Oxygen Fugacity Controls on Deep-Mantle Phase Transitions in Martian Mantle Composition
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资源简介：
New experimental results at 1500 °C from high-pressure experiments on a Khan-based Martian mantle composition quantify the fO₂-dependence of deep-mantle phase transitions.
提供机构：
Center for High Pressure Science and Technology Advanced Research; Vrije Universiteit Amsterdam
