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Gold/Mining/Energy : Nuinsco Resources (NWI) -- Ignore unavailable to you. Want to Upgrade?

To: Buckey who wrote (1934)	3/19/1999 8:57:00 AM
From: mineman	Read Replies (1) \| Respond to of 5821

The wide granite dykes combined with the high-grade nature of the one zone indicate a large batholith is below and the mineralization could be concentrations related to remobilization within the cupola or fractured area above the batholith. This would mean the 2.3 metre thick high-grade zone is not a primary differentiate but rather a high-grade remobilized nickel-rich zone which filled a structurally-controlled fracture. If this origin-theory is correct the 2.3 metre thick bed could have originated from a larger structurally-prepared cavern with similar grade Nickel. If the high-grade widens at depth this theory becomes possible!