1. Center for Geophysical Survey,China Geological Survey,Langfang 065000,China 2. Institute of Geophysical and Geochemical Exploration,Chinese Academy of Geological Sciences,Langfang 065000,China 3. The National Center for Geological Exploration Technology,Langfang 065000, China
The Baoding sag is located on the western margin of the Jizhong depression,Bohai Bay basin.It is adjacent to the uplift of the Taihang Mountains in the west,with the piedmont fault of the Taihang Mountains as the boundary.Identifying the deep structures and fine-scale geological structure of the sag is greatly significant for the hydrocarbon exploration and the survey and evaluation of deep thermal reservoirs in the sag.Meanwhile,it also facilitates the research on the characteristics of the piedmont fault of the Taihang Mountains.Since the exploration using the seismic reflection method feature high precision and high resolution in the detection of deep geological structure,this study conducted the seismic reflection-based exploration in the tectonic units of the Baoding sag and their periphery.First,high-quality original seismic records were obtained by means of explosive source excitation,long-array multi-channel reception,and high coverage times.Then,seismic reflection sections that can clearly reflect the deep geological structure and structural characteristics of the survey area were obtained using high-precision imaging data processing techniques,such as static correction,pre-stack noise attenuation,deconvolution,and offset stack.The obtained seismic sections allowed for determining the characteristics of faults in the sag and internal secondary tectonic units.Based on the angular unconformities identified in the seismic sections,the basement structural layer and the structural layers formed during the faulting stage and the depression stage of the Baoding sag were also determined,and,accordingly,the tectonic evolutionary process of the three structural layers were discussed.
Shan S Q, He D F, Zhang Y Y. Tectono-stratigraphic sequence and basin evolution of Baoding sag in the western Bohai Bay Basin[J]. Chinese Journal of Geology, 2016, 51(2): 402-414.
Chang J, Qiu N S, Zhao X Z, et al. Present-day geothermal regine of the Jizhong depressinn in Bohai Baybasin,East China[J]. Chinese J. Geophys., 2016, 59(3): 1003-1016.
Jin F M, Cui Z Q, Wang Q, et al. Distribution characteristics and main controlling factors of stratigraphiclithologic reservoirs in Jizhong Depression[J]. Lithologic Reservoirs, 2017, 29(2):19-27.
Heng D F, Cui Y Q, Zhang Y Y, et al. Structural genetic types of paleo-buried hill in Jizhong depression,Bohai Bay Basin[J]. Acta Petrologica Sinica, 2017, 33(4): 1338-1356.
Han C Y, Shi Y L, Liu J, et al. Prospect and breakthrough point of oil and gas exploration in Baoding sag,Jizhong depression[J]. China Petroleum Exploration, 2017, 22(4): 61-72.
doi: 10.3969/j.issn.1672-7703.2017.04.006
Ge X H, Liu J L, Ren S M, et al. The formation and evolution of the Mesozoic-Cenozoic continental tectonics in eastern China[J]. Geology in China, 2014, 41(1):19-38.
Shan S Q. Structural geometry and kinematics of the Taihang Mountain Piedmont fault and its controlling on the development of the Bohai Bay Basin[D]. Beijing: China University of Geosciences (Beijing), 2018.
Li W. Mesozoic Basin evolution and the exploration of the Pre-Tertiary petroleum in the area of Bohai Bay Basin[D]. Dongying: China University of Petroleum (Huadong), 2007.
Sun D S, Liu C Y, Yang M H, et al. Study on complex extensional structures in the middle Jizhong Depression in the Bohai Bay Basin[J]. Geological Review, 2004, 50(5): 484-491.
Zhang W Z, Yang D X, Chen Y J, et al. Sedimentary structural characteristics and hydrocarbon distributed rules of Jizhong Depression[J]. Acta Geologica Sinica, 2018, 82(8): 1103-1112.
[14]
Gao C H, Zhang X Z, Cha M, et al. Characteristics of buried hill reservoir in Jizhong depression[J]. Northwest Oil & Gas Exploration, 2011, 23(6): 6-12.
Wang G L, Gao J, Zhang B J, et al. Study on the thermal storage characteristics of the Wumishan Formation and huge capacity geothermal well parameters in the Gaoyang low uplift area of Xiong’an New Area[J]. Acta Geologica Sinica, 2020, 94(7): 1970-1980.
Mao X, Wang X W, Guo S Y, et al. Genetic mechanism of geothermal resources in the Gaoyang geothermal field and adjacent areas[J]. Carsologica Sinica, 2021, 40(2): 273-280.
Xu D S, Feng C Y. The applicition of integrated geophysical technique to geothermal prospecting in ShiJiaZhuang depression[J]. Geophysical and Geochemical Exploration, 2007, 31(5):440-443.
He D F, ShanS Q, Zhang Y Y, et al. 3-D geologic architecture of Xiong'an New Area:Constraints from seismic reflection data[J]. Science China:Earth Sciences, 2018, 48(9): 1207-1222.
[19]
Gao X Z, Wu W T, Lu X J. Multiplicity of hydrocarbon reservoir and accumulation controlling factors within buried hills in Jizhong depression[J]. Journal of China University of Petroleum, 2011, 35(3):31-35.