中非剪切背景下裂陷盆地的发育机制：以Bongor盆地为例

doi:10.3799/dqkx.2025.172

中非剪切背景下裂陷盆地的发育机制：以Bongor盆地为例

doi: 10.3799/dqkx.2025.172

1. 中国石油勘探开发研究院, 北京 100083;
2. 中国地质大学(武汉)构造与油气教育部重点实验室湖北武汉 430074;
3. 中国石油天然气勘探开发公司, 北京 100034

基金项目:

中国石油天然气股份有限公司科技项目“海外油气地质新理论资源评价新技术与超前选区”(No.2023ZZ07)

科学研究与技术开发项目“中西非裂谷系走滑构造数值模拟及构造变形研究”(No.YGJ2024-02)

详细信息

作者简介:
肖坤叶（1969—），男，教授级高级工程师，博士，主要从事海外油气勘探､资源评价与油气地质综合研究。E-mail:xiaokunye@petrochina.com.cn，ORCID:

中图分类号: P541
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出版历程
- 收稿日期: 2025-07-08
- 网络出版日期: 2025-09-08

Formation Mechanism of Rift Basins in the Central African Strike-Slip Tectonic Setting: A Case Study of the Bongor Basin

1. Research Institute of Petroleum Exploration & Development, Beijing 100083, China;
2. Key Laboratory of Tectonics and Petroleum Resources, Ministry of Education, China University of Geosciences, Wuhan 430074, China;
3. China National Oil and Gas Exploration and Development Corporation, Beijing 100034, China

摘要

摘要: 基于地震资料精细解析和构造物理模拟实验，本文研究了中非剪切带Bongor盆地独特的结构构造特征及其形成演化的动力学机制。结果显示Bongor盆地整体表现为南断北超箕状断陷结构，局部发育构造转换带，沉积中心受控于边界主干断裂，现今保留明显的反转裂谷盆地特征，受早白垩世两期裂陷和晚白垩世末期-古近纪挤压反转共同控制。构造物理模拟实验证实了盆地受两期裂陷及其后反转作用的控制机制，并揭示两期裂陷伸展方向夹角为25°～45°。研究认为：早白垩世早期，南大西洋初始扩张引发的南非次板块与东北非次板块间近N-S向拉张，导致包括Bongor盆地在内的中非裂谷系盆地经历第一期近南北向伸展的裂陷作用；早白垩世晚期，大西洋赤道段的扩张以及特提斯洋向欧亚大陆俯冲，导致东北非地块与南非地块之间经历近NE-SW向的伸展作用，北西走向的Bongor经历二期裂陷作用。研究提出了Bongor盆地形成演化的新认识，对指导下一步油气勘探具有重要意义。
- 裂陷盆地 /
- 剪切带 /
- 构造物理模拟 /
- 构造演化 /
- Bongor盆地
Abstract: Integrating detailed seismic interpretation and analogue tectonic modeling experiments, this study investigates the unique structural characteristics and the dynamic formation and evolution mechanisms of the Bongor Basin in the Central African Shear Zone. Geophysical interpretation indicates that the Bongor Basin exhibits characteristics of a typical inverted rift basin. The current structural configuration was controlled by two phases rifting during Early Cretaceous and the compression in Late Cretaceous-Paleogene, with the primary rift-related structures are still clearly identifiable. Multi-stage analogue tectonic modeling further confirm that the formation of the Bongor Basin was controlled by two early phases of rifting and subsequent inversion, with the extension directions of the two rifting stages separated by 25°–45°. Combining these results and context of regional tectonic history, a geological model of the two-phase rifting in the Bongor basin was put forward. In the early Early Cretaceous, the opening of the South Atlantic Ocean triggered near north-south stretching between the South African and the Northeast African subplate. This led to the first phase of rifting n the Central African Rift System basins, including the Bongor Basin. During the late Early Cretaceous, both the shift of the main Atlantic expansion toward the equatorial region and the subduction of the Tethys Ocean toward the Eurasian continent caused a nearly northeast-southwest extensional stress between the northeast African block and the South African block. Unlike other basins parallel to the Central African Rift System, the northwest-trending Bongor Basin underwent a second phase of rifting. The study presents new insights into the formation and evolution of the Bongor Basin, which is of great significance for guiding future oil and gas exploration
- Rift Basin /
- Shear Zone /
- Physical Analog Modeling /
- Tectonic Evolution /
- Bongor Basin

