Controls on Faulted Sub-Depression Patterns in Continental Rifted Basins: The Beier Depression, Hailar Basin, Northeastern China

Authors

  • Fangju Chen

    1. State Key Laboratory of Continental Shale Oil, Daqing 163712, China; 2. Exploration and Development Research Institute of PetroChina Daqing Oilfield Company Limited, Daqing 163712, China
  • Ya Tian

    1. State Key Laboratory of Continental Shale Oil, Daqing 163712, China; 2. Exploration and Development Research Institute of PetroChina Daqing Oilfield Company Limited, Daqing 163712, China
  • Gang Li

    Sanya Offshore Oil & Gas Research Institute, Northeast Petroleum University, Sanya 572025, China
  • Yougong Wang

    Sanya Offshore Oil & Gas Research Institute, Northeast Petroleum University, Sanya 572025, China
  • Huaye Liu

    1. State Key Laboratory of Continental Shale Oil, Daqing 163712, China; 2. Exploration and Development Research Institute of PetroChina Daqing Oilfield Company Limited, Daqing 163712, China
  • Yue Zou

    1. State Key Laboratory of Continental Shale Oil, Daqing 163712, China; 2. Exploration and Development Research Institute of PetroChina Daqing Oilfield Company Limited, Daqing 163712, China
  • Mengxia Li

    1. State Key Laboratory of Continental Shale Oil, Daqing 163712, China; 2. Exploration and Development Research Institute of PetroChina Daqing Oilfield Company Limited, Daqing 163712, China

DOI:

https://doi.org/10.30564/jees.v7i5.8543
Received: 23 January 2025 | Revised: 21 February 2025 | Accepted: 26 February 2025 | Published Online: 6 May 2025

Abstract

In contrast to well-studied rift basins in NE China, the Hailar Basin has received relatively less attention regarding the combined patterns of different types of grabens and half-grabens. This study aims to explore whether the combined patterns of grabens in the Hailar Basin exhibit similar characteristics to those in other NE China rift basins and to identify the underlying causes. To achieve this, a comprehensive analysis of the major fault systems and the combined patterns of faulted sub-depressions, as well as their controlling mechanisms, was conducted. This analysis utilized the latest 3D seismic data that cover nearly the entire Beier Depression. Three groups of pre-existing fault systems were observed in the basement of the Beier Depression, and they are the NEE-EW-trending fault systems, the NE-trending fault systems, and the NW-trending fault systems. The NEE-EW-trending fault systems were distributed in the central part of the Beier Depression and primarily controlled the sedimentary filling of the Tongbomiao and the Lower Nantun Formations. The NE-trending fault systems were distributed in the southwestern part of the Beier Depression and primarily controlled the sedimentary filling of the Upper Nantun Formations. The NW-trending fault systems were distributed rarely in the Beier Depression. Five kinds of combined patterns of the sub-depressions were developed in the Beier Depression, and they are the parallel, en echelon, face-to-face, back-to-back, and S-shaped combined patterns. They were controlled by the NEE-EW-trending and the NE-trending fault systems with different orientations, arrangements, and activation sequences.

Keywords:

NE China; Hailar Basin; Beier Depression; Combined Pattern of Sub-Depressions; Continental Rift Basin

References

[1] Min, A, Na, N., Zhang, F., et al., 2013. Early Cretaceous provenance change in the southern Hailar Basin, northeastern China and its implication for basin evolution. Cretaceous Research. 40, 21–42.

[2] Agostini, A., Corti, G., Zeoli, A., et al., 2009. Evolution, pattern, and partitioning of deformation during oblique continental rifting: Inferences from lithospheric-scale centrifuge models. Geochemistry, Geophysics, Geosystems. 10(11), 154–163.

[3] Bird, P.C., Cartwright, J.A., Davies, T.L., 2015. Basement reactivation in the development of rift basins; an example of reactivated Caledonide structures in the West Orkney Basin. Journal of the Geological Society. 172(1), 77–85.

[4] Bramham, E.K., Wright, T.J., Paton, D.A., et al., 2021. A new model for the growth of normal faults developed above pre-existing structures. Geology. 49(5), 587–591.

[5] Brune, S., Autin, J., 2013. The rift to break-up evolution of the Gulf of Aden: Insights from 3D numerical lithospheric-scale modelling. Tectonophysics. 607, 65–79.

[6] Brune, S., Williams, S.E., Müller, R.D., 2018. Oblique rifting: The rule, not the exception. Solid Earth. 9(5), 1187–1206.

