The electrical conductivity during incipient melting in the oceanic low velocity zone

A low viscosity layer in the upper mantle, the Asthenosphere, is a requirement for plate tectonics(1). The seismic low velocities and the high electrical conductivities of the Asthenosphere are attributed either to sub-solidus water-related defects in olivine minerals(2-4) or to a few volume percent...

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Detalles Bibliográficos
Autores principales: Sifré, David, Gardés, Emmanuel, Massuyeau, Malcolm, Hashim, Leila, Hier-Majumder, Saswata, Gaillard, Fabrice
Formato: Online Artículo Texto
Lenguaje:English
Publicado: 2014
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4010644/
https://www.ncbi.nlm.nih.gov/pubmed/24784219
http://dx.doi.org/10.1038/nature13245

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4010644/
https://www.ncbi.nlm.nih.gov/pubmed/24784219
http://dx.doi.org/10.1038/nature13245

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