Subduction zone fluids and arc magmas conducted by lithospheric deformed regions beneath the central Andes

Dehydration of the oceanic subducting slab promotes the formation of magmatic arcs, intra-slab intermediate-depth seismicity, and hydration of the overlying mantle wedge. However, the complex permeability structure of the overriding plate controls the magma and fluid migration and their accumulation...

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Detalles Bibliográficos
Autores principales: Contreras-Reyes, E., Díaz, D., Bello-González, J. P., Slezak, K., Potin, B., Comte, D., Maksymowicz, A., Ruiz, J. A., Osses, A., Ruiz, S.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8630066/
https://www.ncbi.nlm.nih.gov/pubmed/34845293
http://dx.doi.org/10.1038/s41598-021-02430-9

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8630066/
https://www.ncbi.nlm.nih.gov/pubmed/34845293
http://dx.doi.org/10.1038/s41598-021-02430-9

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