Tracking the oxygen fugacity of enclave-forming granitic melts through plagioclase trace element signatures
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DOI: 10.1007/s00410-020-01702-3
Abstract: Magma mixing and contamination are among the dominant processes in the building of the isotopic diversity of granite rocks. Felsic microgranular enclaves (FMEs) are remnants of magma mixing and they often carry xenocrysts that also… read more here.
Keywords: plagioclase trace; chemistry; oxygen fugacity; trace element ... See more keywords