Simulating tectonically controlled fractal landscape evolution in the Three Rivers Region (SE Tibetan Plateau margin)
文献类型：期刊论文
| 作者 | Yan, Zhenzhen3,4; Shi, Yaolin2; Kang, Lili1; Fan, Xiangtao3,4 |
| 刊名 | GEOMORPHOLOGY
 |
| 出版日期 | 2024-01-15 |
| 卷号 | 445页码:15 |
| ISSN号 | 0169-555X |
| 关键词 | Three Rivers Region Landscape evolution modelling Shortening and dextral shear deformation Fractal dimensions of river networks |
| DOI | 10.1016/j.geomorph.2023.108957 |
| 英文摘要 | The long-term development of fluvial landscapes is sensitive to tectonic movement. This is the case for the Three Rivers Region, located on the southeastern margin of the Tibetan Plateau, where it is critical for understanding the continuous collision and compression between the Indian and Eurasian plates. However, quantitative perspectives on this landscape evolution are lacking. Based on present global positioning system (GPS) data, a quantitative expression of two phases of regional deformation, a northeast-southwest shortening and dextral shear deformation, was proposed to represent the continuous Indian-Eurasian collision. By incorporating this tectonic pattern into a landscape evolution model and integrating the regional differential uplift, the numerical results quantitatively present a dynamic shaping of the Nu, Lancang, and Jinsha rivers in the SE Tibetan plateau margin. Analyses of the fractal dimensions of these river networks indicate that two tectonic deformation phases significantly controlled regional landscape development and its unique drainage features. The numerical simulations depict the river networks to comprise very long and relatively straight stream trunks, and relatively small and short tributaries. The tectonic shortening and its accompanying rapid uplift prevented the development and lengthening of the tributaries, which might have promoted the formation of low-relief surfaces. With comparison to the digital elevation model (DEM), the fractal features of the river networks extracted from the numerical results are consistent with those extracted from the natural river networks, despite the simplicity of the numerical model. More broadly, based on the more realistic kinematic scenarios and reasonable constraints, this study contributes to the development of an effective and applicable model that can reveal important implications for the landscape evolution of the region. |
| WOS关键词 | LOW-RELIEF ; DYNAMICS ; EXHUMATION ; DIMENSION ; INCISION ; NETWORK ; UPLIFT ; MODEL ; BASIN ; EAST |
| 资助项目 | National Natural Science Foundation of China[41974108] |
| WOS研究方向 | Physical Geography ; Geology |
| 语种 | 英语 |
| 出版者 | ELSEVIER |
| WOS记录号 | WOS:001120141400001 |
| 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 ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/111525]  |
| 专题 | 地质与地球物理研究所_深部资源勘探装备研发 |
| 通讯作者 | Yan, Zhenzhen |
| 作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, CAS Engn Lab Deep Resources Equipment & Technol, Beijing 100029, Peoples R China 2.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Key Lab Computat Geodynam, Beijing, Peoples R China 3.Int Res Ctr Big Data Sustainable Dev Goals, Beijing, Peoples R China 4.Chinese Acad Sci, Aerosp Informat Res Inst, Key Lab Digital Earth Sci, Beijing 100094, Peoples R China |
| 推荐引用方式 GB/T 7714 | Yan, Zhenzhen,Shi, Yaolin,Kang, Lili,et al. Simulating tectonically controlled fractal landscape evolution in the Three Rivers Region (SE Tibetan Plateau margin)[J]. GEOMORPHOLOGY,2024,445:15. |
| APA | Yan, Zhenzhen,Shi, Yaolin,Kang, Lili,&Fan, Xiangtao.(2024).Simulating tectonically controlled fractal landscape evolution in the Three Rivers Region (SE Tibetan Plateau margin).GEOMORPHOLOGY,445,15. |
| MLA | Yan, Zhenzhen,et al."Simulating tectonically controlled fractal landscape evolution in the Three Rivers Region (SE Tibetan Plateau margin)".GEOMORPHOLOGY 445(2024):15. |
入库方式： OAI收割
来源：地质与地球物理研究所
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