In situ determination of the phase boundary between Wadsleyite and Ringwoodite in Mg2SiO4
- 15 March 2000
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 27 (6), 803-806
- https://doi.org/10.1029/1999gl008425
Abstract
No abstract availableThis publication has 17 references indexed in Scilit:
- An in situ X ray diffraction study of the α‐β transformation kinetics of Mg2SiO4Geophysical Research Letters, 1998
- In situ X-ray observations of the coesite-stishovite transition: reversed phase boundary and kineticsPhysics and Chemistry of Minerals, 1996
- In situ X ray observation of high‐pressure phase transitions of MgSiO3 and thermal expansion of MgSiO3 perovskite at 25 GPa by double‐stage multianvil systemJournal of Geophysical Research, 1995
- The Phase Boundary Between α- and β-Mg 2 SiO 4 Determined by in Situ X-ray ObservationScience, 1994
- Sharpness of upper-mantle discontinuities determined from high-frequency reflectionsNature, 1993
- Petrology, elasticity, and composition of the mantle transition zoneJournal of Geophysical Research, 1992
- In situ observation of the olivine‐spinel phase transformation in Fe2SiO4 using synchrotron radiationJournal of Geophysical Research, 1987
- Synthesis and crystal-chemical characterization of MgSiO3 perovskiteEarth and Planetary Science Letters, 1978
- Direct determination of coesite- stishovite transition by in-situ X-ray measurementsTectonophysics, 1976
- Synthesis of γ-Mg2SiO4Physics of the Earth and Planetary Interiors, 1974