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Economic Geology; July 1971; v. 66; no. 4; p. 607-610
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Comments on the role of oxygen fugacity in the formation of immiscible sulfide liquids in the H chromitite zone of the Stillwater complex, Montana

Norman J. Page

Separation of sulfide materials due to depletion of FE 2 in melt resulting from precipitation of chromite, not the result of increased oxygen fugacity in magma or temperature changes

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