Isothermal compressibility of hydrous ringwoodite and its relation to the mantle discontinuities
- 1 February 2000
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 27 (3) , 413-416
- https://doi.org/10.1029/1999gl011032
Abstract
No abstract availableKeywords
This publication has 17 references indexed in Scilit:
- Elastic properties of hydrous ringwoodite (γ-phase) in Mg2SiO4Earth and Planetary Science Letters, 1998
- Compressibility of hydrous wadsleyite (β‐phase) in Mg2SiO4 by high pressure X‐ray diffractionGeophysical Research Letters, 1997
- Structure and crystal chemistry of hydrous wadsleyite, Mg1.75SiH0.5O4: possible hydrous magnesium silicate in the mantle transition zonePhysics and Chemistry of Minerals, 1996
- Sound velocities of olivine and beta polymorphs of Mg2SiO4 at Earth's transition zone pressuresGeophysical Research Letters, 1996
- Hydrous modified spinel, Mg1.75SiH0.5O4: A new water reservoir in the mantle transition regionGeophysical Research Letters, 1995
- Synchrotron Infrared Absorbance Measurements of Hydrogen in MgSiO 3 PerovskiteScience, 1994
- Global mapping of topography on the 660-km discontinuityNature, 1992
- Spinel elasticity and seismic structure of the transition zone of the mantleNature, 1991
- Seismic imaging of upper-mantle structure with new evidence for a 520-km discontinuityNature, 1990
- Single-Crystal Elastic Properties of the Modified Spinel (Beta) Phase of Magnesium OrthosilicateScience, 1984