Reduced Volatiles in the System C-O-H: Implications to Mantle Melting, Fluid Formation, and Diamond Genesis
- 1 January 1982
- book chapter
- Published by Springer Nature
Abstract
No abstract availableKeywords
This publication has 23 references indexed in Scilit:
- Lead, uranium, strontium, potassium and rubidium in inclusion-bearing diamonds and mantle-derived xenoliths from Southern AfricaPublished by Elsevier ,2002
- Conditions of origin of natural diamonds of peridotite affinityJournal of Geophysical Research, 1980
- Chemical characteristics of the volcanic gases from Nyiragongo lava lake and the generation of CH4-rich fluid inclusions in alkaline rocksJournal of Volcanology and Geothermal Research, 1980
- The carbon isotopic composition of diamonds: relationship to diamond shape, color, occurrence and vapor compositionGeochimica et Cosmochimica Acta, 1980
- The solubility of carbon monoxide in silicate melts at high pressures and its effect on silicate phase relationsEarth and Planetary Science Letters, 1979
- Experimental studies on the relationship between kimberlite magmas and partial melting of peridotitePublished by Wiley ,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
- Carbon dioxide in silicate melts; II, Solubilities of CO 2 and H 2 O in CaMgSi 2 O 6 (diopside) liquids and vapors at pressures to 40 kbAmerican Journal of Science, 1978
- A comparative trace element study of diamonds from Premier, Finsch and Jagersfontein mines, South AfricaPhysics and Chemistry of the Earth, 1975
- Effect of pressure on the melting of diopside, CaMgSi2O6, and albite, NaAlSi3O8, in the range up to 50 kilobarsJournal of Geophysical Research, 1963