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参考文献(79)

[1]	Alkmim, F.F., Marshak, S., Fonseca, M.A., 2001. Assembling West Gondwana in the Neoproterozoic: Clues from the São Francisco Craton Region, Brazil.Geology, 29(4): 319–322. doi: 10.1130/0091-7613(2001)029<0319:AWGITN>2.0.CO;2
[2]	Azevedo, R.L.M. de., 2004. Paleoceanografia e a Evolução do Atlântico Sul no Albiano.Boletim De Geociências Da Petrobras, 12(2): 231–249.
[3]	Brun, J. P., 1999. Narrow Rifts Versus Wide Rifts: Inferences for the Mechanics of Rifting from Laboratory Experiments.Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences, 357(1753): 695–712. doi: 10.1098/rsta.1999.0349
[4]	Bonifacio, J.F., Ganade, G.E., Santos, A.C.D., et al., 2023. Review and Critical Assessment on Plate Reconstruction Models for the South Atlantic.Earth-Science Reviews, 238: 104333. Doi: 10.1016/j.earscirev.2023.104333
[5]	Chaboureau, A.C., Guillocheau, F., Robin, C., et al., 2013. Paleogeographic Evolution of the Central Segment of the South Atlantic during Early Cretaceous Times: Paleotopographic and Geodynamic Implications.Tectonophysics, 604: 191–223. doi: 10.1016/j.tecto.2012.08.025
[6]	Chen, Z.G., Xu, G. Wang, J.C., et al., 2016. Different Structural Characteristics in the East and West Parts, Bongor Basin, Chad, and Their Influence on Hydrocarbon Accumulation. Oil Geophysical Prospecting, 51(S1): 113–119, 9(in Chinese with English abstract).
[7]	Collettini, C., Sibson, R.H., 2001. Normal Faults, Normal Friction?Geology, 29(10): 927–930. doi: 10.1130/0091-7613(2001)029<0927:NFNF>2.0.CO;2
[8]	Dahlstrom, C.D.A., 1970. Structural Geology in the Eastern Margin of the Canadian Rocky Mountains.Bulletin of Canadian Petroleum Geology, 18(3):332-406. Doi: 10.35767/gscpgbull.18.3.332.
[9]	Darros De Matos, R.M., 2000. Tectonic Evolution of the Equatorial South Atlantic.American Geophysical Union (AGU). doi: 10.1029/GM115p0331
[10]	Davison, I., 2007. Geology and Tectonics of the South Atlantic Brazilian Salt Basins.London, Geological Society of London.
[11]	Dou, L.R., Wang, J.C., Wang, R.C., et al., 2018. Precambrian Basement Reservoirs: Case Study from the Northern Bongor Basin, the Republic of Chad.AAPG Bulletin, 102(09): 1803–1824. doi: 10.1306/02061817090
[12]	Dou, L.R., Wang, J.C., Wang, R.C., et al., 2018. The Precambrian Basement Play in the Central African Rift System.Earth Science Frontiers, 25(2): 015-023(in Chinese with English abstract).
[13]	Dou, L.R., Wang, R.C.., Wang, J.C., et al., 2021. Thermal History Reconstruction from Apatite Fission-Track Analysis and Vitrinite Reflectance Data of the Bongor Basin, the Republic of Chad.AAPG Bulletin, 105(5): 919–944. doi: 10.1306/11182019167
[14]	Dou, L.R., Xiao, K.Y., Du, Y.B., et al., 2024. Tectonics of the West and Central African Strike-Slip Rift System.Petroleum Science, 21(6): 3742–3753. doi: 10.1016/j.petsci.2024.11.017
[15]	Dou, L.R., Xiao, K.Y., Hu, Y., et al., Petroleum Geology and a Model of Hydrocarbon Accumulations in the Bongor Basin the Republic of Chad.Acta Petroleum Sinica, 32(3): 379–386(in Chinese with English abstract).
