Advanced Search
Volume 25 Issue 4
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2003  >  25(4): 353-356
ZHU Guang-you, JIN Qing, GUO Chang-chun, ZHANG Lin-ye, QU Jiang-xiu, ZHANG Ying-li. DIFFERENCES OF HYDROCARBON ACCUMULATIONS IN THE DONGYING AND THE ZHANHUA DEPRESSIONS OF THE BOHAIWAN BASIN AND THEIR CONTROL FACTORS[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2003, 25(4): 353-356. doi: 10.11781/sysydz200304353
Citation: ZHU Guang-you, JIN Qing, GUO Chang-chun, ZHANG Lin-ye, QU Jiang-xiu, ZHANG Ying-li. DIFFERENCES OF HYDROCARBON ACCUMULATIONS IN THE DONGYING AND THE ZHANHUA DEPRESSIONS OF THE BOHAIWAN BASIN AND THEIR CONTROL FACTORS[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2003, 25(4): 353-356. doi: 10.11781/sysydz200304353
shu

DIFFERENCES OF HYDROCARBON ACCUMULATIONS IN THE DONGYING AND THE ZHANHUA DEPRESSIONS OF THE BOHAIWAN BASIN AND THEIR CONTROL FACTORS

doi: 10.11781/sysydz200304353
  • 1.

    University of Petroleum, Dongying, Shandong 257061, China

  • 2. Research Institute of Geosciences, Shengli Oilfield, Dongying, Shandong 257015, China

  • Received Date: 2003-02-07
  • Rev Recd Date: 2003-06-04
  • Publish Date: 2003-07-25
    Abstract
  • Closely neighbouring in the Bohaiwan Basin, the Dongying and the Zhanhua Depressions have distinct discrepancies in the composition of hydrocarbon source rocks and the distribution of oil and gas pools. The master source rocks of the Dongying Depression consist of the Upper Sha 4 and the Lower Sha 3 Members, and the oil and gas pools mainly distributed in the Eogene(accounting for 91%)are dominated by lithological, structural anticline and fault block ones. However, the wource rocks of the Zhanhua Depression consist of the Sha 3 and the Sha 1 Members, and the oil and gas pools mainly distributed in the Neogene(accounting for 90%)are dominated by buried hill draping structure ones. The analyses of subsi dence processes and fault depression extension features showed that the distribution of hydrocarbon was controlled by fault depression tectogenesis, depocenter wandering and effective source rocks.

     