[7] Cheng, Y., Wu, Z., Su, W., et al., 2023. Basement structures exert a crucial influence on the structural configuration of later rift development: Insights from the Shanan and Chengbei depression, Bohai Bay Basin. Marine and Petroleum Geology. 153, 106272.

[8] Cogné, J.P., Kravchinsky, V.A., Halim, N., et al., 2005. Late Jurassic-Early Cretaceous closure of the Mongol-Okhotsk Ocean demonstrated by new Mesozoic palaeomagnetic results from the Trans-Baikal area (SE Siberia). Geophysical Journal International. 163(2), 813–832.

[9] Collanega, L., Siuda, K., Jackson, C.A.L., et al., 2019. Normal fault growth influenced by basement fabrics: The importance of preferential nucleation from pre-existing structures. Basin Research. 31(4), 659–687.

[10] Corti, G., Calignano, E., Petit, C., et al., 2011. Controls of lithospheric structure and plate kinematics on rift architecture and evolution: An experimental modeling of the Baikal rift. Tectonics. 30(3).

[11] Corti, G., Cioni, R., Franceschini, Z., et al., 2019. Aborted propagation of the Ethiopian rift caused by linkage with the Kenyan rift. Nature Communications. 10(1), 1309.

[12] Deng, H., McClay, K., 2019. Development of extensional fault and fold system: Insights from 3D seismic interpretation of the Enderby Terrace, NW Shelf of Australia. Marine and Petroleum Geology. 104, 11–28.

[13] Dong, S., Zhang, Y., Li, H., et al., 2018. The Yanshan orogeny and late Mesozoic multi-plate convergence in East Asia-Commemorating 90th years of the “Yanshan Orogeny”. Science China Earth Sciences. 61, 1888–1909.

[14] Fazlikhani, H., Fossen, H., Gawthorpe, R.L., et al., 2017. Basement structure and its influence on the structural configuration of the northern North Sea Rift. Tectonics. 36(6), 1151–1177.

[15] Gouiza, M., Naliboff, J., 2021. Rheological inheritance controls the formation of segmented rifted margins in cratonic lithosphere. Nature Communications. 12(1), 4653.

[16] Gu, C., Zhu, G., Zhang, S., et al., 2017. Cenozoic evolution of the Yilan-Yitong Graben in NE China: An example of graben formation controlled by pre-existing structures. Journal of Asian Earth Sciences. 146, 168–184.

[17] Guan, W., Huang, L., Liu, C., et al., 2023. Interactions between preexisting structures and rift faults: Implications for basin geometry in the northern South China Sea. Basin Research. 1–27.

[18] Heron, P.J., Peace, A.L., McCaffrey, K.J.W., et al., 2019. Segmentation of rifts through structural inheritance; creation of the Davis Strait. Tectonics. 38(7), 2411–2430.

[19] Henstra, G.A., Kristensen, T.B., Rotevatn, A., et al., 2019. How do pre-existing normal faults influence rift geometry? A comparison of adjacent basins with contrasting underlying structure on the Lofoten Margin, Norway. Basin Research. 31(6), 1083–1097.

[20] Ji, Z., Meng, Q., Wan, C., et al., 2019a. Generation of late Mesozoic felsic volcanic rocks in the Hailar Basin, northeastern China in response to overprinting of multiple tectonic regimes. Scientific Reports. 9(1), 15854.

[21] Ji, Z., Meng, Q.A., Wan, C.B., et al., 2019b. Geodynamic evolution of flat-slab subduction of Paleo-Pacific Plate: Constraints from Jurassic adakitic lavas in the Hailar Basin, NE China. Tectonics. 38(12), 4301–4319.

[22] Ji, Z., Wan, C.B., Meng, Q.A., et al., 2020. Chronostratigraphic framework of late Mesozoic terrestrial strata in the Hailar-Tamtsag Basin, Northeast China, and its geodynamic implication. Geological Journal. 55(7), 5197–5215.

[23] Jia, J., Tao, S., Fang, X., et al., 2021. Deep Jurassic volcano-sedimentary succession, reservoir-seal assemblage and their exploration significance in Northeast China: A case study of Jurassic in the Hailar Basin. Acta Geologica Sinica. 95(2), 377–395.

[24] Keranen, K., Klemperer, S.L., 2008. Discontinuous and diachronous evolution of the Main Ethiopian Rift: Implications for development of continental rifts. Earth and Planetary Science Letters. 265(1–2), 96–111.

[25] Kolawole, F., Firkins, M., Al-Wahaibi, T.S., et al., 2021. Rift interaction zones and the stages of rift linkage in active segmented continental rift systems. Basin Research. 33(6), 2984–3020.

