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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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Detalles Bibliográficos
Autor principal: Smith, Daniel J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Pub. Group 2014
Materias:
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