    • FullText(HTML)
  • loading
    • References(32)
  • [1]
    金强. 关于东部油气富集盆地勘探可持续性的一些思考[J]. 油气地质与采收率,2002,9(1):5-8.
    [2]
    刘兴才, 杨申镳. 济阳复式油气区大油田形成条件及分布规律[J]. 成都理工学院学报,1998,25(2):276-284.
    [3]
    田在艺, 史卜庆, 罗平, 等. 渤海湾盆地复式油气聚集带高勘探程度区进一步挖潜的领域[J]. 石油学报, 2002, 23(5): 1-5.
    [4]
    张春荣. 济阳坳陷下第三系生油洼陷[J]. 复式油气田, 1996,(3):37-41.
    [5]
    Carroll A R, Bohacs K M. Stratigraphic classification of ancient lakes: balancing tectonic and climatic controls [J]. Geology, 1999,27(2): 99-102.
    [6]
    林畅松,李思田,任建业. 断陷湖盆层序地层学研究和计算机模拟[J]. 地学前缘,1995,2(3):124-132.
    [7]
    Derenne S, Largeau C, Brukner-Wein A. Origin of variations in organic mater abundance and composition in a lithologically homogeneous maar-type oil shale deposit[J]. Organic Geochemistry,2000,31: 787-798.
    [8]
    杨明慧,刘池阳. 陆相伸展盆地的层序类型、结构和序列与充填模式[J]. 沉积学报,20(2):222-227.
    [9]
    朱光有, 金强. 烃源岩的非均质性及其研究——以东营凹陷牛38井为例[J]. 石油学报,2002,23(5):34-39.
    [10]
    何斌. 海湾复式盆地动力学探讨[J]. 石油实验地质, 2001, 23(1):27-31.
    [11]
    戴俊生, 陆克政, 漆家福, 等. 渤海湾盆地早第三纪构造样式的演化[J]. 石油学报, 1998, 19(4): 16-20.
    [12]
    朱光有, 金强, 周建林, 等. 东营断陷湖盆充填模式研究[J]. 石油实验地质, 2003, 25(2):143-148.
    [13]
    朱光有, 金强, 周建林, 等. 东营断陷湖盆充填过程对烃源岩的控制作用研究[J]. 地质地球化学, 2003, 31(1).
    [14]
    郭元岭, 赵乐强, 石红霞, 等. 济阳坳陷探明石油地质储量特点分析[J]. 石油勘探与开发, 2001, 28(3):33-37.
    [15]
    胡见义, 徐树宝. 渤海湾盆地复式油气聚集区(带)的形成和分布[J]. 石油勘探与开发,1986(1):5-9.
    [16]
    赵文智, 何登发. 中国复合含油气系统的基本特征与勘探技术[J]. 石油学报, 2001, 22(1): 6-13.
    [17]
    蒋有录, 谭丽娟, 荣启宏, 等. 油气成藏系统的概念及其在东营凹陷博兴地区的应用[J]. 石油大学学报, 2002, 26(6):12-16.
    [18]
    朱光有, 金强, 周建林. 东营凹陷旋回式深湖相烃源岩研究[J]. 地质科学, 2003, 38(2): 254-262.
    [19]
    李丕龙. 富油断陷盆地油气环状分布与惠民凹陷勘探方向[J]. 石油实验地质, 2001,23(2): 146-148.
    [20]
    金强. 有效烃源岩的重要性及其研究[J]. 油气地质与采收率, 2001, 8(1): 1-4.
    [21]
    姜亮,王毅,金强. 东海盆地丽水西凹陷含油气系统与油气勘探目标[J]. 石油实验地质,2001,23(4):368-389.
    [22]
    Soreghan M J, Cohen A S. Textural and compositional variability across littoral segments of lake Tanganyika: the effect of asymmetric basin structure on sedimentation in large rift lakes[J]. AAPG Bull, 1996,80(3): 382-409.
    [23]
    Bertrand P, Lallier-Verges E, Boussafir M. Enhancement of accumulation and anoxic degradation of organic matter controlled by cyclic productivity: a mode[J].Organic Geochemistry,1993, 22: 511-520.
    [24]
    孔凡仙, 张林晔, 周文, 等. 济阳坳陷优质烃源岩层地球化学特征及成烃潜力[J]. 复式油气田, 2000, 7(3): 13-15.
    [25]
    朱光有, 金强. 东营凹陷两套优质烃源岩层地质地球化学特征研究[J]. 沉积学报,2003,21(3).
    [26]
    陈建渝, 熊书权, 毕研鹏, 等. 断陷盆地中含油气系统的特征[J]. 石油学报,2000,21(2):36-41.
    [27]
    朱光有, 金强, 王锐. 有效烃源岩的识别[J]. 石油大学学报, 2003, 27(2): 6-10.
    [28]
    吴根耀. 盆地研究的活动论构造观[J]. 石油实验地质,1998,20(4):309-318.
    [29]
    史卜庆,吴智平,王纪祥,等. 渤海湾盆地东营运动的特征及成因分析[J]. 石油实验地质,1999,21(3):196-200.
    [30]
    宗国洪, 肖焕钦, 李常宝, 等. 济阳坳陷构造演化及其大地构造意义[J]. 高校地质学报, 1999, 5(3): 275-282.
    [31]
    王同和. 中国东部含油气盆地的构造迁移[J]. 中国科学(B辑),1988,(12):1314-1322.
    [32]
    陆克政, 漆家福, 戴俊生, 等. 渤海湾新生代含油气盆地构造模式[M]. 北京: 地质出版社, 1997, 190-196.
    • 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 (867) PDF downloads(349) 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