OLIVINE SILICATE MELT PARTITIONING OF GERMANIUM - AN EXAMPLE OF A NEARLY CONSTANT PARTITION-COEFFICIENT

被引：19

作者：

CAPOBIANCO, CJ ^{[1
]}

WATSON, EB ^{[1
]}

机构：

[1] RENSSELAER POLYTECH INST,DEPT GEOL,TROY,NY 12181

来源：

GEOCHIMICA ET COSMOCHIMICA ACTA | 1982年 / 46卷 / 02期

关键词：

D O I：

10.1016/0016-7037(82)90250-2

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：

引用

页码：235 / 240

页数：6

共 20 条

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[18] DISTRIBUTION OF TRACE QUANTITIES OF GERMANIUM BETWEEN METAL SILICATE AND SULFIDE PHASES [J].

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[19] CHEMICAL CLASSIFICATION OF IRON METEORITES .I. A STUDY OF IRON METEORITES WITH LOW CONCENTRATIONS OF GALLIUM AND GERMANIUM [J].

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[20]

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