Silicate and base-metal sulfide inclusions in chromites from the Maqsad area (Oman ophiolite, Gulf of Oman): A model for entrapment
- 1 March 1989
- Vol. 22 (3) , 173-190
- https://doi.org/10.1016/0024-4937(89)90054-6
Abstract
No abstract availableThis publication has 40 references indexed in Scilit:
- Primary sulphide melt inclusions in mantle-derived megacrysts and pyroxenitesPublished by Elsevier ,2010
- Mantle flow patterns at an oceanic spreading centre: The Oman peridotites recordPublished by Elsevier ,2003
- FeNiCu sulfides in tectonite peridotites from the Maqsad district, Sumail ophiolite, southern Oman: Implications for the origin of the sulfide component in the oceanic upper mantleTectonophysics, 1988
- Structural mapping in the Oman ophiolites: Mantle diapirism along an oceanic ridgeTectonophysics, 1988
- K/Na Variation in Phlogopite and Amphibole of Upper Mantle Peridotites Due to Fractionation of the Metasomatizing FluidsThe Journal of Geology, 1986
- Deformation of chromite: S.E.M. investigationsTectonophysics, 1986
- Platinum-group minerals and other solid inclusions in chromite of ophiolitic complexes: Occurrence and petrological significanceTschermaks Mineralogische und Petrographische Mitteilungen, 1983
- Experimental crystallization of chrome spinel in FAMOUS basalt 527-1-1Earth and Planetary Science Letters, 1980
- The Crystallization of Spinel from Basaltic Liquid as a Function of Oxygen FugacityThe Journal of Geology, 1974
- Plagioclase cation exchange equilibria with aqueous chloride solution; results at 700 degrees C and 2000 bars in the presence of quartzAmerican Journal of Science, 1972