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Coesite and clinopyroxene exsolution lamellae in chromites: In-situ ultrahigh-pressure evidence from podiform chromitites in the Luobusa ophiolite, southern Tibet

BiologyOrganic GeochemistryEngineeringNatural SciencesIn-situ Ultrahigh-pressure EvidenceGeologyAuthigenic Mineral FormationGeochemistryChemistrySouthern TibetClinopyroxene Exsolution LamellaeMineral Geochemistry