Nickel partitioning between olivine and liquid in natural basalts: Henry's Law behavior
- 1 July 1980
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 48 (2) , 293-302
- https://doi.org/10.1016/0012-821x(80)90193-4
Abstract
No abstract availableKeywords
This publication has 24 references indexed in Scilit:
- Nickel content of basaltic magmas: identification of primary magmas and a measure of the degree of olivine fractionationPublished by Elsevier ,2003
- Determination of crystallization temperatures in fractional crystallization series by nickel partitioning equationsEarth and Planetary Science Letters, 1979
- Nickel, and the existence of high-MgO liquids in natureEarth and Planetary Science Letters, 1979
- Comments on: “The partitioning of nickel between olivine and silicate melt” by S.R. Hart and K.E. DavisEarth and Planetary Science Letters, 1979
- Reply to D.B. Clarke and M.J. O'Hara, “nickel, and the existence of high-MgO liquids in nature”Earth and Planetary Science Letters, 1979
- Pressure dependence of nickel partitioning between forsterite and aluminous silicate meltsEarth and Planetary Science Letters, 1979
- Nickel partitioning between olivine and silicate meltEarth and Planetary Science Letters, 1978
- Experimental determination of nickel partition coefficients between liquid, pargasite, and garnet peridotite minerals and concentration limits of behavior according to Henry's law at high pressure and temperatureAmerican Journal of Science, 1978
- The petrogenesis of peridotitic komatiites: Evidence from high-pressure melting experimentsEarth and Planetary Science Letters, 1977
- Calculated diffusion coefficients and the growth rate of olivine in a basalt magmaLithos, 1975