Garnet–ilmenite–perovskite transitions in the system Mg4Si4O12–Mg3Al2Si3O12 at high pressures and high temperatures: phase equilibria, calorimetry and implications for mantle structure
- 15 October 2002
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 132 (4) , 303-324
- https://doi.org/10.1016/s0031-9201(02)00075-4
Abstract
No abstract availableKeywords
Funding Information
- Ministry of Education, Culture, Sports, Science and Technology
This publication has 75 references indexed in Scilit:
- Wavelet transform: A tool for the interpretation of upper mantle converted phases at high frequencyGeophysical Research Letters, 2001
- The mechanism of solution of aluminum oxide in MgSiO3 perovskiteGeophysical Research Letters, 2001
- In situ determination of the phase boundary between Wadsleyite and Ringwoodite in Mg2SiO4Geophysical Research Letters, 2000
- Computation of seismic profiles from mineral physics: the importance of the non-olivine components for explaining the 660 km depth discontinuityPhysics of the Earth and Planetary Interiors, 1998
- An experimental study of the garnet-perovskite transformation in the system MgSiO3Mg3Al2Si3O12Physics of the Earth and Planetary Interiors, 1996
- Synthesis and re-investigation of the elastic properties of single-crystal magnesium silicate perovskitePhysics of the Earth and Planetary Interiors, 1994
- Elastic wave velocities of a pyrope-majorite garnet to 3 GPaPhysics of the Earth and Planetary Interiors, 1994
- Ultrahigh-pressure phase relations in the system Mg4Si4O12Mg3Al2Si3O12Physics of the Earth and Planetary Interiors, 1987
- Elasticity of MgSiO3 in the ilmenite phasePhysics of the Earth and Planetary Interiors, 1985
- Wüstite (Fe1‐x O): A review of its defect structure and physical propertiesReviews of Geophysics, 1984