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komatiite
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komatiite

Oldest volcanic rock with three times as much magnesium as other volcanic rocks. Unlike basaltic lavas, which comprise oceanic crust, komatiites have the chemical composition of peridotite, the primary constituent rock of the upper mantle. Komatiites were extruded as a liquid at high temperatures, perhaps more than 1,600°C/2,912°F. They have low titanium and high magnesium, nickel, and chromium content.

Discovered in 1969 by Morris and Richard Viljoen, komatiites are named after the Komati River, Transvaal, South Africa, where they were first identified. The term is also used more loosely to refer to suites of other unusual basaltic rocks with which they are often associated.



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In the Gayot Lake area, Virginia Gold Mines and partner BHP Minerals discovered several Ni-Cu-PGE showings in komatiitic lavas and ultramafic intrusive rocks of the Venus volcano-sedimentary belt.
The pyrite-bearing mineralization appears structurally controlled within highly reactive rocks including widespread komatiites, komatiitic basalts and basalts.
Hot spot basaltic magmatism is now seen as the most likely cause of giant komatiitic Ni-Cu deposits in the Archean, and Norilsk-type deposits in the Paleozoic (Yakubchuk and Nikishin 2004).
 
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