The partitioning of Fe and Mg between olivine and carbonate and the stability of carbonate under mantle conditions
We have investigated the effect of Fe on the stabilities of carbonate (carb) in lherzolite assemblages by determining the partitioning of Fe and Mg between silicate (olivine; ol) and carbonates (magnesite, dolomite, magnesian calcite) at high pressures and temperatures. Fe enters olivine preferentia...
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| 格式: | Journal article |
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1993
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