Thermal evolution of cratons in China
文献类型：期刊论文
| 作者 | He, Lijuan1; Zhang, Linyou |
| 刊名 | JOURNAL OF ASIAN EARTH SCIENCES
 |
| 出版日期 | 2018-09-15 |
| 卷号 | 164页码:237-247 |
| 关键词 | North China Craton Tarim Craton Yangtze Craton Heat flow Thermal history Craton destruction |
| ISSN号 | 1367-9120 |
| DOI | 10.1016/j.jseaes.2018.06.028 |
| 英文摘要 | Craton's thermal state is one of the main gateways to understand the craton dynamics. Three cratons in China, the Tarim, North China, and Yangtze cratons, are in different thermal states and differ in their stabilities. Low heat flow usually corresponds to stable craton but not vice versa. The Tarim Craton is cold (similar to 44 mW/m(2)) and still keeps its stability now. The western North China Craton and the upper Yangtze Craton are not too cold (50-60 mW/m(2)) but also remain stable. The eastern North China Craton and the Middle-Lower Yangtze Craton are relatively hot with heat flow of 60-70 mW/m(2), both have been heated and destroyed in the Mesozoic. All these cratons have experienced complex tectonothermal events since their formation. Some tectonothermal events only thin and heat craton but others can destroy craton. Several sedimentary basins are developed in these cratons, which recorded individual thermal histories. These thermal records could help to understand the thermal evolution of these cratons and provide constraints on craton dynamics including stability or destruction. The thermal results indicate parts of craton in western China (Tarim and Sichuan) have secular cooling histories, which were locally disturbed by mantle plume activities in the Permian. The Middle-Lower Yangtze Craton has undergone similar thermal evolution as the eastern North China Craton. All parts of cratons in eastern China might all have been destroyed due to subduction and dehydration of the Pacific Plate during the Mesozoic. |
| WOS关键词 | EASTERN NORTH CHINA ; BOHAI BAY BASIN ; LITHOSPHERIC MANTLE BENEATH ; ARCHEAN CONTINENTAL-CRUST ; SURFACE-WAVE TOMOGRAPHY ; SINO-KOREAN CRATON ; HEAT-FLOW ; SOUTH CHINA ; ORDOS BASIN ; TARIM BASIN |
| 资助项目 | National Natural Science Foundation of China[41574075] ; National Key Research and Development Program of China[2016YFC0601005] |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000442706000015 |
| 出版者 | PERGAMON-ELSEVIER SCIENCE LTD |
| 资助机构 | National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China ; National Key Research and Development Program of China |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/75882]  |
| 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 | He, Lijuan |
| 作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 2.Chinese Acad Sci, Inst Earth Sci, Beijing 100029, Peoples R China 3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China |
| 推荐引用方式 GB/T 7714 | He, Lijuan,Zhang, Linyou. Thermal evolution of cratons in China[J]. JOURNAL OF ASIAN EARTH SCIENCES,2018,164:237-247. |
| APA | He, Lijuan,&Zhang, Linyou.(2018).Thermal evolution of cratons in China.JOURNAL OF ASIAN EARTH SCIENCES,164,237-247. |
| MLA | He, Lijuan,et al."Thermal evolution of cratons in China".JOURNAL OF ASIAN EARTH SCIENCES 164(2018):237-247. |
入库方式： OAI收割
来源：地质与地球物理研究所
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