Episodic Meso-Cenozoic denudation of Chinese Tianshan: evidence from detrital apatite fission track and zircon U-Pb data, southern Junggar Basin margin, NW China

doi:10.1016/j.jseaes.2018.07.042

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

	Episodic Meso-Cenozoic denudation of Chinese Tianshan: evidence from detrital apatite fission track and zircon U-Pb data, southern Junggar Basin margin, NW China
	Xiang, Dunfeng 1,2; Zhang, Zhiyong 1,3; Xiao, Wenjiao 1,4; Zhu, Wenbin 5; Zheng, Dewen 6; Li, Guangwei 3; Zheng, Bihai 5; Song, Dongfang 1; Han, Chunming 1; Pang, Jianzhang 6
刊名	JOURNAL OF ASIAN EARTH SCIENCES
	2019-05-15
卷号	175 页码:199-212
关键词	Central Asian Orogenic Belt Tianshan Junggar Basin Detrital zircon U-Pb dating Apatite fission track thermochronology
ISSN号	1367-9120
DOI	10.1016/j.jseaes.2018.07.042
英文摘要	It is generally accepted that the Tianshan was reactivated repeatedly throughout Meso-Cenozoic time. However, the extent of these episodes has not been fully understood. Using a previous magnetostratigraphic baseline, this study reports a detrital zircon U-Pb and apatite fission track dating study along the similar to 4 km thick Cenozoic Jingou River section at the southern margin of the Junggar Basin. Our results provide direct insight into the denudation history of the bordering Tianshan Mountains and suggest that they experienced two phases of rapid cooling in the Jurassic and Cretaceous. These cooling phases are attributed to tectonic events at distant plate margins such as the Late Triassic-Cretaceous accretion of peri-Gondwartan blocks (e.g. Qiangtang and Lhasa). The detrital zircon U-Pb ages range widely from similar to 58 to 3055 Ma with a majority falling between similar to 58 and 600 Ma. They can be statistically separated into two primary age peaks at 300-290 Ma and 450-410 Ma, as well as two secondary peaks at 170 Ma and 850 Ma. Detrital zircon U-Pb dating results suggest that the Central Tianshan may have still shed detritus into the Junggar Basin during the Early Palaeogene. In the Late Oligocene-Early Miocene, the modern North Tianshan started to form a topographic barrier that blocked all northward rivers flowing from the Central Tianshan to the Junggar Basin. Progressive northward indentation of India into Eurasia, caused a final intense phase of cooling and denudation of the Tianshan between similar to 11 and 3 Ma, leading to deposition of the Xiyu Formation, a widely distributed thick conglomerate.
资助项目	National Key R&D Program of China[2017YFC0601206] ; 973 Program[2014CB440801] ; NSFC[41390441] ; NSFC[41230207] ; NSFC[41302167] ; NSFC[41472208] ; State Key Laboratory of Earthquake Dynamics[LED2013B03] ; China Postdoctoral Council[20100480452] ; China Postdoctoral Council[2012T50135] ; China Postdoctoral Council (International Postdoctoral Exchange Fellowship Program)
WOS关键词	PALEOZOIC TECTONIC EVOLUTION ; ASIAN OROGENIC BELT ; NORTHERN TIEN-SHAN ; WESTERN TIANSHAN ; NORTHWEST CHINA ; TARIM BASIN ; INTRACONTINENTAL DEFORMATION ; SEDIMENTARY RECORD ; TIBETAN PLATEAU ; TURPAN BASINS
WOS研究方向	Geology
语种	英语
出版者	PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号	WOS:000464298500016
资助机构	National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; 973 Program ; 973 Program ; 973 Program ; 973 Program ; NSFC ; NSFC ; NSFC ; NSFC ; State Key Laboratory of Earthquake Dynamics ; State Key Laboratory of Earthquake Dynamics ; State Key Laboratory of Earthquake Dynamics ; State Key Laboratory of Earthquake Dynamics ; China Postdoctoral Council ; China Postdoctoral Council ; China Postdoctoral Council ; China Postdoctoral Council ; China Postdoctoral Council (International Postdoctoral Exchange Fellowship Program) ; China Postdoctoral Council (International Postdoctoral Exchange Fellowship Program) ; China Postdoctoral Council (International