Element partitioning between silicate minerals and coexisting melts at pressures of 1–27 GPa, and implications for mantle evolution
- 1 July 1992
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 111 (2-4) , 241-255
- https://doi.org/10.1016/0012-821x(92)90182-u
Abstract
No abstract availableKeywords
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