南海北部陆坡流花碳酸盐台地地球物理响应

张广旭, 吴时国, 朱伟林, 施和生, 陈端新. 南海北部陆坡流花碳酸盐台地地球物理响应[J]. 海洋地质与第四纪地质, 2011, 31(4): 105-112. doi: 10.3724/SP.J.1140.2011.04105
引用本文: 张广旭, 吴时国, 朱伟林, 施和生, 陈端新. 南海北部陆坡流花碳酸盐台地地球物理响应[J]. 海洋地质与第四纪地质, 2011, 31(4): 105-112. doi: 10.3724/SP.J.1140.2011.04105
ZHANG Guangxu, WU Shiguo, ZHUWeilin, SHI Hesheng, CHEN Duanxin. GEOPHYSICAL RESPONSE OF THE LIUHUA CARBONATE PLATFORM IN NORTHERN SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2011, 31(4): 105-112. doi: 10.3724/SP.J.1140.2011.04105
Citation: ZHANG Guangxu, WU Shiguo, ZHUWeilin, SHI Hesheng, CHEN Duanxin. GEOPHYSICAL RESPONSE OF THE LIUHUA CARBONATE PLATFORM IN NORTHERN SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2011, 31(4): 105-112. doi: 10.3724/SP.J.1140.2011.04105

南海北部陆坡流花碳酸盐台地地球物理响应

  • 基金项目:

    国家重点基础研究发展规划项目(2009CB219406)

详细信息
    作者简介: 张广旭(1986-),男,硕士研究生,从事海洋地球物理研究
  • 中图分类号: P738

GEOPHYSICAL RESPONSE OF THE LIUHUA CARBONATE PLATFORM IN NORTHERN SOUTH CHINA SEA

  • 碳酸盐岩储层发育和成岩作用复杂性导致了储层物性非均质特征。对东沙海区流花油田碳酸盐岩测井曲线进行交汇分析,得出速度、密度和中子孔隙度与波阻抗有良好的线性对应关系。通过对流花地区的三维地震和测井资料分析运算,总结碳酸盐台地非均质地震反射特征,利用地震属性和反演技术描述了该区生物礁碳酸盐岩储层的物性特征。结果表明,地震反射强度、波阻抗反演、振幅类属性和相干体等,可展示该区碳酸盐岩储层物性的非均质性特征,另外,影响流花非均质的主要因素,为岩溶以及酸性气体造成的垮塌灰岩坑。
  • 加载中
  • [1]

    Roehl P O,Choquette P W.Carbonate Petroleum Reservoirs[M].Berlin,Heidelberg,New York:Springer Verlag,1985,1-15.

    [2]

    吕炳全,徐国强,王红罡,等.南海新生代碳酸盐台地淹没事件记录的海底扩张[J].地质科学,2002,37(4):405-414.

    [LÜ Bingquan,XU Guoqiang,WANG Hongzhi,et al.Sea floor spreading recorded by drowning events of Cenozoic carbonate platforms in the South China Sea[J].Chinese Journal of Geology,2002,37(4):405-414.]

    [3]

    姚伯初,万玲,吴能友.南海新生代构造演化及岩石圈三维结构特征[J].地质通报,2005,24(1):1-8.

    [YAO Bochu,WAN Ling,WU Nengyou.Cenozoic tectonic evolution and the 3D structure of lithosphere of the South China Sea.Geological Bulletin of China,2005,24(1):1-8.]

    [4]

    ZampettiT V,Sattler H,Braaksma U.Well log and seismic character of Liuhua11-1 Field,South China Sea:relationship between diagenesis and seismic reflections[J].Sedimentary Geology,2005,175:217-236.

    [5]

    Sattler U,Zampetti V,Schlager W,et al.Late leaching under deep burial conditions:a case study from the Miocene Zhu-jiang carbonate reservoir,South China Sea[J].Marine and Petroleum Geology,2004,21:977-992.

    [6]

    岳大力,吴胜和,林承焰,等.流花11-1油田礁灰岩油藏储层非均质性及剩余油分布规律[J].地质科技情报,2005,24(6):90-96.

    [YUE Dali,WU Shenghe,LIN Chengyan,et al.Reservoir heterogeneity and remaining oil distribution pattern of reef limestone reservoir in Liuhua11-1 oilfield[J].Geological Science and Technology Information.2005,24(6):90-96.]

