Ontario Geological Survey
Permanent Link to this Record:
MDI52F13SW00046
| Record Name(s) | Pine Road - 1987, R. Fairservice - 1987 |
|---|---|
| Related Record Type | Simple |
| Related Record(s) | |
| Record Status | Occurrence |
| Date Created | 1987-Apr-10 |
| Date Last Modified | 2023-Oct-25 |
| Created By | |
| Revised By |
Primary Commodities: Uranium
Secondary Commodities: Thorium
Township or Area: Silvery Lake Area
Latitude: 49° 47' 6.81" Longitude: -93° 48' 53.59"
UTM Zone: 15 Easting: 441340.003 Northing: 5515070.001 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52F13SW
Point Location Description: Site determined from sample location in Kenora Assessment File 52F13SE KK-2 AFRO 2.41986
Location Method: Conversion from MDI
Access Description: The western part of uranium-bearing areas is located approximately 30km east of the city of Kenora and the eastern boundary of area is located 50km west of the town of Dryden. Access to the area is via the Trans Canada Highway, bush roads and all terrain vehicle. The Trans Canada Pipeline, the Canadian National Railway and the Canadian Pacific Railway all lie parallel to the Trans Canada Highway for the majority of the property - see topo maps or Landsat images for best access to site.
Uranium was first discovered in the Kenora area in 1949 near the shore of Willard Lake. This was followed by the discovery of the Richard Lake deposit by Campbell and McFarland in the early 1950s and numerous other occurrences, including Hawk Lake, Bee Lake, Kenoratomic, Quebec Ascot, and Viceroy. To date 2008, Richard Lake MDI52F13SW00044) still shows the highest uranium concentrations. Falling uranium prices in the 1950's lead to little exploration in the area until the 1970's when the Ontario Geological Survey (OGS) mapped west of Richard Lake and found numerous additional showings (Pryslak, 1976). In 2008 Delta Uranium Inc. conducted a sampling program to test historical and mineral occurrences and target anomalous areas identified by their airborne radiometric geophysical survey. A surface sampling master map illustrating sampling location and assay results in presented in Kenora District Geologists Assessment File, Delta Uranium Inc., 52F13SE KK-2 AFRO 2.41986
| Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
|---|---|---|
| 2.2768 | 52F11NW0102 | 52F11NW0102 |
Province: Superior
Geological Age: Precambrian
Mar 03, 2011 (C Ravnaas) - The felsic intrusions of the Kenora area consist of granitoid stocks and plutons with the Dryberry Batholith Complex (DBC) encompassing the southern intrusive portion of the Kenora property. Sanborn?Barrie (1991) investigated the DBC in order to determine if the Archean batholithic complex played a role in the mineralization of the adjacent metavolcanic sequences, such as the Lake of the Woods and Vermillion Bay belts. Numerous occurrences of uranium and base metal mineralization are found within the area. Uranium occurrences are often found associated with granite/pegmatite dykes and sills, while base metal mineralization is found within volcanic rocks. Reference: Kenora District Geologists Assessment File, Delta Uranium Inc., 52F13SE KK-2 AFRO 2.41986
Mar 03, 2011 (C Ravnaas) - Uranium occurrences are often found associated with granite/pegmatite dykes and sills. During the 2008 Delta Uranium's sampling program, 99% of samples taken were of granites or pegmatitic granites found in either massive form or dykes. The uranium mineralization found in the granitic and pegmatitic rocks are commonly found on the flanks of the felsic intrusions and at the margins of metasedimentary rafts. The high uranium areas are often found near uranium depleted metasedimentary rocks. Metasedimentary rocks are often observed in bands intersecting the granites. These metasedimentary rocks are thought to be raft pieces, resulting from the intrusion of the granites. These metasedimentary rafts do not host uranium mineralization. The contact reaction that is the cause of the uranium concentrations is thought to be caused by magmatic and possibly late magmatic?hydrothermal processes during emplacement. Another unique relationship is the association between massive magnetite and the occurrence of high uranium concentrations. Disseminated magnetite is also associated with higher concentrations of uranium in many other occurrences. Mineralization consists of fine?grained uraninite (and probably uranothorite), while on surface one can often observe yellow, powdery secondary uranium minerals (probably including uranophane). In many areas of the Kenora property, a relationship is observed between high uranium occurrences and the presence of biotite (less commonly the presence of muscovite). Reference: Kenora District Geologists Assessment File, Delta Uranium Inc., 52F13SE KK-2 AFRO 2.41986
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 5 | Uranophane | Economic | Ore |
Mar 03, 2011 (C Ravnaas) - The granitoid intrusions in this part of the Kenora District have potential for hosting a low-grade, high tonnage uranium deposit, similar to a Rossing-type uranium model. Rossing-type mineralization consists of disseminated uranium in coarse-grained felsic intrusive, often referred to as alaskite. A 2008 surface sampling master map illustrating sampling location and assay results presented by Delta Uranium indicate the site returned one sample which returned between 1000 to 2000 ppm U3O8. More than five samples which returned between 100 to 1000 ppm U3O8 (20000004302).
Mono - Uranium and thorium deposits of northern Ontario
Publication Number: MDC025 Page: 89-90 Date: 1984
Author: Robertson J.A., Gould K.L.
Publisher Name: Ontario Geological Survey
Location:
Mono - Building and ornamental stone inventory in the districts of Kenora and Rainy River
Publication Number: MDC027 Page: 44 Date: 1986
Author: Storey C.C.
Publisher Name: Ontario Geological Survey
Location:
Book - Resident Geologist personal communication, 78-02-15
Publication Number: Date: 1996
Author:
Publisher Name:
Location:
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