中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Linking environmental changes and organic matter enrichment in the middle part of the Yanchang Formation (Ordos Basin, China) to the rollback of an oceanic slab in the eastern Paleo-Tethys

文献类型:期刊论文

作者Zhang, Jiaqiang1,2,3; Qiu, Zhen3,4; Li, Shutong5; Gao, Shanlin6; Guo, Ruiliang7; Ma, Xiaofeng5; Qiu, Junli5; Li, Shixiang8; Tao, Huifei5; Chen, Junlin1,5
刊名SEDIMENTARY GEOLOGY
出版日期2023-09-01
卷号455页码:17
ISSN号0037-0738
关键词Organic matter enrichment Yanchang Formation Ordos Basin Paleo-Tethys
DOI10.1016/j.sedgeo.2023.106480
英文摘要The Yanchang Formation, which records the whole evolutionary history of the Middle-Late Triassic lacustrine basin in the western part of the North China Block, provides an opportunity to understand the relationship between the tectono-sedimentary evolution and massive organic matter burial in lacustrine systems. The present study investigates the changes in the lithofacies association, provenance, regional tectonism, depositional environment, and organic matter accumulation in the lower-middle part of the Yanchang Formation, aiming to unravel their links. As a result of the rapid deepening of the southern Ordos Basin, the deposits in the depocenter of the basin shifted dramatically from shallow lacustrine sandstones of the lower part of the Yanchang Formation (i.e., Chang 8 Member) to deep lacustrine shales and gravity flow deposits of the middle part of the Yanchang Formation (i.e., Chang 7 Member). The provenance of the overlying Chang 7 Member is distinct from that of the underlying Chang 8 Member. It is proposed that crustal extension caused by the southwestward rollback of an oceanic slab in the eastern Paleo-Tethys may have triggered the rapid extensional subsidence in the southern Ordos Basin during the early Ladinian. In response to this deep geodynamic process, the depositional environment of the contemporaneous Ordos Basin changed significantly, as reflected by improved primary productivity, enhanced bottom-water anoxia, as well as reduced terrigenous clastic supply in the Ordos Lake. The coupling of these processes further led to the enrichment of organic matter in the Chang 7 Member. (c) 2023 Elsevier B.V. All rights reserved.
WOS关键词GRAVITY-FLOW DEPOSITS ; QINLING OROGEN ; TECTONIC EVOLUTION ; CARBON ; GEOCHEMISTRY ; RICH ; SEDIMENTS ; ZIRCON ; ORIGIN ; MEMBER
资助项目National Natural Science Foundation of China[42222209] ; National Natural Science Foundation of China[41888101] ; National Natural Science Foundation of China[41772142] ; Scientific Research and Technological Development Programs of CNPC[2021yjcq02]
WOS研究方向Geology
语种英语
出版者ELSEVIER
WOS记录号WOS:001077807700001
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 ; Scientific Research and Technological Development Programs of CNPC ; Scientific Research and Technological Development Programs of CNPC ; Scientific Research and Technological Development Programs of CNPC ; Scientific Research and Technological Development Programs of CNPC ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Scientific Research and Technological Development Programs of CNPC ; Scientific Research and Technological Development Programs of CNPC ; Scientific Research and Technological Development Programs of CNPC ; Scientific Research and Technological Development Programs of CNPC ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Scientific Research and Technological Development Programs of CNPC ; Scientific Research and Technological Development Programs of CNPC ; Scientific Research and Technological Development Programs of CNPC ; Scientific Research and Technological Development Programs of CNPC ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Scientific Research and Technological Development Programs of CNPC ; Scientific Research and Technological Development Programs of CNPC ; Scientific Research and Technological Development Programs of CNPC ; Scientific Research and Technological Development Programs of CNPC
源URL[http://ir.iggcas.ac.cn/handle/132A11/110798]  
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Qiu, Zhen; Li, Shutong; Xiao, Wenjiao
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
3.China Natl Petr Corp, Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China
4.Natl Energy Shale Gas Res & Dev Expt Ctr, Beijing, Peoples R China
5.Chinese Acad Sci, Key Lab Petr Resources, Northwest Inst Ecoenvironm & Resources, Lanzhou 730000, Gansu Province, Peoples R China
6.SINOPEC, Petr Explorat & Prod Res Inst, Beijing 100083, Peoples R China
7.Xian Shiyou Univ, Sch Earth Sci & Engn, Xian 710065, Peoples R China
8.PetroChina Changqing Oil Field Co, Res Inst Explorat & Dev, Xian 710018, Peoples R China
9.Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Xinjiang Res Ctr Mineral Resources, Urumqi 830011, Peoples R China
推荐引用方式
GB/T 7714
Zhang, Jiaqiang,Qiu, Zhen,Li, Shutong,et al. Linking environmental changes and organic matter enrichment in the middle part of the Yanchang Formation (Ordos Basin, China) to the rollback of an oceanic slab in the eastern Paleo-Tethys[J]. SEDIMENTARY GEOLOGY,2023,455:17.
APA Zhang, Jiaqiang.,Qiu, Zhen.,Li, Shutong.,Gao, Shanlin.,Guo, Ruiliang.,...&Xiao, Wenjiao.(2023).Linking environmental changes and organic matter enrichment in the middle part of the Yanchang Formation (Ordos Basin, China) to the rollback of an oceanic slab in the eastern Paleo-Tethys.SEDIMENTARY GEOLOGY,455,17.
MLA Zhang, Jiaqiang,et al."Linking environmental changes and organic matter enrichment in the middle part of the Yanchang Formation (Ordos Basin, China) to the rollback of an oceanic slab in the eastern Paleo-Tethys".SEDIMENTARY GEOLOGY 455(2023):17.

入库方式: OAI收割

来源:地质与地球物理研究所

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