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Formation of the Zengmu and Beikang Basins, and West Baram Line in the southwestern South China Sea margin

  • Geomorphology and geological structure of South China Sea
  • Published:
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Abstract

The Zengmu and Beikang Basins, separated by the West Baram Line (WBL) in the southwestern South China Sea margin, display distinct geological and geophysical features. However, the nature of the basins and the WBL are debated. Here we explore this issue by conducting the stratigraphic and structural interpretation, faults and subsidence analysis, and lithospheric finite extension modelling using seismic data. Results show that the WBL is a trans-extensional fault zone comprising normal faults and flower structures mainly active in the Late Eocene to Early Miocene. The Zengmu Basin, to the southwest of the WBL, shows an overall synformal geometry, thick folded strata in the Late Eocene to Late Miocene (40.4–5.2 Ma), and pretty small normal faults at the basin edge, which imply that the Zengmu Basin is a foreland basin under the Luconia and Borneo collision in the Sarawak since the Eocene. Furthermore, the basin exhibits two stages of subsidence (fast in 40.4–30 Ma and slow in 30–0 Ma); but the amount of observed subsidence and heat flow are both greater than that predicted by crustal thinning. The Beikang Basin, to the NE of the WBL, consists of the syn-rift faulted sub-basins (45–16.4 Ma) and the post-rift less deformed sequences (16.4–0 Ma). The heat flow (∼60 mW/m2) is also consistent with that predicted based on crustal thinning, inferring that it is a rifted basin. However, the basin shows three stages of subsidence (fast in 45–30 Ma, uplift in 30–16.4 Ma, and fast in 16.4–0 Ma). In the uplift stage, the strata were partly folded in the Late Oligocene and partly eroded in the Early Miocene, which is probably caused by the flexural bulging in response to the paleo-South China Sea subduction and the subsequent Dangerous Grounds and Borneo collision in the Sabah to the east of the WBL.

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Data Availability Statement

All data generated and/or analyzed during this study are available from the corresponding author upon reasonable request.

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Acknowledgment

Thank Editor in Chief and the anonymous reviewers for the valuable and constructive comments to improve the manuscript.

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Authors and Affiliations

  1. Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, 511458, China

    Bing Han, Zhongxian Zhao, Xiaofang Wang, Zhen Sun & Fucheng Li

  2. Key Laboratory of Marine Mineral Resources, Ministry of Natural Resources, Guangzhou, 511458, China

    Bing Han, Benduo Zhu, Yongjian Yao, Liqiang Liu & Tianyue Peng

  3. Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou, 511458, China

    Bing Han, Zhongxian Zhao, Xiaofang Wang, Zhen Sun & Fucheng Li

  4. Guangzhou Marine Geological Survey, China Geological Survey, Guangzhou, 511458, China

    Bing Han, Benduo Zhu, Yongjian Yao, Liqiang Liu & Tianyue Peng

  5. University of Chinese Academy of Sciences, Beijing, 100049, China

    Bing Han

  6. Hainan Key Laboratory of Marine Geological Resources and Environment, Haikou, 570206, China

    Genyuan Long

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  1. Bing Han
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Correspondence to Zhongxian Zhao.

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Supported by the Youth Innovation Promotion Association CAS, the National Key Research and Development Program of China (No. 2021YFC3100604), the Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) (No. GML2019ZD0205), the Guangzhou Municipal Science and Technology Program (No. 201904010285), the K. C. Wong Education Foundation (No. GJTD-2018-13), the Hainan Key Laboratory of Marine Geological Resources and Environment (No. HNHYDZZYHJKF003), the China Geological Survey (No. DD20190378), and the National Natural Science Foundation of China (No. 42076077)

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Han, B., Zhao, Z., Wang, X. et al. Formation of the Zengmu and Beikang Basins, and West Baram Line in the southwestern South China Sea margin. J. Ocean. Limnol. 41, 592–611 (2023). https://doi.org/10.1007/s00343-022-1430-9

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