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High- and low-Cr chromitite and dunite in a Tibetan ophiolite: evolution from mature subduction system to incipient forearc in the Neo-Tethyan Ocean

Marine GeologyEngineeringMature Subduction SystemTectonic EvolutionMarine ChemistryGeologyNeo-tethyan OceanGeochemistryTibetan OphiolitePetrologyAuthigenic Mineral FormationEarth ScienceTectonics