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Mesozoic-Cenozoic exhumation history of the Qimen Tagh Range, northeastern margins of the Tibetan Plateau: Evidence from apatite fission track analysis

文献类型：期刊论文

作者Wang, Yadong1; Zheng, Jianjing1; Zheng, Youwei1,2
刊名GONDWANA RESEARCH
出版日期2018-06-01
卷号58页码:16-26
关键词Apatite fission track Qimen Tagh Range Northeastern Tibetan Plateau Mesozoic Rapid uplift
ISSN号1342-937X
DOI10.1016/j.gr.2018.01.014
文献子类Article
英文摘要The Tibetan Plateau (TP) is the highest plateau in the world. It is composed of a series of E-W stretched blocks/terranes originating from the Gondwana super-continent. As such, the TP has become one of the world's critical foci of Cenozoic geological studies. The Paleozoic and Mesozoic tectonic histories of the Proto-Tibetan region played an important role in the Cenozoic evolution of the TP. Understanding the pre-Cenozoic building of the Qimen Tagh Range located along the northeastern margins of the TP will help to constrain the development of the northern boundaries of the Proto-Tibetan region. Here, we present apatite fission track data for six granite samples along two vertical transects in the North Qimen Tagh Range. These thermochronometric data indicate that the North Qimen Tagh Range experienced a four-stage cooling history, i.e., during the periods similar to 262-240 Ma, similar to 165-160 Ma, 105-80 Ma and similar to 14/10-0 Ma. They reveal that the initial uplift of the northern margins of the TP (i.e., the Qimen Tagh and East Kunlun mountain ranges) during the Late Permian-Middle Triassic separated the paleo-Qaidam Basin from the paleo-Hoh Xil Basin. We therefore suggest that these North Qimen Tagh Range cooling events most probably correspond with the diachronous collisions of the Qiangtang and Lhasa terranes during the Mesozoic, as well as the Endo-Eurasian continental collision which occurred during the Cenozoic. (C) 2018 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
WOS关键词ZIRCON U-PB ; EASTERN KUNLUN MOUNTAINS ; INDIA-ASIA COLLISION ; PALEO-TETHYS OCEAN ; FORE-ARC BASIN ; QAIDAM BASIN ; TECTONIC EVOLUTION ; SOUTHERN TIBET ; QILIAN SHAN ; NORTHERN TIBET
WOS研究方向Geology
语种英语
WOS记录号WOS:000440265500002
出版者ELSEVIER SCIENCE BV
资助机构National Natural Science Foundation of China(41601007 ; National Natural Science Foundation of China(41601007 ; 41772200) ; 41772200) ; National Natural Science Foundation of China(41601007 ; National Natural Science Foundation of China(41601007 ; 41772200) ; 41772200) ; National Natural Science Foundation of China(41601007 ; National Natural Science Foundation of China(41601007 ; 41772200) ; 41772200) ; National Natural Science Foundation of China(41601007 ; National Natural Science Foundation of China(41601007 ; 41772200) ; 41772200)
源URL[http://ir.iggcas.ac.cn/handle/132A11/88135]  
专题地质与地球物理研究所_兰州油气中心
通讯作者Wang, Yadong
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources Res, Gansu Prov Key Lab Petr Resources, Lanzhou 730000, Gansu, Peoples R China
2.Inner Mongolia Univ Sci & Technol, Baotou 014070, Peoples R China
推荐引用方式
GB/T 7714		 Wang, Yadong,Zheng, Jianjing,Zheng, Youwei. Mesozoic-Cenozoic exhumation history of the Qimen Tagh Range, northeastern margins of the Tibetan Plateau: Evidence from apatite fission track analysis[J]. GONDWANA RESEARCH,2018,58:16-26.
APA Wang, Yadong,Zheng, Jianjing,&Zheng, Youwei.(2018).Mesozoic-Cenozoic exhumation history of the Qimen Tagh Range, northeastern margins of the Tibetan Plateau: Evidence from apatite fission track analysis.GONDWANA RESEARCH,58,16-26.
MLA Wang, Yadong,et al."Mesozoic-Cenozoic exhumation history of the Qimen Tagh Range, northeastern margins of the Tibetan Plateau: Evidence from apatite fission track analysis".GONDWANA RESEARCH 58(2018):16-26.

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来源：地质与地球物理研究所

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