Re: olivine-bearing peridotite

HIGH-GRADE NI-CU-PT-PD-ZN-CR-AU-V-TI DISCOVERIES IN THE "RING OF FIRE"

NI 43-101 Update (September 2012): 11.1 Mt @ 1.68% Ni, 0.87% Cu, 0.89 gpt Pt and 3.09 gpt Pd and 0.18 gpt Au (Proven & Probable Reserves) / 8.9 Mt @ 1.10% Ni, 1.14% Cu, 1.16 gpt Pt and 3.49 gpt Pd and 0.30 gpt Au (Inferred Resource)

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HSS

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Re: olivine-bearing peridotite

in response to

Re: olivine-bearing peridotite

HSS

posted on May 06, 2008 12:51PM

Chemical and mineralogical evidence from other parts of DE's suggests that the processes that formed the discordant bodies may have influenced other cumulates.
It appears that the same processes that formed discordant bodies operated within an anorthositic layer strongly modifying the chemistry of the rock but leaving no mineralogical or textural evidence.

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