(Table A1) Chemical composition of abyssal peridotites from ODP Hole 153-920
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The compatibility of vanadium (V) during mantle melting is a function of oxygen fugacity (fO2): at high fO2's, V becomes more incompatible. The prospects and limitations of...
地幔熔融过程中钒（V）的相容性是氧逸度（fO2）的函数：当氧逸度较高时，钒的不相容性会增强。……的应用前景与局限性
