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喀麦隆里奥—德雷盆地泥岩底辟构造与油气分布规律

袁井菊 丁一萍 苏玉山 陈占坤 哈里

袁井菊, 丁一萍, 苏玉山, 陈占坤, 哈里. 喀麦隆里奥—德雷盆地泥岩底辟构造与油气分布规律[J]. 石油实验地质, 2018, 40(4): 508-512. doi: 10.11781/sysydz201804508
引用本文: 袁井菊, 丁一萍, 苏玉山, 陈占坤, 哈里. 喀麦隆里奥—德雷盆地泥岩底辟构造与油气分布规律[J]. 石油实验地质, 2018, 40(4): 508-512. doi: 10.11781/sysydz201804508
YUAN Jingju, DING Yiping, SU Yushan, CHEN Zhankun, KHALID Abuganaya. Mud shale diapir structure and hydrocarbon distribution in the Rio del Rey Basin of Cameroon[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(4): 508-512. doi: 10.11781/sysydz201804508
Citation: YUAN Jingju, DING Yiping, SU Yushan, CHEN Zhankun, KHALID Abuganaya. Mud shale diapir structure and hydrocarbon distribution in the Rio del Rey Basin of Cameroon[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2018, 40(4): 508-512. doi: 10.11781/sysydz201804508

喀麦隆里奥—德雷盆地泥岩底辟构造与油气分布规律

doi: 10.11781/sysydz201804508
基金项目: 

国家科技重大专项“重点盆地油气勘探目标评价与优选”(2016ZX05033-002)资助。

详细信息
    作者简介:

    袁井菊(1971-),女,博士,高级工程师,从事地球物理勘探研究。E-mail:yuanjj.syky@sinopec.com。

  • 中图分类号: TE121.2

Mud shale diapir structure and hydrocarbon distribution in the Rio del Rey Basin of Cameroon

  • 摘要: 里奥-德雷(Rio del Rey)盆地位于喀麦隆境内、尼日尔三角洲(Niger Delta)东北缘,油气资源十分丰富,已有30余年油气勘探开发历史。古新世以来发生的长期海退和三角洲沉积作用,形成了现今的里奥-德雷被动大陆边缘盆地,其主要发育3个地层单元,自下而上分别为阿卡塔(Akata)组、阿格巴达(Agbada)组和贝宁(Benin)组。在三角洲进积推进过程中,由于大陆边缘的重力作用和三角洲泥岩的塑性推覆作用,由陆向海、自北向南形成了3个构造区,即伸展构造区、泥岩底辟构造区和逆冲推覆构造区。其中,在泥岩底辟构造区形成了许多与泥岩底辟或泥岩脊相关的辟顶背斜、断背斜构造圈闭或辟边岩性遮挡圈闭,现今已发现的大型油气田主要与这些圈闭有关。同时,泥岩底辟的活动也形成了储集和运移方面的优势条件,促使油气在泥岩底辟构造区富集高产。因此,未来泥岩底辟构造区以及与泥岩底辟相关的圈闭仍然是里奥-德雷盆地进一步寻找勘探潜力的主要地区。

     

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出版历程
  • 收稿日期:  2017-12-10
  • 修回日期:  2018-05-22
  • 刊出日期:  2018-07-28

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