Water in the Earth's mantle: A solid-state NMR study of hydrous wadsleyite


Wadsleyite, β-(Mg,Fe)2SiO4, is the main component of the transition zone in the Earth's mantle, at depths of 410-530 km below the surface. This mineral has received considerable interest as a potential reservoir for the vast amount of hydrogen, as hydro

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The Australian National University

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oai:openresearch-repository.anu.edu.au:1885/77486Last time updated on 4/26/2018

This paper was published in The Australian National University.

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