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H2O storage capacity of olivine at 5–8 GPa and consequences for dehydration partial melting of the upper mantle

✍ Scribed by P. Ardia; M.M. Hirschmann; A.C. Withers; T.J. Tenner

No coin nor oath required. For personal study only.

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H2O storage capacity of olivine at 5–8&#xa0;GPa and consequences for dehydration partial melting of the upper mantle