Adiabats of quartz, coesite, olivine, and magnesium oxide to 50 kbar and 1000 K, and the adiabatic gradient in the Earth's mantle
- 10 July 1982
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 87 (B7) , 5501-5506
- https://doi.org/10.1029/jb087ib07p05501
Abstract
No abstract availableKeywords
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