Postdoctoral Exchange Fellowship Program) ; China Postdoctoral Council (International Postdoctoral Exchange Fellowship Program) ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; 973 Program ; 973 Program ; 973 Program ; 973 Program ; NSFC ; NSFC ; NSFC ; NSFC ; State Key Laboratory of Earthquake Dynamics ; State Key Laboratory of Earthquake Dynamics ; State Key Laboratory of Earthquake Dynamics ; State Key Laboratory of Earthquake Dynamics ; China Postdoctoral Council ; China Postdoctoral Council ; China Postdoctoral Council ; China Postdoctoral Council ; China Postdoctoral Council (International Postdoctoral Exchange Fellowship Program) ; China Postdoctoral Council (International Postdoctoral Exchange Fellowship Program) ; China Postdoctoral Council (International Postdoctoral Exchange Fellowship Program) ; China Postdoctoral Council (International Postdoctoral Exchange Fellowship Program) ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; 973 Program ; 973 Program ; 973 Program ; 973 Program ; NSFC ; NSFC ; NSFC ; NSFC ; State Key Laboratory of Earthquake Dynamics ; State Key Laboratory of Earthquake Dynamics ; State Key Laboratory of Earthquake Dynamics ; State Key Laboratory of Earthquake Dynamics ; China Postdoctoral Council ; China Postdoctoral Council ; China Postdoctoral Council ; China Postdoctoral Council ; China Postdoctoral Council (International Postdoctoral Exchange Fellowship Program) ; China Postdoctoral Council (International Postdoctoral Exchange Fellowship Program) ; China Postdoctoral Council (International Postdoctoral Exchange Fellowship Program) ; China Postdoctoral Council (International Postdoctoral Exchange Fellowship Program) ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; 973 Program ; 973 Program ; 973 Program ; 973 Program ; NSFC ; NSFC ; NSFC ; NSFC ; State Key Laboratory of Earthquake Dynamics ; State Key Laboratory of Earthquake Dynamics ; State Key Laboratory of Earthquake Dynamics ; State Key Laboratory of Earthquake Dynamics ; China Postdoctoral Council ; China Postdoctoral Council ; China Postdoctoral Council ; China Postdoctoral Council ; China Postdoctoral Council (International Postdoctoral Exchange Fellowship Program) ; China Postdoctoral Council (International Postdoctoral Exchange Fellowship Program) ; China Postdoctoral Council (International Postdoctoral Exchange Fellowship Program) ; China Postdoctoral Council (International Postdoctoral Exchange Fellowship Program)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/91288]
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	Zhang, Zhiyong
作者单位	1.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.Univ Melbourne, Sch Earth Sci, Melbourne, Vic 3010, Australia 4.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China 5.Nanjing Univ, Dept Earth Sci, State Key Lab Mineral Deposits Res, Nanjing 210093, Jiangsu, Peoples R China 6.China Earthquake Adm, Inst Geol, State Key Lab Earthquake Dynam, Beijing 100029, Peoples R China
推荐引用方式 GB/T 7714	Xiang, Dunfeng,Zhang, Zhiyong,Xiao, Wenjiao,et al. Episodic Meso-Cenozoic denudation of Chinese Tianshan: evidence from detrital apatite fission track and zircon U-Pb data, southern Junggar Basin margin, NW China[J]. JOURNAL OF ASIAN EARTH SCIENCES,2019,175:199-212.
APA	Xiang, Dunfeng.,Zhang, Zhiyong.,Xiao, Wenjiao.,Zhu, Wenbin.,Zheng, Dewen.,...&Pang, Jianzhang.(2019).Episodic Meso-Cenozoic denudation of Chinese Tianshan: evidence from detrital apatite fission track and zircon U-Pb data, southern Junggar Basin margin, NW China.JOURNAL OF ASIAN EARTH SCIENCES,175,199-212.
MLA	Xiang, Dunfeng,et al."Episodic Meso-Cenozoic denudation of Chinese Tianshan: evidence from detrital apatite fission track and zircon U-Pb data, southern Junggar Basin margin, NW China".JOURNAL OF ASIAN EARTH SCIENCES 175(2019):199-212.