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Steam quantitative analysis and its implication in the Rehai geothermal field, Tengchong

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【作者】 赵平廖志杰过帼颖赵凤三

【Author】 ZHAO Ping(Institute of Geology, Chinese Academy of Sciences, Beijing 100029, China)LIAO Zhijie GUO Guoying and ZHAO Fengsan(Department of Geology, Peking University, Beijing 100871, China)

【机构】 Institute of GeologyChinese Academy of SciencesBeijing 100029ChinaDepartment of GeologyPeking UniversityBeijing 100871China

【摘要】 <正> 1 Geological background The Rehai high-temperature geothermal field is located at the convergent collision zonebetween the Indian and Eurasian plates, in Tengchong County, Yunnan Province. There isplenty of fractures and faults in the region. The gravestone of the Neogene Nanling For-mation is observed, which rests on Yanshanian granites or metamorphic rocks of thePrecambrian Gaoligongshan Group. Geothermal manifestations include fumaroles, boilingspringr, warm springs, steaming ground, sulphur, siliceous sinter, etc. The latesthydrothermal explosion occurred last year. Magntotelluric signals revealed the crustal

  • 【文献出处】 Chinese Science Bulletin ,科学通报(英文版) , 编辑部邮箱 ,1996年06期
  • 【分类号】P314
  • 【被引频次】4
  • 【下载频次】29
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