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Occurrence Details


Occurrence Number
115N 041
Occurrence Name
Per
Occurrence Type
Hard-rock
Status
Prospect


General Information

Secondary Commodities: gold, lead, zinc, silver, mercury
Deposit Type(s): Vein Polymetallic Ag-Pb-Zn+/-Au
Location(s): 63.983610 N, -140.784440 W
NTS Mapsheet(s): 115N15
Location Comments: .5 Kilometres
Hand Samples Available at YGS: No

Capsule

Exploration History

Apparently found by placer miners prior to 1920 and first staked as Per, etc cl (76620) in Jun/65 by Per Johnson, who optioned it to General Enterprises Ltd. General Enterprises carried out bulldozer trenching and drilled two short holes in 1965.

Restaked as Dana, etc cl (Y56827) in Jun/70 by J. Bailey, etc, who carried out hand trenching. Cogasa Mines Ltd staked 6 claims (called mineral claims 1 to 6 - YA10391) 3.2 km northeast in Jul/77 in connection with nearby placer work and carried out bulldozer trenching in 1979. J. Trottier staked Martin cl 1-8 (YA47786), Rodger cl 1-8 (YA47818) and YBS cl 1-8 (YA47866) 4.8 km to the southeast in Oct/79. Trottier carried out trenching later in the year. In Jan/80, J. Millhouse staked Vance cl 1-2 (YA52675) 1 km to the north and in May/84, R. Stirling staked Quartz cl 1-4 (YA79880) between the occurrence location and the Vance claims.

Restaked as Delia cl 1-6 (YA87688) in Aug/85 by E. Kreft, who carried out trenching and geochemical sampling later that year. Kreft added Wendy cl 1-9 (YA88114) in 1986 and carried out additional trenching and sampling. Esso Minerals Canada briefly optioned the Delia and Wendy claims later in 1986 and carried out geological mapping and geochemical sampling in August. In Oct/86 Esso staked Sixty Mile cl 1-51 (YA88238) along strike to the southwest and northeast and carried out geological mapping and geochemical rock sampling in 1987. Esso carried out additional geological mapping and geochemical sampling of the northeast block of Sixty Mile claims and magnetometer surveying over their entire claims holdings in 1988. Kreft optioned the Delia and Wendy claims to Klondike Gold Mining Corporation which carried out magnetometer surveying in 1988 and diamond drilling of 4 holes (192 m) in 1989.

Homestake Mining (Canadan) Ltd optioned the Sixty Mile claims in Apr/89 and carried out geological mapping and geochemical rock sampling of newly exposed bedrock in placer pits later in the year.

In May/92, R. Stirling transferred the Quartz claims to J. McFaull. K. Hawker partially restaked the northeast block of Sixty Mile claims as Kurt cl 1-4 (YB81760) in May/96 and Kreft carried out trenching on the Delia claims in the summer of 1996. J. Millhouse staked Vance cl 3-5 (YC04305) to adjoin the northeast end of his existing Vance claims in Jun/97.

Restaked as Dorothy cl 1 (YC07261) by F. Travis and Jay cl 1 (YC07262) by J. Murtagh in May/98. In Aug/98 Kennecott Cananda Exploration Inc staked Sixty cl 1-143 (YC12289) to the northeast, forming a contiguous claim block with other claim groups they had staked or optioned over the previous year in the area to the north (Minfile Occurrences #116C 019, 020, 082 and 146). In Apr/99 Kennecott staked Sixty cl 144-257 (YC13419) at the southeast end of their assembled land package, surrounding this occurrence, and carried out prospecting, geochemical sampling and airborne geophysical surveying over their combined holdings. The following year, Kennecott dropped all of its options in the area.

In 2000, McFaull contracted Amerock Geosciences Ltd to carry out VLF-EM geophysical surveying and prospecting of his Quartz claims.