[16]	Eagles, G., 2007. New angles on South Atlantic Opening.Geophysical Journal International, 168(1): 353–361. doi: 10.1111/j.1365-246X.2006.03206.x
[17]	Fairhead, J.D., 2020. Regional Tectonics and Basin Formation: The Role of Potential Field Studies – An Application to the Mesozoic West and Central African Rift System. In:Regional Geology and Tectonics (Second Edition) (N. Scarselli, J. Adam, D. Chiarella, D. G. Roberts & A. W. Bally, Eds.), Elsevier: p. 541–556. doi: 10.1016/B978-0-444-64134-2.00018-3
[18]	Fairhead, J.D., 2023. The Mesozoic West and Central Africa Rift System (WCARS) and the Older Kandi Shear Zone (KSZ): Rifting and Tectonics of North Africa and South America and Fragmentation of Gondwana Based on Geophysical Investigations.Journal of African Earth Sciences, 199: 104817. doi: 10.1016/j.jafrearsci.2022.104817
[19]	Fairhead, J.D., Green, C.M., Masterton, S.M., et al. 2013. The Role that Plate Tectonics, Inferred Stress Changes and Stratigraphic Unconformities have on the Evolution of the West and Central African Rift System and the Atlantic Continental Margins.Tectonophysics, 594: 118–127. doi: 10.1016/j.tecto.2013.03.021
[20]	Franke, D., 2013. Rifting, Lithosphere Breakup and Volcanism: Comparison of Magma-Poor and Volcanic Rifted Margins.Marine and Petroleum Geology, 43: 63–87. doi: 10.1016/j.marpetgeo.2012.11.003
[21]	Frindt, S., Trumbull, R.B., Romer, R.L., 2004. Petrogenesis of the Gross Spitzkoppe Topaz Granite, Central Western Namibia: a Geochemical and Nd–Sr–Pb Isotope Study,Chemical Geology, 206(1): 43–71. doi: 10.1016/j.chemgeo.2004.01.015
[22]	Gao, H.H., Du, Y.B., Wang, L., et al., 2023. Tectonic Features, Genetic Mechanisms and Basin Evolution of the Eastern Doseo Basin, Chad.Petroleum Exploration and Development, 50(5): 1003-1015(in Chinese with English abstract).
[23]	Genik, G.J., 1993. Petroleum Geology of Cretaceous-Tertiary Rift Basins in Niger, Chad, and Central African Republic1.AAPG Bulletin, 77(8): 1405–1434. doi: 10.1306/BDFF8EAC-1718-11D7-8645000102C1865D
[24]	Gladczenko, T.P., Hinz, K., Eldholm, O., et al. 1997. South Atlantic Volcanic Margins.Journal of the Geological Society, 154(3): 465–470.
[25]	Gupta, S., Cowie, P.A., Dawers, N.H., et al., 1998. A mechanism to Explain Rift-Basin Subsidence and Stratigraphic Patterns through Fault-Array Evolution.Geology, 26(7): 595-598. Doi: 10.1130/0091-7613(1998)026<0595:AMTERB>2.3.CO;2.
[26]	Gürer, D., Granot, R., Hinsbergen, D.J.J. 2022. Plate Tectonic Chain Reaction Revealed by Noise in the Cretaceous Quiet Zone.Nature Geoscience, 15(3): 233–239. doi: 10.1038/s41561-022-00893-7
[27]	Hao, L.L., Hu, W.L., Wang, Q., et al., 2025. Bangong-Nujiang Neo-Tethyan Ocean (Central Tibet): Geodynamics, Crustal Evolution, Metallogeny, and Linkages to the “Yanshan Movement.”Earth-Science Reviews, 265: 105119. doi: 10.1016/j.earscirev.2025.105119
[28]	Harding, T. P., Lowell, J. D., 1979. Structural Styles, Their Plate-Tectonic Habitats, and Hydrocarbon Traps in Petroleum Provinces.AAPG Bulletin, 63(7):1016-1058. doi: 10.1306/2F9184B4-16CE-11D7-8645000102C1865D
[29]	Hu, W.L., Wang, Q., Tang, G.J., et al., 2022. Late Early Cretaceous Magmatic Constraints on the Timing of Closure of the Bangong–Nujiang Tethyan Ocean, Central Tibet.Lithos, 416–417: 106648. doi: 10.1016/j.lithos.2022.106648
