PARTITIONING OF RARE-EARTH ELEMENTS BETWEEN PHOSPHATE-RICH CARBONATITE MELTS AND MANTLE PERIDOTITES

被引：19

作者：

RYABCHIKOV, ID ^{[1
]}

ORLOVA, GP ^{[1
]}

SENIN, VG ^{[1
]}

TRUBKIN, NV ^{[1
]}

机构：

[1] VI VERNADSKY GEOCHEM & ANALYT CHEM INST,MOSCOW,RUSSIA

来源：

MINERALOGY AND PETROLOGY | 1993年 / 49卷 / 1-2期

关键词：

D O I：

10.1007/BF01162922

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：

Near solidus equilibria in the system mantle peridotite-carbonate-phosphate doped with Ce and Yb have been studied at 20 kbar and 950-degrees-C. Carbonatitic melts in this system may be quenched into homogeneous glasses. Such melts intensely extract REE from rock-forming mantle minerals, and their migration may cause processes of mantle metasomatism.

引用

页码：1 / 12

页数：12

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