ORIGIN OF JOSEPHINITE

被引:14
作者
BIRD, JM
WEATHERS, MS
机构
[1] Department of Geological Sciences, Cornell University, Ithaca, New York
关键词
D O I
10.2343/geochemj.13.41
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
Josephinite is a nickel-iron alloy-bearing rock from Josephine County, southwestern Oregon. Josephinite had been thought to be the same as the metallic nickel-iron mineral awaruite (KRlSHNARAO, 1962, 1964; ramdohr, 1950), but recently it has been shown to be a complex assemblage of minerals (BIRD and Weathers, 1975a). Although most samples of josephinite are somewhat altered, least-altered josephinite consists of several nickel-iron alloys, one intergrown with andradite garnet, an iron-cobalt alloy, and minor amounts of iron-nickel arsenides, iron-nickel-copper sulphides, and various unidentified phases. The intergrown metal-garent assemblage is apparently unique to josephinite. Alteration phases include Serpentine minerals and magnetite. © 1979, GEOCHEMICAL SOCIETY OF JAPAN. All rights reserved.
引用
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页码:41 / 55
页数:15
相关论文
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