Element partitioning between silicate perovskites and calcic ultrabasic melt

被引：24

作者：

Kato, T ^{[1
]}

Ohtani, E ^{[1
]}

Ito, Y ^{[1
]}

Onuma, K ^{[1
]}

机构：

[1] TOHOKU UNIV,FAC SCI,SENDAI,MIYAGI 98077,JAPAN

来源：

PHYSICS OF THE EARTH AND PLANETARY INTERIORS | 1996年 / 96卷 / 2-3期

关键词：

D O I：

10.1016/0031-9201(96)03151-2

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

Element partitioning between Mg- and Ca-perovskites and anhydrous calcic ultrabasic melt was studied experimentally at 25 GPa and 2200 degrees C. The observed partitioning relationships in this system are similar to the results of previous studies in magnesian ultrabasic and basaltic systems, and are consistent with predictions based on crystal chemical considerations. These results provide new insights into early global mantle differentiation, and kimberlite petrogenesis from the lower-mantle source regions.

引用

页码：201 / 207

页数：7

共 28 条

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