Triple-stage India-Asia collision involving arc-continent collision and subsequent two-stage continent-continent collision
文献类型：期刊论文
| 作者 | Yuan, Jie5; Deng, Chenglong4,5; Yang, Zhenyu6; Krijgsman, Wout1; Qin, Huafeng4,5; Shen, Zhongshan5; Hou, Yifei4,5; Zhang, Shuai4,5; Yu, Zhiqiang5; Zhao, Pan4,5 |
| 刊名 | GLOBAL AND PLANETARY CHANGE
 |
| 出版日期 | 2022-05-01 |
| 卷号 | 212页码:17 |
| 关键词 | Multistage India-Asia collision Continental breakup Tethyan Himalaya terrane Tibetan Himalaya terrane North India Sea Neo-Tethys Ocean |
| ISSN号 | 0921-8181 |
| DOI | 10.1016/j.gloplacha.2022.103821 |
| 英文摘要 | The enigmatic geodynamic processes involved in the India-Asia collision shape our understanding of uplift and deformation of the Tibetan Plateau and the subsequent changes in the land-sea distribution pattern, monsoon arid environments and biotic evolution in Central-Eastern Asia. However, the current geodynamic models dealing with the India-Asia collision history exhibit significant discrepancies in how, when and where exactly the collision of India with Asia occurred. Recently, we proposed a new hypothesis that favored the opening and closure of a North India Sea during the late Cretaceous to Paleogene. Here we present new additional paleomagnetic data from the red siliceous shales and cherts of the Sangdanlin Formation, which were deposited on the most distal continental margin of the Tethyan Himalaya terrane, i.e. the southern margin of the Neo-Tethys Ocean, during the middle Paleocene. The combination of our new and previously reported paleomagnetic data shows that the Tethyan Himalaya was at a paleolatitude of 14.1 degrees +/- 1.9 degrees N during the interval 62.5-59.2 Ma and refines the maximum size of the North India Sea to about 2200 +/- 500 km. Combining our geodynamic model with recently published paleomagnetic data from the Kohistan-Ladakh arc, we conclude that the India-Asia collision was a triple-stage process, which involved an arc-continent collision followed by a two-stage continent-continent collision. The arc-continent collision occurred at ca. 64 Ma between the Tibetan Himalaya (Tethyan Himalaya plus Greater Himalaya) and the Trans-Tethyan subduction zone at a paleolatitude of similar to 8N. The initial continent-continent collision took place at ca. 61 Ma between the Tibetan Himalaya (plus the accreted Trans-Tethyan subduction zone) and Lhasa terranes at a paleolatitude of similar to 14 degrees N. The final continent-continent collision occurred during 53-47 Ma between India and the Tibetan Himalaya, diachronously suturing the North India Sea from west to east. The triple-stage collision scenario is in agreement with the history of India Asia convergence rates, and is reflected by the presence of three slab remnants below Tibet and India as documented by seismic tomographic imaging. Our updated collision scenario reconciles multidisciplinary evidence for the India-Asia collision and provides better constraints on the resulting paleoclimatic and paleoenvironmental changes in Central-Eastern Asia. |
| WOS关键词 | FOLD-THRUST BELT ; HF ISOTOPIC CONSTRAINTS ; FORELAND BASIN DEPOSITS ; YARLUNG-ZANGBO SUTURE ; SOUTHERN TIBET ; TETHYAN HIMALAYA ; TECTONIC EVOLUTION ; U-PB ; DETRITAL GEOCHRONOLOGY ; GEOLOGICAL EVOLUTION |
| 资助项目 | National Natural Science Foundation of China[41888101] ; National Natural Science Foundation of China[91855216] ; National Natural Science Foundation of China[42104067] ; National Natural Science Foundation of China[92155203] ; National Natural Science Foundation of China[41621004] ; International Partnership Program of Chinese Academy of Sciences[GJHZ1776] ; China Postdoctoral Science Foundation[2021M693152] |
| WOS研究方向 | Physical Geography ; Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000794133200006 |
| 出版者 | ELSEVIER |
| 资助机构 | National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; International Partnership Program of Chinese Academy of Sciences ; International Partnership Program of Chinese Academy of Sciences ; International Partnership Program of Chinese Academy of Sciences ; International Partnership Program of Chinese Academy of Sciences ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; International Partnership Program of Chinese Academy of Sciences ; International Partnership Program of Chinese Academy of Sciences ; International Partnership Program of Chinese Academy of Sciences ; International Partnership Program of Chinese Academy of Sciences ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; International Partnership Program of Chinese Academy of Sciences ; International Partnership Program of Chinese Academy of Sciences ; International Partnership Program of Chinese Academy of Sciences ; International Partnership Program of Chinese Academy of Sciences ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; International Partnership Program of Chinese Academy of Sciences ; International Partnership Program of Chinese Academy of Sciences ; International Partnership Program of Chinese Academy of Sciences ; International Partnership Program of Chinese Academy of Sciences ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/105982]  |
| 专题 | 地质与地球物理研究所_岩石圈演化国家重点实验室 地质与地球物理研究所_中国科学院新生代地质与环境重点实验室 |
| 通讯作者 | Deng, Chenglong |
| 作者单位 | 1.Univ Utrecht, Dept Earth Sci, NL-3584 HD Utrecht, Netherlands 2.Tibet Univ, Coll Sci, Lhasa 850000, Peoples R China 3.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China 4.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China 5.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 6.Capital Normal Univ, Coll Resources, Environm & Tourism, Beijing 100048, Peoples R China |
| 推荐引用方式 GB/T 7714 | Yuan, Jie,Deng, Chenglong,Yang, Zhenyu,et al. Triple-stage India-Asia collision involving arc-continent collision and subsequent two-stage continent-continent collision[J]. GLOBAL AND PLANETARY CHANGE,2022,212:17. |
| APA | Yuan, Jie.,Deng, Chenglong.,Yang, Zhenyu.,Krijgsman, Wout.,Qin, Huafeng.,...&Thubtantsering, Zhengtang.(2022).Triple-stage India-Asia collision involving arc-continent collision and subsequent two-stage continent-continent collision.GLOBAL AND PLANETARY CHANGE,212,17. |
| MLA | Yuan, Jie,et al."Triple-stage India-Asia collision involving arc-continent collision and subsequent two-stage continent-continent collision".GLOBAL AND PLANETARY CHANGE 212(2022):17. |
入库方式： OAI收割
来源：地质与地球物理研究所
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