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Original Sedimentary Pattern of an Inverted Basin: A Case Study from the Bozhong Depression, Offshore Bohai Bay Basin

文献类型：期刊论文

作者Zhao Junfeng1; Liu Chiyang1; Huang Lei1; Mountney, Nigel2; Han Shaojia3; Liu Peng4; Hu Junhao5
刊名ACTA GEOLOGICA SINICA-ENGLISH EDITION
出版日期2016-12-01
卷号90期号:6页码:2163-2181
关键词Eocene Shahejie Formation Basin Inversion Bozhong Depression Bohai Bay Basin
ISSN号1000-9515
DOI10.1111/1755-6724.13029
文献子类Article
英文摘要The third member of Shahejie Formation (Sha-3 member; 42-38Ma of Eocene) in the Bozhong Depression, offshore Bohai Bay Basin was subject to multiple post-depositional modifications. The present structural framework of the Bozhong Depression, which is characterized by sags alternating with uplifts, does not reflect its original sedimentary pattern. Previous studies have not discussed the post-depositional modification of this succession, including the sedimentary pattern variations and the depositional geodynamic setting. This work determined the characteristics of the post-depositional modification and original sedimentary pattern of the Bozhong Depression through analysis of seismic data, well-log data and fission-track ages. The results demonstrate that the Shijiutuo rise, a major structural feature of the current basin, did not exist during the major depositional stage of the Sha-3 member, when the Qinnan sag was largely connected to the Bozhong sag to form a single contiguous deposition area within the basin. By contrast, the Shaleitian and Chengbei rises, located in the western part of the Bozhong Depression, have existed before the depositional period of the Eocene Sha-3 member; these features were manifested as syn-depositional tilted fault blocks, the uplifted footwall blocks of which provided sediments for the neighboring Shanan and Chengbei sags. The western part of the Bonan low rise, located in the southern part of the Bozhong Depression, did not experience uplifting during the depositional phase of the Eocene Sha-3 member. The Huanghekou sag was connected with the Bozhong sag in the western part of the Bozhong Depression. The original sedimentary boundary of the southern Miaoxi sag possibly extended eastward about 10 km and connected with the Bozhong sag at its northern part. The present-day Bodong low rise, which is bounded by the Tan-Lu fault zone, also formed after the depositional period of Eocene Sha-3 member. It is thus concluded that the Bozhong Depression formed a connected large-scale sub-basin during the depositional stage of the Eocene Sha-3 member. Several neighboring sags that are now separated by rises, including the Qinnan, Shanan, Chengbei, Huanghekou, Miaoxi and Bodong sags, formed a single contiguous depositional area during the Eocene. The significant differences between the present and original basin patter and framework provide valuable information for better understanding the history of basin inversion and its impact on related hydrocarbon-system evolution.
WOS关键词NORTH CHINA CRATON ; LU FAULT ZONE ; ORDOS BASIN ; EASTERN CHINA ; TECTONIC EVOLUTION ; INVERSION ; SAG ; DESTRUCTION ; DYNAMICS ; DEFORMATION
WOS研究方向Geology
语种英语
WOS记录号WOS:000392873500017
出版者WILEY-BLACKWELL
资助机构National Natural Science Foundation of China(41330315) ; National Science and Technology Major Project(2011ZX05023001-002) ; MOST Special Funds from State Key Laboratory of Continental Dynamics(BJ081334) ; National Natural Science Foundation of China(41330315) ; National Science and Technology Major Project(2011ZX05023001-002) ; MOST Special Funds from State Key Laboratory of Continental Dynamics(BJ081334) ; National Natural Science Foundation of China(41330315) ; National Science and Technology Major Project(2011ZX05023001-002) ; MOST Special Funds from State Key Laboratory of Continental Dynamics(BJ081334) ; National Natural Science Foundation of China(41330315) ; National Science and Technology Major Project(2011ZX05023001-002) ; MOST Special Funds from State Key Laboratory of Continental Dynamics(BJ081334)
源URL[http://ir.iggcas.ac.cn/handle/132A11/53137]  
专题地质与地球物理研究所_兰州油气中心
通讯作者Zhao Junfeng
作者单位1.Northwest Univ, Dept Geol, State Key Lab Continental Dynam, Xian 710069, Shaanxi, Peoples R China
2.Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England
3.Gansu Coal Geol Res Inst, Lanzhou 730000, Gansu, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources Res, Lanzhou 730000, Gansu, Peoples R China
5.Chinese Acad Sci, Inst Geochem, Guiyang 550002, Guizhou, Peoples R China
推荐引用方式
GB/T 7714		 Zhao Junfeng,Liu Chiyang,Huang Lei,et al. Original Sedimentary Pattern of an Inverted Basin: A Case Study from the Bozhong Depression, Offshore Bohai Bay Basin[J]. ACTA GEOLOGICA SINICA-ENGLISH EDITION,2016,90(6):2163-2181.
APA Zhao Junfeng.,Liu Chiyang.,Huang Lei.,Mountney, Nigel.,Han Shaojia.,...&Hu Junhao.(2016).Original Sedimentary Pattern of an Inverted Basin: A Case Study from the Bozhong Depression, Offshore Bohai Bay Basin.ACTA GEOLOGICA SINICA-ENGLISH EDITION,90(6),2163-2181.
MLA Zhao Junfeng,et al."Original Sedimentary Pattern of an Inverted Basin: A Case Study from the Bozhong Depression, Offshore Bohai Bay Basin".ACTA GEOLOGICA SINICA-ENGLISH EDITION 90.6(2016):2163-2181.

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来源：地质与地球物理研究所

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