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陆地水热系统气体地球化学研究进展
引用本文:高博,陈践发,王先彬.陆地水热系统气体地球化学研究进展[J].地球科学进展,2004,19(2):211-217.
作者姓名:高博  陈践发  王先彬
作者单位:1. 中国科学院地球化学研究所,贵州,贵阳,550002;云南大学地球科学系,云南,昆明,650091
2. 石油大学,北京,昌平,102249
3. 中国科学院兰州地质研究所,甘肃,兰州,730000
摘    要:地表水热活动常伴有通量不等的气体释放,作为水-岩反应和地球深部脱气的产物,泉气的化学和同位素组成因其热储所处的大地构造单元、岩性和应力状态的差异而有所不同。对泉气化学和同位素组成时空变化的观测和研究是了解地壳-岩石圈动力学的重要方面,有助于地震、火山活动等地质灾害的监测和地热资源的开发利用。

关 键 词:水热系统  泉气  稀有气体  同位素
文章编号:1001-8166(2004)02-0211-07
修稿时间:2003年4月16日

A REVIEW OF GAS GEOCHEMISTRY OF CONTINENTAL GEOTHERMAL SYSTEM
GAO Bo ,CHEN Jian fa ,WANG Xian bin.A REVIEW OF GAS GEOCHEMISTRY OF CONTINENTAL GEOTHERMAL SYSTEM[J].Advance in Earth Sciences,2004,19(2):211-217.
Authors:GAO Bo    CHEN Jian fa  WANG Xian bin
Institution:1. Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550000,China;2.Yunnan University, Kunming,650091,China;3.Lanzhou Institute of Geology,Chinese Academy of Sciences, Lanzhou,730000,China;4.Petroleam University, Beijing 102249,China
Abstract:Hot spring water and gases are always concomitant and the fluxes of gases released from different geothermal systems are various. As a results of water rock reaction and degassing from the deep,the chemical and isotopic composition of geothermal spring gases are diverse because of different settings of the geothermal reservoir in the aspect of tectonic position, lithology and stress status. It is of significance to study the spatio temporal changes of chemical and isotopic component of hot sprig gases and that may help us realize crust lithosphere kinetic status. Furthermore, there will be application foreground in the monitoring or predicting earthquake and volcano activity as well as geothermal exploitation and utilization.
Keywords:Geothermal system  Gases of thermal spring  Noble gas  Isotope  
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