Capsule Geology

Galena, sphalerite and arsenopyrite occur in a northeast trending vein which cuts a small down-faulted block of Late Cretaceous volcanics that are correlative with Carmacks Group volcanic rocks. The volcanic rocks overlie Late Devonian (?) to mid-Mississippian aged Nasina assemblage schists of the Yukon Tanana Terrane. The vein is about 8 to 60 cm wide and is exposed for up to 60 m along strike. The best chip assay reported was 428.6 g/t Ag, 26.4% Pb, 4.7% Zn, and 1.4 g/t Au across 76 cm. 
Kreft's 1986 trenching tested a 91 m wide zone of altered andesite containing massive pyrite lenses, quartz stockworks, and disseminated chalcopyrite and galena. Specimens from the trenches assayed up to 26 g/t Au and 42.5 g/t Ag. The highest silver values were obtained 460 m north of the main showing area. All four of Klondike's drillholes intersected granodiorite dykes of probable Late Cretaceous age (unit lKgdr) containing quartz veins and stockworks with pyrite and arsenopyrite. DDH #2 intersected 12 m grading 7.1 g/t Au, including 1.5 m grading 41.1 g/t Au. The mineralized intersection was also enriched in Zn and Hg (E. Kreft, personal communication).

Homestake's 1989 samples contained up to 402 ppb Au and 7.9 ppm Ag. Brecciated andesite with 1-2% pyrite returned a value of 204 ppb Au and was also anomalous levels of silver, arsenic, bismuth, copper and tellurium.

Cinnabar was recovered in sluice boxes by placer miners along this portion of the Sixty Mile River gravels but the source was never found. Esso investigated strongly fractured andesite flows and andesite breccia with local clay alteration but obtained disappointing results.

Glasmacher and Friedrich (1992) recognized two types of veins in this area: a gold-bearing pyrite-arsenopyrite type and a silver-bearing galena-sphalerite type, both of which they related to Late Cretaceous volcanic activity. The Miller Creek veins are of the second type, and this is reflected in the notably higher silver content (9 to 35 weight %) of gold nuggets from the lower part of Miller Creek. Four stages of mineralization are recognized: (1) iron-poor sphalerite-galena-quartz; (2) iron-rich sphalerite-pyrite-pyrrhotite-arsenopyrite-chalcopyrite-galena-siderite; (3) sphalerite-pyrite-marcasite-chalcopyrite-galena-siderite-ankerite-dolomite-calcite; (4) iron-poor sphalerite-pyrite-tetrahedrite-polybasite-pearcite-pyrostilpnite-chalcedony-ankerite-dolomite-calcite. Most of the silver was deposited during Stage 4. Fluid inclusions indicate that the veins formed from low temperature, low salinity fluids with a pH of about 4.6.

Geophysical surveying carried out on McFaull¿s Quartz claims located four weak VLF-EM conductors. Limited prospecting and sampling (two grab samples) carried out at the same time as the surveying failed to detect any significant mineral occurrences. Analysis of quartz vein material collected just east of the claim block returned 13 ppb Au and 858 ppm As.

Location Map

Last Updated: Jul 7, 2022

Work History

Year Work Type Comment
2020 Airphotography: Orthophoto
2011 Ground Geophysics: EM
2011 Ground Geophysics: IP
2011 Other: Line Cutting
2010 Airborne Geophysics: Gamma-Ray Spectrometry
2010 Airborne Geophysics: Magnetic
2010 Drilling: Auger
2010 Drilling: Diamond
2010 Geochemistry: Rock
2010 Geochemistry: Soil
2010 Trenching: Mechanical
1999 Airborne Geophysics: Magnetic Also radiometric survey.
1999 Geochemistry: Soil Also rock sampling.
1999 Other: Prospecting
1996 Trenching: Mechanical
1990 Drilling: Auger
1990 Geochemistry: Drill Cuttings
1989 Drilling: Diamond Four holes, 192 m.
1988 Geochemistry: Rock
1988 Geology: Bedrock Mapping
1988 Ground Geophysics: Magnetics
1988 Drilling: Diamond 7 holes, 770.34 m
1986 Geochemistry: Rock
1986 Geology: Bedrock Mapping
1986 Trenching: Hand
1986 Other: Prospecting
1979 Trenching: Mechanical
1970 Trenching: Hand
1969 Drilling: Diamond
1969 Geochemistry: Drill Core
1969 Geochemistry: Rock
1969 Geochemistry: Silt
1969 Geochemistry: Soil
1969 Geology: Bedrock Mapping
1969 Other: Cursory Property Visit
1969 Trenching: Mechanical
1965 Drilling: Diamond Two short holes, footage unknown.
1965 Trenching: Mechanical

Regional Geology - Terrane

Group: Intermontane
Affinity: W Laurentia
Name: Yukon-Tanana
Realm: peri-Laurentian


