Partitioning of MgO, FeO, NiO, MnO and Cr2O3 between magnesian silicate perovskite and magnesiowüstite: implications for the origin of inclusions in diamond and the composition of the lower mantle
- 1 July 1992
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 111 (2-4) , 229-240
- https://doi.org/10.1016/0012-821x(92)90181-t
Abstract
No abstract availableKeywords
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