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Published in 2018 at "Lithosphere"
DOI: 10.1130/l715.1
Abstract: Ophiolitic peridotites represent variously depleted residues of the primitive mantle after multiple episodes of partial melting, melt extraction, and melt-rock interactions. They display a wide range of compositional and geochemical heterogeneities at different scales, and…
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Keywords:
ultrahigh pressure;
mantle petrogenesis;
ophiolites diamonds;
upper mantle ... See more keywords