[30]	Huang, C., Yu, Z.H., Xiao, G.J., et al. 2012. Tectonic Evolution and its Influence to Hydrocarbon Accumulation in B basin, Central and Western African System.Science Technology and Engineering, 12(17): 1671-1815(in Chinese with English abstract).
[31]	Hubbert, M.K., 1951. Mechanical Basis for Certain Familiar Geologic Structures.GSA Bulletin, 62(4): 355–372. doi:10.1130/0016-7606(1951)62[355:MBFCFG] 2.0.CO;2
[32]	Lenhardt, N., Omietimi, E.J., Edegbai, A.J., et al., 2024. Traversing the Rift: A Review of the Evolution of the West and Central African Rift System and its Economic Potential.Earth-Science Reviews, 104999. doi: 10.1016/j.earscirev.2024.104999
[33]	Li, Z.H., Cui, F.Y., Yang, S.T. et al., 2023. Key Geodynamic Processes and Driving Forces of Tethyan Evolution.Science China Earth Sciences, 66(12): 2666–2685(in Chinese with English abstract).
[34]	Liu, C.Z., Chung, S.L., Wu, F.Y., et al., 2016. Tethyan Suturing in Southeast Asia: Zircon U-Pb and Hf-O Isotopic Constraints from Myanmar Ophiolites.Geology, 44(4): 311–314. doi: 10.1130/G37342.1
[35]	Liu, H.F., 1993. Dynamic Classification of Sedimentary Basin and Their Structural Styles.Earth Science, 18(6):699-724+814(in Chinese with English abstract).
[36]	Lustrino, M., Melluso, L., Brotzu, P., et al., 2005. Petrogenesis of the Early Cretaceous Valle Chico Igneous Complex (SE Uruguay): Relationships with Paraná–Etendeka Magmatism.Lithos, 82(3): 407–434. doi: 10.1016/j.lithos.2004.07.004
[37]	Marzoli, A., Melluso, L., Morra, V., et al., 1999. Geochronology and Petrology of Cretaceous Basaltic Magmatism in the Kwanza Basin (Western Angola), and Relationships with the Paranà-Etendeka Continental Flood Basalt Province.Journal of Geodynamics, 28(4): 341–356. doi: 10.1016/S0264-3707(99)00014-9
[38]	Matos, R.M.D.D., Krueger, A., Norton, I. & Casey, K. 2021, The Fundamental role of the Borborema and Benin–Nigeria provinces of NE Brazil and NW Africa during the development of the South Atlantic Cretaceous Rift system,Marine and Petroleum Geology, 127: 104872. doi: 10.1016/j.marpetgeo.2020.104872
[39]	Min, G., Hou, G.T., 2019. Mechanism of the Mesozoic African rift system: Paleostress field modeling.Journal of Geodynamics, 132: 101655. doi: 10.1016/j.jog.2019.101655
[40]	Moulin, M., Aslanian, D., Unternehr, P., 2010. A new starting point for the South and Equatorial Atlantic Ocean.Earth-Science Reviews, 98(1–2): 1–37. doi: 10.1016/j.earscirev.2009.08.001
[41]	Qu, X.M., Wang, R.J., Xin, H.B., et al., 2012. Age and Petrogenesis of A-Type Granites in the Middle Segment of the Bangonghu–Nujiang Suture, Tbetan Plateau.Lithos, 146–147: 264–275. doi: 10.1016/j.lithos.2012.05.006
[42]	Scotese, C.R., 2014. Atlas of Plate Tectonic Reconstructions (Mollweide Projection). Volumes 1-6, Paleomap Project PaleoAtlas for ArcGIS, Paleomap Project, Evanston, IL. doi: 10.13140/2.1.1046.4967
[43]	Scotese, C.R., Vérard, C., Burgener, L., et al., 2025. The Cretaceous World: Plate Tectonics, Palaeogeography and Palaeoclimate.Geological Society, London, Special Publications, 544(1): 31–202. doi: 10.1144/SP544-2024-28
