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DOI	10.1016/j.tecto.2021.228769
	Tectonothermal events in the central North China Craton since the Mesozoic and their tectonic implications: Constraints from low-temperature thermochronology
	Zhang J.; Wang Y.; Zhang B.; Qu J.; Li J.; Long Y.; Niu P.; Zhao H.; Hui J.
发表日期	2021
ISSN	00401951
卷号	804
英文摘要	The North China Craton (NCC) experienced important tectonic events during the Meso-Cenozoic as implied by many geological studies. Combined with existing low-temperature thermochronological data, new apatite fission track (AFT) and zircon (U–Th)/He data from the Lüliangshan and Taihangshan mountains in this study reveal that the central NCC experienced tectonothermal events during the Meso-Cenozoic, i.e., ca. 150 Ma, 110–80 Ma, 50–40 Ma and 30–20 Ma. The Late Jurassic event caused the formation of the Lüliangshan basement-involved anticline. The main folding and thrusting in the central NCC developed in the Mesozoic instead of the Cenozoic and resulted from the low-angle subduction of the Paleo-Pacific ocean plate beneath the Eurasian Plate during the Late Jurassic; and the Late Cretaceous tectonic event stopped the Early Cretaceous extension across the eastern Asia, thrusting and sinistral strike-slip faulting occurred across the central NCC, which was possibly caused by a collision along the southeastern boundary of eastern Asia. The early Cenozoic event in central NCC was coeval with an event occurring throughout eastern Asia and may have been a regional response to changes in the movement direction and velocity of the Pacific Plate, and this event may have resulted in the formation of rift basins in the eastern NCC. The whole central NCC experienced uplift during this period in isostatic readjustment to this extension. © 2021 Elsevier B.V.
关键词	Apatite fission track Intraplate deformation Lüliangshan North China Craton Taihangshan Zircon (U–Th)/He
英文关键词	Fission reactions; Phosphate minerals; Silicate minerals; Strike-slip faults; Zircon; Apatite fission tracks; Low temperatures; North China Craton; Regional response; Strike slip faulting; Tectonic implications; Tectono-thermal event; Thermochronology; Temperature; crustal deformation; fission track dating; low temperature; Mesozoic; plate tectonics; thermochronology; uranium series dating; zircon; China; Luliang Mountains; North China Block; Shanxi; Taihang Mountains
语种	英语
来源期刊	Tectonophysics
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/208111
作者单位	Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing, 100037, China; Key Laboratory for Resource Exploration Research of Hebei Province, Hebei University of Engineering, Handan, 056038, China; Shandong Key Laboratory of Depositional Mineralization & Sedimentary Mineral, Shandong University of Science and Technology, Qingdao, 266590, China; Beijing Research Institute of Uranium Geology, Beijing, 100029, China; University of Chinese Academy of Sciences, Beijing, 100049, China
推荐引用方式 GB/T 7714	Zhang J.,Wang Y.,Zhang B.,et al. Tectonothermal events in the central North China Craton since the Mesozoic and their tectonic implications: Constraints from low-temperature thermochronology[J],2021,804.
APA	Zhang J..,Wang Y..,Zhang B..,Qu J..,Li J..,...&Hui J..(2021).Tectonothermal events in the central North China Craton since the Mesozoic and their tectonic implications: Constraints from low-temperature thermochronology.Tectonophysics,804.
MLA	Zhang J.,et al."Tectonothermal events in the central North China Craton since the Mesozoic and their tectonic implications: Constraints from low-temperature thermochronology".Tectonophysics 804(2021).