Ideal mixing of divalent cations in mafic magma. II. The solution of NiO and the partitioning of nickel between coexisting olivine and liquid
- 1 February 1987
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 51 (2) , 213-219
- https://doi.org/10.1016/0016-7037(87)90233-x
Abstract
No abstract availableKeywords
This publication has 15 references indexed in Scilit:
- Ideal mixing of divalent cations in mafic magma and its effect on the solution of ferrous oxideGeochimica et Cosmochimica Acta, 1986
- Determination of the mixing properties of molten silicates by Knudsen cell mass spectrometry—II. The systems (NaK)AlSi4O10, and (Na-K)AlSi5O12Geochimica et Cosmochimica Acta, 1985
- Nickel partitioning between olivine and silicate meltEarth and Planetary Science Letters, 1978
- A review of experimental studies of crystal/liquid trace element partitioningGeochimica et Cosmochimica Acta, 1978
- Distribution of the Period Four Transition Elements among Olivine, Calcic Clinopyroxene and Mafic Silicate Liquid: Experimental ResultsJournal of Petrology, 1976
- The fractionation of nickel between olivine and augite as a geothermometerGeochimica et Cosmochimica Acta, 1967
- Distribution of elements in geological processesChemical Geology, 1966
- Behaviour of Nickel during Magmatic CrystallizationNature, 1966
- Site of Preference Energy and Selective Uptake of Transition-Metal Ions from a MagmaScience, 1964
- Chemical and spectrochemical analysis of standard silicate samplesGeochimica et Cosmochimica Acta, 1963