石油学报 ›› 2009, Vol. 30 ›› Issue (6): 816-823.DOI: 10.7623/syxb200906005

• 地质勘探 • 上一篇    下一篇

渤海湾盆地变换构造特征及其成藏意义

杨明慧1,2   

  1. 1. 中国石油大学资源与信息学院, 北京, 102249;
    2. 中国石油大学油气资源与探测国家重点实验室, 北京, 102249
  • 收稿日期:2008-12-26 修回日期:2009-02-12 出版日期:2009-11-25 发布日期:2009-05-25
  • 作者简介:杨明慧,男,1962年8月生,1998年获中国地质大学(武汉)博士学位,现在中国石油大学(北京)从事盆地构造分析等方面的教学和研究工作.E-mail:yangmh@cup.edu.cn
  • 基金资助:

    国家自然科学基金重点项目(No.90814005)资助

Transfer structure and its relation to hydrocarbon exploration in Bohai Bay Basin

YANG Minghui1,2   

  1. 1. Faculty of Natural Resource and Information Technology, China University of Petroleum, Beijing 102249, China;
    2. State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249, China
  • Received:2008-12-26 Revised:2009-02-12 Online:2009-11-25 Published:2009-05-25

摘要:

依据前人对变换构造的分类研究,分析了渤海湾盆地变换构造的特征。将渤海湾盆地变换构造分为变换带和变换断层两种类型:一般表现为变换带样式,尤其是在盆地或坳陷层次;而变换断层仅在局部的控凹层次上有所体现。高级别的变换带大多数是由一系列不同类型的传递斜坡横向串联而成,间或发育变换断层。北西西—北西向的变换构造是渤海湾盆地"南北分块"构造格局的主控构造样式,而渤海湾盆地油气储量的差异与变换构造控制的富生烃凹陷及洼陷分布有关。变换构造控制的古地形和富砂水系通道有利于形成岩性油气藏,变换构造邻区的高部位则是发现(潜山)构造油气藏的重要地区。

关键词: 变换带, 变换断层, 变换构造, 油气成藏, 渤海湾盆地

Abstract:

On the basis of the previous classification research, the features of transfer structure in Bohai Bay Basin were analyzed. The transfer structures in Bohai Bay Basin can be divided into two styles of transfer zone and transfer fault according to the connection or non-connection status. The transfer structure in Bohai Bay Basin is mainly exhibited in the style of transfer zone, especially in basin or depression, while the transfer fault only militates in the sag-control level. With the occasional development of transfer fault, most of high-level transfer zones are horizontally connected with different relay ramps. These strike transfer structures in NWW-NW direction are the most important structure styles to control the "north-south segmentation" tectonic framework in Bohai Bay Basin. The difference of oil and gas reserves in Bohai Bay Basin is related to the distribution of prolific hydrocarbon depressions and sags controlled by transfer structure. The paleotopography and rich-sand drainage channels controlled by transfer structure are favorable to the formation of lithologic reservoirs. The adjacent zones of the transfer structure are the important regions for finding the buried-hill structure reservoirs.

Key words: transfer structure, transfer zone, transfer fault, hydrocarbon accumulation, Bohai Bay Basin

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