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Gold/Mining/Energy : Canadian Rocket Red's Picks -- Ignore unavailable to you. Want to Upgrade?

To: Rocket Red who wrote (16268)	8/22/2007 12:05:09 AM
From: Proud Deplorable	Read Replies (1) \| Respond to of 19697

CME Voisey # 2 read below The massive sulphides are found adjacent to an olivine-rich ultramafic layer or dike which is subparallel to the underlying enderbitic gneiss. The ultramafic layer/dike is interpreted to be a massive to gneissic olivine norite to troctolite. The enderbitic gneiss is in contact to the west with Tasiuyak paragneiss, a relationship which is similar to the geological situation at the Voisey's Bay mine site. Significantly, the massive sulphides and ultramafic layer/dike are found within a 2.5-kilometre-by-3.5-kilometre, three-milligal gravity (density) anomaly, the centre of which is located 1.75 km to the south of the new prospect. Modelling of the gravity anomaly, infers a 300-metre-thick troctolite body, synformal in shape, at about 150 m to 250 m depth of burial.