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Abstract
Olivine-liquid partition coefficients for Ni(DNi), calculated from Ni vs MgO abundance variations in komatiite series basalts, compare favourably with experimentally determined values, if Ni variations in olivine-controlled basalts can be modelled with an equation that assumes equilibrium between the entire olivine crystal and its coexisting liquid.-J.A.Z.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Evidence for equilibrium conditions during the partitioning of nickel between olivine and komatiite liquids. |
| Series title | American Mineralogist |
| Volume | 71 |
| Issue | 11-12 |
| Year Published | 1986 |
| Language | English |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | American Mineralogist |
| First page | 1337 |
| Last page | 1342 |
| Google Analytic Metrics | Metrics page |