Ontario Geological Survey
Permanent Link to this Record:
MDI000000002047
Record Name(s) | Dead Horse Creek West - 1977, Dead Horse Creek West Subcomplex - 1987 |
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Related Record Type | |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 2017-Jan-23 |
Date Last Modified | 2024-Apr-30 |
Created By | |
Revised By |
Primary Commodities: Uranium, Thorium, Beryllium, Vanadium, Rare Earth Elements, Yttrium, Zircon
Township or Area: Walsh
Latitude: 48° 50' 21.77" Longitude: -86° 40' 49.51"
UTM Zone: 16 Easting: 523450 Northing: 5409650 UTM Datum: NAD83
Resident Geologist District: Thunder Bay South
NTS Grid: 42D15NE
Point Location Description: Map in 2009 NI 43-101
Location Method: Data Compilation
Access Description: The showing is easily accessed via an all-weather dirt road, Dead Horse Creek, that begins at Provincial Highway 17, the Trans-Canada Highway, about 43 km east of the town of Terrace Bay and 25 km west of the town of Marathon in Northern Ontario. The showing is on the west side of Dead Horse Creek so travel north 3.6 km over the Dead Horse Cr.with acces by foot 665 to the SSW.
1977: Gulf Minerals Canada Ltd. staked a claim group to cover a radioactivity anomaly. Limited prospecting was completed. 1978: Gulf Minerals Canada Ltd. completed geological mapping and diamond drilling (8 holes). 1981: Gulf Minerals Canada Ltd. completed one diamond drill hole (130.1 m). 1982: Property re-staked by D.O. Walsten. No work recorded. 1984: Property re-staked by O. Belisle. 1985: Property optioned to Highwood Resources. A grid was cut and geochemical sampling conducted. Property returned to O. Belisle. 1987: Unocal Canada Ltd. optioned the property from Jet Exploration-O. Belisle. An exploration program of geological mapping, soil geochemistry, stripping, and scintillometer and geophysical (Magnetometer and Radiometric) surveys were completed. 1988: Unocal Canada Ltd. relogged and sampled the Gulf Minerals Canada Ltd. diamond drill holes and carried out channel sampling of the surface trenches. 1991: Unocal Canada Ltd. returned the property to O. Belisle. 2008: J. Ternoskwsky staked the property. 2009: Canadian International Minerals Inc. optioned the property. 2010: Canadian International Minerals contracted Fugro Airborne Surveys to fly a high-resolution magnetic and radiometric survey. 2011: Canadian International Minerals completed prospecting, geological mapping, rock sampling, spectrometer (radiometric) surveys, trenching and channel sampling
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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2.8901 | 42D15NE0029 | 42D15NE0029 |
20 | 42D15NE0052 | 42D15NE0052 |
2.46804 | 20000005831 | 20000005831 |
2.52396 | 20000007356 | 20000007356 |
2.11145 | 42D15NE0023 | 42D15NE0023 |
2.2844 | 42D15NE0051 | 42D15NE0051 |
Province: Superior
Subprovince: Wawa
Terrane: Wawa-Abitibi
Belt: Schreiber-Hemlo
Geological Age: Archean Geochronological Age: 1085 +/- 15Ma max age for Geochron. Age Ref.: Bell et al 1979
Jan 23, 2017 (Andrew Tims) - The West Diatreme appears to narrows from 30 m to a width of 2 m at a vertical depth of 40 m but it is possible that the hole intersected a narrow sheared keel and the diatreme is actually plunging eastward. The breccias have highly varying textures, with wide ranges in fragment size, shape, color, and composition. The Red Breccia dominates the West diatreme. Locally, the rims of the clasts are more intensely altered than the centers of the clasts. The intense red coloration of the clasts implies that possibly hematite has been added, but the conchoidal fracturing and strong response to the potassium channel on the spectrometer would seem to indicate that possibly potassium feldspar has been introduced during metasomatism. fragments weather in relief but the matrix shows pronounced silification. Fragment density is variable although the trend is toward 60 % to 70 % closely packed fragments.
Rock Type | Rank | Composition | Texture | Relationship | Breccia-unsubdivided | 1 | Diatreme | Brecciated | Host |
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Syenite | 2 | Intrudes |
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Aegirine-Augite | Economic | Ore | ||||
2 | Hollandite | Economic | Ore | ||||
3 | Coffinite | Economic | Ore | ||||
4 | Hematite | Economic | Ore | ||||
5 | Magnetite | Economic | Ore | ||||
6 | Rutile | Economic | Ore | ||||
7 | Thorite | Economic | Ore | ||||
8 | Thorogummite | Economic | Ore | ||||
9 | Uraninite | Economic | Ore | ||||
10 | Xenotime | Economic | Ore | ||||
11 | Zircon | Economic | Ore | ||||
1 | Barite | Economic | Gangue | ||||
2 | Pyrite | Economic | Gangue |
Sep 12, 2019 (Andrew Tims) - Grab sample results of:0.6% Be, 1.84% Th, 0.79% U. Rare Earth and beryllium mineralization has been documented. The REE mineralization located so far seems to be associated with uranium and thorium-bearing minerals. Significant U-Be-Zr mineralization lies in Western subcomplex, but not genetically related. Max dimensions are 130 m x 40 m. The western complex is composed of three separate units: An unmineralized volcaniclastic breccia. A cross-cutting main U-Be-Zr mineralized zone and a carbonate dyke. The main U-Be-Zr mineralized zone is easily recognized by its chocolate-brown color and aphanitic-to-vitreous texture, which contrasts strongly with the leucocratic breccia.
Sep 12, 2019 (Therese Pettigrew) - Sample C048072, taken from mafic breccias of the West Diatreme and having 20,000 counts per second reading on a scintillometer, returned assays of 0.22% U, 0.13% Th, 3250 ppm V, 524 ppm Y, and 2.96% Zr (Arseneau and Elliot, 2009).
Rank | Classification |
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1 | Diatreme |
2 | Vein |
Rank | Characteristic |
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1 | Breccia |
Journal - Mineralogy of the Deadhorse Creek Volcaniclastic Breccia Complex, Northwestern Ontario, Canada, pp 212–229
Publication Number: Vol 150,2 Date: 2005
Author: Potter, E., Mitchell, R.
Publisher Name: Contributions to Mineralogy and Petrology
Location:
Publication - Dead Horse Creek Rare Earth Project, Walsh Township Northern Ontario
Publication Number: 2009 43-101 Date: 2009
Author: Arseneau,G., Elliot, C.
Publisher Name: Canadian International MiInerals Inc
Location: SEDAR, filed under Canadian Energy
Thesis - Rare and exotic mineralogy of the western subcomplex of the Deadhorse Creek "diatreme", Northwestern Ontario
Publication Number: Thesis Date: 2004
Author: Potter, E.G.
Publisher Name: Lakehead University
Location: https://knowledgecommons.lakeheadu.ca/handle/2453/4062
Journal - Geology and Geochemistry of the West Dead Horse Creek Rare-Metal Occurrence, Northwestern Ontario.
Publication Number: EMG Vol 2 No 3 Date: 1993
Author: Smyk, M.C., Taylor, R.P., Jones, P.C., Kingston, D.M.
Publisher Name: Exploration Mining Geology
Location:
MonoMap - Geology of the Jackfish-Middleton area, District of Thunder Bay
Publication Number: R050 Date: 1997
Author: Walker J.W.R.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Mineralization in diatreme structures north of Lake Superior
Publication Number: S027 Date: 1982
Author: Sage R.P.
Publisher Name: Ontario Geological Survey
Location:
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