The system Mg2SiO4MgOH2O at high pressures and temperatures — Possible hydrous magnesian silicates in the mantle transition zone
Authors:
- S. AkimotoSAS. Akimoto
- M. AkaogiMAM. Akaogi
- 1 December 1980
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 23 (4) , 268-275
Abstract
No abstract availableKeywords
This publication has 9 references indexed in Scilit:
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- Direct determination of coesite- stishovite transition by in-situ X-ray measurementsTectonophysics, 1976
- Titanochondrodite and titanoclinohumite derived from the upper mantle in the Buell Park Kimberlite, Arizona, USAContributions to Mineralogy and Petrology, 1976
- Synthesis of γ-Mg2SiO4Physics of the Earth and Planetary Interiors, 1974
- High pressure and high temperature investigations in the system MgOSiO2H2OJournal of Solid State Chemistry, 1974
- A comparison of the anelasticity structure beneath western South America and JapanPhysics of the Earth and Planetary Interiors, 1974
- Titanoclinohumite: A possible mineralogical site for water in the upper mantleJournal of Geophysical Research, 1970
- High-pressure reconnaissance investigations in the system Mg2SiO4 - MgO - H2OEarth and Planetary Science Letters, 1967