ZHAO Zhongquan, ZHONG Guangjian, FENG Changmao, TU Guanghong, JIN Huafeng. CENOZOIC SEQUENCE STRATIGRAPHY AND SEISMIC FACIES ANALYSIS OF XISHA TROUGH BASIN IN NORTHERN SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2016, 36(1): 15-26. DOI: 10.16562/j.cnki.0256-1492.2016.01.002
Citation: ZHAO Zhongquan, ZHONG Guangjian, FENG Changmao, TU Guanghong, JIN Huafeng. CENOZOIC SEQUENCE STRATIGRAPHY AND SEISMIC FACIES ANALYSIS OF XISHA TROUGH BASIN IN NORTHERN SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2016, 36(1): 15-26. DOI: 10.16562/j.cnki.0256-1492.2016.01.002
shu

CENOZOIC SEQUENCE STRATIGRAPHY AND SEISMIC FACIES ANALYSIS OF XISHA TROUGH BASIN IN NORTHERN SOUTH CHINA SEA

  • 1. MLR Key Laboratory of Marine Mineral Resources, Guangzhou, 510760;

  • 2. Guangzhou Marine Geological Survey, Guangzhou, 510760

More Information
  • Received Date: April 06, 2015
  • Revised Date: July 17, 2015
    Graphical Abstract
    • Abstract
  • The Xisha Trough Basin is a large Cenozoic deep-water sedimentary basin with lower exploration degree, which is located in the western part of the north slope of the South China Sea. New high-precision multichannel seismic data combined with geological character of the surrounding area were used to analyze the sequence stratigraphy of the basin. 8 seismic reflection interfaces were identified in the study area. Combined with seismic amplitude cyclic changes, 3 seismic super sequences and 8 seismic sequences were divided for the Cenozoic of the study area, and the top-bottom contact relationship, reflection characteristics, formation thickness, velocity and Ps of each seismic sequence were described in detail. 5 types of typical seismic facies were identified within the sequence framework:parallel and sub-parallel facies, wedge-shaped divergent facies, foreset facies, chaotic configuration and channel-filled facies. Based on the analysis of seismic facies and sedimentary facies, the sedimentary characteristics and sedimentary history of each sequence were analyzed, it suggested that since Eocene, the study area showed the characteristics of nonmarine facies lake basin sedimentary system. Oligocene period, the basin suffered transgression and accepted the littoral and shallow marine deposition. Early Miocene, bathyal deposits were developed widely in central of the basin. In the late middle Miocene, the sea level decline and slope-bathyal environment reduced, Xisha Trough turbidite channel brought its prototype. From late Miocene to Quaternary, it came into stable regional subsidence stage in the study area, and bathyal-abyssal mudstone were developed mainly. In addition, as a result of uplifted area in the north and south edges of the study area provided provenance, nearshore submerged aprons and delta and fan delta also developed inside the sequences. Controlled by the terrain elevation difference the slope fans and turbidite bodies formed in steep slope belt or fault lower plate.
    • FullText(HTML)
    • References (24)
  • [1]
    Pinder D. Offshore oil and gas:global resource knowledge and technological change[J].Ocean & Coastal Managenent,2001,44(9-10):576-600.
    [2]
    Pettinggill H S,Weiner P.Worldwide deepwater exploration and production:past,present,and future[J].The leading Edge,2002,21(4):371-376.
    [3]
    吴时国,袁圣强.世界深水油气勘探进展与我国南海深水油气前景[J].天然气地球科学,2005,16(6):693-699.

    [WU Shiguo,YUAN Shengqiang.Advance of exploration and petroleum geological features of deepwater hydrocarbon in the world[J].Natural gas geoscience,2005,16(6):693-699.]
    [4]
    何家雄,夏斌,施小斌,等.世界深水油气勘探进展与南海深水油气勘探前景[J].天然气地球科学,2006,17(6):747-752.

