| High-quality heat flow determination from the crystalline basement of the south-east margin of North China Craton | |
| Jiang, GZ (Jiang, Guangzheng)1,2; Tang, XY (Tang, Xiaoyin)3; Rao, S (Rao, Song)4; Gao, P (Gao, Peng)1,2; Zhang, LY (Zhang, Linyou)1,2; Zhao, P (Zhao, Ping)5; Hu, SB (Hu, Shengbiao)1,2; Jiang, GZ | |
| Source Publication | JOURNAL OF ASIAN EARTH SCIENCES
 |
| 2016 | |
| Volume | 118Issue:0Pages:1-10 |
| DOI | 10.1016/j.jseaes.2016.01.009 |
| Abstract | Very few of heat flow data have come from the crystalline basement in the North China Craton but rather from boreholes in the sedimentary cover of oil-gas basins. Explorations for hot dry rock (HDR) geothermal resources and porphyry gold deposits in eastern China offer now valuable opportunities to study the terrestrial heat flow in the crystalline basement. In this study, we obtained continuous temperature logs from two boreholes (the LZ borehole with a depth of 3471 m and the DR borehole with a depth of 2179 m) located in the south-east margin of the North China Craton. The boreholes have experienced long shut-in times (442 days and 261 days for the LZ borehole and DR borehole, respectively); thus, it can be expected that the temperature conditions have re-equilibrated after drilling and drill-mud circulation. Rock thermal conductivity and radiogenic heat production were measured for 68 crystalline rock samples from these two boreholes. The measured heat-flow density was determined to be 71.8 +/- 2.3 mW m(-2) (for the 12 borehole) and 91.5 +/- 1.2 mW m(-2) (for the DR borehole). The heat flow for the 12 borehole is close to the value of 75 mW m-2 determined in the Chinese Continental Scientific Drilling main hole (CCSD MH), both being in the Sulu-Dabie orogenic belt and thus able to verify each other. The value for the DR borehole is higher than the above two values, which supports former high heat-flow values determined in the Bohai Bay Basin. (C) 2016 Elsevier Ltd. All rights reserved. |
| Subject Area | 地质学 |
| WOS ID | WOS:000370087000001 |
| Language | 英语 |
| Indexed By | SCI |
| Keyword | Tan-lu Fault Bohai Bay Basin Thermal-conductivity Lithospheric Thickness Tectonic Implications Jiaodong Peninsula Rocks Zone Destruction Petrogenesis |
| Cooperation Status | 国内 |
| Department | 碰撞与隆升 |
| Subtype | Article |
| Citation statistics | |
| Document Type | 期刊论文 |
| Identifier | http://ir.itpcas.ac.cn/handle/131C11/7735 |
| Collection | 图书馆 |
| Corresponding Author | Jiang, GZ |
| Affiliation | 1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 2.Univ Chinese Acad Sci, Beijing 100101, Peoples R China 3.Xi An Jiao Tong Univ, Inst Global Environm Change, Xian 710049, Peoples R China 4.Yangtze Univ, Yangtze 434023, Hubei, Peoples R China 5.Chinese Acad Sci, Inst Tibetan Plateau Res, Beijing 100029, Peoples R China |
| Recommended Citation GB/T 7714 | Jiang, GZ ,Tang, XY ,Rao, S ,et al. High-quality heat flow determination from the crystalline basement of the south-east margin of North China Craton[J]. JOURNAL OF ASIAN EARTH SCIENCES,2016,118(0):1-10. |
| APA | Jiang, GZ .,Tang, XY .,Rao, S .,Gao, P .,Zhang, LY .,...&Jiang, GZ.(2016).High-quality heat flow determination from the crystalline basement of the south-east margin of North China Craton.JOURNAL OF ASIAN EARTH SCIENCES,118(0),1-10. |
| MLA | Jiang, GZ ,et al."High-quality heat flow determination from the crystalline basement of the south-east margin of North China Craton".JOURNAL OF ASIAN EARTH SCIENCES 118.0(2016):1-10. |
| Files in This Item: | ||||||
| File Name/Size | DocType | Version | Access | License | ||
| V.118 1-10 2016.pdf（2265KB） | 期刊论文 | 作者接受稿 | 开放获取 | CC BY-NC-SA | View Application Full Text | |
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