With regard specifically to your statement "considerable thickness of peridotite (solid purple) encountered in MTJV001", layered intrusions with cumulate peridotite are typically associated with sulfide or chromite ores.
Sulfides associated with peridotites usually form nickel ores and platinoid metals.
Indeed, most of the platinum used in the world today comes from the mines in the "Bushveld Igneous Complex in South Africa".
In addition, the chromite bands found in peridotites are the world's major source of chromium.
Your thoughts?
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