    [HE Jiaxiong,XIA Bin,SHI Xiaobin,et al.Prospect and progress for oil and gas in deep waters of the world,and the potential and prospect foreground for oil and gas in deep waters of the South China Sea[J].Natural gas geoscience,2006,17(6):747-752.]
    [5] 刘铁树,何仕斌.南海北部陆缘盆地深水区油气勘探前景[J].中国海上油气(地质),2001,15(3):164-170.[LIU Tieshu,HE Shibin.Deepwater hydrocarbon potential along the north continental margin,the South China Sea[J].China offshore Oil and Gas(Geology),2001,15(3):164-170.]
    [6]
    袁玉松,丁玫瑰.南海北部深水区盆地特征及其动力学背景[J].海洋科学,2008,32(12):102-110.

    [YUAN Yusong,DING Meigui.Characteristics and geodynamic setting of the basins in deepwater area of the Northern South China Sea Margin[J].Marine Sciences,2008,32(12):102-110.]
    [7]
    冯常茂,钟广见,金华峰.西沙海槽盆地古近系沉积特征[J].石油天然气学报,2012,34(8):6-11.

    [FENG Changmao,ZHONG Guangjian,JIN Huafeng.Sedimentary characteristics of Paleogene in Xisha Trouth Basin[J].Journal of Oil and Gas Technology,2012,34(1):6-11.]
    [8]
    钟广见,冯常茂,韦振权. 南海西沙海槽盆地地质构造特征[J].海洋地质与第四纪地质,2012,22(3):63-68.

    [ZHONG Guangjian,FENG Changmao,WEI Zhenquan.The structural features of Xisha Trouth Basin[J].Marine Geology and Quaternary Geology,2012,22(3):63-68.]
    [9]
    张义娜,张功成,梁建设,等. 琼东南盆地长昌凹陷渐新统崖城组沉积充填及烃源岩特征[J].海洋地质前沿,2012,28(5):7-14.

    [ZHANG Yina,ZHANG Gongcheng,LIANG Jianshe,et al. Sediment filling and source rock characteristics of oligocene Yacheng formation in Changchang depression of QiongDongNan basin[J].Marine Geology Frontiers,2012,28(5):7-14.]
    [10]
    苏明,李俊良,姜涛,等.琼东南盆地中央峡谷的形态及成因[J].海洋地质与第四纪地质,2009,29(4):85-93.

    [SU Ming,LI Junliang,JIANG Tao,et al. Morphological features and formation mechanism of central canyon in the Qiong Dong-nan basin,northern South China Sea[J].Marine Geology and Quaternary Geology,2009,29(4):85-93.]
    [11]
    袁圣强,吴时国,姚根顺.琼东南陆坡深水水道主控因素及勘探应用[J].海洋地质与第四纪地质,2010,30(2):61-66.

    [YUAN Shengqiang,WU Shiguo,YAO Genshun.The controlling factors analysis of QiongDong-nan slope deepwater channels and its significance to the hydrocarbon exploration[J].Marine Geology and Quaternary Geology,2010,30(2):61-66.]
    [12]
    李俊良,左倩媚,解习农,等.琼东南盆地深水区新近系沉积特征与有利储盖组合[J].海洋地质与第四纪地质,2011,31(6):109-116.

    [LI Junliang,ZUO Qianmei,XIE Xinong,et al. Neogene depositional features and favorable reservoir-cap combinations in the deepwater of Qiongdongnan basin,north south China sea[J].Marine Geology and Quaternary Geology,2011,31(6):109-116.]
    [13]
    王衍棠,陈玲,吴大明.南海中建南盆地速度资料分析与应用[J].热带海洋学报,2006,25(5):49-55.

    [WANG Yantang,CHEN Ling,WU Daming. Velocity data analysis and its application to Zhongjiannan Basin in South China Sea[J].Journal of Tropical Oceanography,2006,25(5):49-55.]
    [14]
    雷超,任建业,裴健翔,等.琼东南盆地深水区构造格局和幕式演化过程[J].地球科学-中国地质大学学报,2011,36(1):151-162.

    [LEI Chao,REN Jianye,PEI Jianxiang,et al.Tectonic framework and multiple tectonic evolution in deepwater area of Qiongdongnan basin,northern continental margin of south China sea[J].Earth Science-Journal of China University of Geosciences,2011,36(1):151-162.]
    [15]
    张志杰,于兴河.南海西沙海槽典型地震相识别与分析[J].海洋地质动态,2011,36(1):151-162.