    [7]

    Zampetti V,Schlager W.Architecture and growth history of a Miocene carbonate plateform from 3D seismic reflection data:Luconia province,offshore Sarawak,Malaysia[J].Marine and Petroleum Geology,2004,21:517-534.

    [8]

    Robert Riding.Structure and composition of organic reefs and carbonate mud mounds:concepts and categories[J].Earth Science Reviews,2002,58:163-231.

    [9]

    岳大力,吴胜和,林承焰,等.流花11-1油田礁灰岩油藏沉积-成岩演化模式[J].石油与天然气地质,2005,26(4):518-529.

    [YUE Dali,WU Shenghe,LIN Chengyan,et al.Sedimentary and diagenetic evolution pattern of reef limestone reservoirs in Liuhua 11-1 oilfield[J].Oil&Gas Geology,2005,26(4):518-529.]

    [10]

    Uwe Strecker,Maggie Smith,Richard U den,et al.Seismic attribute analysis in hydrothermal dolomite,Devonian Slave Point Formation,Northeast British Columbia,Canada[C]//SEG Technical Program Expanded Abstracts.2004:378-381.

    [11]

    Erlichr N,Barrett S F,Ju GB.Seismic and geologic characteristics of drowning events on carbonate platforms[J].AAPG Bulletin,1990,74(10):1523-1537.

    [12]

    Kusumastu TI A,Van Rensburgen P,Warren J K.Seismic sequence analyses and reservoir potential of drowned Miocene carbonate platforms in the Madura Strait,East Java,Indonesia[J].AAPG Bulletin,2002,86(2):213-232.

    [13]

    Wu Shiguo,Yuan Shengqiang,Zhang Guangxu,et al.Seismic Characteristics of a reef carbonate reservoir and implications for hydrocarbon exploration in deepwater of the Qiongdongnan Basin,northern SCS[J].Marine and Petroleum Geology,2008,26(6):817-823.

    [14]

    Brown A R.Interpretation of Three-Dimensional Seismic Data[M].Tulsa:The American Association of Petroleum Geologists and the Society of Exploration Geophysics.1999.

    [15]

    Brown A R.Interpretation of Three-Dimensional Seismic Data[M].Tulsa:The American Association of Petroleum Geologists and the Society of Exploration Geophysics.1999.

    [16]

    Kusumastu T A,van Rensburgen P,Warren J K.Seismic sequence analyses and reservoir potential of drowned Miocene carbonate platforms in the Madura Strait,East Java,Indonesia[J].AAPG Bulletin,2002,86.

    [17]

    Moldovanyi E P,Waal F M,Yan Z J.Regional exposure events and platform evolution of Zhujiang Formation carbonates,Pearl river Mouth Basin:evidence for primary and diagenetic seismic facies.[C]//Unconformities and porosity in carbonate strata.American Association of Petroleum Geologists Memoir.1995,63:13345.

    [18]

    Chip Story,Patrick Peng,Jian Donglin.Liuhua 11-1 field,South China Ssea:a shallow carbonate reservoir developed using ultrahigh-resolution 3-d seismic,inversion,and attribute-based reservoir modeling[C]//.the Leading Edge,2000,19:834-844.

    [19]

    Gong Z,Jin Q,Qin Z,et al.Geology,tectonics and evolution of the Pear River Mouth Basin.In:Zhu X ed.[C]//Chinese Sedimentary Basin.1989:181-196.

    [20]

    刘军,施和生,杜家元,等.东沙隆起台地生物礁、滩油藏成藏条件及勘探思路探讨.热带海洋学报,2007,26:22-27.[LIU Jun,SHI Hesheng,DU Jiayuan,et al.Forming conditions and exploration direction of reef oil-gas pool in carbonate platform of Dongsha Massif[J].Journal Of Tropical Oceanography,2007

    ,26:22-27.]

    [21]

    朱伟林,张功成,杨少坤,等.南海北部大陆边缘盆地天然气地质.北京:石油工业出版社,2007.[ZHU Weilin,ZHANG Gongcheng,YANG Shaokun,et al.Geology of natural gas of continental margin of the northern South China Sea[M],Beijing:Petroleum Industry Press,2007.]

  • 加载中
计量
  • 文章访问数:  1072
  • PDF下载数:  3
  • 施引文献:  0
出版历程
收稿日期:  2011-02-10
修回日期:  2011-03-10

目录