Primary sulphide melt inclusions in mantle-derived megacrysts and pyroxenites
Authors:
- T. AndersenTAT. Andersen
- W.L. GriffinWGW.L. Griffin
- Suzanne Y. O'REillySuzanne Y. O'REilly
Abstract
No abstract availableKeywords
This publication has 30 references indexed in Scilit:
- OXIDATION STATUS OF THE MANTLE: PAST AND PRESENTAnnual Review of Earth and Planetary Sciences, 1985
- A xenolith-derived geotherm for southeastern australia and its geophysical implicationsTectonophysics, 1985
- Instability of Cylindrical Voids in AluminaJournal of the American Ceramic Society, 1978
- Effect of enstatite activity and oxygen partial pressure on the point-defect chemistry of olivinePhysics of the Earth and Planetary Interiors, 1978
- Textures and genesis of phenocrysts and megacrysts in basaltic lavas from the Pinacate volcanic fieldAmerican Journal of Science, 1977
- Point defects and non-stoichiometry in forsteritePhysics of the Earth and Planetary Interiors, 1975
- The Crystallization of Spinel from Basaltic Liquid as a Function of Oxygen FugacityThe Journal of Geology, 1974
- Megacrysts from the Newer Basalts and Other Basaltic Rocks of Southeastern AustraliaGeological Society of America Bulletin, 1974
- Oxides of low pressure origin from alkali basaltic rocks, southern highlands, N.S.W., and their bearing on the petrogenesis of alkali basaltic magmasJournal of the Geological Society of Australia, 1973
- The origin and petrogenetic significance of hour-glass zoning in titaniferous clinopyroxenesMineralogical Magazine, 1973