Volume 42 Issue 6
Nov.  2023
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Su Haixia, Liu Shan, Zhang Li, Su Ming, Huang Shuqin, Lei Zhenyu. Spatiotemporal distribution characteristics and controlling factors of deep-water sediments in the Beikang Basin since the Late Miocene, southern South China Sea[J]. Bulletin of Geological Science and Technology, 2023, 42(6): 129-139. doi: 10.19509/j.cnki.dzkq.tb20220126
Citation: Su Haixia, Liu Shan, Zhang Li, Su Ming, Huang Shuqin, Lei Zhenyu. Spatiotemporal distribution characteristics and controlling factors of deep-water sediments in the Beikang Basin since the Late Miocene, southern South China Sea[J]. Bulletin of Geological Science and Technology, 2023, 42(6): 129-139. doi: 10.19509/j.cnki.dzkq.tb20220126

Spatiotemporal distribution characteristics and controlling factors of deep-water sediments in the Beikang Basin since the Late Miocene, southern South China Sea

doi: 10.19509/j.cnki.dzkq.tb20220126
  • Received Date: 23 Mar 2022
  • Accepted Date: 15 Aug 2022
  • Rev Recd Date: 07 Aug 2022
  • Objective

    The Beikang Basin, located in the southern South China Sea, is a significant area for offshore oil and gas exploration in China. Previous studies in this region have primarily focused on the Palaeogene source rock and the Middle Miocene carbonate reservoirs, neglecting the investigation of deep-water sediments since the Late Miocene.

    Methods

    Therefore, this study aims to explore the spatiotemporal distribution, characteristics, and controlling factors of deep-water sediments in the Beikang Basin since the Late Miocene, utilizing 2D seismic data.

    Results

    Three types of sedimentary deposits have been identified in the Beikang Basin since the Late Miocene: draping strates, mass-transport deposits (MTDs), and turbidites. Turbidites can be further classified into confined turbidites and delta-front ones. The study reveals that the draping state is predominantly developed in the forebulge tectonic regions of the Beikang Basin, with a decreasing thickness from South to North. MTDs, on the other hand, are mainly distributed in the Backbulge zone, with a thickness that decreases from Southwest to Northeast. The findings indicate that the development and distribution of sediments in the Beikang Basin are influenced by various factors, including sedimentary supply, geomorphic features, tectonic activity, and eustatic sea level changes. The location and thickness of deep-water sediments are primarily controlled by the supply of materials. Additionally, the distribution range of gravity flow deposits and draping states is influenced by the topography of the area.

    Conclusion

    These results provide a theoretical foundation for understanding the development and controlling factors of deep-water sediments in the Beikang Basin.

     

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  • [1]
    Pickering K, Hiscott R. Deep marine systems: Processes, deposits, environments, tectonics and sedimentation[M]. Washington, DC, USA: Wiley & American Geophysical Union, 2016.
    [2]
    Huneke H, Mulder T. Deep-sea sediments[M]. Amsterdam, the Netherlands: Elsevier, 2011.
    [3]
    Rebesco M, Camerlenghi A. Contourites[M]. Amsterdam, the Netherlands: Elsevier, 2008: 457-489.
    [4]
    孙国桐. 深水重力流沉积研究进展[J]. 地质科技情报, 2015, 34(3): 30-36. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201503005.htm

    Sun G T. A review of deep-water gravity-flow deposition research[J]. Geological Science and Technology Information, 2015, 34(3): 30-36(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201503005.htm
    [5]
    解习农, 任建业, 王振峰, 等. 南海大陆边缘盆地构造演化差异性及其与南海扩张耦合关系[J]. 地学前缘, 2015, 22(1): 77-87. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201501009.htm

    Xie X N, Ren J Y, Wang Z F, et al. Difference of tectonic evolution of continental marginal basins of South China Sea and relationship with SCS spreading[J]. Earth Science Frontiers, 2015, 22(1): 77-87(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201501009.htm
    [6]
    Banerjee A, Salim A M A. Seismic attribute analysis of deep-water dangerous grounds in the South China Sea, NW Sabah Platform region, Malaysia[J]. Journal of Natural Gas Science and Engineering, 2020, 83: 103534. doi: 10.1016/j.jngse.2020.103534
    [7]
    何玉林, 匡增桂, 徐梦婕. 北康盆地第四纪块体搬运沉积地震反射特征及成因机制[J]. 地质科技情报, 2018, 37(4): 258-268. doi: 10.19509/j.cnki.dzkq.2018.0435

