2011•Contributions to Mineralogy and PetrologyRequires access

H2O storage capacity of olivine and low-Ca pyroxene from 10 to 13 GPa: consequences for dehydration melting above the transition zone

Travis J. Tenner, M. M. Hirschmann, Anthony C. Withers, P. Ardia

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Key concepts: Peridotite, Pyroxene, Olivine, Geology, Transition zone, Mantle (geology), Partial melting, Mineralogy

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H2O storage capacity of olivine and low-Ca pyroxene from 10 to 13 GPa: consequences for dehydration melting above the transition zone — Research Paper | ScholarLens