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Compilation of heat flow data in the continental area of China (4th edition)
Jiang, GZ (Jiang Guang-Zheng)1,2; Gao, P (Gao Peng)1,2; Rao, S (Rao Song)3; Zhang, LY (Zhang Lin-You)1,2; Tang, XY (Tang Xiao-Yin)4; Huang, F (Huang Fang)5; Zhao, P (Zhao Ping)6; Pang, ZH (Pang Zhong-He)1; He, LJ (He Li-Juan)1; Hu, SB (Hu Sheng-Biao)1; Wang, JY (Wang Ji-Yang)1; Rao, S
Source PublicationCHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION
2016
Volume59Issue:8Pages:2892-2910
DOI10.6038/cjg20160815
AbstractTerrestrial heat flow provides a direct surface indication of the thermal state within the Earth. It is a crucial parameter to reveal the lithospheric thermal structure, geodynamic processes and to evaluate the potential of geothermal resources. Measurements and compilations of heat flow data are considered as a fundamental work for geothermal study. Heat flow data in continental China have been published in three editions and the total number has reached 862 in 2001. Since then, no more compilation has been accomplished in the last 15 years. Upon the 3rd edition, 368 new heat flow data have been compiled in this paper as the 4th edition. We gathered 345 newly published data during 2002 to 2016, together with 23 newly measured heat flow values in the blank areas e.g. the hinter land of the Tibetan Plateau, Changbai Mountain etc. In this updated heat flow data set (4th edition), the total number of data has reached 1230 and the data categories for A, B, C and D account for 49.3%, 34.2%, 12.6% and 3.9%, respectively. The heat flow values range from 30 to 140 mW . m(-2) with a mean of 60.4 +/- 12.3 mW . m(-2) excluded the data for category D. Based on the new data base, we updated the geographic distribution of heat flow sites in the continental area of China, which manifests significantly improvement on the coverage and the inhomogeneity of heat flows patial distribution. The overall heat flow pattern of in the continental area of China is featured as "high" in the eastern and southwestern areas while "low" in the central and northwestern parts. Affected by the far-field effect of the westward subduction of the pacific plate, the eastern high heat flow province extends from southeastern China to Songliao Basin and Changbai Mountain. Mainly controlled by the collision between the India Plate and the Eurasia Plate, the southwestern high heat flow province shows a belt distribution in the Yarlung-Zangbo Suture Zone in E-W direction and rift zones in S-N direction, meanwhile the values decreased from the south to the north. The central China, with relative week tectonic activities since Cenozoic, is a low-medium heat flow province.
Subject Area地质学
WOS IDWOS:000381166400015
Language英语
Indexed BySCI
KeywordBorehole Temperature Geothermal-field Northwest China Sichuan Basin South China Data Set Lithosphere Tibet Earth Hole
Cooperation Status国内
Department碰撞与隆升
Citation statistics
Cited Times:56[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/7646
Collection图书馆
Corresponding AuthorRao, S
Affiliation1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.Yangtze Univ, Minist Educ, Key Lab Explorat Technol Oil & Gas Resources, Wuhan 430100, Peoples R China
4.Xi An Jiao Tong Univ, Xian 710049, Peoples R China
5.China Earthquake Adm, Inst Geophys, Beijing 100081, Peoples R China
6.Chinese Acad Sci, Inst Tibetan Plateau Res, Beijing 100101, Peoples R China
Recommended Citation
GB/T 7714
Jiang, GZ ,Gao, P ,Rao, S ,et al. Compilation of heat flow data in the continental area of China (4th edition)[J]. CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,2016,59(8):2892-2910.
APA Jiang, GZ .,Gao, P .,Rao, S .,Zhang, LY .,Tang, XY .,...&Rao, S.(2016).Compilation of heat flow data in the continental area of China (4th edition).CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION,59(8),2892-2910.
MLA Jiang, GZ ,et al."Compilation of heat flow data in the continental area of China (4th edition)".CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION 59.8(2016):2892-2910.
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