天然气地球科学 ›› 2011, Vol. 22 ›› Issue (4): 670–673.doi: 10.11764/j.issn.1672-1926.2011.04.670

• 天然气地质学 • 上一篇    下一篇

缅甸俯冲增生带的构造特征及勘探前景

 蔡文杰, 朱光辉, 姜烨, 杨松岭, 李爱山, 谢楠   

  1. 中海油研究总院,北京 100027
  • 收稿日期:2010-11-12 修回日期:2011-01-31 出版日期:2011-08-10 发布日期:2011-08-10
  • 通讯作者: 蔡文杰caiwj@cnooc.com.cn. E-mail:caiwj@cnooc.com.cn.
  • 作者简介:蔡文杰(1980-),男,河北保定人,工程师,硕士,主要从事石油地质和层序地层学研究.
  • 基金资助:

    中海石油(中国) 有限公司科技攻关项目(编号:2010-HW-03-02) 资助.

Structurl Features and Exploration Prospect ofSubduction-accretionary Belt in Myanmar

 CAI   Wen-Jie, ZHU   Guang-Hui, JIANG  Ye, YANG  Song-Ling, LI  Ai-Shan, XIE  Nan   

  1. CNOOC Research Institute,Beijing 100027,China
  • Received:2010-11-12 Revised:2011-01-31 Online:2011-08-10 Published:2011-08-10

摘要:

汇聚板块边缘俯冲增生带的构造活动与油气勘探潜力研究一直都是石油地质界的难点,地处印度板块与欧亚板块交会处的缅甸若开海岸是开展这一研究的绝佳区域。通过对缅甸俯冲增生带的钻井、地质露头以及地震资料的认真分析,将研究区划分为增生楔主体、斜坡盆地和海沟3个构造单元,并在此基础上探讨了各构造单元的油气勘探前景,指出位于孟加拉湾东侧的海沟地区油气成藏条件最为优越,寻找深水浊积砂体应成为该区重点勘探方向之一。

关键词: 俯冲增生带, 增生楔, 斜坡盆地, 海沟, 缅甸

Abstract:

The tectonic activity and exploration potential analysis of subduction-accretionary belt at plate convergent margins are always difficult problems in oil geologic field.Myanmar is a favorite place for the study,which lies in the conjunction area of the Eurasian Plate and Indian Plate.The tectonic evolution,structural domain division and petroleum exploration prospects are studied based on the carefully study on the wells,outcrops,seismic data and regional background information.It can be divided into three structural domains:Accretionary wedge,slope basin and trench.The hydrocarbon accumulation condition is favorable in Bengal fan trench region,and hunting for turbidite sand bodies and subtle reservoirs is the key to petroleum exploration.

Key words: Subduction-accretionary belt, Accretionary wedge, Slope basin, Trench, Myanmar.

中图分类号: 

  • TE121.2

[1]Howell D G.The Future of Energy Gases[M].Translated by Yang Dengwei,Li Dagen,et al.Beijing:Petroleum Industry Press,1999:374-384.[豪厄尔 D G.能源气的未来[M].杨登维,李大艮,等译.北京:石油工业出版社,1999:374-384.]
[2]Ding Weiwei,Cheng Xiaogan,Chen Hanlin,et al.Geological characteristics and tectonic mechanism of Taiwan accretionary prism:Evidences from a muti-channel seismic profile of a “973”survey[J].Journal of Tropical Oceanography,2005,24(5):53-59.[丁巍伟,程晓敢,陈汉林,等.台湾增生楔的构造单元划分及其变形特征[J].热带海洋学报,2005,24(5):53-59.]
[3]Huang C H,Wu W Y,Chang C P.Tectonic evolution of accretionary prism in the arc-continent collision terrane of Taiwan[J].Tectonophysics,1997,281:31-51.
[4]Westbrook G K,Ladd J W,Buhl P.Cross section of an accretionary wedge:Barbados ridge complex[J].Geology:Boulder,1998,16(7):631-635.
[5]Xie Nan,Jiang Ye,Zhu Guanghui,et al.The mechanism of  secondary porosity in Oligocene reservoir in Southern Shewbo basin,Myanmar[J].Natural Gas Geoscience,2010,21(2):289-294.[谢楠,姜烨,朱光辉,等.缅甸睡宝盆地南部地区渐新统储层次生孔隙形成机理分析[J].天然气地球科学,2010,21(2):289-294.]
[6]Lai Jiangde,Zhang Jinduo,Cai Dongdi,et al.An analysis of the seismic structural style of the M block in Myanmar[J].Geophysical & Geochemical Exploration,2009,33(1):24-26.[赖江德,张进铎,蔡东地,等.缅甸M区块地震构造样式分析与研究[J].物探与化探,2009,33(1):24-26.]
[7]Hu Ziduo,He Zhenhua,Wang Yuchao,et al.Comprehensive static correction and its application for high-steep structure in east Sichuan basin[J].Natural Gas Geoscience,2010,21(6):1046-1053.[胡自多,贺振华,王宇超,等.综合静校正技术及其在川东高陡构造区应用效果[J].天然气地球科学,2011,21(6):1046-1053.]
[8]Mahmood Alam,M  Mustafa Alam,Joseph R  Curray,et al.An overview of the sedimentary geology of the Bengal basin in relation to the regional tectonic framework and basin-fill history[J].Sedimentary Geology,2003,155(3/4):179-208.

 

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[2] 蔡文杰,朱光辉,姜烨,杨松岭,李爱山. 增生楔油气地质特征及勘探潜力——以缅甸某区块为例[J]. 天然气地球科学, 2012, 23(4): 742-747.
[3] 谢楠, 姜烨, 朱光辉, 李爱山, 蔡文杰, 吕栋, 聂志勐. 缅甸睡宝盆地南部地区渐新统储层次生孔隙形成机理分析[J]. 天然气地球科学, 2010, 21(2): 289-294.
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