Processes of initial collision and suturing between India and Asia
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 th...
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| Published in | Science China. Earth sciences Vol. 60; no. 4; pp. 635 - 651 |
|---|---|
| Main Authors | , , , , , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Beijing
Science China Press
01.04.2017
Springer Nature B.V |
| Subjects | |
| Online Access | Get full text |
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| Abstract | 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 and50 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. |
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| AbstractList | 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. 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 and50 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. |
| Author | DING Lin Satybaev MAKSATBEK CAI FuLong WANG HouQi SONG PeiPing JI WeiQiang XU Qiang ZHANG LiYun Qasim MUHAMMAD Baral UPENDRA |
| AuthorAffiliation | Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, and Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing 100101, China University of the Chinese Academy of Sciences, Beijing 100049, China Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China |
| Author_xml | – sequence: 1 givenname: Lin surname: Ding fullname: Ding, Lin email: dinglin@itpcas.ac.cn organization: Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, and Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, University of the Chinese Academy of Sciences – sequence: 2 givenname: Satybaev surname: Maksatbek fullname: Maksatbek, Satybaev organization: Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, and Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, University of the Chinese Academy of Sciences – sequence: 3 givenname: FuLong surname: Cai fullname: Cai, FuLong organization: Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, and Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences – sequence: 4 givenname: HouQi surname: Wang fullname: Wang, HouQi organization: Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, and Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences – sequence: 5 givenname: PeiPing surname: Song fullname: Song, PeiPing organization: Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, and Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences – sequence: 6 givenname: WeiQiang surname: Ji fullname: Ji, WeiQiang organization: Institute of Geology and Geophysics, Chinese Academy of Sciences – sequence: 7 givenname: Qiang surname: Xu fullname: Xu, Qiang organization: Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, and Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences – sequence: 8 givenname: LiYun surname: Zhang fullname: Zhang, LiYun organization: Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, and Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences – sequence: 9 givenname: Qasim surname: Muhammad fullname: Muhammad, Qasim organization: Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, and Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, University of the Chinese Academy of Sciences – sequence: 10 givenname: Baral surname: Upendra fullname: Upendra, Baral organization: Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, and Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences |
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| ContentType | Journal Article |
| Copyright | Science China Press and Springer-Verlag Berlin Heidelberg 2017 Science China Earth Sciences is a copyright of Springer, 2017. |
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| DocumentTitleAlternate | Processes of initial collision and suturing between India and Asia |
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| ID | FETCH-LOGICAL-c442t-20f114590b76cbc0a6ed89a2a02906e1dcc85d821f5cd3eb12f45e1c763c1a8b3 |
| IEDL.DBID | U2A |
| ISSN | 1674-7313 |
| IngestDate | Fri Jul 11 12:27:52 EDT 2025 Sun Jul 13 04:53:17 EDT 2025 Tue Aug 05 12:03:54 EDT 2025 Thu Apr 24 23:07:58 EDT 2025 Fri Feb 21 02:32:51 EST 2025 Wed Feb 14 10:03:16 EST 2024 |
| IsPeerReviewed | true |
| IsScholarly | true |
| Issue | 4 |
| Keywords | Tibetan Plateau Initial collision Suturing processes Indian Plate Asian Plate |
| Language | English |
| LinkModel | DirectLink |
| MergedId | FETCHMERGED-LOGICAL-c442t-20f114590b76cbc0a6ed89a2a02906e1dcc85d821f5cd3eb12f45e1c763c1a8b3 |
| Notes | 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 and50 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. Timing of initial collision between the Indian and Asian continents Collision criteria Transform fault Subduction zone Magmatism Deformation 11-5843/P ObjectType-Article-1 SourceType-Scholarly Journals-1 content type line 14 ObjectType-Literature Review-2 ObjectType-Feature-2 content type line 23 |
| PQID | 1883505132 |
| PQPubID | 54336 |
| PageCount | 17 |
| ParticipantIDs | proquest_miscellaneous_1891877019 proquest_journals_1883505132 crossref_citationtrail_10_1007_s11430_016_5244_x crossref_primary_10_1007_s11430_016_5244_x springer_journals_10_1007_s11430_016_5244_x chongqing_primary_671710108 |
| PublicationCentury | 2000 |
| PublicationDate | 2017-04-01 |
| PublicationDateYYYYMMDD | 2017-04-01 |
| PublicationDate_xml | – month: 04 year: 2017 text: 2017-04-01 day: 01 |
| PublicationDecade | 2010 |
| PublicationPlace | Beijing |
| PublicationPlace_xml | – name: Beijing – name: Dordrecht |
| PublicationTitle | Science China. Earth sciences |
| PublicationTitleAbbrev | Sci. China Earth Sci |
| PublicationTitleAlternate | SCIENCE CHINA Earth Sciences |
| PublicationYear | 2017 |
| Publisher | Science China Press Springer Nature B.V |
| Publisher_xml | – name: Science China Press – name: Springer Nature B.V |
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| SubjectTerms | Climate change Continental dynamics Earth and Environmental Science Earth Sciences Geological time Geophysics Metamorphism Paleomagnetism Plate tectonics Quantitative research Review 亚洲大陆 印度 周缘前陆盆地 喜马拉雅造山带 地质事件 大陆碰撞 岩浆作用过程 雅鲁藏布江缝合带 |
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| Title | Processes of initial collision and suturing between India and Asia |
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