Stability of dense hydrous magnesium silicate phases in the systems Mg2SiO4-H2O and MgSiO3-H2O at pressures up to 27 GPa

By E. Ohtani, H. Mizobata, H. Yurimoto. 2000

163 citations recorded by the source corpus.

Subfields: Geophysics

View Paper: https://www.semanticscholar.org/paper/57036cf2cb27b092171b4c827951220854e4ca09

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In Geophysics

1. D. Frost
2. Russell J. Hemley
3. S. Demouchy
4. H. Keppler
5. M. Hirschmann
6. L. Elkins‐Tanton

Citations in the corpus

• Pressure and temperature-dependence of water solubility in Fe-free wadsleyite (2005, background): “In addition, Ohtani et al. (2000) showed that the water content of ringwoodite, co-existing with a hydrous liquid, decreases with increasing temperature.”
• Hydrogen in the Deep Earth (2001, background): “Phase D has been shown to be stable to lower mantle conditions (Frost & Fei 1998, Ohtani et al 2000) and reported to coexist with silicate perovskite and stishovite (Li & Jeanloz 1991).”