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Clinopyroxene precursors to amphibole sponge in arc crust
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...
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Pub. Group
2014
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4102121/ https://www.ncbi.nlm.nih.gov/pubmed/25002269 http://dx.doi.org/10.1038/ncomms5329 |