Melting of garnet peridotite to 13 GPa and the early history of the upper mantle
- 1 July 1986
- journal article
- Published by Springer Nature in Nature
- Vol. 322 (6077), 354-356
- https://doi.org/10.1038/322354a0
Abstract
No abstract availableKeywords
This publication has 21 references indexed in Scilit:
- Melting of peridotite to 14 GPa and the genesis of komatiiteNature, 1985
- THE MAGMA OCEAN CONCEPT AND LUNAR EVOLUTIONAnnual Review of Earth and Planetary Sciences, 1985
- The mineralogy and chemistry of the lower mantle: an implication of the ultrahigh-pressure phase relations in the system MgO FeO SiO2Earth and Planetary Science Letters, 1984
- The Earth as a Planet: Paradigms and ParadoxesScience, 1984
- Fusion of pyrope at high pressures and rapid crystal growth from the pyrope meltNature, 1981
- Melting of forsterite Mg2SiO4 up to 15 GPaPhysics of the Earth and Planetary Interiors, 1981
- Chemical stratification of the mantleJournal of Geophysical Research, 1979
- The effect of CO<2) upon partial melting of peridotite in the system Na<2) O-CaO-Al<2) O<3) -MgO-SiO<2) -CO<2) to 35 kb, with an analysis of melting in a peridotite-H<2) O-CO<2) systemAmerican Journal of Science, 1978
- Rare earth elements in garnets and clinopyroxenes from garnet lherzolite nodules in kimberlitesEarth and Planetary Science Letters, 1975
- Effect of pressure on the melting of diopside, CaMgSi2O6, and albite, NaAlSi3O8, in the range up to 50 kilobarsJournal of Geophysical Research, 1963