Processes of initial collision and suturing between India and Asia
文献类型:期刊论文
作者 | Ding Lin1,2,3; Maksatbek, Satybaev1,2,3; Cai FuLong1,2; Wang HouQi1,2; Song PeiPing1,2; Ji WeiQiang4; Xu Qiang1,2; Zhang LiYun1,2; Muhammad, Qasim1,2,3; Upendra, Baral1,2 |
刊名 | SCIENCE CHINA-EARTH SCIENCES
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出版日期 | 2017-04-01 |
卷号 | 60期号:4页码:635-651 |
关键词 | Tibetan Plateau Indian Plate Asian Plate Initial collision Suturing processes |
ISSN号 | 1674-7313 |
DOI | 10.1007/s11430-016-5244-x |
文献子类 | Review |
英文摘要 | The initial collision between Indian and Asian continents marked the starting point for transformation of land-sea thermal contrast, uplift of the Tibet-Himalaya orogen, and climate change in Asia. In this paper, we review the published literatures from the past 30 years in order to draw consensus on the processes of initial collision and suturing that took place between the Indian and Asian plates. Following a comparison of the different methods that have been used to constrain the initial timing of collision, we propose that the tectono-sedimentary response in the peripheral foreland basin provides the most sensitive index of this event, and that paleomagnetism presents independent evidence as an alternative, reliable, and quantitative research method. In contrast to previous studies that have suggested collision between India and Asia started in Pakistan between ca. 55 Ma and 50 Ma and progressively closed eastwards, more recent researches have indicated that this major event first occurred in the center of the Yarlung Tsangpo suture zone (YTSZ) between ca. 65 Ma and 63 Ma and then spreading both eastwards and westwards. While continental collision is a complicated process, including the processes of deformation, sedimentation, metamorphism, and magmatism, different researchers have tended to define the nature of this event based on their own understanding, an intuitive bias that has meant that its initial timing has remained controversial for decades. Here, we recommend the use of reconstructions of each geological event within the orogenic evolution sequence as this will allow interpretation of collision timing on the basis of multidisciplinary methods. |
WOS关键词 | SOUTHERN TIBET IMPLICATIONS ; EASTERN HIMALAYAN SYNTAXIS ; CRETACEOUS VOLCANIC-ROCKS ; FORELAND BASIN EVOLUTION ; TETHYAN HIMALAYA ; LHASA TERRANE ; U-PB ; EURASIA COLLISION ; PALEOMAGNETIC CONSTRAINTS ; TECTONIC IMPLICATIONS |
WOS研究方向 | Geology |
语种 | 英语 |
WOS记录号 | WOS:000400551300003 |
出版者 | SCIENCE PRESS |
资助机构 | Chinese Academy of Sciences(XDB03010401) ; National Key Research and Development Plan(2016YFC0600303) ; National Natural Science Foundation of China(41490615) ; Chinese Academy of Sciences(XDB03010401) ; National Key Research and Development Plan(2016YFC0600303) ; National Natural Science Foundation of China(41490615) ; Chinese Academy of Sciences(XDB03010401) ; National Key Research and Development Plan(2016YFC0600303) ; National Natural Science Foundation of China(41490615) ; Chinese Academy of Sciences(XDB03010401) ; National Key Research and Development Plan(2016YFC0600303) ; National Natural Science Foundation of China(41490615) |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/39139] ![]() |
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 | Ding Lin |
作者单位 | 1.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing 100101, Peoples R China 2.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China 3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 4.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China |
推荐引用方式 GB/T 7714 | Ding Lin,Maksatbek, Satybaev,Cai FuLong,et al. Processes of initial collision and suturing between India and Asia[J]. SCIENCE CHINA-EARTH SCIENCES,2017,60(4):635-651. |
APA | Ding Lin.,Maksatbek, Satybaev.,Cai FuLong.,Wang HouQi.,Song PeiPing.,...&Upendra, Baral.(2017).Processes of initial collision and suturing between India and Asia.SCIENCE CHINA-EARTH SCIENCES,60(4),635-651. |
MLA | Ding Lin,et al."Processes of initial collision and suturing between India and Asia".SCIENCE CHINA-EARTH SCIENCES 60.4(2017):635-651. |
入库方式: OAI收割
来源:地质与地球物理研究所
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