Formation of the Zengmu and Beikang Basins, and West Baram Line in the southwestern South China Sea margin
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...
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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/m
2
) 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. |
|---|---|
| AbstractList | 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. 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/m 2 ) 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. 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. 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. |
| Author | Peng, Tianyue Zhao, Zhongxian Yao, Yongjian Li, Fucheng Long, Genyuan Wang, Xiaofang Liu, Liqiang Sun, Zhen Han, Bing Zhu, Benduo |
| AuthorAffiliation | Key Laboratory of Ocean and Marginal Sea Geology,South China Sea Institute of Oceanology,Chinese Academy of Sciences,Guangzhou 511458,China;Key Laboratory of Marine Mineral Resources,Ministry of Natural Resources,Guangzhou 511458,China;Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou),Guangzhou 511458,China;Guangzhou Marine Geological Survey,China Geological Survey,Ministry of Natural Resources,Guangzhou 511458,China;University of Chinese Academy of Sciences,Beijing 100049,China%Key Laboratory of Ocean and Marginal Sea Geology,South China Sea Institute of Oceanology,Chinese Academy of Sciences,Guangzhou 511458,China;Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou),Guangzhou 511458,China%Key Laboratory of Marine Mineral Resources,Ministry of Natural Resources,Guangzhou 511458,China;Guangzhou Marine Geological Survey,China Geological Survey,Ministry of Natural Resources,Guangzhou 511458,China%Hainan Key Laboratory of Marine Geological Resource |
| AuthorAffiliation_xml | – name: Key Laboratory of Ocean and Marginal Sea Geology,South China Sea Institute of Oceanology,Chinese Academy of Sciences,Guangzhou 511458,China;Key Laboratory of Marine Mineral Resources,Ministry of Natural Resources,Guangzhou 511458,China;Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou),Guangzhou 511458,China;Guangzhou Marine Geological Survey,China Geological Survey,Ministry of Natural Resources,Guangzhou 511458,China;University of Chinese Academy of Sciences,Beijing 100049,China%Key Laboratory of Ocean and Marginal Sea Geology,South China Sea Institute of Oceanology,Chinese Academy of Sciences,Guangzhou 511458,China;Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou),Guangzhou 511458,China%Key Laboratory of Marine Mineral Resources,Ministry of Natural Resources,Guangzhou 511458,China;Guangzhou Marine Geological Survey,China Geological Survey,Ministry of Natural Resources,Guangzhou 511458,China%Hainan Key Laboratory of Marine Geological Resources and Environment,Haikou 570206,China |
| Author_xml | – sequence: 1 givenname: Bing surname: Han fullname: Han, Bing organization: Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Key Laboratory of Marine Mineral Resources, Ministry of Natural Resources, Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou Marine Geological Survey, China Geological Survey, University of Chinese Academy of Sciences – sequence: 2 givenname: Zhongxian surname: Zhao fullname: Zhao, Zhongxian email: zxzhao@scsio.ac.cn organization: Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) – sequence: 3 givenname: Xiaofang surname: Wang fullname: Wang, Xiaofang organization: Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) – sequence: 4 givenname: Zhen surname: Sun fullname: Sun, Zhen organization: Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) – sequence: 5 givenname: Fucheng surname: Li fullname: Li, Fucheng organization: Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) – sequence: 6 givenname: Benduo surname: Zhu fullname: Zhu, Benduo organization: Key Laboratory of Marine Mineral Resources, Ministry of Natural Resources, Guangzhou Marine Geological Survey, China Geological Survey – sequence: 7 givenname: Yongjian surname: Yao fullname: Yao, Yongjian organization: Key Laboratory of Marine Mineral Resources, Ministry of Natural Resources, Guangzhou Marine Geological Survey, China Geological Survey – sequence: 8 givenname: Liqiang surname: Liu fullname: Liu, Liqiang organization: Key Laboratory of Marine Mineral Resources, Ministry of Natural Resources, Guangzhou Marine Geological Survey, China Geological Survey – sequence: 9 givenname: Tianyue surname: Peng fullname: Peng, Tianyue organization: Key Laboratory of Marine Mineral Resources, Ministry of Natural Resources, Guangzhou Marine Geological Survey, China Geological Survey – sequence: 10 givenname: Genyuan surname: Long fullname: Long, Genyuan organization: Hainan Key Laboratory of Marine Geological Resources and Environment |
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| CitedBy_id | crossref_primary_10_1007_s00343_023_3403_2 crossref_primary_10_1016_j_earscirev_2024_105028 crossref_primary_10_1007_s00343_024_4145_2 crossref_primary_10_3390_jmse11122226 |
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| Copyright | Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag GmbH Germany, part of Springer Nature 2023 Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag GmbH Germany, part of Springer Nature 2023. Copyright © Wanfang Data Co. Ltd. All Rights Reserved. |
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| Publisher | Science Press Springer Nature B.V Guangzhou Marine Geological Survey,China Geological Survey,Ministry of Natural Resources,Guangzhou 511458,China%Hainan Key Laboratory of Marine Geological Resources and Environment,Haikou 570206,China University of Chinese Academy of Sciences,Beijing 100049,China%Key Laboratory of Ocean and Marginal Sea Geology,South China Sea Institute of Oceanology,Chinese Academy of Sciences,Guangzhou 511458,China Guangzhou Marine Geological Survey,China Geological Survey,Ministry of Natural Resources,Guangzhou 511458,China Key Laboratory of Marine Mineral Resources,Ministry of Natural Resources,Guangzhou 511458,China Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou),Guangzhou 511458,China Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou),Guangzhou 511458,China%Key Laboratory of Marine Mineral Resources,Ministry of Natural Resources,Guangzhou 511458,China Key Laboratory of Ocean and Marginal Sea Geology,South China Sea Institute of Oceanology,Chinese Academy of Sciences,Guangzhou 511458,China |
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| Snippet | The Zengmu and Beikang Basins, separated by the West Baram Line (WBL) in the southwestern South China Sea margin, display distinct geological and geophysical... The Zengmu and Beikang basins, separated by the West Baram Line (WBL) in the southwestern South China Sea margin, display distinct geological and geophysical... |
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| SubjectTerms | Basins Borneo China Earth and Environmental Science Earth Sciences Eocene Eocene epoch Fault lines Fault zones Faults flowers Geological faults geometry Geomorphology and geological structure of South China Sea geophysics Heat flow Heat transfer Heat transmission Miocene Miocene epoch Ocean basins Oceanography Oligocene Oligocene epoch Seismic data South China Sea Strata Stratigraphy Subduction Subduction (geology) Subsidence Thinning Uplift |
| Title | Formation of the Zengmu and Beikang Basins, and West Baram Line in the southwestern South China Sea margin |
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