Constraining the sub-arc, parental magma composition for the giant Altiplano-Puna Volcanic Complex, northern Chile

The Andean continental arc is built upon the thickest crust on Earth, whose eruption products reflect varying degrees of crustal assimilation. In order to robustly model magma evolution and assimilation at subduction zones such as the Andes, the compositions of parental magmas feeding crustal magma...

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Detalles Bibliográficos
Autores principales: González-Maurel, Osvaldo, Deegan, Frances M., le Roux, Petrus, Harris, Chris, Troll, Valentin R., Godoy, Benigno
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7176692/
https://www.ncbi.nlm.nih.gov/pubmed/32321945
http://dx.doi.org/10.1038/s41598-020-63454-1

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7176692/
https://www.ncbi.nlm.nih.gov/pubmed/32321945
http://dx.doi.org/10.1038/s41598-020-63454-1

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