 |
Please click on diagram and table for larger view in PDF SYLVIE The Sylvie Zone was discovered by prospecting during the 2004 field season and is located approximately one kilometre east of the Getty Prospect and 5.5 km NNE of the Belanger base camp. The surface showing consists of disseminated sulphides in frost heaved sub-crop and is exposed over a strike length of approximately 150 metres with a width of up to 40 metres. Sylvie is hosted within the gabbro-pyroxenite margin at the east end of an ultramafic-mafic intrusive complex; the same ultramafic-mafic intrusive body as the Getty Zone.  Flying into the Belanger base camp
In total fifty-five drill holes have been drilled on the Sylvie Prospect (9,162.7 m). Historic and current drilling data indicate that Ni-Cu-PGE sulphide mineralization has been intersected intermittently for approximately 125 metres along strike and to depths of up to 200 metres down dip at Sylvie. The Sylvie Prospect is shallow and remains open to the west and down-dip. Mineralization consists of disseminated, net-textured and massive pyrrhotite, pentlandite, and chalcopyrite. The Sylvie prospect underlies a strong bulls-eye, moving-loop TEM (SQUID) conductor. Table 1 documents the significant mineralized intervals identified during the 2007 drilling program.
Core technician labelling box ends in the core shack  |
