石油与天然气地质 ›› 2021, Vol. 42 ›› Issue (6): 1435-1439, 1474.doi: 10.11743/ogg20210617

• 油气地质 • 上一篇    下一篇

尼日尔三角洲里奥-德雷盆地泥底辟变形与形成演化特征

余一欣1,2(), 王涛1,2, 陈占坤3, 苏玉山3, 张纪新1,2, 吴世祥3   

  1. 1. 中国石油大学(北京) 油气资源与探测国家重点实验室, 北京 102249
    2. 中国石油大学(北京) 地球科学学院, 北京 102249
    3. 中国石化 石油勘探开发研究院, 北京 100083
  • 收稿日期:2021-02-15 出版日期:2021-12-28 发布日期:2021-12-16
  • 第一作者简介:余一欣(1977-), 男, 博士、副教授, 盆地分析和构造地质学。E-mail: yuxin0707@163.com
  • 基金项目:
    国家科技重大专项(2016ZX05033-002);国家科技重大专项(2016ZX05033-001);国家重点研发计划项目(2017YFC0603105)

Deformation and evolution of mud diapirs in Rio Del Rey Basin, Niger Delta

Yixin Yu1,2(), Tao Wang1,2, Zhankun Chen3, Yushan Su3, Jixin Zhang1,2, Shixiang Wu3   

  1. 1. State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum(Beijing), Beijing 102249, China
    2. College of Geosciences, China University of Petroleum(Beijing), Beijing 102249, China
    3. Research Institute of Petroleum Exploration and Development, SINOPEC, Beijing 100083, China
  • Received:2021-02-15 Online:2021-12-28 Published:2021-12-16

摘要:

尼日尔三角洲东北部的里奥-德雷盆地发育多条阿卡塔组泥底辟构造带,对油气成藏产生了重要影响。根据泥岩隆升幅度及其与周围地层的接触关系,可将泥底辟划分为复杂形态刺穿型和简单形态隐伏型两类。平面上,泥底辟主要呈近SN向的条带状和圆点状展布,并影响上覆地层的发育,形成3类正断层。泥底辟主要经历了中渐新世之前的初始沉积-微弱活动期、晚渐新世-中新世的强烈隆升活动期以及上新世至今的微弱活动-整体埋藏期等3个形成演化阶段。泥底辟的发育除受到重力滑动作用及上覆地层的差异负载作用影响外,还受到盆地东南部大西洋转换断层及泥下基底断裂的影响。对里奥-德雷盆地泥底辟构造发育特征的研究,有助于分析泥底辟对圈闭、储层发育以及油气运移的影响。

关键词: 阿卡塔组, 泥底辟, 断层, 里奥-德雷盆地, 尼日尔三角洲

Abstract:

Several mud diapir belts developed in the Akata Formation mudstone are closely linked to the accumulation of hydrocarbon in the Rio Del Rey Basin, northeast Niger delta. According to their heights and contact relationships to peripheral strata, the mud diapirs can be divided into complicated pierced and simple buried styles, with S-N trending elongations or scattering dots in a plane view. Influenced by mud diapirs, three kinds of normal faults have developed in the overburden. The evolution of mud diapirs experienced three stages: the deposition and weak activity stage before the middle Oligocene, intense rising stage during the late Oligocene and Miocene, and weak activity and buried stage after the Miocene. In addition to the influence exerted by gravitational sliding and differential loading induced from the overburden, the formation of mud diapirs are also subjected to some Atlantic transform faults in the southeast part of the Rio Del Rey Basin and basement faulting activities. The study is helpful to the analysis of the impact of these diapirs upon the development of traps and reservoirs as well as hydrocarbon migration in the basin.

Key words: Akata Formation, mud diaper, fault, Rio Del Rey Basin, Niger Delta

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