Loss of Chromium from Olivine During the Metamorphism of Chondrites

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Scientific paper

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Scientific paper

Unmetamorphosed chondrites contain high levels of Cr_2O_3 in ferroan
olivine. During metamorphism to type 3.2, Cr is lost from olivine by a
complex mechanism. Histograms of Cr_2O_3 in olivine can be used to
discriminate type 3.0 3.1 3.2 chondrites.

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