Effects of fO2, fS2, temperature, and melt composition on Fe-Ni exchange between olivine and sulfide liquid: implications for natural olivine–sulfide assemblages
- 15 July 2003
- journal article
- Published by Elsevier BV in Geochimica et Cosmochimica Acta
- Vol. 67 (14), 2663-2681
- https://doi.org/10.1016/s0016-7037(02)01416-3
Abstract
No abstract availableKeywords
This publication has 35 references indexed in Scilit:
- The solubility of ruthenium in sulfide liquid: implications for platinum group mineral stability and sulfide melt–silicate melt partitioningChemical Geology, 2002
- A comment on “Fe-Ni exchange between olivine and sulphide liquid: Implications for oxygen barometry in sulphide-saturated magmas” byGeochimica et Cosmochimica Acta, 2001
- Fe–Ni exchange between olivine and sulphide liquid: implications for oxygen barometry in sulphide-saturated magmasGeochimica et Cosmochimica Acta, 2000
- Sulfur in basaltic magmasGeochimica et Cosmochimica Acta, 1992
- Oxidation states of mid-ocean ridge basalt glassesEarth and Planetary Science Letters, 1986
- Dissolved carbon dioxide in basaltic glasses: concentrations and speciationEarth and Planetary Science Letters, 1986
- The partition of nickel between olivine, magma and immiscible sulfide liquidChemical Geology, 1981
- Carbon dioxide in silicate melts and crystals; Part I, Solubility measurementsAmerican Journal of Science, 1976
- Least squares fitting of a straight line with correlated errorsEarth and Planetary Science Letters, 1968
- A thermodynamic study of pyrite and pyrrhotiteGeochimica et Cosmochimica Acta, 1964