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Gold/Mining/Energy : Nuinsco Resources (NWI)

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To: E. Charters who wrote (1221)	3/5/1999 4:49:00 PM
From: 1king	Read Replies (3) of 5821

Where are the papers!!! I offered to educate myself....where are all the papers supporting your "theory"!!! I asked for the titles of the five or six papers you quoted, please! "I have viewed the Vosiey Bay footwall core and it is clear that the basal rocks are a seabed sediment and juvenile at that. Clast of quartz where clearly visible. The rock below the sulphide contact was brown, totally unaltered and mildly banded like a varve clay. You could run a thumbnail along the fresh contact line of the sulphide layer that did not penetrate one millimetre into the footwall rock. This is obviously a sea bed vent deposit in character. To accept magmatic segregation in face of the obvious geological evidence is pathetic." you saw the core.......SO FREAKING WHAT... I DRILLED IT!!!!! I was willing to let things go but you blither on! The basal material is GNEISS, the dark grey / white bands are mineral segregation......one of the defining characteristic of ANY GNEISS!! It is the country rock into which the "troctolite" was intruded. Check any of the geology maps for the area. I find it amusing you are unable to distinguish primary sed features from metamorphism. If this geo-flailing is because I have stepped on your toes somewhere else let me know and I will make amends.....anything to stop this embarrassment. 1King

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