drilled |
---|---|---|---|---|---|
095055 | 2007 | Geological Report on the OZ 1-14 Claims | Detailed Bedrock Mapping - Geology | ||
094886 | 2006 | Geochemical Report on the OZ 1-14 Claims | Soil - Geochemistry | ||
093600 | 1996 | Logistics Report for a Helicopter Magneitc and Gamma-Ray Spectrometer Survey of the MONSTER Property | Gamma-Ray Spectrometry - Airborne Geophysics, Magnetic - Airborne Geophysics | ||
091631 | 1982 | Report on Topographic Mapping Harp 1-10 Mineral Claims | Orthophoto - Airphotography, Surveying - Other, Data Compilation - Pre-existing Data | ||
061213 | 1974 | Geological and Geochemical Report on the 1974 Field Work on the OZ Claims | Rock - Geochemistry, Silt - Geochemistry, Soil - Geochemistry, Bedrock Mapping - Geology, Line Cutting - Other, Prospecting - Other |
Related References
Number | Title | Page(s) | Document Type |
---|---|---|---|
ARMC007794 | Detail area map - Coal Creek dome - Reef project - Figure 11 | Geochemical Map | |
ARMC007851 | Orthophoto map - Coal Creek - Oz claims - Job No. 06153-1 | Geoscience Map (General) | |
ARMC016781 | Geochemical map - 116B/12 | Geochemical Map | |
ARMC016782 | Geochemical map - 116B/13 | Geochemical Map | |
ARMC011311 | Coal Creek Dome detail area map - Reef project - Fig. 13 | Geoscience Map (General) | |
ARMC019476 | Field notes - Oz | Miscellaneous Company Documents | |
ARMC011370 | Detailed geochemistry map - Oz claim group - Reef project | Geochemical Map | |
ARMC011372 | Zinc geochemistry contour map - Oz claim group - Reef project | Geochemical Map | |
ARMC011384 | Geology map - Oz group - Reef project - HF9-140 | Geoscience Map (Geological - Bedrock) | |
ARMC011385 | Geology map - Oz group - Reef project - HF9-141 | Geoscience Map (Geological - Bedrock) | |
ARMC013221 | A brief geological report on the Oz and Tart groups | Report | |
ARMC011302 | Geology of Coal Creek Dome - Reef project | Geoscience Map (Geological - Bedrock) | |
ARMC011371 | Lead geochemistry contour map - Oz claim group - Reef project | Geochemical Map | |
ARMC011340 | Geochemical values map - Coal Creek Dome detail area - Reef project - Fig. 13 | Geochemical Map | |
ARMC018621 | Field notes - Reconnaissance contour geochem lines - Kiwi, Tart, Oz, Will | Miscellaneous Company Documents | |
ARMC011303 | Detail area map - Coal Creek Dome - Reef project - Fig. 12 | Geoscience Map (General) |
Citations |
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