Genesis of the Ray-Iz chromitite, Polar Urals: Inferences to mantle conditions and recycling processes

LITHOS, pp. 1056992020.

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Ophiolitic chromitites in the eastern sector of the Alpine-Himalayan and Polar Ural orogenic belts preserve evidence of formation under ultra-high-pressure (UHP), deep mantle conditions. The textural and compositional characteristics of microscopic and submicroscopic inclusions in magnesiochromite from the Ray-lz ophiolites are considered...More



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