[26] Kravchinsky, V.A., Jean-Pascal, C., Harbert, W.P., et al., 2002. Evolution of the Mongol-Okhotsk ocean as constrained by new palaeomagnetic data from the Mongol-Okhotsk suture zone, Siberia. Geophysical Journal International. 148 (1), 34–57.

[27] Li, G., Mei, L., Ye, Q., et al., 2023. Post-rift faulting controlled by different geodynamics in the Pearl River Mouth Basin, northern South China Sea margin. Earth-Science Reviews. 237, 104311.

[28] Li, S.C., Liu, Z.H., Xu, Z.Y., et al., 2015. Age and tectonic setting of volcanic rocks of the Tamulangou Formation in the Great Xing’an Range, NE China. Journal of Asian Earth Sciences. 113, 471–480.

[29] Liu, S., Fu, X., Wang, Y., et al., 2020. Depression evolution in muti-phase rifts: Case study on the Paleogene of Qikou Depression. Chinese Journal of Geology. 55(1), 81–92.

[30] Liu, Z.H., Wan, C.B., Ren, Y.G., et al., 2006. Geological features and the rule of oil and gas accumulation of Wurxun-Beier Subbasin in Hailaer Basin. Journal of Jilin University. 36, 527–534.

[31] Luo, J., Sun, Y., Wang, Y., et al., 2021. Cenozoic tectonic evolution of the eastern Liaodong Bay sub-basin, Bohai Bay basin, eastern China-Constraints from seismic data. Marine and Petroleum Geology. 134, 105346.

[32] Manatschal, G., Lavier, L., Chenin, P., 2015. The role of inheritance in structuring hyperextended rift systems: Some considerations based on observations and numerical modeling. Gondwana Research. 27(1), 140–164.

[33] McClay, K.R., White, M.J., 1995. Analogue modelling of orthogonal and oblique rifting. Marine and Petroleum Geology. 12, 137–151.

[34] Meng, E., Xu, W.L., Yang, D.B., et al., 2011. Zircon U-Pb chronology, geochemistry of Mesozoic volcanic rocks from the Lingquan basin in Manzhouli area, and its tectonic implications. Acta Petrologica Sinica. 27(4), 1209–1226.

[35] Meng, Q.R., 2003. What drove late Mesozoic extension of northern China-Mongolia tract? Tectonophysics. 369, 155–174

[36] Meng, Q., Zhu, D., Chen, J., et al., 2012. Styles of complex faulted depressions in rifting basin and its significance for petroleum geology: An example from Hailar-Tamtsag Early Cretaceous Basin. Earth Science Frontiers. 19(5), 76–85.

[37] Meng, Q.A., Wan, C.B., Zhu, D.F., 2013. Age assignment and geological significance of the ‘Budate Group’ in the Hailar Basin. Science China: Earth Sciences. 56, 970–979.

[38] Morley, C.K., 2014. The widespread occurrence of low-angle normal faults in a rift setting: Review of examples from Thailand, and implications for their origin and evolution. Earth-Science Reviews. 133, 18–42.

[39] Muirhead, J.D., Kattenhorn, S.A., 2018. Activation of preexisting transverse structures in an evolving magmatic rift in East Africa. Journal of Structural Geology. 106, 1–18.

[40] Odepressioniede, E.E., Rotevatn, A., Gawthorpe, R., et al., 2020. Pre-existing intrabasement shear zones influence growth and geometry of noncolinear normal faults, western Utsira High–Heimdal Terrace, North Sea. Journal of Structural Geology. 130, 103908.

[41] Parfenov, L.M., Popeko, L.I., Tomurtogoo, O., 2001. Problems of tectonics of the Mongol-Okhotsk orogenic belt. Geology of the Pacific Ocean. 16, 797–830.

[42] Phillips, T.B., Fazlikhani, H., Gawthorpe, R.L.,et al., 2019. The influence of structural inheritance and multiphase extension on rift development, the northern North Sea. Tectonics. 38(12), 4099–4126.

[43] Pichel, L.M., Antunes, A.F., Fossen, H., et al., 2023. The interplay between basement fabric, rifting, syn-rift folding, and inversion in the Rio do Peixe Basin, NE Brazil. Basin Research. 35(1), 61–85.

[44] Jian, Ren., Dingyou, L.Y.U., Xingpeng, C.H.E.N., et al., 2019. Oblique extension of pre-existing structures and its control on oil accumulation in eastern Bohai Sea. Petroleum Exploration and Development. 46(3), 553–564.

