2015•Geochimica et Cosmochimica ActaRequires access

Effect of oxygen fugacity on OH dissolution in olivine under peridotite-saturated conditions: An experimental study at 1.5–7 GPa and 1100–1300 °C

Xiaozhi Yang

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Key concepts: Mineral redox buffer, Peridotite, Olivine, Fugacity, Dissolution, Oxygen, Forsterite, Mantle (geology)

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Effect of oxygen fugacity on OH dissolution in olivine under peridotite-saturated conditions: An experimental study at 1.5–7 GPa and 1100–1300 °C — Research Paper | ScholarLens