Calcium isotopic signatures of depleted mid-ocean ridge basalts from the northeastern Pacific
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DOI: 10.1007/s00343-020-0045-2
Abstract: A number of high-temperature processes (e.g., melt-rock reactions, metasomatism, partial melting) can produce significant Ca isotopic fractionation and heterogeneity in the mantle, but the mechanism for such fractionation remains obscure. To investigate the effect of… read more here.
Keywords: mantle partial; depleted mid; partial melting; isotopic fractionation ... See more keywords