Fluids in equilibrium with peridotite minerals: Implications for mantle metasomatism
- 1 May 1986
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 50 (5) , 711-724
- https://doi.org/10.1016/0016-7037(86)90347-9
Abstract
No abstract availableThis publication has 46 references indexed in Scilit:
- The trapped fluid phase in upper mantle xenoliths from Victoria, Australia: implications for mantle metasomatismContributions to Mineralogy and Petrology, 1984
- CO2-CO fluid inclusions in a composite peridotite xenolith: implications for upper mantle oxygen fugacityContributions to Mineralogy and Petrology, 1984
- Oxidation states of the upper mantle recorded by megacryst ilmenite in kimberlite and type A and B spinel lherzolitesContributions to Mineralogy and Petrology, 1984
- Pyroxene-carbonate reactions in the upper mantleEarth and Planetary Science Letters, 1983
- Mantle metasomatism—continuing chemical change within the EarthNature, 1982
- Intrinsic oxygen fugacity measurements: techniques and results for spinels from upper mantle peridotites and megacryst assemblagesGeochimica et Cosmochimica Acta, 1981
- 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
- Correction factors for electron probe microanalysis of silicates, oxides, carbonates, phosphates, and sulfatesAnalytical Chemistry, 1970
- On the solubility of albite in supercritical water in the range of 400 degrees to 600 degrees C and 750 to 3500 barsAmerican Journal of Science, 1968
- Reactions of quartz and corundum with aqueous chloride and hydroxide solutions at high temperatures and pressuresAmerican Journal of Science, 1967