Water Solubility in Fe‐Bearing Wadsleyite at Mantle Transition Zone Temperatures
Author:
Affiliation:
1. Bayerisches Geoinstitut Universität Bayreuth Bayreuth Germany
2. Center for High Pressure Science and Technology Advanced Research Beijing P.R. China
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GL092836
Reference44 articles.
1. Examination of Water Quantification and Incorporation in Transition Zone Minerals: Wadsleyite, Ringwoodite and Phase D Using ERDA (Elastic Recoil Detection Analysis)
2. High-pressure single-crystal elasticity of wadsleyite and the seismic signature of water in the shallow transition zone
3. Effect of water on olivine-wadsleyite phase boundary in the (Mg, Fe)2SiO4system
4. Electrical conductivity of wadsleyite at high temperatures and high pressures
5. Pressure and temperature-dependence of water solubility in Fe-free wadsleyite
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1. Stability of H2O‐Rich Fluid in the Deep Mantle Indicated by the MgO‐SiO2‐H2O Phase Relations at 23 GPa and 2,000 K;Journal of Geophysical Research: Solid Earth;2024-07
2. First-principles study of water incorporation in Fe-containing wadsleyite;Physics of the Earth and Planetary Interiors;2022-12
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4. Hydrous peridotitic fragments of Earth’s mantle 660 km discontinuity sampled by a diamond;Nature Geoscience;2022-09-26
5. Water Enhancement of Si Self‐Diffusion in Wadsleyite;Journal of Geophysical Research: Solid Earth;2022-03
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