Ontario Geological Survey
Permanent Link to this Record:
MDI000000001037
| Record Name(s) | Pond T9 Zone - 2005 |
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| Related Record Type | |
| Related Record(s) | |
| Record Status | Occurrence |
| Date Created | 2011-Mar-04 |
| Date Last Modified | 2022-Jul-27 |
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| Revised By |
Primary Commodities: Copper
Secondary Commodities: Gold, Silver
Township or Area: Halkirk
Latitude: 48° 42' 4.59" Longitude: -93° 2' 49.29"
UTM Zone: 15 Easting: 496540.002 Northing: 5394250.005 UTM Datum: NAD83
Resident Geologist District: Kenora
NTS Grid: 52C11NE
Point Location Description: Taken from geology map with occurrences AFRO 2.32111
Location Method: Data Compilation
Access Description: The property is accessed from Highway 11 east of Fort Frances. There is a series of logging roads which provide access to the internal parts of the Grassy Portage intrusive rocks.
There is a long history of base metals exploration within the North Rock area, with the earliest recorded work occurring in 1918, with possible, unrecorded work as early as 1902. Research suggests that there has been little exploration for the platinum group elements (PGE's) and only minor interest in Au. Most of the exploration activity occurred between 1958 and 1978 and was sporadic before or since.2001, 2003 to 2006 as presented in MetalCORP, Kenora assessment file 52C11NE BBB-8 AFRO 2.37249 Two prospecting programs were completed during 2003 and 2004. The property was optioned to MetalCORP Ltd (MTC) during October 2004. During 2005 and 2006 MTC completed an AeroTEM IT helicopter-borne survey, Phase 1 and II diamond drill programs, linecutting, detailed prospecting, and geological mapping.
Mar 04, 2011 (C Ravnaas) - The North Rock Property is primarily underlain by the differentiated Grassy Portage Intrusion (GPI) with lesser amounts of the Grassy Portage ultramafic pyroclastic sequence (GUP); clastic metasedimentary rocks of the Couchiching Metasediments; granitoid rocks of the Bear Passage and Blind Bay plutons; sections of2 formational, composite, chemical/clastic metasedimtmtary sequences; two narrow mafic metavolcanic units; and a few, possibly subvolcanic gabbro sills. All observed rocks-types comprise the southern limb of a large-scale open, antiformal fold cored by the Rice Bay Dome located approximately 1.50 km north of the property (Figure 3). Most rock-types have been regionally metamorphosed to lower amphibolite-grade. The southwestern two-thirds of the Grassy Portage Intrusion underlies the core of the property (~75%). This large, sill-like, mafic complex intrudes all observed supracrustal rock-types, and is composed ofa well-differentiated, locally layered, cumulate sequence of medium- to coarse-grained, melagabbro, gabbro and leucogabbro; coarsely plagiophyric to glomero-plagiophyric gabbro to leucogabbro; localized intervals ofmedium- to coarse-grained anOlthosite; and a discontinuous, noncumulate, ophitic-textured, melagabbroic border phase that is present along both the upper and lower contacts ofthe complex. The intrusion is structurally overturned and stratigraphically south-facing. Cha1copyrite-dominated mineralization concentrates along both upper and lower contacts with the greatest sulphide abundances observed near the basal or northern contact. Reference MetalCORP, Kenora assessment file 52C11NE BBB-8 AFRO 2.37249
Mar 04, 2011 (C Ravnaas) - Most of the presently defined, surface mineralized zones are aligned roughly subparallel to the basal contact of the Grassy Portage Intrusion, are elongate in outline with diffuse margins, and contain highly variable amounts of sulphides with highly variable, but internally consistent, base and precious metals grades associated with a confined range of rock-types. The 2005 prospecting program discovered at least 28 new occurrences and diffuse zones and numerous low-grade showings (not described) from the 489 grab samples Reference MetalCORP, Kenora assessment file 52C11NE BBB-3 AFRO 2.32111
Mar 04, 2011 (C Ravnaas) - The Pond Zone was discovered during 2004 MTC prospecting, presently exhibits a 115 m strike-length, and is located 40 to 50 m south of a small lake/large pond, -500 m southeast of the East Zone. It occurs within a rusty-weathered, malachite-stained, medium- to coarse-grained, often gabbro containing between 2 and 15% disseminated pyrrhotite and chalcopyrite. The mineralization within 2 of the samples taken occurs between 2.5 and 7 m northwest of the northwestern edge of a 15 to 25 m thick pyroxenite dyke. The third sample is located 20 m southeast of the southeastern contact of the dyke. Two MTC 2004 grab samples contained up to 1.02% Cu, 4.5ppm Ag, and333ppb Au. A single 2005 prospecting sample contained 7780ppm Cu, 5.1 ppm Ag, and 222 ppb Au. T-9 Occurrence This isolated occurrence is located near the contact between fine- to medium-grained gabbro and coarse-grained melagabbro, -525 m southeast ofthe East Zone and 235 m southwest of the Pond Zone. It consists of coarse-grained, rusty, non-magnetic, dark grey to black melagabbro or pyroxenite containing 2 to 4% disseminated chalcopyrite and a narrow, massive chalcopyrite seam. Several northeast-trending, fine-grained, mafic dykes crosscut the outcrop and may defme localized extension associated with a coincident, aero-magnetically-interpreted, northeast-southwest-trending fault. The single 2005 sample graded 1.16% Cu and1.7ppmAg. Reference MetalCORP, Kenora assessment file 52C11NE BBB-3 AFRO 2.32111.
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