Provenance transition of the Mesoproterozoic-Neoproterozoic Xuhuai Basin: Constraining the accretion of the Northern Qinling Terrane with the North China Craton
文献类型：期刊论文
| 作者 | Li, Zhensheng2; Ma, Xueting2; An, Wei2; Mitchell, Ross N.1,3; Li, Quanzhong2; Lan, Zhongwu1,3; Dong, Yinxiao2; Zhang, Yan2; Li, Jianxun2 |
| 刊名 | JOURNAL OF ASIAN EARTH SCIENCES
 |
| 出版日期 | 2023-08-01 |
| 卷号 | 251页码:21 |
| 关键词 | North China Craton North Qinling Terrane Provenance analysis Mesoproterozoic -Neoproterozoic Rodinia supercontinent |
| ISSN号 | 1367-9120 |
| DOI | 10.1016/j.jseaes.2023.105675 |
| 英文摘要 | Dispute exists over the accretion timing of the North Qinling Terrane (NQT) to North China Craton (NCC), and the Bagongshan Group (BGG) of the Xuhuai Basin of southeastern NCC provides a window to constrain the accretion process. Integrated field investigation, and element geochemistry and detrital zircon U-Pb-Hf isotope analyses, on the BGG provide important constraints on its depositional age and provenance change. The Wushan Formation in the lower BGG is characterized by ultra-high maturity, and detrital zircons of the Archean-Paleoproterozoic (especially similar to 2.35 Ga) and dominantly negative epsilon(Hf)(t) values. The Liulaobei and Sishilichangshan formations in the upper BGG are characterized by high maturity, and detrital zircons clustering between 1.9 and 0.98 Ga with dominantly positive epsilon(Hf)(t) values. The depositional age of the BGG is limited to 1.18-0.94 Ga, placing the Mesoproterozoic-Neoproterozoic boundary between the lower and upper Liulaobei Formation. The Wushan Formation was deposited in a passive continental margin basin, sourced from an EWstriking Paleoproterozoic belt to the south of the Xuhuai Basin, as represented by the Taihua complex in the southern NCC. In contrast, the Liulaobei and Sishilichangshan formations were formed in a collisional basin, derived from a Grenvillian orogen, as represented by the NQT. The accretion of NQT to NCC started before deposition of the Liulaobei Formation at ca. 1.18 Ga, related to the assembly of supercontinent Rodinia. Combined with recent paleomagnetic and paleontological data, it is supported that the NQT is a missing piece of the Grenvillian orogen between southeastern NCC and northwestern Laurentia in the reconstruction of supercontinent Rodinia. |
| WOS关键词 | ZIRCON U-PB ; WHOLE-ROCK GEOCHEMISTRY ; LA-ICP-MS ; TECTONIC EVOLUTION ; OROGENIC BELT ; DETRITAL ZIRCONS ; PENGLAI GROUP ; SOUTH CHINA ; LU-HF ; CONTINENTAL-CRUST |
| 资助项目 | National Natural Science Foundation of China[42273025] ; National Natural Science Foundation of China[41972106] ; National Natural Science Foundation of China[41372194] ; Fundamental Research Funds for the Central Universities[JZ2021HGQA0266] ; China Geological Survey Project[1211302108023-1] |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000987081400001 |
| 出版者 | PERGAMON-ELSEVIER SCIENCE LTD |
| 资助机构 | National Natural Science Foundation of China ; National Natural Science Foundation of China ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; China Geological Survey Project ; China Geological Survey Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; China Geological Survey Project ; China Geological Survey Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; China Geological Survey Project ; China Geological Survey Project ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Fundamental Research Funds for the Central Universities ; Fundamental Research Funds for the Central Universities ; China Geological Survey Project ; China Geological Survey Project |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/110928]  |
| 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 | Li, Zhensheng; An, Wei |
| 作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 2.Hefei Univ Technol, Sch Resources & Environm Engn, Hefei 230009, Anhui, Peoples R China 3.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China |
| 推荐引用方式 GB/T 7714 | Li, Zhensheng,Ma, Xueting,An, Wei,et al. Provenance transition of the Mesoproterozoic-Neoproterozoic Xuhuai Basin: Constraining the accretion of the Northern Qinling Terrane with the North China Craton[J]. JOURNAL OF ASIAN EARTH SCIENCES,2023,251:21. |
| APA | Li, Zhensheng.,Ma, Xueting.,An, Wei.,Mitchell, Ross N..,Li, Quanzhong.,...&Li, Jianxun.(2023).Provenance transition of the Mesoproterozoic-Neoproterozoic Xuhuai Basin: Constraining the accretion of the Northern Qinling Terrane with the North China Craton.JOURNAL OF ASIAN EARTH SCIENCES,251,21. |
| MLA | Li, Zhensheng,et al."Provenance transition of the Mesoproterozoic-Neoproterozoic Xuhuai Basin: Constraining the accretion of the Northern Qinling Terrane with the North China Craton".JOURNAL OF ASIAN EARTH SCIENCES 251(2023):21. |
入库方式： OAI收割
来源：地质与地球物理研究所
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