Dehydration of chlorite explains anomalously high electrical conductivity in the mantle wedges

Mantle wedge regions in subduction zone settings show anomalously high electrical conductivity (~1 S/m) that has often been attributed to the presence of aqueous fluids released by slab dehydration. Laboratory-based measurements of the electrical conductivity of hydrous phases and aqueous fluids are...

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Detalles Bibliográficos
Autores principales: Manthilake, Geeth, Bolfan-Casanova, Nathalie, Novella, Davide, Mookherjee, Mainak, Andrault, Denis
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2016
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4928900/
https://www.ncbi.nlm.nih.gov/pubmed/27386526
http://dx.doi.org/10.1126/sciadv.1501631

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4928900/
https://www.ncbi.nlm.nih.gov/pubmed/27386526
http://dx.doi.org/10.1126/sciadv.1501631

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