Crystal chemistry of phase B and an anhydrous analogue: implications for water storage in the upper mantle
- 1 September 1989
- journal article
- Published by Springer Nature in Nature
- Vol. 341 (6238), 140-142
- https://doi.org/10.1038/341140a0
Abstract
No abstract availableKeywords
This publication has 17 references indexed in Scilit:
- Geochemical implications of the formation of the Moon by a single giant impactNature, 1989
- Infrared spectra of high-pressure hydrous silicates in the system MgO-SiO2-H2OPhysics and Chemistry of Minerals, 1986
- Phase transformations in serpentine at high pressures and temperatures and implications for subducting lithospherePhysics of the Earth and Planetary Interiors, 1986
- Melting experiment on natural lherzolite at 20 GPa: Formation of phase B coexisting with garnetGeophysical Research Letters, 1986
- Stability of phase B, A hydrous magnesium silicate, to 2300°C at 20 GPAGeophysical Research Letters, 1985
- MITHRIL–an integrated direct-methods computer programJournal of Applied Crystallography, 1984
- The Bond-Valence Method: An Empirical Approach to Chemical Structure and BondingPublished by Elsevier ,1981
- High‐pressure stability of a dense hydrous magnesian silicate Mg23Si8O42H6 and some geophysical implicationsJournal of Geophysical Research, 1980
- The crystal structure of magnesium germanate: A reformulation of Mg4GeO6 as Mg28Ge10O48Journal of Solid State Chemistry, 1970
- High-pressure reconnaissance investigations in the system Mg2SiO4 - MgO - H2OEarth and Planetary Science Letters, 1967