Ontario Geological Survey
Permanent Link to this Record:
MDI52G15NW00014
Record Name(s) | Williams Showing - 1939, Dan's Lake - 1939 |
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Related Record Type | SIMPLE |
Record Status | Occurrence |
Date Created | 1995-May-30 |
Date Last Modified | 2021-Nov-23 |
Created By | Q Unknown |
Revised By | Therese Pettigrew |
Primary Commodities: Gold
Township or Area: Six Mile Lake Area
Latitude: 49° 59' 37.36" Longitude: -90° 46' 12.68"
UTM Zone: 15 Easting: 659818 Northing: 5540314 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52G15NW
Point Location Description: Trenching map in Assessment report 52G15NW0021
Location Method: Conversion from MDI
Access Description: Light aircraft equipped with floats or skis can land on sturgeon Lake within 600 m of the prospect. Boats or snow-mobiles can reach the lake from access points off Hwy 599 from OBriens Landing to Cobb Bay.
1939: A.D. Williams did trenching on a showing to the southeast of Dans Lake. Surface sample assays up to 0.024 ounce gold per ton were reported. 1968-69: W.G. Wahl did ground geophysical surveys over the area. 1973: Northex Management carried out mapping and sampling. 1983: Canadex Resources Limited and associated companies conducted a mapping and sampling program on the property. 1984: Canadex carried out trenching.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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52G15NW0078C1 | 52G15NW9257 | 52G15NW9257 |
52G15NW FH-0090A1 | 52G15NW0006 | 52G15NW0006 |
52G15NW-0050 | 52G15NW0021 | 52G15NW0021 |
52G15NW-0088-A1 | 52G15NW0019 | 52G15NW0019 |
Province: Superior
Subprovince: Wabigoon
Belt: Sturgeon Lake
Geological Age: Archean
Dec 07, 2005 (R TUOMI) - The area surrounding the occurrence is underlain by an east trending sequence of massive to pillowed metabasalt and felsic metavolcanics, mainly lithic and crystal tuff. Several outcrops of clastic sediments are interfingered with mafic metabasalt. The sequence is intruded by gabbro and small quartz porphyry intrusives. The largest of these porphyry intrusives is mineralised by fine grained pyrite at its southern contact and this area was trenched by A. D. Williams in 1939.
Rock Type | Rank | Composition | Texture | Relationship | Quartz Porphyry | 1 | Quartz | Host |
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Mafic lava flow-unsubdivided | 2 | Gossanous | Host | |
Vein | 3 | Quartz |
Dec 07, 2005 (R TUOMI) - MINERALIZATION OCCURS IN: contact between porphyry and mafic basalt HOST ROCK: porphyry and mafic basalt OTHER ASSOCIATED ROCK TYPES: 1) clastic metasediments, 2) gabbro.
Feb 13, 2020 (Therese Pettigrew) - South of Dan's Lake a second intrusive, a pink equigranular to porphyritic syenite body (Williams porphyry), is found at the contact between the volcanic cycles. Strongly carbonatized felsic pyroclastics are found to the north of this intrusive (underlying it) and mafic flow and intercalated tuff and chert overlie it (Assessment report 52G15NW0019).
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrite | Economic | Ore | ||||
2 | Gold | Economic | Ore | ||||
Quartz | Alteration | Silicification | 1 | Unknown | Disseminated | ||
Carbonate | Alteration | Carbonatization | 2 | Unknown | Disseminated |
Feb 13, 2020 (Therese Pettigrew) - In 1939, A. Williams submitted sketches of trenching and assays on an 8-claim block. The sketch shows extensive trenching along a syenite/greenstone contact. Marginal notes refer to heavy mineralization in all trenches and state "well mineralized body probably 50 to 60 feet wide and trenched for approximately 1000 feet. Assays made at St. Anthony Mine.” The following assays (grab samples?) are shown: 0.04 opt Au, 0.21 to 2.36 opt Au, 1.6 opt Au, 0.35 opt Au, 0.14 opt Au, and 0.18 opt Au. Mapping and drilling in 1973 revealed a pyritic-carbonate felsic tuff cut by quartz-carbonate veining which returned 0.055 oz. gold per ton over 9 feet in one of two short holes (Assessment report 52G15NW0019).
Dec 07, 2005 (R TUOMI) - Shearing.
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