Temperature and discontinuities in the transition layer within the Earth's mantle: Geophysical application of the olivine-spinel transition in the Mg2SiO4-Fe2SiO4System
- 15 May 1968
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 73 (10) , 3281-3294
- https://doi.org/10.1029/jb073i010p03281
Abstract
No abstract availableKeywords
This publication has 34 references indexed in Scilit:
- Phase Changes in the Upper MantleScience, 1967
- The pyroxene-garnet transformation in the earth's mantleEarth and Planetary Science Letters, 1967
- High-pressure transformations in pyroxenesEarth and Planetary Science Letters, 1966
- High-pressure synthesis of Mg2SiO4 spinelEarth and Planetary Science Letters, 1966
- High-pressure transformation in CoSiO3 pyroxene and some geochemical implicationsEarth and Planetary Science Letters, 1966
- High-pressure transformation of FeSiO3 pyroxene to spinel plus stishoviteEarth and Planetary Science Letters, 1966
- XII.—Petrology and Petrogenesis of some Garnetiferous PeridotitesTransactions of the Royal Society of Edinburgh, 1963
- Temperatures in the earth's interiorJournal of Atmospheric and Terrestrial Physics, 1957
- Temperature Distributions within the Earth.Journal of Physics of the Earth, 1954
- Thermo-Electromotive Force, Peltier Heat, and Thomson Heat under PressureProceedings of the American Academy of Arts and Sciences, 1918