The dependence of the Fe2+-Mg cation-partitioning between olivine and basaltic liquid on pressure, temperature and composition
- 1 March 1989
- journal article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 101 (3) , 261-273
- https://doi.org/10.1007/bf00375311
Abstract
No abstract availableKeywords
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