Phase relations in peridotite+CO2 Systems to 12 GPa: Implications for the origin of kimberlite and carbonate stability in the Earth's upper mantle
- 10 September 1990
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 95 (B10) , 15805-15816
- https://doi.org/10.1029/jb095ib10p15805
Abstract
No abstract availableKeywords
This publication has 48 references indexed in Scilit:
- Ultrahigh-pressure phase relations in the system Mg4Si4O12Mg3Al2Si3O12Physics of the Earth and Planetary Interiors, 1987
- Discussion of recent papers on carbonated peridotite, bearing on mantle metasomatism and magmatism: an alternativeEarth and Planetary Science Letters, 1987
- Evidence for carbonate in the mantleNature, 1986
- K/Na Variation in Phlogopite and Amphibole of Upper Mantle Peridotites Due to Fractionation of the Metasomatizing FluidsThe Journal of Geology, 1986
- Upper mantle oxidation state: Evidence from olivine‐orthopyroxene‐ilmenite assemblagesGeophysical Research Letters, 1983
- An ultrahigh‐pressure furnace assembly to 100 Kbar and 1500°C with minimum temperature uncertaintyGeophysical Research Letters, 1982
- Origin of olivine melilitites — chemical and experimental constraintsJournal of Volcanology and Geothermal Research, 1978
- Direct determination of coesite- stishovite transition by in-situ X-ray measurementsTectonophysics, 1976
- Some basaltic and andesitic gasesReviews of Geophysics, 1975
- Lattice energies, phase transformations and volatiles in the mantlePhysics of the Earth and Planetary Interiors, 1970