[45] Rotevatn, A., Kristensen, T.B., Ksienzyk, A.K., et al., 2018. Structural inheritance and rapid rift‐length establishment in a multiphase rift: The East Greenland rift system and its Caledonian orogenic ancestry. Tectonics. 37(6), 1858–1875.

[46] Rotevatn, A., Jackson, C.A.L., Tvedt, A.B., et al., 2019. How do normal faults grow?. Journal of Structural Geology. 125, 174–184.

[47] Salazar-Mora, C.A., Huismans, R.S., Fossen, H., et al., 2018. The Wilson cycle and effects of tectonic structural inheritance on rifted passive margin formation. Tectonics. 37(9), 3085–3101.

[48] Samsu, A., Micklethwaite, S., Williams, J.N., et al., 2023. Structural inheritance in amagmatic rift basins: Manifestations and mechanisms for how pre-existing structures influence rift-related faults. Earth-Science Reviews. 246, 104568.

[49] Scholz, C.A., Shillington, D.J., Wright, L.J.M., et al., 2020. Intrarift fault fabric, segmentation, and basin evolution of the Lake Malawi (Nyasa) Rift, East Africa. Geosphere. 16(5), 1293–1311.

[50] Shaban, S.N., Kolawole, F., Scholz, C.A., 2023. The deep basin and underlying basement structure of the Tanganyika Rift. Tectonics. 42(7), e2022TC007726.

[51] Song, J., Liu, Z., Wang, C., et al., 2019. Multistage structural deformations of a superimposed basin system and its tectonic response to regional geological evolution: A case study from the Late Jurassic-Early Cretaceous Tanan depression, Hailar-Tamtsag basin. Marine and Petroleum Geology. 110, 1–20.

[52] Sorokin, A.A., Kudryashov, N.M., Sorokin, A.P., 2005. Late Paleozoic Urusha Magmatic Complex in the southern framing of the Mongolia-Okhotsk Belt (Amur Region): Age and geodynamic setting. Petrology. 13, 596–610.

[53] Sun, W., Zhang, L., 2022. Preface: Pacific plate subduction and the Yanshanian movement in Eastern China. Journal of Earth Science. 33(3), 541–543.

[54] Tang, J., Xu, W.L., Wang, F., et al., 2015. Geochronology, geochemistry, and deformation history of Late Jurassic-Early Cretaceous intrusive rocks in the Erguna Massif, NE China: constraints on the Late Mesozoic tectonic evolution of the Mongol-Okhotsk orogenic belt. Tectonophysics. 658, 91–110.

[55] Tong, H., Koyi, H., Huang, S., et al., 2014. The effect of multiple pre-existing weaknesses on formation and evolution of faults in extended sandbox models. Tectonophysics. 626, 197–212.

[56] Walsh, J.J., Nicol, A., Childs, C., 2002. An alternative model for the growth of faults. Journal of Structural Geology. 24(11), 1669–1675.

[57] Wan, C.B., 2006. Cretaceous Palynological Flora in Hailar Basin [PhD thesis]. Changchun, China: Jilin University. pp. 1–209.

[58] Wang, D., Li, P., Shan, X., et al., 2019. Seismic evidence for nappes in basins west of the Da Hinggan Mountains. Chinese Journal of Geophysics. 62(3), 1129–1138.

[59] Wang, D., Zhang, X., Yang, L., et al., 2022. Influence of pre-existing faults on Cenozoic structures in the Chengbei depression and the Wuhaozhuang area, Bohai Bay Basin, East China. Marine and Petroleum Geology. 138, 105539.

[60] Wang, T., Guo, L., Zhang, L., et al., 2015. Timing and evolution of Jurassic-Cretaceous granitoid magmatisms in the Mongol-Okhotsk belt and adjacent areas, NE Asia: Implications for transition from contractional crustal thickening to extensional thinning and geodynamic settings. Journal of Asian Earth Sciences. 97, 365–392.

[61] Wang, Y., Lu, Y., Fu, G., et al., 2014. Structure features and natural gas enrichment regularity in Changling fault depression groups. Oil Geophysical Prospecting. 49(6), 1204–1212.

[62] Wu, L., Mei, L., Paton, D.A., et al., 2020. Basement structures have crucial influence on rift development: Insights from the Jianghan Basin, Central China. Tectonics. 39(2), e2019TC005671.

[63] Wu, L., Shen, C., Paton, D A., et al., 2023. A rift-scale view at strain partitioning during multiphase rifting: Insights from the Hailar Basin, northeast Asia. Basin Research. 00, 1–24

[64] Wu, L., Shen, C., Paton, D.A., et al., 2024. Rift segmentation caused by reactivation of multiple basement structure systems: Evidence from the Hailar-Tamtsag Rift, Northeast Asia. Basin Research. 36, e12841.

