Thermochronology quantifying exhumation history of the Wudang Complex in the South Qinling Orogenic Belt, central China

doi:10.1017/S0016756816001047

	Thermochronology quantifying exhumation history of the Wudang Complex in the South Qinling Orogenic Belt, central China
	Shen, Chuanbo 1,2; Hu, Di 1,3; Shao, Chun 1; Mei, Lianfu 1
刊名	GEOLOGICAL MAGAZINE
	2018-05-01
卷号	155 期号:4 页码:893-906
关键词	thermochronology fission track cooling/exhumation tectonic evolution Qinling Orogen
ISSN号	0016-7568
DOI	10.1017/S0016756816001047
文献子类	Article
英文摘要	The Wudang Complex located in the central part of South Qinling, has been inferred to be a segment of the Yangtze Craton involved in the orogen. In this study, the cooling/exhumation history of the Wudang Complex is revealed through combined published geochronology data and new apatite fission-track results. Three rapid exhumation episodes related to relevant geodynamic events have been identified. Previous Ar-40-Ar-39 and (U-Th)/He data indicate that the most significant exhumation, induced by the collision between the North and South China Blocks, occurred from c. 237 to 220 Ma after long-term subsidence and sedimentation of the passive continental margin. The second exhumation event, related to the long-distance effect of the Pacific subduction, occurred during the period from c. 126 to 90 Ma. Following the late Cretaceous - Eocene peneplanation stage, the final late Cenozoic exhumation since c. 15 Ma may be attributed to the combined effect of the eastward growth of the Tibetan Plateau uplift and the Asian monsoon.
WOS关键词	FISSION-TRACK THERMOCHRONOLOGY ; ULTRAHIGH-PRESSURE METAMORPHISM ; INTERTROPICAL CONVERGENCE ZONE ; PB ZIRCON GEOCHRONOLOGY ; LOWER CRUSTAL FLOW ; KYRGYZ TIEN-SHAN ; TIBETAN PLATEAU ; U-PB ; TECTONIC EVOLUTION ; EASTERN MARGIN
WOS研究方向	Geology
语种	英语
出版者	CAMBRIDGE UNIV PRESS
WOS记录号	WOS:000426671600007
资助机构	National Natural Science Foundation of China(41372140 ; National Natural Science Foundation of China(41372140 ; Fundamental Research Fund for the Central Universities, China University of Geosciences (Wuhan)(201536) ; Fundamental Research Fund for the Central Universities, China University of Geosciences (Wuhan)(201536) ; Natural Science Foundation of Hubei Province(2016CFA055) ; Natural Science Foundation of Hubei Province(2016CFA055) ; Wuhan Science and Technology Project(2016070204010145) ; Wuhan Science and Technology Project(2016070204010145) ; China Scholarship Council ; China Scholarship Council ; 40902038) ; 40902038) ; National Natural Science Foundation of China(41372140 ; National Natural Science Foundation of China(41372140 ; Fundamental Research Fund for the Central Universities, China University of Geosciences (Wuhan)(201536) ; Fundamental Research Fund for the Central Universities, China University of Geosciences (Wuhan)(201536) ; Natural Science Foundation of Hubei Province(2016CFA055) ; Natural Science Foundation of Hubei Province(2016CFA055) ; Wuhan Science and Technology Project(2016070204010145) ; Wuhan Science and Technology Project(2016070204010145) ; China Scholarship Council ; China Scholarship Council ; 40902038) ; 40902038) ; National Natural Science Foundation of China(41372140 ; National Natural Science Foundation of China(41372140 ; Fundamental Research Fund for the Central Universities, China University of Geosciences (Wuhan)(201536) ; Fundamental Research Fund for the Central Universities, China University of Geosciences (Wuhan)(201536) ; Natural Science Foundation of Hubei Province(2016CFA055) ; Natural Science Foundation of Hubei Province(2016CFA055) ; Wuhan Science and Technology Project(2016070204010145) ; Wuhan Science and Technology Project(2016070204010145) ; China Scholarship Council ; China Scholarship Council ; 40902038) ; 40902038) ; National Natural Science Foundation of China(41372140 ; National Natural Science Foundation of China(41372140 ; Fundamental Research Fund for the Central Universities, China University of Geosciences (Wuhan)(201536) ; Fundamental Research Fund for the Central Universities, China University of Geosciences (Wuhan)(201536) ; Natural Science Foundation of Hubei Province(2016CFA055) ; Natural Science Foundation of Hubei Province(2016CFA055) ; Wuhan Science and Technology Project(2016070204010145) ; Wuhan Science and Technology Project(2016070204010145) ; China Scholarship Council ; China Scholarship Council ; 40902038) ; 40902038)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/83108]
专题	中国科学院地质与地球物理研究所
通讯作者	Shen, Chuanbo
作者单位	1.China Univ Geosci, Key Lab Tecton & Petr Resources, Minist Educ, Wuhan 430074, Hubei, Peoples R China 2.China Univ Geosci, Fac Earth Resources, Wuhan 430074, Hubei, Peoples R China 3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
推荐引用方式 GB/T 7714	Shen, Chuanbo,Hu, Di,Shao, Chun,et al. Thermochronology quantifying exhumation history of the Wudang Complex in the South Qinling Orogenic Belt, central China[J]. GEOLOGICAL MAGAZINE,2018,155(4):893-906.
APA	Shen, Chuanbo,Hu, Di,Shao, Chun,&Mei, Lianfu.(2018).Thermochronology quantifying exhumation history of the Wudang Complex in the South Qinling Orogenic Belt, central China.GEOLOGICAL MAGAZINE,155(4),893-906.
MLA	Shen, Chuanbo,et al."Thermochronology quantifying exhumation history of the Wudang Complex in the South Qinling Orogenic Belt, central China".GEOLOGICAL MAGAZINE 155.4(2018):893-906.