Trace element partitioning between mantle minerals and silico-carbonate melts at 6-12 GPa and applications to mantle metasomatism and kimberlite genesis
Trace element partitioning between mantle minerals and silico-carbonate melts at 6-12 GPa and applications to mantle metasomatism and kimberlite genesis
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DOI：
10.1016/j.lithos.2012.11.027
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发表时间：
2013-02-01
期刊：
影响因子：
3.5
通讯作者：
Hoefer, H. E.
中科院分区：
文献类型：
--
作者：
Girnis, A. V.;Bulatov, V. K.;Hoefer, H. E.
实验研究了地幔矿物（橄榄石、辉石、石榴石）和硅-碳酸盐熔体在6 ~ 12 GPa和1300 ~ 1700℃条件下的LILE、HFSE、REE、Cu、Pb、Co、Ni等微量元素的分配
The partitioning of a number of trace elements (LILE, HFSE, REE, Cu, Pb, Co, Ni) between mantle minerals (olivine, pyroxenes and garnet) and silico-carbonate melts was experimentally studied at 6-12 GPa and 1300-1700 degrees C. The starting compositions were model kimberlitic with similar to 30 wt.% SiO2, which differentiated to carbonatite-like melts with