Regional Geology - Bedrock

Supergroup:
Group/Suite: Finlayson
Formation:
Member:
Terrane: Yukon-Tanana
Period Max: Devonian
Age Max: 365 MA
Period Min: Carboniferous
Age Min: 345 MA
Rock Major: cl-bi-schist/amphibolite/hb-gneiss/ac-pg-cl-bi-schist/pg-ac-cl-schist/phyllite/quartzite/ultramafics
Rock Minor:
Reference: Mortensen (1996) - YGS OF 1996-1(G)
Geological Unit (1M): DMF
Geological Unit (250K): DMF1

Assessment Reports that overlap occurrence

Report Number Year Title Worktypes Holes Drilled Meters Drilled
096208 2010 SIXTY MILE Property-2010 Geological, Geochemical, Geophysical and Auger, RAB and Diamond Drilling Gamma-Ray Spectrometry - Airborne Geophysics, Magnetic - Airborne Geophysics, Auger - Drilling, Diamond - Drilling, Rotary - Drilling, Drill Core - Geochemistry, Rock - Geochemistry, Soil - Geochemistry, Bedrock Mapping - Geology, Mechanical - Trenching 443 7289.37
094055 1999 Report on the 1999 Geological, Geochemical and Geophysical Work on the SIXTY MILE Property Gamma-Ray Spectrometry - Airborne Geophysics, Magnetic - Airborne Geophysics, Rock - Geochemistry, Silt - Geochemistry, Soil - Geochemistry, Bedrock Mapping - Geology, Detailed Bedrock Mapping - Geology, Gravity Survey - Ground Geophysics, Petrographic - Lab Work/Physical Studies, Prospecting - Other, Mechanical - Trenching
120128 1990 Auger Drilling Report for Prospecting Lease 7684, Sixtymile River, Dawson Mining District Auger - Drilling, Drill Cuttings - Geochemistry, Panning - Placer Processing 8 72.50
091734 1986 1986 Exploration Program-Geological Mapping and Sampling on the Delia and Wendy Quartz Claims, Yukon Territory Rock - Geochemistry, Detailed Bedrock Mapping - Geology, Prospecting - Other
061130 1969 Report on the 1969 Exploration Program in the Sixtymile River Area, Yukon Territory Diamond - Drilling, Drill Core - Geochemistry, Rock - Geochemistry, Silt - Geochemistry, Soil - Geochemistry, Detailed Bedrock Mapping - Geology, Mechanical - Trenching 8 431.59
060840 1969 Summary Report for the Connaught Mines Ltd.-Sixty Mile Area, Yukon Cursory Property Visit - Other, Data Compilation - Pre-existing Data

Related References

Number Title Page(s) Document Type
ARMC004674 Correspondences Re: Activities in Miller Creek, Fifty mile resources Miscellaneous Company Documents
88-004 Gold-Silver Property 'Delia-Wendy' Sixtymile River Area, Yukon Territory, Canada YMEP Report
Citations
GEOLOGICAL SURVEY OF CANADA, Memoir 123, p. 52.
GEOLOGICAL SURVEY OF CANADA, Paper 66-31, p. 26-28.
GLASMACHER, U., 1985. Geology, Petrography and Mineralization in the Sixty Mile River Area, Yukon Territory, Canada. Unpublished Diploma thesis, Technical University of Aachen, Germany.
GLASMACHER, U., and FRIEDRICH, G., 1992. Volcanic-hosted epithermal-type gold-sulphide mineralization and associated enrichment processes, Sixtymile River area, Yukon Territory, Canada. In: Yukon Geology Vol. 3, Exploration and Geological Services Division, DIAND, p. 271-291.
MORTENSEN, J.K., 1988. Geology of Southwestern Dawson Map Area, scale 1:250 000, Geological Survey of Canada, Open File 1927.
MORTENSEN, J.K., 1990. Geology and U-Pb geochronology of the Klondike District, west central Yukon Territory. Canadian Journal of Earth Sciences, v. 27, p. 903-914.
MORTENSEN, J.K., 1996. Geological Compilation Maps of the Northern Stewart River map area Klondike and Sixtymile Districts (115N/15,16; 115O/13,14 and parts of 115O/15,16), scale 1:50 000. Exploration and Geological Services Division, Yukon, Indian and Northern Affairs Canada, Open File 1996-1 (G).
YUKON EXPLORATION 1985-86, p. 369, 377; 1987, p. 287; 1988, p. 39, 199, 205; 1989, p. 126.
YUKON EXPLORATION AND GEOLOGY 1999, p. 15.

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