Computation of seismic profiles from mineral physics: the importance of the non-olivine components for explaining the 660 km depth discontinuity
- 1 April 1998
- journal article
- review article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 106 (3-4) , 275-298
- https://doi.org/10.1016/s0031-9201(98)00076-4
Abstract
No abstract availableKeywords
This publication has 125 references indexed in Scilit:
- Shear and compressional mode measurements with GHz ultrasonic interferometry and velocity-composition systematics for the pyrope-almandine solid solution seriesPhysics of the Earth and Planetary Interiors, 1997
- 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
- Mineral physics constraints on the chemical composition of the Earth's lower mantlePhysics of the Earth and Planetary Interiors, 1994
- On the stability of a fluid layer containing a univariant phase transition: application to planetary interiorsPhysics of the Earth and Planetary Interiors, 1989
- The single-crystal elastic properties of jadeitePhysics of the Earth and Planetary Interiors, 1988
- 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
- Preliminary reference Earth modelPhysics of the Earth and Planetary Interiors, 1981