    He Y L, Kuang Z G, Xu M J. Seismic reflection characteristics and triggering mechanism of mass transport deposits of Quaternary in Beikang Basin[J]. Geological Science and Technology Information, 2018, 37(4): 258-268(in Chinese with English abstract). doi: 10.19509/j.cnki.dzkq.2018.0435
    [8]
    Liu S, Hernández-Molina F J, Lei Z Y, et al. Fault-controlled contourite drifts in the southern South China Sea: Tectonic, oceanographic, and conceptual implications[J]. Marine Geology, 2021, 433: 106420. doi: 10.1016/j.margeo.2021.106420
    [9]
    Hutchison C S. Marginal basin evolution: The southern South China Sea[J]. Marine and Petroleum Geology, 2004, 21(9): 1129-1148. doi: 10.1016/j.marpetgeo.2004.07.002
    [10]
    Madon M, Ly K C, Wong R. The structure and stratigraphy of deepwater Sarawak, Malaysia: Implications for tectonic evolution[J]. Journal of Asian Earth Sciences, 2013, 76(S1): 312-333.
    [11]
    王龙樟, 姚永坚, 张莉, 等. 中中新世以来南海南部前隆的迁移: 来自北康盆地的证据[J]. 石油与天然气地质, 2019, 40(1): 123-132. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201901013.htm

    Wang L Z, Yao Y J, Zhang L, et al. Forebulge migration since the Mid-Miocene in the southern South China Sea: Evidences from the Beikang Basin[J]. Oil & Gas Geology, 2019, 40(1): 123-132(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201901013.htm
    [12]
    Banerjee A, Salim A M A. Stratigraphic evolution of deep-water dangerous grounds in the South China Sea, NW Sabah Platform Region, Malaysia[J]. Journal of Petroleum Science and Engineering, 2021, 201: 108434. doi: 10.1016/j.petrol.2021.108434
    [13]
    黄维, 汪品先. 南海沉积物总量的统计: 方法与结果[J]. 地球科学进展, 2006, 21(5): 465-473. https://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ200605003.htm

    Huang W, Wang P X. The statistics of sediment mass in the South China Sea: Method and result[J]. Advances in Earth Science, 2006, 21(5): 465-473(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ200605003.htm
    [14]
    雷振宇, 张莉, 苏明, 等. 南海南部北康盆地中中新世深水沉积体类型、特征及意义[J]. 海洋地质与第四纪地质, 2017, 37(6): 110-118. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ201706013.htm

    Lei Z Y, Zhang L, Su M, et al. Middle Miocene deep-water sediments in the Beikang Basin, southern South China Sea: Types, characteristics and implications[J]. Marine Geology & Quaternary Geology, 2017, 37(6): 110-118(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ201706013.htm
    [15]
    王宏斌, 姚伯初, 梁金强, 等. 北康盆地构造特征及其构造区划[J]. 海洋地质与第四纪地质, 2001, 21(2): 49-54.

    Wang H B, Yao B C, Liang J Q, et al. Tectonic characteristics and division of the Beikang Basin[J]. Marine Geology & Quaternary Geology, 2001, 21(2): 49-54(in Chinese with English abstract).
    [16]
    张莉, 王嘹亮, 易海. 北康盆地的形成与演化[J]. 中国海上油气地质, 2003, 17(4): 23-26.

    Zhang L, Wang L L, Yi H. The formation and evolution of Beikang Basin[J]. China Offshore Oil and Gas, 2003, 17(4): 23-26(in Chinese with English abstract).
    [17]
    骆帅兵, 王笑雪, 张莉, 等. 南海南部北康-曾母盆地早中新世层序内部优质砂岩精细刻画[J]. 海洋地质与第四纪地质, 2020, 40(2): 111-123.