    [ZHANG Zhijie,YU Xinghe.Identification and analysis of typical seismic facies of the Xisha trough in the south China sea[J].Marine Geology Letter,2011,36(1):151-162.]
    [16] 廖计华,王华,孙志鹏,等.琼东南盆地深水区长昌凹陷构造演化及其对层序样式的控制[J].中南大学学报(自然科学版),2012,43(8):3121-3132.[LIAO Jihua,WANG Hua,SEN Zhipeng,et al. Tectonic evolution and its controlling on sequence pattern of Chang-chang sag,deepwater area of Qiongdongnan basin,South China Sea[J].Journal of Central South University(Science and Technology),2012,43(8):3121-3132.]
    [17]
    许怀智,蔡东升,孙志鹏,等.琼东南盆地中央峡谷沉积充填特征及油气地质意义[J].地质学报,2012,86(4):641-650.

    [XU Huaizhi,CAI Dongsheng,SUN Zhipeng,et al.Filling characters of central submarine canyon of Qiongdongnan basin and its significance of petroleum geology[J].Acta Geological Sinica,2012,86(4):641-650.]
    [18]
    钟志洪,王良书,李绪宣,等.琼东南盆地古近纪沉积充填演化及其区域构造意义[J].海洋地质与第四纪地质,2004,24(1):29-36.

    [ZHONG Zhihong,WANG Liangshu,LI Xuxuan,et al.The paleogene basin-filling evolution of Qiongdongnan basin annd its relation with seafloor spreading of the south China sea[J].Marine Geology and Quaternary Geology,2004,24(1):29-36.]
    [19]
    能源,吴景富,漆家福,等.琼东南-珠江口盆地深水区构造样式及其分布特征[J]. 天然气工业,2011,31(8):32-37.

    [NENG Yuan,WU Jingfu,QI Jiafu,et al.Structural styles and distribution features in the deep water of the Pearl River Mouth and Qiongdongnan basins[J].Natural Gas Industry,2011,31(8):32-37(in Chinese).]
    [20] 马玉波,吴时国,邢树文,等.南海北部陆坡混合沉积地层模式及地震响应特征[J].吉林大学学报(地球科学版),2012,42(1):88-95.[MA Yubo,WU Shiguo,XING Shuwen,et al.Stratigraphic model and seismic characteristics of the mixed sedimentation in the slope area of north south China sea[J].Journal of Jilin University (Earth Science Edition),2012,42(1):88-95.]
    [21]
    王振峰.深水重要油气储层-琼东南盆地中央峡谷体系[J],沉积学报,2012,30(4):646-653.

    [WANG Zhenfeng. Important deepwater hydrocarbon reservoir:the central canyon system in the Qiong Dongnan basin[J],Acta Sedimentologica Sinica,2012,30(4):646-653.]
    [22]
    刘正华,陈红汉.琼东南盆地东部地区油气形成期次和时期[J]. 现代地质,2011,25(2):279-288.

    [LIU Zhenghua,CHEN Honghan.Hydrocarbon charging orders and times in the eastern area of Qiongdongnan basin[J].Geoscience,2011,25(2):279-288.]
    [23]
    唐武,王英民,黄志超,等.琼东南盆地南部深水区中新统层序地层地震相与沉积演化特征[J]. 海相油气地质,2012,17(2):20-25.

    [LIU Zhenghua,CHEN Honghan.Hydrocarbon charging orders and times in the eastern area of Qiongdongnan basin[J]. Marine Qrigin Petroleum Geology,2011,25(2):279-288.]
    [24]
    甘华军,王华,肖军,等.琼东南盆地东部构造坡折样式与层序地层发育特征[J]. 高校地质学报,2008,14(1):99-105.

