Advanced Search
Volume 33 Issue 3
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2011  >  33(3): 307-309
Zhang Yonggui, Song Zaichao, Zhou Xiaojin, Wu Li, Zhang Xike, Ran Jing. Identification of reef in Miocene, south of Qiongdongnan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2011, 33(3): 307-309. doi: 10.11781/sysydz201103307
Citation: Zhang Yonggui, Song Zaichao, Zhou Xiaojin, Wu Li, Zhang Xike, Ran Jing. Identification of reef in Miocene, south of Qiongdongnan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2011, 33(3): 307-309. doi: 10.11781/sysydz201103307
shu

Identification of reef in Miocene, south of Qiongdongnan Basin

doi: 10.11781/sysydz201103307
  • 1.

    SINOPEC Exploration and Production Research Institute, Beijing 100083, China

  • 2. Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214151, China

  • Received Date: 2011-03-07
  • Rev Recd Date: 2011-05-17
  • Publish Date: 2011-06-28
    Abstract
  • The southern part of the Qiongdongnan Basin was suitable for reef generation when the Meishan Formation deposited during Miocene.Seismic data collected in this region during the past few years have indicated that the Meishan Formation is characterized by typical mound reflection,mainly on ancient uplifts.The formation is flat at the bottom and convex at the top.There is clear boundary between top and bottom.The reflection is strong.Progradational or random reflection exists in the formation,while on the 2 flanks there is onlapping,and on the top there is drape.The wave impendence value is(8-10)×106kg/(m2·s).The formation is regarded as reef according to present studies.Comparisons between reef and mud structure have been carried out based on the studies of regional sedimentary background,mound structure generation location and seismic reflection characteristics,indicating that it is impossible for shale diapire generation in the formation.

     

    • FullText(HTML)
  • loading
    • References(16)
  • [1]
    龚再升,杨甲明,杨祖序,等.中国近海大油气田[M].北京:石油工业出版社,1997.
    [2]
    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.
    [3]
    李绪宣,朱光辉.琼东南盆地断裂系统及其油气输导特征[J].中国海上油气,2005,17(1):127.
    [4]
    许红,蔡峰,王玉净,等.西沙中新世生物礁演化与藻类的造礁作用[J].科学通报,1999,44(13):1435-1439.
    [5]
    邱燕,王英民.南海第三纪生物礁分布与古构造和古环境[J].海洋地质和第四纪,2001,21(1):65-73.
    [6]
    陈平,陆永潮,许红.南沙海域第三纪生物礁层序构成和演化[J].地质科学,2003,38(4):514-518.
    [7]
    龚再升.生物礁是南海北部深水区的重要勘探领域[J].中国海上油气,2009,21(5):289-295.
    [8]
    魏喜,邓晋福,谢文彦,等.南海盆地演化对生物礁的控制及礁油气藏潜力分析[J].地学前缘,2005,12(3):245-252.
    [9]
    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,2001,15(3):171-175.
    [10]
    Sattler U,Zampetti V,Schlager W,et al.Late Leaching under deep burial conditions: a case study from the Miocene Zhujiang Carbonate Reservoir,South China Sea[J].Marine and Petroleum Geology,2004,21(8):977-992.
    [11]
    Erlich R N,Barrett S F,Guo Baiju.Seismic and geological characteristics of drowning events on carbonate platforms[J].AAPG Bulletin,1990,74:1523-1537.
    [12]
    吴时国,袁圣强,董冬冬,等.南海北部深水区中新世生物礁发育特征[J].海洋与湖沼,2009,40(2):117-121.
    [13]
    郝芳,李思田,龚再升,等.莺歌海盆地底辟发育机制与流体幕式充注[J].中国科学D辑,2001,31(6):471-476.
    [14]
    何家雄,夏斌,刘宝明,等.莺歌海盆地泥底辟热流体上侵活动与天然气及CO2运聚规律剖析[J].石油实验地质,2004,26(4):349-358.
    [15]
    王家豪,庞雄,王存武,等.珠江口盆地白云凹陷中央底辟带的发现及识别[J].地球科学——中国地质大学学报,2006,31(2):209-213.
    [16]
    孙昶旭,崔永刚.罗文生,等.东营凹陷东营三角洲与中央隆起带盐—泥构造形成的关系及其对隐蔽油气藏勘探的意义[J].石油地球物理勘探,2006,41(4):462-467.
    • 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 (3679) PDF downloads(987) 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