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云南金沙江蛇绿岩的地球化学特征及其成因的初步研究
引用本文:韩 松,贾秀勤,黄忠祥,董金泉,张 旗,陈 雨,李秀云.云南金沙江蛇绿岩的地球化学特征及其成因的初步研究[J].岩石矿物学杂志,1996,15(3):203-212.
作者姓名:韩 松  贾秀勤  黄忠祥  董金泉  张 旗  陈 雨  李秀云
作者单位:中国科学院高能物理研究所,中国科学院地质研究所
摘    要:本文报道了出露于云南省德钦县白马雪山、书松、共卡及吉义独地区的金沙江蛇绿岩的地球化学特征。该蛇绿岩各岩石单元均为LREE富集型。文中讨论了金沙江蛇绿岩的成因及其形成的构造环境,指出该区玄武岩的微量元素和REE分布可用NMORB与OIB的混合来解释,推测形成于类似现今冰岛的扩张脊与地幔热柱重叠的构造环境

关 键 词:云南  金沙江  蛇绿岩  地球化学  岩石  成因  构造  环境

A Preliminary Geochemical and Genetic Study of Jinsha River Ophiolites, Yunnan Province
Abstract:The present paper describes geochemical characteristics of Jinsha River ophiolites in Baimaxueshan, Shusong, Gongka and Jiyidu areas of Deqen County. Verious rocks assemblages of the ophiolites are exclusively of LREE-enriched patterns, and their genesis and tectonic setting are discussed here. It is pointed out that the trace element and REE characteristics of basalts could be interpreted by mixing N-MORB with OIB, and that Jinsha River Ophiolites were probably formed in a tectonic environment characterized by the superimposition of spreading ridge and mantle plume, similar to things of Iceland.
Keywords:Jinsha River ophiolite  geochemistry  genesis of rocks  tectonic setting
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