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西藏地热活动中铯的富集过程探讨
引用本文:李振清,侯增谦,聂凤军,杨竹森,曲晓明,孟祥金,赵元艺.西藏地热活动中铯的富集过程探讨[J].地质学报,2006,80(9):1457-1464.
作者姓名:李振清  侯增谦  聂凤军  杨竹森  曲晓明  孟祥金  赵元艺
作者单位:中国地质科学院矿产资源研究所,北京,100037
基金项目:国家重点基础研究规划“973”项目“印度-亚洲大陆主碰撞带成矿作用”(编号2002CB412606),国家自然科学基金项目“青藏高原热水活动的时空格架和氦同位素研究”(编号40302028)资助成果
摘    要:硅华铯矿是青藏高原独特的铯矿床,它赋存在高温地热活动的产物——硅华中,主要分布在高原的强烈地热活动区。为什么硅华铯矿目前仅在青藏高原发现,别的地方尚未见报导,显然跟青藏高原在近期的构造运动有关。本文详细研究了Cs元素在地热流体和泉华中的特征,以及与Rb、Cl等离子的相关关系,探讨了Cs元素的地球化学行为,总结Cs元素在地热活动中的富集过程:地壳的局部重熔作用导致了Cs的预富集;岩浆的结晶、分异使Cs再次浓集;大规模的水/岩反应使流体中Cs更加富集。

关 键 词:西藏  地热活动  硅华铯矿  富集过程
修稿时间:2006年7月15日

Enrichment of Element Cesium during Modern Geothermal Action in Tibet,China
LI Zhenqing,HOU Zengqian,NIE Fengjun,YANG Zhusen QU Xiaoming,MENG Xiangjin,ZHAO YuanyiInstitute of mineral resources,Chinese Academy of Geological sciences,Beijing.Enrichment of Element Cesium during Modern Geothermal Action in Tibet,China[J].Acta Geologica Sinica,2006,80(9):1457-1464.
Authors:LI Zhenqing  HOU Zengqian  NIE Fengjun  YANG Zhusen QU Xiaoming  MENG Xiangjin  ZHAO YuanyiInstitute of mineral resources  Chinese Academy of Geological sciences  Beijing
Abstract:Geyserite Cs-deposit, occurring in the sediment of high-temperature geothermal action, is the particular Cs-deposit in Tibet. They mainly distribute in the violent geothermal active regions. The fact that the geyserite Cs-deposit is discovered only in Tibet has relation with the modern tectogenetic movement of the Tibet plateau by all appearances. This paper studied the geochemical characteristic of Cs in geothermal fluid and geyserite, the correlation with some irons (including Rb, Cl, Li et al.). Based on the research of the geochemical activity of Cs, the paper sum up the enrichment process of Cs in geothermal activity: partial anatexis of crust conduced the preconcentrating of Cs; crystallizing, separation of magma resulted in the re-concentrating of Cs; large scale reaction of fliud-rock induced Cs more enrichment in fluid.
Keywords:Tibet  geothermal activity  geyserite Cs-deposit  enrichment process
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