Entrenchment of the Yellow River since the late Miocene under changing tectonics and climate
文献类型：期刊论文
| 作者 | Xiong, Jianguo6,7; Liu, Yunming5; Zhang, Peizhen6,7; Deng, Chenglong4; Picotti, Vincenzo3; Wang, Weitao6; Zhang, Ke6; Liang, Hao6; Zhao, Xudong7; Zhong, Yuezhi3 |
| 刊名 | GEOMORPHOLOGY
 |
| 出版日期 | 2022-11-01 |
| 卷号 | 416页码:28 |
| ISSN号 | 0169-555X |
| 关键词 | Yellow River Jinshaan Gorge Magnetostratigraphy Zircon U-Pb chronology Tectonic and climatic impacts Northeastern Tibetan Plateau |
| DOI | 10.1016/j.geomorph.2022.108428 |
| 英文摘要 | The distinctive right-angled bend of the Yellow River around the Ordos Block, a large Permo-Mesozoic continental block in East Asia, has attracted much attention from geomorphologists and geologists concerning its formation and evolution for more than a century. The Jinshaan Gorge, an over 600 km long entrenched reach of the Yellow River, currently connecting the Hetao Graben to the north and the Weihe Graben to the south, is considered to have developed in very recent geological time. However, the timing and processes of drainage integration between the two grabens and formation of the Jinshaan Gorge as a deeply incised form are still under debate, owing to limited data and various interpretations of them. In order to better understand the geomorphological evolution of the Yellow River, we investigated the sedimentology, magnetostratigraphy, and detrital zircon U-Pb dating in the upper Neogene and Quaternary deposits along the Jinshaan Gorge. We further integrated the new data with the sedimentary record of the adjacent basins in the northeastern Tibetan Plateau (NTP) and the basins around the Ordos Block, as well as the incision history of the Yellow River inferred from its terrace sequence. We show that the upper Neogene alluvial sediments preserved in the broad Tangxian valley along the Jinshaan Gorge are a mixture of materials from the Lvliang Shan and the Ordos Block. Importantly, they share almost the same provenance and zircon age spectra with the Pleistocene and Holocene Yellow River deposits. The broad Tangxian valley commenced incision during the Late Pliocene, followed by the formation of two Early Pleistocene terraces dated to similar to 2.2 Ma and similar to 1.2 Ma. The incision of the Yellow River and the accumulation in the basins were characterized by steady and slow rates before the Late Pleistocene, but an acceleration thereafter. We propose a three-stage evolutionary model for the development of the Yellow River, controlled by changing tectonics and climate during the Neogene. Before the late Miocene, an endorheic river system was developing in the Longzhong Basin. From the late Miocene to Early Pliocene, the Yellow River developed the current drainage system from the Longzhong Basin to the lower reach, constrained by the topographic pattern of the Ordos Block and its periphery, in turn controlled by coeval tectonic movements. Since the Late Pliocene, the Yellow River has undergone rapid incision with integration of the upper reach in the NTP and entrenchment in the upper and middle reaches, which were controlled by the continuously rising NTP and a deteriorating climate. The Tangxian valley developed and was filled between the end of the Miocene and Pliocene, approximately 8 to 3 Ma, and it was abandoned in the Late Pliocene in response to important climatic variations. The next acceleration in both incision and subsidence around the Ordos Block in the Late Pleistocene was also coeval with strong climatic oscillations, suggesting a possible link between climate and tectonics in the Neogene entrenchment history of the Yellow River. |
| WOS关键词 | APATITE FISSION-TRACK ; NE TIBETAN PLATEAU ; SHANXI GRABEN SYSTEM ; NORTH QILIAN SHAN ; U-PB AGE ; NORTHEASTERN MARGIN ; LOESS PLATEAU ; CHINA IMPLICATIONS ; THERMOCHRONOLOGICAL CONSTRAINTS ; MAGNETOSTRATIGRAPHIC RECORD |
| 资助项目 | Second Tibetan Plateau Scientific Expedition and Research Program (STEP)[2019QZKK0704] ; Natural Science Foundation of China[41888101] ; Natural Science Foundation of China[41971002] ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration |
| WOS研究方向 | Physical Geography ; Geology |
| 语种 | 英语 |
| 出版者 | ELSEVIER |
| WOS记录号 | WOS:000852597100001 |
| 资助机构 | Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Natural Science Foundation of China ; Natural Science Foundation of China ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration ; State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Natural Science Foundation of China ; Natural Science Foundation of China ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration ; State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Natural Science Foundation of China ; Natural Science Foundation of China ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration ; State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Natural Science Foundation of China ; Natural Science Foundation of China ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; Institute of Geology and Geophysics, Chinese Academy of Sciences ; State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration ; State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/108381]  |
| 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 | Liu, Yunming |
| 作者单位 | 1.China Earthquake Adm, Inst Geol, Key Lab Seism & Volcan Hazards, Beijing 100029, Peoples R China 2.Peking Univ, Key Lab Earth Surface Proc, Minist Educ, Beijing 100871, Peoples R China 3.Swiss Fed Inst Technol, Dept Earth Sci, CH-8092 Zurich, Switzerland 4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 5.Anqing Normal Univ, Coll Resources & Environm, Anqing 246133, Peoples R China 6.Sun Yat sen Univ, Sch Earth Sci & Engn, Guangdong Prov Key Lab Geodynam & Geohazards, Guangzhou 510275, Peoples R China 7.China Earthquake Adm, Inst Geol, State Key Lab Earthquake Dynam, Beijing 100029, Peoples R China |
| 推荐引用方式 GB/T 7714 | Xiong, Jianguo,Liu, Yunming,Zhang, Peizhen,et al. Entrenchment of the Yellow River since the late Miocene under changing tectonics and climate[J]. GEOMORPHOLOGY,2022,416:28. |
| APA | Xiong, Jianguo.,Liu, Yunming.,Zhang, Peizhen.,Deng, Chenglong.,Picotti, Vincenzo.,...&Li, Youli.(2022).Entrenchment of the Yellow River since the late Miocene under changing tectonics and climate.GEOMORPHOLOGY,416,28. |
| MLA | Xiong, Jianguo,et al."Entrenchment of the Yellow River since the late Miocene under changing tectonics and climate".GEOMORPHOLOGY 416(2022):28. |
入库方式： OAI收割
来源：地质与地球物理研究所
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