SI
SI
discoversearch

We've detected that you're using an ad content blocking browser plug-in or feature. Ads provide a critical source of revenue to the continued operation of Silicon Investor.  We ask that you disable ad blocking while on Silicon Investor in the best interests of our community.  If you are not using an ad blocker but are still receiving this message, make sure your browser's tracking protection is set to the 'standard' level.
Gold/Mining/Energy : Nuinsco Resources (NWI) -- Ignore unavailable to you. Want to Upgrade?


To: Brumell who wrote (2047)3/21/1999 11:37:00 PM
From: mineman  Respond to of 5821
 
Brumell, the surface exposures, mag anomalies, and drill intersecting show the gabbro is a relatively small 120 metre wide plug.

There would not have been enough nickel in the 120 metre gabbro-norite melt to give the higher grades and widths at the base of the plug.

Perhaps the pyrrhotite-nickel-sulphide-enriched norite-gabbro rock in the plug was originally a melt forced out of a large differentiating ultramafic intrusive below or alongside Lac Rocher to fill a fracture zone above or alongside the intrusive, and then this melt differentiated within the small 120 metre wide plug to produce the lightly disseminated .5% nickel upper portion of the plug exposed on surface, the strongly disseminated 1% nickel lower portion, and the massive 8% nickel bed.

Perhaps others have an idea how the large amount of sulphides could have differentiated from such a narrow plug??