Thermal evolution of cratons in China

doi:10.1016/j.jseaes.2018.06.028

CORC > 地质与地球物理研究所 > 中国科学院地质与地球物理研究所 > 岩石圈演化国家重点实验室

	Thermal evolution of cratons in China
	He, Lijuan 1; Zhang, Linyou
刊名	JOURNAL OF ASIAN EARTH SCIENCES
	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.
资助项目	National Natural Science Foundation of China[41574075] ; National Key Research and Development Program of China[2016YFC0601005]
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
WOS研究方向	Geology
语种	英语
出版者	PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号	WOS:000442706000015
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
内容类型	期刊论文
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.