[44]	Segall, P., Pollard, D.D., 1980. Mechanics of Discontinuous Faults.Journal of Geophysical Research: Solid Earth, 85(B8): 4337–4350. doi: 10.1029/JB085iB08p04337
[45]	Sibson, R.H., 1985. A Note on Fault Reactivation.Journal of Structural Geology, 7(6): 751–754. doi: 10.1016/0191-8141(85)90150-6
[46]	Sibson, R.H., Xie, G., 1998. Dip Range for Intracontinental Reverse Fault Ruptures: Truth not Stranger than Friction?Bulletin of the Seismological Society of America, 88(4): 1014–1022. doi: 10.1785/BSSA0880041014
[47]	Simmons, N.A., Myers, S.C., Johannesson, G., et al., 2015. Evidence for Long-Lived Subduction of an Ancient Tectonic Plate Beneath the Southern Indian Ocean.Geophysical Research Letters, 42(21): 9270–9278. doi: 10.1002/2015GL066237
[48]	Song, Y.F., Dou, L.R., Cheng, D.S., et al., 2024. Driving Mechanism of Tectonic Inversion in Intra-Plate Rift Basins and its Impact on Oil: A Case Study of the Bongor Basin in Central Africa. Geological Review, 70(S1): 239–240(in Chinese with English abstract).
[49]	Stampfli, G.M., Borel, G.D., 2002. A Pplate Tectonic Model for the Paleozoic and Mesozoic Constrained by Dynamic Plate Boundaries and Restored Synthetic Oceanic Isochrons.Earth and Planetary Science Letters, 196(1): 17–33. doi: 10.1016/S0012-821X(01)00588-X
[50]	Sun, W.D., Liu, L.J., Hu, Y.B., et al., 2018. Post-Ridge-Subduction Acceleration of the Indian Plate Induced by Slab Rollback.Solid Earth Sciences, 3(1): 1–7. doi: 10.1016/j.sesci.2017.12.003
[51]	Tian, N.X., Xie, X.N., Sun, Q.L., et al., 2023. Formation Evolution and Structural Architectures of Conjugated Continental Margin Basins in the Equatorial Segment of South Atlantic. Earth Science, 1-15(in Chinese with English abstract).
[52]	Turner, J.P., Williams, G.A., 2004. Sedimentary Basin Inversion and Intra-Plate Shortening.Earth-Science Reviews, 65(3–4): 277–304. doi: 10.1016/j.earscirev.2003.10.002
[53]	Wan, B., Wu, F.Y., Chen, L., et al., 2019. Cyclical One-Way Continental Rupture-Drift in the Tethyan Evolution: Subduction-Driven Plate Tectonics.Science China Earth Sciences, 62(12): 2005–2016. doi: 10.1007/s11430-019-9393-4
[54]	Wang, E.Q., Meng, K., Xu, G., 2018. Cenozoic Two-Stage Obduction of the Indian Subcontinent: On the Interaction between the Indian Ocean, Tethyan and Eurasian Plates.Acta Petrologica Sinica,34( 7) : 1867 - 1875(in Chinese with English abstract).
[55]	Wang, H.X., Lv, T.F., Fu, X.F., et al., 2012. Formation, Evolution and Reservoir-Controlling Mechanism of Relay Zone in Rift Basin.Geological Science and Technology Information, 32(4): 102–110(in Chinese with English abstract).
[56]	Wang, L., Zhang, X.S., Xiao, K.Y., et al., 2022. Formation and Evolution of Baobab Structural Zone and Controlling Factors of Hydrocarbon Accumulation in Bongor Basin, Chad.China Petroleum Exploration, 27(2):84-92(in Chinese with English abstract).
[57]	Wang, W.L., Yang, J.G., Sun, Q.Q., et al., 2017. Research Progress and Development Trends of the Transfer Zone.Geology and Resources, 26(2): 195-202(in Chinese with English abstract).