[65] Xu, M.J., Xu, W.L. Meng, E., 2011. LA-ICP-MS zircon U-Pb chronology and geochemistry of Mesozoic volcanic rocks from the Shanghulin-Xiangyang basin in Ergun area, northeastern Inner Mongolia. Geological Bulletin of China. 30, 1321–1338.

[66] Yang, G., Yin, H., Gan, J., et al., 2022. Explaining structural difference between the eastern and western zones of the Qiongdongnan Basin, northern South China Sea: Insights from scaled physical models. Tectonics. 41(2), e2021TC006899.

[67] Yang, Y., Guo, Z., Song, C., et al., 2015. A short-lived but significant Mongol-Okhotsk collisional orogeny in latest Jurassic-earliest Cretaceous. Gondwana Research. 28(3), 1096–1116.

[68] Yi, Z., Meert, J.G., 2020. A closure of the Mongol-Okhotsk Ocean by the Middle Jurassic: Reconciliation of paleomagnetic and geological evidence. Geophysical Research Letters. 47(15), e2020GL088235.

[69] Zhang, F., Dilek, Y., Chen, H., et al., 2017. Structural architecture and stratigraphic record of Late Mesozoic sedimentary basins in NE China: Tectonic archives of the Late Cretaceous continental margin evolution in East Asia. Earth-Science Reviews. 171, 598–620.

[70] Zhang, J.H., Ge, W.C., Wu, F.Y., 2006. Mesozoic bimodal volcanic suite in Zhalantun of the Da Hinggan Range and its geological significance: Zircon U-Pb age and Hf isotopic constraints. Acta Geologica Sinica-English Edition. 80, 58–69.

[71] Zhang, K., Deng, B., Zhang, F., et al., 2016. Determination of early stage of Early Cretaceous compressive event in Hailar Basin, NE China, and its tectonic significance. Earth Science-Journal of China University of Geosciences. 41(7), 1141–1155.

[72] Zhang, Y., Dong, S., 2019. East Asia multi-plate convergence in Late Mesozoic and the development of continental tectonic systems. Journal of Geomechanics. 25(5), 613–641.

[73] Zhang, Y., Qiu, E., Dong, S., et al., 2022. Late Mesozoic intracontinental deformation and magmatism in North and NE China in response to multi-plate convergence in NE Asia: An overview and new view. Tectonophysics. 835, 229377.

[74] Zhao, P., Xu, B., Chen, Y., 2023. Evolution and final closure of the Mongol-Okhotsk Ocean. Science China Earth Sciences. 66(11), 2497–2513.

[75] Zhao, X.Z., Jin, F.M., Qi, J.F., et al., 2015. The structural types and petroleum geological significance of Early Cretaceous complex faulted depression in Erlian Basin. Natural Gas Geoscience. 26(7), 1289–1298.

[76] Zheng, C.Q., Zhou, J.B., Jin, W., 2009. Geochronology in the north segment of the Derbugan fault zone, Great Xing’an Range, NE China. Acta Petrologica Sinica. 25, 1989–2000.

[77] Zhou, J., Li, L., 2017. The Mesozoic accretionary complex in Northeast China: Evidence for the accretion history of Paleo-Pacific subduction. Journal of Asian Earth Sciences. 145, 91–100.

[78] Zhou, Y., Ji, Y.L., Pigott, J.D., et al., 2014. Tectono-stratigraphy of Lower Cretaceous Tanan sub-basin, Tamtdepression Basin, Mongolia: Sequence architecture, depositional systems and controls on sediment infill. Marine and Petroleum Geology 49, 176–202.

[79] Zwaan, F., Schreurs, G., 2017. How oblique extension and structural inheritance influence rift segment interaction: Insights from 4D analog models. Interpretation. 5(1), SD119–SD138.

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How to Cite

Chen, F., Tian, Y., Li, G., Wang, Y., Liu, H., Zou, Y., & Li, M. (2025). Controls on Faulted Sub-Depression Patterns in Continental Rifted Basins: The Beier Depression, Hailar Basin, Northeastern China. Journal of Environmental & Earth Sciences, 7(5), 188–202. https://doi.org/10.30564/jees.v7i5.8543

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Vol. 7 , Iss. 5 (May 2025)

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Copyright © 2025 Fangju Chen, Ya Tian, Gang Li, Yougong Wang, Huaye Liu, Yue Zou, Mengxia Li

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This is an open access article under the Creative Commons Attribution-NonCommercial 4.0 International (CC BY-NC 4.0) License.

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