Cenozoic source-to-sink relations between the West Kunlun Mountains and SW Tarim Basin: Evidence from an integrated provenance analysis
文献类型：期刊论文
| 作者 | Zhang, Zhiliang1,3; Sun, Jimin1,2; Zhang, Bin1; Ren, Zhikun3 |
| 刊名 | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
 |
| 出版日期 | 2023-12-15 |
| 卷号 | 632页码:21 |
| ISSN号 | 0031-0182 |
| 关键词 | Provenance Zircon U-Pb Keliyang West Kunlun Mountains Cenozoic |
| DOI | 10.1016/j.palaeo.2023.111858 |
| 英文摘要 | The tectonic evolution of West Kunlun Mountains (WKM), which is located in the NW margin of the Tibetan Plateau, plays an essential role in understanding the source-to-sink relationship between this orogenic belt and SW Tarim Basin. In this study, we conduct an integrated research incorporating detrital zircon U-Pb geochronology, petrography, and heavy mineral analysis of the Cenozoic synorogenic sediments from Keliyang section, SW Tarim Basin, together with the published data in the WKM forelands, and thus we can discuss the Cenozoic tectonic evolution in this activate tectonic domain. The results suggest that the NW Tibetan Plateau has experienced a four-stage evolution during the Cenozoic, characterized by three notable provenance changes occurring in the late Eocene (-40 Ma), late Oligocene (-26 Ma) and latest Miocene-early Pliocene, respectively. In the early Middle Eocene, the Tarim-Tajik basin was still occupied by an epicontinental sea belonging to the Neotethys Sea. Sediments in the forelands were mainly originated from erosion of the residual relief of WKM. By -40 Ma, the new additions of sediments from the uplifted Tianshuihai and/or South Kunlun terranes occurred, which can be attributed to the uplift of central Tibet due to the ongoing Indian northward indentation. This scenario was roughly synchronous with the final open marine seawater retreat from the Tarim Basin. We propose that the Cenozoic uplift of the Tianshuihai/South Kunlun terranes may be initiated prior to -40 Ma, indicating that the collision-induced deformation has propagated to the southern part of WKM by that time. Since -26 Ma, distal deposits increased abruptly, which can be attributed to the outward growth of the Tibetan Plateau and/or regional climate change. Finally, the shift in provenance since the latest Miocene-early Pliocene was related to the intensive uplift of WKM. |
| WOS关键词 | DETRITAL-ZIRCON GEOCHRONOLOGY ; HEAVY MINERAL ASSEMBLAGES ; NW CHINA IMPLICATIONS ; U-PB AGES ; TECTONIC EVOLUTION ; KARAKORAM FAULT ; CONTINENTAL-CRUST ; NORTHERN TIBET ; ISOTOPIC CONSTRAINTS ; KINEMATIC EVOLUTION |
| 资助项目 | Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration[IGCEA2113] ; National Natural Science Foundation of China[42272219] ; National Science and Technology Basic Resources Investigation Program of China[2021FY100102] |
| WOS研究方向 | Physical Geography ; Geology ; Paleontology |
| 语种 | 英语 |
| 出版者 | ELSEVIER |
| WOS记录号 | WOS:001103717500001 |
| 资助机构 | Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Basic Resources Investigation Program of China ; National Science and Technology Basic Resources Investigation Program of China ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Basic Resources Investigation Program of China ; National Science and Technology Basic Resources Investigation Program of China ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Basic Resources Investigation Program of China ; National Science and Technology Basic Resources Investigation Program of China ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; Basic Scientific Research Fund, Institute of Geology, China Earthquake Administration ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Science and Technology Basic Resources Investigation Program of China ; National Science and Technology Basic Resources Investigation Program of China |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/111183]  |
| 专题 | 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 | Zhang, Zhiliang; Sun, Jimin; Zhang, Bin |
| 作者单位 | 1.Chinese Acad Sci, Key Lab Cenozo Geol & Environm, Inst Geol & Geophys, Beijing 100029, Peoples R China 2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 3.China Earthquake Adm, Inst Geol, Beijing 100029, Peoples R China |
| 推荐引用方式 GB/T 7714 | Zhang, Zhiliang,Sun, Jimin,Zhang, Bin,et al. Cenozoic source-to-sink relations between the West Kunlun Mountains and SW Tarim Basin: Evidence from an integrated provenance analysis[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2023,632:21. |
| APA | Zhang, Zhiliang,Sun, Jimin,Zhang, Bin,&Ren, Zhikun.(2023).Cenozoic source-to-sink relations between the West Kunlun Mountains and SW Tarim Basin: Evidence from an integrated provenance analysis.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,632,21. |
| MLA | Zhang, Zhiliang,et al."Cenozoic source-to-sink relations between the West Kunlun Mountains and SW Tarim Basin: Evidence from an integrated provenance analysis".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 632(2023):21. |
入库方式： OAI收割
来源：地质与地球物理研究所
浏览0
下载0
收藏0
其他版本
除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。