[58]	Xiao, K.Y., Zhao, J., Yu, Z.H., et al., 2014. Structural Characteristics of Intensively Inversed Bongor Basin in CARS and their Impacts on Hydrocarbon Accumulation.Earth Science Frontiers, 21(3):172-180(in Chinese with English abstract).
[59]	Xu, C.C., 2012. The Characteristics of Inversion Structures in Bongor Basin and its Relationship with Hydrocarbon Accumulation. Beijing, China University of Geosciences (Beijing) (in Chinese with English abstract).
[60]	Yang, S.T., Li, Z.H., Wan, B., et al., 2021. Subduction-Induced Back-Arc Extension Versus Far-Field Stretching: Contrasting Modes for Continental Marginal Break-Up.Geochemistry, Geophysics, Geosystems, 22(3): e2020GC009416. doi: 10.1029/2020GC009416
[61]	Yu, Z.H., Xiao, K.Y., Zhang, G.L., et al., 2018. Analysis on Inverted Structure Characteristics and its Forming Mechanism in the Bongor Basin, Chad.China Petroleum Exploration, 23(3):90-98(in Chinese with English abstract).
[62]	Zhu, R.X., Zhao, P., Zhao, L., 2021. Tectonic Evolution and Geodynamics of the Neo-Tethys Ocean.Science China Earth Sciences, 52(1): 1–25(in Chinese with English abstract).
[63]	余朝华, 肖坤叶, 张桂林, 等 2018, 乍得Bongor盆地反转构造特征及形成机制分析, 中国石油勘探, 23(3): 90–98.
[64]	宋一帆, 窦立荣, 程顶胜, 等 2024, 板内裂谷盆地构造反转驱动机制以及对油气的影响--以中非Bongor盆地为例, 地质论评, 70(S1): 239–240. 2
[65]	朱日祥, 赵盼, 赵亮, 2021, 新特提斯洋演化与动力过程, 中国科学: 地球科学, 52(1): 1–25.
[66]	李忠海, 崔峰源, 杨舒婷, 等 2023, 特提斯演化的关键动力学过程与驱动力, 中国科学: 地球科学, 53(12): 2701–2722.
[67]	王二七, 孟恺, 许光, 等 2018, 印度陆块新生代两次仰冲事件及其构造驱动机制:论印度洋、特提斯和欧亚板块相互作用, 岩石学报, 34(7): 1867–1875.
[68]	王利, 张新顺, 肖坤叶, 等 2022, 乍得邦戈盆地Baobab构造带形成演化及油气成藏控制因素, 中国石油勘探, 27(2): 84–92.
[69]	王海学, 吕延防, 付晓飞, 等 2013, 裂陷盆地转换带形成演化及其控藏机理, 地质科技情报, 32(4): 102–110.
[70]	窦立荣, 王景春, 王仁冲, 等 2018, 中非裂谷系前寒武系基岩油气成藏组合, 地学前缘, 25(2): 15–23.
[71]	窦立荣, 肖坤叶, 胡勇, 等 2011, 乍得Bongor盆地石油地质特征及成藏模式, 石油学报, 32(3): 379–386.
[72]	肖坤叶, 赵健, 余朝华, 等 2014, 中非裂谷系Bongor盆地强反转裂谷构造特征及其对油气成藏的影响, 地学前缘, 21(3): 172–180.
[73]	许长春 2012, Bongor盆地反转构造特征及其与油气聚集关系, 北京, 中国地质大学(北京).
[74]	陈志刚, 徐刚, 王景春, 等 2016, 乍得Bongor盆地东、西部构造特征差异及其对油气富集的影响, 石油地球物理勘探, 51(S1): 113–119, 9.
[75]	高华华, 杜业波, 王林, 等 2023, 乍得Doseo盆地东部构造特征、成因机制与盆地演化, 石油勘探与开发, 50(5): 1003–1015.
[76]	黄超, 余朝华, 肖高杰, 等 2012, 中西非裂谷系B盆地构造演化及其对油气成藏的影响研究, 科学技术与工程, 12(17): 1671-1815.
[77]	王文龙, 杨济广, 孙乔琪, 等 2017, 构造转换带研究进展与发展趋势, 地质与资源, 26(2): 195-202.
[78]	刘和甫, 1993, 沉积盆地地球动力学分类及构造样式分析, 地球科学, 18(6): 699-724+814.
[79]	田纳新,解习农,孙启良,等 2023,南大西洋赤道段两岸共轭陆缘盆地形成演化及结构差异,地球科学,1-15.

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中非剪切背景下裂陷盆地的发育机制：以Bongor盆地为例

doi: 10.3799/dqkx.2025.172

作者简介:
肖坤叶（1969—），男，教授级高级工程师，博士，主要从事海外油气勘探､资源评价与油气地质综合研究。E-mail:xiaokunye@petrochina.com.cn，ORCID:

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Formation Mechanism of Rift Basins in the Central African Strike-Slip Tectonic Setting: A Case Study of the Bongor Basin

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留言板

中非剪切背景下裂陷盆地的发育机制：以Bongor盆地为例

doi: 10.3799/dqkx.2025.172

作者简介: 肖坤叶（1969—），男，教授级高级工程师，博士，主要从事海外油气勘探､资源评价与油气地质综合研究。E-mail:xiaokunye@petrochina.com.cn，ORCID:

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出版历程

Formation Mechanism of Rift Basins in the Central African Strike-Slip Tectonic Setting: A Case Study of the Bongor Basin

计量

出版历程

目录

作者简介:
肖坤叶（1969—），男，教授级高级工程师，博士，主要从事海外油气勘探､资源评价与油气地质综合研究。E-mail:xiaokunye@petrochina.com.cn，ORCID: