Distribution and genesis of the eastern Tibetan Plateau geothermal belt, western China
Tang, Xianchun1,2; Zhang, Jian2; Pang, Zhonghe3; Hu, Shengbiao3; Wu, Ying2; Bao, Shujing1
刊名ENVIRONMENTAL EARTH SCIENCES
2017
卷号76期号:1
关键词Hot Spring Eastern Himalayan Syntaxis Eastern Tibetan Plateau Geothermal Belt Kangding Geothermal System
ISSN号1866-6280
DOI10.1007/s12665-016-6342-6
文献子类Article
英文摘要More than 185 hot springs have been recently discovered in the eastern Tibetan Plateau geothermal belt (also called the Kangding-Litang-Batang geothermal belt) (98-102 degrees E, 28-32 degrees N). Among them, more than 60% of springs have temperatures of >40 degrees C, and 11 springs have temperature higher than the local water boiling point. These hot springs are mostly exposed near the fault or valley areas, as bandings in reservoirs of Triassic carbonate rocks and clastic quartz sandstone or in fractured granite and intrusive rocks. The geothermal belt can be subdivided into the Batang-Xiangcheng geothermal field, the Ganzi-Litang geothermal field, and the Luhuo-Kangding geothermal field, which are controlled by the Jinsa fault, Xiangcheng fault, Litang fault, and Xianshuihe fault, respectively. Radiogenic heat from the Mesozoic and Cenozoic granites, possible ductile crustal flow beneath the lower crust, and frictional heat generated by active strike-slipping along faults are the significant heat resources for the geothermal genesis. Frictional heat caused by the slipping along the Xianshuihe fault is the main thermal source for the Luhuo-Kangding geothermal field, whereas magma melting heat is the main source for the Batang-Xiangcheng geothermal field. Glacier water and river water are the main water supply sources, and the fracture serves as the main channel for runoff and hot water flow. The activity intensity and magnitude of the Kangding-Litang-Batang geothermal anomaly were lower than those of the geothermal fields of Yangbajing and Tengchong in the central and southern Tibetan Plateau, respectively, which indicates that the eastern Tibetan Plateau has a strong heat flow background.
WOS关键词GARZE FOLD BELT ; XIANSHUIHE FAULT ZONE ; MESOZOIC TECTONIC EVOLUTION ; SONGPAN-GANZI FLYSCH ; NORTHERN TIBET ; HEAT-FLOW ; CENTRAL QIANGTANG ; ADJACENT AREAS ; YIDUN TERRANE ; SW CHINA
WOS研究方向Environmental Sciences & Ecology ; Geology ; Water Resources
语种英语
出版者SPRINGER
WOS记录号WOS:000392286300031
资助机构Open Foundation of Oil and Gas Survey ; Chinese Geological Survey(DD20160177-03-01) ; National Science Foundation of China(41602257 ; China Postdoctoral Science Foundation(2016M591236) ; 41430319 ; 41574074) ; Open Foundation of Oil and Gas Survey ; Chinese Geological Survey(DD20160177-03-01) ; National Science Foundation of China(41602257 ; China Postdoctoral Science Foundation(2016M591236) ; 41430319 ; 41574074) ; Open Foundation of Oil and Gas Survey ; Chinese Geological Survey(DD20160177-03-01) ; National Science Foundation of China(41602257 ; China Postdoctoral Science Foundation(2016M591236) ; 41430319 ; 41574074) ; Open Foundation of Oil and Gas Survey ; Chinese Geological Survey(DD20160177-03-01) ; National Science Foundation of China(41602257 ; China Postdoctoral Science Foundation(2016M591236) ; 41430319 ; 41574074)
内容类型期刊论文
源URL[http://ir.iggcas.ac.cn/handle/132A11/53148]  
专题地质与地球物理研究所_岩石圈演化国家重点实验室
通讯作者Tang, Xianchun
作者单位1.China Geol Survey, Key Lab Unconvent Petr Geol Oil & Gas Survey, Beijing 100030, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Tang, Xianchun,Zhang, Jian,Pang, Zhonghe,et al. Distribution and genesis of the eastern Tibetan Plateau geothermal belt, western China[J]. ENVIRONMENTAL EARTH SCIENCES,2017,76(1).
APA Tang, Xianchun,Zhang, Jian,Pang, Zhonghe,Hu, Shengbiao,Wu, Ying,&Bao, Shujing.(2017).Distribution and genesis of the eastern Tibetan Plateau geothermal belt, western China.ENVIRONMENTAL EARTH SCIENCES,76(1).
MLA Tang, Xianchun,et al."Distribution and genesis of the eastern Tibetan Plateau geothermal belt, western China".ENVIRONMENTAL EARTH SCIENCES 76.1(2017).
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