    Luo S B, Wang X X, Zhang L, et al. Study of high-quality sandstone in Early Miocene sequence of Beikang-Zengmu Basin, the southern South China Sea[J]. Marine Geology & Quaternary Geology, 2020, 40(2): 111-123(in Chinese with English abstract).
    [18]
    姚永坚, 杨楚鹏, 李学杰, 等. 南海南部海域中中新世(T3界面)构造变革界面地震反射特征及构造含义[J]. 地球物理学报, 2013, 56(4): 1274-1286. https://www.cnki.com.cn/Article/CJFDTOTAL-DQWX201304024.htm

    Yao Y J, Yang C P, Li X J, et al. The seismic reflection characteristics and tectonic significance of the tectonic revolutionary surface of Mid-Miocene(T3 seismic interface) in the southern South China Sea[J]. Chinese Journal of Geophysics, 2013, 56(4): 1274-1286(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQWX201304024.htm
    [19]
    Koša E. Sea-level changes, shoreline journeys, and the seismic stratigraphy of Central Luconia, Miocene-present, offshore Sarawak, NW Borneo[J]. Marine and Petroleum Geology, 2015, 59: 35-55.
    [20]
    Madon M, Redzuan A H. West Luconia Province//Anon. The petroleum geology and resources of Malaysia[M]. Kuala Malaysia, Malaysia: Petroliam Nasional Berhad, 1999: 427-436.
    [21]
    Petronas. The petroleum geology and resources of malaysia[M]. Kuala Lumpur, Malaysia: Petronas, 1999.
    [22]
    Mitchum R M J, Vail P R, Sangree J B. Seismic stratigraphy and global changes of sea level: Part 6. Stratigraphic interpretation of seismic reflection patterns in depositional sequences[M]//Payton C E. Seismic stratigraphy: Applications to hydrocarbon exploration. Tulsa, USA: AAPG Memoir, 1977: 17-133.
    [23]
    Madon M. North Luconia Province//Anon. The petroleum geology and resources of Malaysia[M]. Kuala Lumpur: Petroliam Nasional Berhad, 1999: 441-454.
    [24]
    Omosanya K O. Episodic fluid flow as a trigger for Miocene-Pliocene slope instability on the Utgard High, Norwegian Sea[J]. Basin Research, 2018, 30(5): 942-964.
    [25]
    Masson D G, Hyggett Q J, Brunsden D. The surface texture of the Saharan debris flow deposit and some speculations on submarine debris flow processes[J]. Sedimentology, 1993, 40(3): 583-598.
    [26]
    Steventon M J, Jackson C A L, Hodgson D M, et al. Strain analysis of a seismically imaged mass-transport complex, offshore Uruguay[J]. Basin Research, 2019, 31(3): 600-620.
    [27]
    朱本铎, 关水贤, 黄文星, 等. 南海地质地球物理图系(1∶200万)[CM]. 广州: 中国航海图书出版社, 2015.

    Zhu B D, Guan S X, Huang W X, et al. Atlas of geology and geophysics of South China Sea(1∶2 000 000)[CM]. Guangzhou: China Navigation Publication Press, 2015(in Chinese).
    [28]
    Stow D, Smillie Z. Distinguishing between deep-water sediment facies: Turbidites, contourites and hemipelagites[J]. Geosciences, 2020, 10(2): 68.
    [29]
    Stow D, Tabrez A R. Hemipelagites: Processes, facies and model[M]. United Kingdom: Geological Society of London Special Publications, 1998: 317-337.
    [30]
    Takano S, Ito M, Nakano T, et al. Sequence-stratigraphic signatures of hemipelagic siltstones in deep-water successions: The Lower Pleistocene Kiwada and Otadai Formations, Boso Peninsula, Japan[J]. Sedimentary Geology, 2004, 170(3/4): 189-206.
    [31]
    雷振宇, 张莉, 王龙樟, 等. 南海南部北康盆地晚渐新世-中中新世物源变化[J]. 地球科学, 2020, 45(5): 1855-1864.

    Lei Z Y, Zhang L, Wang L Z, et al. The provenance migration in the Beikang Basin of the southern South China Sea during the Oligocene to the Mid-Miocene[J]. Earth Science, 2020, 45(5): 1855-1864(in Chinese with English abstract).
    [32]
    张晋, 李安春, 万世明, 等. 南海南部表层沉积物粒度分布特征及其影响因素[J]. 海洋地质与第四纪地质, 2016, 36(2): 1-10.

