Diachronous uplift in intra-continental orogeny: 2D thermo-mechanical modeling of the India-Asia collision
文献类型：期刊论文
| 作者 | Bian, Shuang1,3; Gong, Junfeng1,3; Chen, Lin4; Zuza, Andrew, V2; Chen, Hanlin1,3; Lin, Xiubin1,3; Cheng, Xiaogan1,3; Yang, Rong1,3 |
| 刊名 | TECTONOPHYSICS
 |
| 出版日期 | 2020-01-20 |
| 卷号 | 775页码:19 |
| 关键词 | Diachronous uplift Thermo-mechanical modeling India-Asia collision Far-field stress transfer West Kunlun Tian Shan |
| ISSN号 | 0040-1951 |
| DOI | 10.1016/j.tecto.2019.228310 |
| 英文摘要 | The Cenozoic India-Asia collision reactivated several ancient thrust belts in the interior of the Asian continent, including the West and East Kunlun ranges in central Tibet, and the Tian Shan and Qilian Shan further north. Both basin sedimentary records and thermochronological data show that the uplift of the South Tian Shan and Qilian Shan at the north occurred earlier than that of the West and East Kunlun ranges at the south. Diachronous continental deformation and initiation of uplift during orogeny are contrary to the general notion that the stress transfer in response to the India-Asia collision should propagate sequentially from south to north. Here we systematically conducted 2D thermo-mechanical simulations to investigate possible factors for this diachronous deformation pattern. The results show that a hotter Tian Shan lithosphere, with Moho temperature > 100 degrees C hotter than that of the proto-southern Asia, leads to an earlier and higher uplift of the Tian Shan. Additionally, a faster convergence rate of the India-Asia collision results in a more efficient transfer of boundary force into the upper plate's interior, giving rise to a larger amount of uplift in the Tian Shan. We conclude that intra-continental ranges with weaker lithosphere, such as the Tian Shan or Qilian Shan, uplift earlier than stronger regions, such as the West and East Kunlun ranges. Faster convergence rates amplify this situation. Our results imply that the unique diachronous growth of the Tibetan plateau arises from its complex pre-collisional history, which includes collided arc-continent terranes with hotter and weaker lithosphere that respond to the effects of far-field stress transfer. |
| WOS关键词 | NORTHERN TIBETAN PLATEAU ; CENOZOIC TECTONIC EVOLUTION ; EASTERN KUNLUN RANGE ; FISSION-TRACK EVIDENCE ; U-PB GEOCHRONOLOGY ; CHINESE TIEN-SHAN ; TIAN-SHAN ; TARIM BASIN ; QILIAN SHAN ; QAIDAM BASIN |
| 资助项目 | Strategic Priority Research Program (B) of the Chinese Academy of Sciences[XDB18000000] ; National Natural Science Foundation of China[41472182] ; National Natural Science Foundation of China[41474084] ; National Natural Science Foundation of China[41472181] ; National Natural Science Foundation of China[41602210] ; National Natural Science Foundation of China[41330207] ; National Natural Science Foundation of China[41720104003] ; National Major Science and Technology Projects of China[2017ZX05008-001] ; National Major Science and Technology Projects of China[2017ZX05003-001] ; National Science Foundation[EAR 1914501] |
| WOS研究方向 | Geochemistry & Geophysics |
| 语种 | 英语 |
| WOS记录号 | WOS:000515211300012 |
| 出版者 | ELSEVIER |
| 资助机构 | Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Major Science and Technology Projects of China ; National Major Science and Technology Projects of China ; National Major Science and Technology Projects of China ; National Major Science and Technology Projects of China ; National Science Foundation ; National Science Foundation ; National Science Foundation ; National Science Foundation ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Major Science and Technology Projects of China ; National Major Science and Technology Projects of China ; National Major Science and Technology Projects of China ; National Major Science and Technology Projects of China ; National Science Foundation ; National Science Foundation ; National Science Foundation ; National Science Foundation ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Major Science and Technology Projects of China ; National Major Science and Technology Projects of China ; National Major Science and Technology Projects of China ; National Major Science and Technology Projects of China ; National Science Foundation ; National Science Foundation ; National Science Foundation ; National Science Foundation ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Major Science and Technology Projects of China ; National Major Science and Technology Projects of China ; National Major Science and Technology Projects of China ; National Major Science and Technology Projects of China ; National Science Foundation ; National Science Foundation ; National Science Foundation ; National Science Foundation |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/95646]  |
| 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 | Gong, Junfeng; Chen, Lin |
| 作者单位 | 1.Minist Educ, Res Ctr Struct Oil & Gas Bearing Basins, Hangzhou 310027, Peoples R China 2.Univ Nevada, Nevada Bur Mines & Geol, Reno, NV 89557 USA 3.Zhejiang Univ, Sch Earth Sci, Hangzhou 310027, Peoples R China 4.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China |
| 推荐引用方式 GB/T 7714 | Bian, Shuang,Gong, Junfeng,Chen, Lin,et al. Diachronous uplift in intra-continental orogeny: 2D thermo-mechanical modeling of the India-Asia collision[J]. TECTONOPHYSICS,2020,775:19. |
| APA | Bian, Shuang.,Gong, Junfeng.,Chen, Lin.,Zuza, Andrew, V.,Chen, Hanlin.,...&Yang, Rong.(2020).Diachronous uplift in intra-continental orogeny: 2D thermo-mechanical modeling of the India-Asia collision.TECTONOPHYSICS,775,19. |
| MLA | Bian, Shuang,et al."Diachronous uplift in intra-continental orogeny: 2D thermo-mechanical modeling of the India-Asia collision".TECTONOPHYSICS 775(2020):19. |
入库方式： OAI收割
来源：地质与地球物理研究所
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