    [GAN Huajun,WANG Hua,XIAO Jun,et al.2008. The patterns of tectonic slope-break zones and characteristics of sequence stratigraphy in the east of southeastern Hainan basin[J]. Geological Journal of China Universities,14(1):99-105(in Chinese).]
    • Related Articles

  • Related Articles

    [1]WANG Wenjuan, ZHANG Yinguo, CHEN Jianwen, YANG Yanqiu. Sequence stratigraphy and sedimentary evolution in the Lower Cretaceous of the Eastern Depression in the North Yellow Sea Basin[J]. Marine Geology & Quaternary Geology, 2024, 44(3): 125-135. DOI: 10.16562/j.cnki.0256-1492.2023100701
    [2]LUO Shuaibing, ZHANG Li, WANG Xiaoxue, YU Qiuhua, LEI Zhenyu, SHUAI Qingwei. The tectono-sedimentary evolution characteristics and regional reservoir-forming model of Nan’an Basin in the Cenozoic[J]. Marine Geology & Quaternary Geology, 2023, 43(4): 116-128. DOI: 10.16562/j.cnki.0256-1492.2022082901
    [3]LUO Shuaibing, ZHANG Li, XU Guoqiang, WANG Xiaoxue, LEI Zhenyu, SHUAI Qingwei. Reconstruction of Late Oligocene depositional systems in the Beikang Basin by seismic facies analysis[J]. Marine Geology & Quaternary Geology, 2022, 42(1): 123-134. DOI: 10.16562/j.cnki.0256-1492.2021051001
    [4]CHEN Mei, ZHANG Li, SHI Xiaobin, LUO Shuaibing, YU Chuanhai, GUO Lei, FENG Yingci. The Cenozoic evolution of sedimentary environment of Xisha Trough Basin[J]. Marine Geology & Quaternary Geology, 2019, 39(1): 15-24. DOI: 10.16562/j.cnki.0256-1492.2016090401
    [5]YANG Chaoyun, HAN Xiaohui, LUO Kun, FENG Yasheng, LIU Gang, CHEN Wanli, LI Xuelin, WU Shiguo. Seismic sequence stratigrahy of the Xuande Atoll in the Xisha Islands[J]. Marine Geology & Quaternary Geology, 2018, 38(6): 25-36. DOI: 10.16562/j.cnki.0256-1492.2018.06.003
    [6]QIU Erkang, YANG Fengli, ZHANG Ruoyu, ZHOU Xiaofeng. Seismic and sedimentary facies analysis and prediction of favorable Permian source rocks in the South Yellow Sea basin[J]. Marine Geology & Quaternary Geology, 2018, 38(3): 96-106. DOI: 10.16562/j.cnki.0256-1492.2018.03.009
    [7]ZHONG Guangjian, FENG Changmao, WEI Zhenquan. THE STRUCTURAL FEATURES OF XISHA TROUGH BASIN[J]. Marine Geology & Quaternary Geology, 2012, 32(3): 63-86. DOI: 10.3724/SP.J.1140.2012.03063
    [8]WANG Lifei, WANG Yantang, HU Xiaoqiang. STRATIGRAPHY AND SEDIMENTARY CHARACTERS OF THE WESTERN DEPRESSION,NORTH YELLOW SEA BASIN[J]. Marine Geology & Quaternary Geology, 2010, 30(3): 97-104. DOI: 10.3724/SP.J.1140.2010.03097
    [9]HU Xiaoqiang, LIU Zhenhu, CHEN Ling, WANG Lifei. CYCLE SEQUENCE STRATIGRAPHY AND SEDIMENTARY CHARACTERISTICS OF STUDY AREA X IN THE NORTH YELLOW SEA BASIN[J]. Marine Geology & Quaternary Geology, 2009, 29(2): 103-110. DOI: 10.3724/SP.J.1140.2009.02103
    [10]LIU Fang-lan, WU Lu-shan. TOPOGRAPHIC AND MORPHOLOGIC CHARACTERISTICS AND GENESIS ANALYSIS OF XISHA TROUGH SEA AREA IN THE SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2006, 26(3): 7-14.

Catalog

    Get Citation
    PDF
    XML
    Article views (2233) PDF downloads (17) Cited by()
    Turn off MathJax
    Article Contents
    Abstract
    References
    Related Articles
    WeChat WeChat
    Order Code Order Code

    Copyright © Marine Geology & Quaternary Geology Editorial Office;   Record No: 鲁ICP备15036216号-7

    Address: 62 Fuzhou South Road, Qingdao City    Post: 266237    Tel: 0532-85755823    E-mail: hydzdsjdz@163.com

    Supported by: Beijing Renhe Information Technology Co., Ltd. support: info@rhhz.net Baidu Analytics

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return