Source-to-sink of Late carboniferous Ordos Basin: Constraints on crustal accretion margins converting to orogenic belts bounding the North China Block
文献类型：期刊论文
| 作者 | Chen, Anqing1,2; Zou, Hao2,3,4; Ogg, James G.1,2; Yang, Shuai2; Hou, Mingcai2; Jiang, Xiuwei4; Xu, Shenglin2; Zhang, Xiaoxing2 |
| 刊名 | GEOSCIENCE FRONTIERS
 |
| 出版日期 | 2020-11-01 |
| 卷号 | 11期号:6页码:2031-2052 |
| ISSN号 | 1674-9871 |
| 关键词 | Benxi formation Detrital zircons Central asian orogen belt Tectonics Paleogeography Moscovian and kasimovian |
| DOI | 10.1016/j.gsf.2020.05.008 |
| 英文摘要 | The Upper Carboniferous Benxi Formation of the Ordos Basin is the lowest strata overlying Middle Ordovician above the major ca. 150-Myr sedimentary gap that characterizes the entire North China Block (NCB). We apply an integrated analysis of stratigraphy, petrography, and U-Pb dates and Hf isotopes on detrital zircons to investigate its provenance and relationships to the progressive collisions that formed the Xing'an-Mongolia Orogenic Belt to the north and the Qinling Orogenic Belt to the south. The results show that, in addition to regional patterns of siliciclastic influx from these new uplifted sources, the Benxi Formation is composed of two sequences corresponding to long-term glacial-interglacial cycles during the Moscovian to lower Gzhelian stages which drove global changes of eustatic sea level and weathering. The spatio-temporal distribution of sediment isopachs and facies indicate there were two sediment-infilling pulses, during which the southern and the northern Ordos Basin developed tidal-reworked deltas. The age spectra from detrital zircons, trace element patterns and epsilon(Hf)(t) values reveal that the siliciclastics forming the southern delta was sourced in the Qinling Orogenic Belt, whereas the northern delta was derived from the Xing'an-Mongolia Orogenic Belt. The source-to-sink evolution of this Upper Paleozoic system records the progressive development of orogenic belts and uplifts forming on the southern and northern margins of the NCB prior to its collisions with the South China and the Siberian plates, respectively. |
| WOS关键词 | DETRITAL ZIRCON REFERENCE ; PALEO-ASIAN OCEAN ; TECTONIC EVOLUTION ; INNER-MONGOLIA ; U-PB ; QINLING OROGEN ; SOUTH CHINA ; GEOCHEMICAL DATA ; HF ISOTOPES ; CONTINENT |
| 资助项目 | National Natural Science Foundation of China[41872109] ; National Natural Science Foundation of China[41702108] ; China Postdoctoral Science Foundation[2019M650833] ; Everest Scientific Research Program of Chengdu University of Technology ; Chengdu University of Technology |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| 出版者 | CHINA UNIV GEOSCIENCES, BEIJING |
| WOS记录号 | WOS:000583042200009 |
| 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 ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; Everest Scientific Research Program of Chengdu University of Technology ; Everest Scientific Research Program of Chengdu University of Technology ; Everest Scientific Research Program of Chengdu University of Technology ; Everest Scientific Research Program of Chengdu University of Technology ; Chengdu University of Technology ; Chengdu University of Technology ; Chengdu University of Technology ; Chengdu University of Technology ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; Everest Scientific Research Program of Chengdu University of Technology ; Everest Scientific Research Program of Chengdu University of Technology ; Everest Scientific Research Program of Chengdu University of Technology ; Everest Scientific Research Program of Chengdu University of Technology ; Chengdu University of Technology ; Chengdu University of Technology ; Chengdu University of Technology ; Chengdu University of Technology ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; Everest Scientific Research Program of Chengdu University of Technology ; Everest Scientific Research Program of Chengdu University of Technology ; Everest Scientific Research Program of Chengdu University of Technology ; Everest Scientific Research Program of Chengdu University of Technology ; Chengdu University of Technology ; Chengdu University of Technology ; Chengdu University of Technology ; Chengdu University of Technology ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; China Postdoctoral Science Foundation ; Everest Scientific Research Program of Chengdu University of Technology ; Everest Scientific Research Program of Chengdu University of Technology ; Everest Scientific Research Program of Chengdu University of Technology ; Everest Scientific Research Program of Chengdu University of Technology ; Chengdu University of Technology ; Chengdu University of Technology ; Chengdu University of Technology ; Chengdu University of Technology |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/98213]  |
| 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 | Zou, Hao |
| 作者单位 | 1.Purdue Univ, Dept Earth Atmospher & Planetary Sci, W Lafayette, IN 47907 USA 2.Chengdu Univ Technol, State Key Lab Oil & Gas Reservoir Geol & Exploita, Chengdu 610059, Sichuan, Peoples R China 3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 4.Chengdu Univ Technol, Minist Land & Resources, Key Lab Tecton Controls Mineralizat & Hydrocarbon, Chengdu 610059, Peoples R China |
| 推荐引用方式 GB/T 7714 | Chen, Anqing,Zou, Hao,Ogg, James G.,et al. Source-to-sink of Late carboniferous Ordos Basin: Constraints on crustal accretion margins converting to orogenic belts bounding the North China Block[J]. GEOSCIENCE FRONTIERS,2020,11(6):2031-2052. |
| APA | Chen, Anqing.,Zou, Hao.,Ogg, James G..,Yang, Shuai.,Hou, Mingcai.,...&Zhang, Xiaoxing.(2020).Source-to-sink of Late carboniferous Ordos Basin: Constraints on crustal accretion margins converting to orogenic belts bounding the North China Block.GEOSCIENCE FRONTIERS,11(6),2031-2052. |
| MLA | Chen, Anqing,et al."Source-to-sink of Late carboniferous Ordos Basin: Constraints on crustal accretion margins converting to orogenic belts bounding the North China Block".GEOSCIENCE FRONTIERS 11.6(2020):2031-2052. |
入库方式： OAI收割
来源：地质与地球物理研究所
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