Hydrogen self-diffusion in single crystal olivine and electrical conductivity of the Earth’s mantle

Abstract Nominally anhydrous minerals formed deep in the mantle and transported to the Earth’s surface contain tens to hundreds of ppm wt H2O, providing evidence for the presence of dissolved water in the Earth’s interior. Even at these low concentrations, H2O greatly affects the physico-chemical pr...

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Autores principales: Davide Novella, Benjamin Jacobsen, Peter K. Weber, James A. Tyburczy, Frederick J. Ryerson, Wyatt L. Du Frane
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2017
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Acceso en línea:https://doaj.org/article/c4c4aea43983455aaccfe7ff2219ce62
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