The Inference of Magmatic Heat Source Beneath the Rehai (Hot Sea) Field of Tengchong From the Result of Magnetotelluric Sounding  

作　　者：白登海 廖志杰 赵国泽 王绪本 

机构地区：[1]Institute of Geophysics, Academia Sinica, Beijing 100101, PRC [2]Department of Geology, Peking University, Beijing 100871, PRC [3]Institute of Geology, State Seismologic Bureau, Beijing 100029, PRC [4]Department of Geophysical Exploration, Chengdu Geologic College, Chengdu 610059, PRC

出　　处：《Chinese Science Bulletin》1994年第7期572-577,共6页

基　　金：The project of "Eighth Five" scientific and technological research of the State Science and Technology Commission of China.

摘　　要：1 Geothermal Geology The Rehai （Hot Sea） geothermal field is at 24°57.5′N and 98°26.5′E in amountainous （1400-1800 m） area, approximately 18 km southwest of TengchongTown. The Rehai field has noticeable surface manifestations including boiling springsand fumaroles with a maximum temperature of about 96℃. The thermal springsdischarge water of the sodium-chloride-bicarbonate type with TDS of 2. 8 g/l and SiO₂of 450 mg/l. By geothermometers, the reservoir temperature is generally 23O℃.

关 键 词：geothermal FIELD MAGMATIC heat source MAGNETOTELLURIC sounding. 

分 类 号：P314[天文地球—固体地球物理学]