Water in the Earth's mantle: a solid-state NMR study of hydrous wadsleyite†
Abstract
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
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* Corresponding authors
a
School of Chemistry and EaStCHEM, University of St Andrews, North Haugh, St Andrews KY16 9ST, UK
E-mail:
sema@st-andrews.ac.uk
b Department of Earth Science and Engineering, Imperial College London, South Kensington SW7 2AZ, UK
c Department of Earth Sciences, Natural History Museum, Cromwell Road, London SW7 5BD, UK
d Bayerisches Geoinstitut, Universität Bayreuth, Bayreuth 95440, Germany
e
School of Chemistry and WestCHEM, University of Glasgow, Glasgow G12 8QQ, UK
E-mail:
stephen.wimperis@glasgow.ac.uk
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
J. M. Griffin, A. J. Berry, D. J. Frost, S. Wimperis and S. E. Ashbrook, Chem. Sci., 2013, 4, 1523 DOI: 10.1039/C3SC21892A
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