    Zhang J, Li A C, Wan S M, et al. Grain size distribution of surface sediments in the southern South China Sea and influencing factors[J]. Marine Geology & Quaternary Geology, 2016, 36(2): 1-10(in Chinese with English abstract).
    [33]
    Wang P, Prell W L, Blum P, et al. Proceedings of the ocean drilling program, Initial Reports 184[R]. Texas: Texas A & M University, 2000.
    [34]
    Ding W, Franke D, Li J, et al. Seismic stratigraphy and tectonic structure from a composite multi-channel seismic profile across the entire dangerous grounds, South China Sea[J]. Tectonophysics, 2013, 582: 162-176.
    [35]
    Huang J, Jiao W, Liu J, et al. Sediment distribution and dispersal in the southern South China Sea: Evidence from clay minerals and magnetic properties[J]. Marine Geology, 2021, 439: 106560.
    [36]
    张厚和, 刘鹏, 廖宗宝, 等. 南沙海域主要盆地地质特征与油气分布[J]. 中国石油勘探, 2018, 23(1): 62-70. https://www.cnki.com.cn/Article/CJFDTOTAL-KTSY201801007.htm

    Zhang H H, Liu P, Liao Z B, et al. Geological characteristics and hydrocarbon distribution in major sedimentary basins in Nansha sea areas[J]. China Petroleum Exploration, 2018, 23(1): 62-70(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-KTSY201801007.htm
    [37]
    Abdul M M, Robert H, Wong F. Seismic sequence stratigraphy of the Tertiary sediments, offshore Sarawak deep-water area, Malaysia[J]. Geology Society of Malaysia Bulletin, 1995, 57: 545-561.
    [38]
    Xu J, Ren J, Luo P. The evolution of a gravity-driven system accompanied by diapirism under the control of the prograding West Luconia Deltas in the Kangxi Depression, southern South China Sea[J]. Marine Geophysical Research, 2019, 40(2): 199-221.
    [39]
    王华, 陈思, 刘恩涛, 等. 南海北部莺-琼盆地典型重力流沉积特征与物源体系[J]. 地质科技通报, 2022, 41(5): 5-18. doi: 10.19509/j.cnki.dzkq.2022.0245

    Wang H, Chen S, Liu E T, et al. Typical gravity flow sedimentary features and provenance system in Yinggehai-Qiongdongnan Basin, northern South China Sea[J]. Bulletin of Geological Science and Technology, 2022, 41(5): 5-18(in Chinese with English abstract). doi: 10.19509/j.cnki.dzkq.2022.0245
    [40]
    裴健翔, 张成, 王亚辉, 等. 南海南部陆缘盆地裂陷-漂移-前陆期构造演化及沉积响应: 以礼乐盆地为例[J]. 地质科技通报, 2021, 40(2): 42-53. doi: 10.19509/j.cnki.dzkq.2021.0205

    Pei J X, Zhang C, Wang Y H, et al. Tectonic evolution and depositional response in southern continental marginal basins of South China Sea during period of rift-drift-foreland: A case study from the Liyue Basin[J]. Bulletin of Geological Science and Technology, 2021, 40(2): 42-53(in Chinese with English abstract). doi: 10.19509/j.cnki.dzkq.2021.0205
    [41]
    周蒂, 吴世敏, 陈汉宗. 南沙海区及邻区构造演化动力学的若干问题[J]. 大地构造与成矿学, 2005, 29(3): 339-345. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK200503008.htm

    Zhou D, Wu S M, Chen H Z. Some remarks on the tectonic evolution of Nansha and its adjacent regions in southern South China Sea[J]. Geotectonica et Metallogenia, 2005, 29(3): 339-345(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK200503008.htm
    [42]
    Hall R. Reconstructing Cenozoic SE Asia[J]. Geological Society, 1996, 106: 153-184.
    [43]
    孙珍, 赵中贤, 周蒂, 等. 南沙海域盆地的地层系统与沉积结构[J]. 地球科学: 中国地质大学学报, 2011, 36(5): 798-806.

    Sun Z, Zhao Z X, Zhou D, et al. The stratigraphy and the sequence achitecture of the basins in Nansha Region[J]. Earth Science: Journal of China University of Geosciences, 2011, 36(5): 798-806(in Chinese with English abstract).
    [44]
    雷振宇, 刘晓峰, 张莉, 等. 南海南部北康盆地构造样式及构造演化[J]. 大地构造与成矿学, 2021, 45(5): 861-874.

    Lei Z Y, Liu X F, Zhang L, et al. Structural styles and evolution of Beikang Basin, southern South China Sea[J]. Geotectonica et Metallogenia, 2021, 45(5): 861-874(in Chinese with English abstract).
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