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

作　　者：赵平 廖志杰 过帼颖 赵凤三 

机构地区：[1]Institute of Geology, Chinese Academy of Sciences, Beijing 100029, China [2]Department of Geology, Peking University, Beijing 100871, China

出　　处：《Chinese Science Bulletin》1996年第6期501-505,共5页

摘　　要：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

关 键 词：GEOTHERMAL FIELD GEOTHERMAL STEAM RESERVOIR temperature. 

分 类 号：P314[天文地球—固体地球物理学]