Ontario Geological Survey
Permanent Link to this Record:
MDI000000000179
| Record Name(s) | Ontex DH FY-03-02 - 2003 |
|---|---|
| Related Record Type | Partial |
| Related Record(s) | |
| Record Status | Occurrence |
| Date Created | 2006-Dec-13 |
| Date Last Modified | 2022-Nov-07 |
| Created By | |
| Revised By |
Primary Commodities: Gold
Township or Area: Deloro
Latitude: 48° 24' 40.4" Longitude: -81° 14' 49.29"
UTM Zone: 17 Easting: 481720 Northing: 5362037.002 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 42A06NE
Point Location Description: Collar DH FY-03-02
Location Method: Based on Assessment
Access Description: The ONTEX Resources Inc. properties located in Deloro Township are approximately 7.5km south of the city of Timmins. Access is by means of the Timmins Gold Mine Road (previously known as 'back road') to the Buffalo Ankerite Mine turnoff, then south to the McKay Lake gravel road for approximately 4.5 km to the Faymar Mine road, which crosses onto the property area in approximately l km. (T-4955 & T-4599)
Claim HR 1168 part of the original Faymar patents, east of and adjoining Faymar minesite claim:. 1937, Nakhodas Mining Co.: Geology, diamond drilling (T-349) 2000, Ontex Resources Limited: Geophysical surveys (T-4599) 2002 - 2003, Ontex Resources Limited: Compilation (T-4955); geophysical surveys (T-4966); diamond drilling, assays (T-4963)
| Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
|---|---|---|
| T-349 / 63.3629 | 42A06NE0465 | 42A06NE0465 |
| 63.3629, T-0349 | 42A06NE0465 | 42A06NE0465 |
| T-4599 / 2.21018 | 42A06NE2022 | 42A06NE2022 |
| T-4955 / 2.26984 | 42A06NE2037 | 42A06NE2037 |
| T-4963 / 2.27226 | 42A06NE2034 | 42A06NE2034 |
| T-4966 / 2.26871 | 42A06NE2036 | 42A06NE2036 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Abitibi
Tectonic Assemblage: Deloro
Geological Age: Archean
Dec 13, 2006 (D Draper) - The Faymar property is underlain by rocks of the Deloro Group of the Abitibi Greenstone Belt. These rocks include a series of intermediate to ultramafic volcanics, quartz breccia, iron formation, and carbonatized, fuchsitic volcanics in the north end of the property. Structurally, the property is transected by three notable faults, the most prominent being the Shaw Creek Fault, which cuts roughly through the east-central portion of the property in a northsouth direction about 400 metres east of the Faymar Shaft. (T-4599)
| Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Calcium Carbonate | Host |
|---|---|---|---|---|
| Intermediate lava flow-unsubdivided | 2 | Andesite | Contains | |
| Diorite | 3 | Diorite | Contains | |
| Quartz Diorite | 4 | Quartz Diorite | Contains |
Dec 13, 2006 (D Draper) - Best assay from drillhole FY-03-02 was 24.34 g/t Au over 0.65m @ 57.6m downhole, in andesite with carbonate veining mineralized with pyrite and chalcopyrite. Best assay from FY-03-04 (drilled 20m W of -02) was 4.73 g/t Au over 0.2m @ 84.78m downhole in quartz diorite. Hole FY-03-05 (20m SE of -02) returned 0.80 g/t Au over 1m @ 51.6m in calcium carbonate veined diorite. All holes drilled Az 000. (T-4963)
Dec 13, 2006 (D Draper) - Alteration on the Faymar property consists of talc, chlorite, carbonate, sericite and fuchsite in varying degrees (T-4599)
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For detailed information regarding this mineral record please contact the Timmins Resident Geologist District Office