Effect of pressure on the melting of olivine and spinel polymorph of Fe2SiO4
- 15 January 1967
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 72 (2), 679-686
- https://doi.org/10.1029/jz072i002p00679
Abstract
No abstract availableKeywords
This publication has 6 references indexed in Scilit:
- The olivine-spinel transition in Fe2SiO4and Ni2SiO4Journal of Geophysical Research, 1965
- Demonstration of the electrical conductivity jump produced by the olivine-spinel transitionJournal of Geophysical Research, 1965
- The melting of forsterite up to 50 kilobarsJournal of Geophysical Research, 1964
- Effect of pressure on the melting of diopside, CaMgSi2O6, and albite, NaAlSi3O8, in the range up to 50 kilobarsJournal of Geophysical Research, 1963
- A method of estimating the melting‐point gradient in the Earth's mantleEOS, Transactions American Geophysical Union, 1952
- The system MgO-FeO-SiO 2American Journal of Science, 1935