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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...
| Autores principales: | , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
2014
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| Materias: | |
| 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 |