Extremely light potassium isotope compositions of the continental eclogites and high-pressure metamorphic veins reveal the fluid-rock interactions in subduction zones
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Table S1-S3 report the mineral assemblages, K isotopic compositions and reconstructed K budgets of the investigated eclogites, amphibolites, and veins. Table S4 shows the metamorphic dehydration modelling results of K isotope system during subduction. Table S5 shows mass balance calculations results between the K loss fraction and their isotopic compositions during fluid escape.
提供机构:
Institute of Oceanology Chinese Academy of Sciences; Institute of Geology and Geophysics Chinese Academy of Sciences; Washington University in St. Louis; Hefei University of Technology



