Spinels and Oxygen Fugacity in Olivine-Phyric and Lherzolitic Shergottites

Physics

Scientific paper

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Scientific paper

Oxygen fugacities are determined from olivine-pyroxene-spinel
assemblages in four olivine-phyric shergottites. Results, combined with
previous fO2 determinations, suggest that shergottites may form two
groups: a reduced, LREE-depleted group, and a more oxidized and enriched
group.

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