Olivine compositional changes in primitive magmatic skarn environments: A reassessment of divalent cation partitioning models to quantify the effect of carbonate assimilation
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DOI: 10.1016/j.lithos.2018.07.008
Abstract: Abstract The geochemical evolution of olivine from primitive magmatic skarn environments has been studied by atmospheric pressure experiments carried out at 1250, 1200, and 1150 °C under QFM oxygen buffering conditions. The starting materials were three… read more here.
Keywords: assimilation; cation; primitive magmatic; skarn ... See more keywords