Phase boundary deflections at 660‐km depth and episodically layered isochemical convection in the mantle
- 10 August 1994
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 99 (B8) , 15861-15875
- https://doi.org/10.1029/94jb00730
Abstract
No abstract availableKeywords
This publication has 25 references indexed in Scilit:
- Three-Dimensional Instabilities of Mantle Convection with Multiple Phase TransitionsScience, 1993
- Subducting slabs stagnant in the mantle transition zoneJournal of Geophysical Research, 1992
- Intermittent layered convection in a model mantle with an endothermic phase change at 670 kmNature, 1991
- Negative Pressure-Temperature Slopes for Reactions Formign MgSiO 3 Perovskite from CalorimetryScience, 1990
- Olivine‐modified spinel‐spinel transitions in the system Mg2SiO4‐Fe2SiO4: Calorimetric measurements, thermochemical calculation, and geophysical applicationJournal of Geophysical Research, 1989
- Postspinel transformations in the system Mg2SiO4‐Fe2SiO4 and some geophysical implicationsJournal of Geophysical Research, 1989
- Layered convection induced by phase transitionsJournal of Geophysical Research, 1985
- The interaction of a subducting lithospheric slab with a chemical or phase boundaryJournal of Geophysical Research, 1984
- Lattice thermal conductivity within the Earth and considerations of a relationship between the pressure dependence of the thermal diffusivity and the volume dependence of the Grüneisen parameterJournal of Geophysical Research, 1976
- The Earth's mantleEOS, Transactions American Geophysical Union, 1954