Clinopyroxene precursors to amphibole sponge in arc crust
Clinopyroxene precursors to amphibole sponge in arc crust
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London: Nature Publishing Group UK
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English
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London: Nature Publishing Group UK
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The formation of amphibole cumulates beneath arc volcanoes is a key control on magma geochemistry, and generates a hydrous lower crust. Despite being widely inferred from trace element geochemistry as a major lower crustal phase, amphibole is neither abundant nor common as a phenocryst phase in arc lavas and erupted pyroclasts, prompting some autho...
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Clinopyroxene precursors to amphibole sponge in arc crust
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TN_cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_4102121
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_pubmedcentral_primary_oai_pubmedcentral_nih_gov_4102121
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ISSN
2041-1723
E-ISSN
2041-1723
DOI
10.1038/ncomms5329