Please click on diagram and table for full view in PDF
GETTY
The Getty Zone is comprised of Ni-Cu-PGE sulphide mineralization hosted by pyroxenite. The mineralized zone consists of disseminated/interstitial sulphides, net-textured sulphides and massive sulphides comprised largely of pyrrhotite, pentlandite, and chalcopyrite. The Getty mineralization is exposed on surface over a strike length of approximately 325 metres with a width from 15 to 50 metres. Drilling has intersected mineralization to a depth of 200 metres although the deposit is also open to depth toward the west and northwest. Getty is located one kilometre west of the Sylvie Zone and about 5 km NNE of the company’s Belanger base camp.
The Getty Zone was initially discovered during property wide prospecting and AeroTEM surveys during the 2003 field season. Drilling commenced in the summer of 2004, and a total of 84 holes have been completed for a total of 13,522.5 metres so far on the Getty Zone. The Showing also exhibits coincident TEM (SQUID) conductors, positive airborne VTEM and Magnetic signatures. Table 1 documents the significant mineralized intervals identified during the 2007 drilling program.
Geologist Ginette Carter inspecting rocks in the vicinity of the Getty prospect.
The Getty Intrusion occurs within the “Belanger Trend” which consists of a series of ultramafic-mafic intrusive rocks interpreted as part of the regional “Southern Trend” of ultramafic-mafic rocks in the Ragland District. Mineralization along the South Raglan Trend includes a number of other Ni-Cu-PGE sulphide deposits and showings discovered by Canadian Royalties Inc.
Getty drill hole section 499925E displaying Ni, Cu and major lithology for drill holes GET07-004, GET07-005, GET07-006, GET07-013, GET07-024, and GET07-025
Getty drill hole section 500000E displaying Ni, Cu and major lithology for drill holes GET07-007, GET07-008, GET07-009, GET07-010, GET07-019, and BEL04-16
Helicopter assisted drill move on the Goldbrook Ventures tenure
