Advanced Search
Volume 28 Issue 6
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2006  >  28(6): 554-559
Tao Weixiang, He Shibin, Zhao Zhigang, Ding Fang. RESERVOIR DISTRIBUTION IN DEEPWATER AREA OF THE QIONGDONGNAN BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2006, 28(6): 554-559. doi: 10.11781/sysydz200606554
Citation: Tao Weixiang, He Shibin, Zhao Zhigang, Ding Fang. RESERVOIR DISTRIBUTION IN DEEPWATER AREA OF THE QIONGDONGNAN BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2006, 28(6): 554-559. doi: 10.11781/sysydz200606554
shu

RESERVOIR DISTRIBUTION IN DEEPWATER AREA OF THE QIONGDONGNAN BASIN

doi: 10.11781/sysydz200606554
  • 1.

    Faculty of Earth Resources, China University of Geosciences, Wuhan, Hubei 430074, China

  • 2. CNOOC Research Center, CNOOC, Beijing 100027, China

  • Received Date: 2006-07-31
  • Rev Recd Date: 2006-10-09
  • Publish Date: 2006-11-28
    Abstract
  • The Qiongdongnan Basin has undergone 3 stages of tectonic-sedimentary evolution,i.e.rift-ing,fault-depressing and depressing.There are 4 sedimentary systems which respectively develop 4 major types of reservoirs:a) the fan deltaic or littoral sandstone of Ling-III Member;b) the littoral facies sandstone of Sanya-Meishan Formations;c) the sandstone of lowstand system tract of Sanya-Yinghuang Formations;and d) the Miocene platform limestone of Meishan Formation.Spatially the reservoirs develop in 3 different zones,i.e.the northern shallow shelf zone developing deltaic and littoral facies sandstones,the central depression zone developing LST sand bodies,and the southern Yongle Uplift zone developing carbonate rocks.The deepwater area mainly covers the latter 2 zones.Due to the difference of controlling factors,each reservoir zone can be further divided into several areas,and each area may develop several reservoir-seal combinations.The Miocene platform limestone may be an important exploration reservoir in the southern Yongle Uplift.

     

    • FullText(HTML)
  • loading
    • References(24)
  • [1]
    Henry S P,Paul W.Deepwater remains immature frontier[J].Offshore,2002,62(10):48～50.
    [2]
    Marshall D.Beyond "big three" theaters,other countries expanding deepwater search[J].Offshore,1999,59(9):50～51.
    [3]
    Richard N.As US Gulf discoveries move down the slope,will deepwater reserve additions continue?[J].Offshore,2001,61(6):32～35.
    [4]
    王春修.国外深水油气勘探动态及经验[J].中国海上油气(地质),2002,16(2):141～143.
    [5]
    杨川恒,杜栩,潘和顺等.国外深水领域油气勘探新进展及我国南海北部陆坡深水区油气勘探潜力[J].地学前缘,2000,7(3):247～253.
    [6]
    Bourgeois T M,Godfrey D G,Bailey M J.Race on for deepwater acreage,3 500-meter depth capability[J].Offshore,1998,58(10):40～41.
    [7]
    周小鹰,魏魁生.QDN盆地层序地层及生储盖组合分析[J].石油与天然气地质,2000,21(4):244～248.
    [8]
    Chen P H Percy,Chen Z Y,Zhang Q M.Sequence stratigraphy and continental margin development of the northwestern shelf of the South China Sea[J].AAPG Bulletin,1993,77 (5):842～862.
    [9]
    王春修.琼东南盆地晚新生代层序地层学研究[J].中国海上油气(地质),1992,6(5):11～19.
    [10]
    王淑兰.琼东南盆地第三纪沉积特征、生储盖组合及含油气远景探讨[J].海洋地质与第四纪地质,1995,15(增):72～78.
    [11]
    解习农,葛立刚.琼东南盆地断陷期层序地层模式[J].地质科学,1997,32(1):47～55.
    [12]
    吕明.莺歌海-琼东南盆地第三纪层序地层特征[J].南海石油,1997,14(1):1～7.
    [13]
    王根发,吴冲龙,周江羽等.琼东南盆地第三系层序地层分析[J].石油实验地质,1998,20(2):124～127.
    [14]
    龚再升,李思田,谢泰俊等.南海北部大陆边缘盆地分析与油气聚集[M].北京:科学出版社,1997.
    [15]
    魏魁生,崔旱云,叶淑芬.琼东南盆地高精度层序地层学研究[J].地球科学——中国地质大学学报,2001,26(1):59～66.
    [16]
    吕明.莺-琼盆地低位沉积模式的新探讨[J].中国海上油气(地质),2002,16(4):221～230.
    [17]
    陶维祥,梁建设,吕建军.琼东南盆地BD19—2构造形成机理初步研究[J].中国海上油气(地质),2000,14(5):315～319.
    [18]
    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.
    [19]
    刘春兰,冯正祥.宝岛23—1构造生物礁地质评价[J].中国海上油气(地质),2001,15(3):171～175.
    [20]
    解习农,李思田,葛立刚等.琼东南盆地崖南凹陷海湾扇三角洲体系沉积构成及演化模式[J].沉积学报,1996,14(3):64～71.
    [21]
    龚再升.中国海上大油气田[M].北京:石油工业出版社,1997.
    [22]
    冯正祥,刘春兰.琼海36—2礁油藏地质评价[J].中国海上油气(地质),1996,10(5):339～342.
    [23]
    张明书,何起祥,业治净.西沙生物礁碳酸盐沉积地质学研究[M].北京:科学出版社,1989.
    [24]
    张炳.琼东南盆地L27—1砂体特征及其形成机理的地质分析[J].中国海上油气(地质),1997,11(4):281～288
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索
    Citation
    XML
    PDF-CN

    Article Metrics

    Article views (1122) PDF downloads(352) Cited by()
    Proportional views
    Related

    Website Copyright © Wuxi Research Institute of Petroleum Geology, SINOPEC 苏ICP备15009037号 苏公网安备32021102000780号

    Address：No. 2060, Lihu Avenue, Wuxi, Jiangsu   (214126) Tel：0510-68787204，68787203 Fax：0510-68787113 Email：sysydz.syky@sinopec.com

    Supported by: Beijing Renhe Information Technology Co. Ltd    

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return