油气勘探

尼日尔Termit裂谷型叠合盆地油气成藏特征与主控因素

  • 周立宏 ,
  • 苏俊青 ,
  • 董晓伟 ,
  • 史卜庆 ,
  • 孙志华 ,
  • 钱茂路 ,
  • 楼达 ,
  • 刘爱平
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  • 1. 中国石油大港油田公司勘探开发研究院,天津 300280;
    2. 中国石油天然气勘探开发公司,北京 100034
周立宏(1968- ),男,河北故城人,博士,中国石油大港油田公司教授级高级工程师,主要从事油气勘探开发科研与管理工作。地址:天津市滨海新区,大港油田勘探开发研究院502室,邮政编码:300280。E-mail: zhoulh@petrochina.com.cn.

收稿日期: 2017-02-13

  修回日期: 2017-04-27

  网络出版日期: 2017-05-26

基金资助

中国石油海外科技专项(CNPCNP/01/2015-0790; CNPCNP/01/2016-0920)

Controlling factors of hydrocarbon accumulation in Termit rift superimposed basin, Niger

  • ZHOU Lihong ,
  • SU Junqing ,
  • DONG Xiaowei ,
  • SHI Buqing ,
  • SUN Zhihua ,
  • QIAN Maolu ,
  • LOU Da ,
  • LIU Aiping
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  • 1. Exploration & Development Research Institute of PetroChina Dagang Oilfield Company, Tianjin 300280, China;
    2. China National Oil and Gas Exploration and Development Corporation, Beijing 100034, China

Received date: 2017-02-13

  Revised date: 2017-04-27

  Online published: 2017-05-26

摘要

基于中—西非裂谷系构造演化及沉积充填特征研究,结合区域地质背景,对尼日尔Termit裂谷型叠合盆地的油气成藏特征进行剖析,并探讨其油气富集主控因素。Termit盆地是早白垩世、古近纪2期断陷活动形成的裂谷型叠合盆地,发育1套广泛分布的上白垩统Yogou组海相烃源岩。古近系Sokor组1段和白垩系Yogou组2套储集层以石英砂岩为主,具有较好的孔渗特征,在古近系Sokor组2段区域盖层之下可形成多套有利储盖组合。断裂样式与油气运聚方式决定了构造带油气运聚模式,形成Araga地堑“Y”型油气侧向及垂向运聚模式、Dinga断阶“多阶型”油气垂向运聚模式和Fana转换带“复式”油气运聚模式。油气富集受裂谷盆地构造控制,即2期裂谷作用形成的断裂带控制油气的平面展布,晚期裂谷层序内的有利储盖组合控制油气垂向富集程度。图13表1参23

本文引用格式

周立宏 , 苏俊青 , 董晓伟 , 史卜庆 , 孙志华 , 钱茂路 , 楼达 , 刘爱平 . 尼日尔Termit裂谷型叠合盆地油气成藏特征与主控因素[J]. 石油勘探与开发, 2017 , 44(3) : 330 -339 . DOI: 10.11698/PED.2017.03.02

Abstract

Based on the tectonic evolution and depositional characteristics of Central-West African Rift System and regional geologic background, the characteristics of oil and gas accumulation in the Termit rift superimposed basin were examined, and the factors controlling oil and gas accumulation there were discussed. The Termit basin is a rift superimposed basin formed by two stages of rifting in the early Cretaceous and Paleogene, where the Yogou Formation marine source rock is widespread. The two sets of reservoirs, the first member of the Paleogene Sokor Formation and the Cretaceous Yogou Formation, dominated by quartz sandstone, have relatively good porosity-permeability characteristics. They can form multiple sets of favorable caprock-reservoir assemblage below the regional caprock of the second member of Paleogene Sokor Formation. It is found that fault pattern and oil and gas migration pattern control the oil and gas accumulation patterns in the basin, including “Y-shaped” hydrocarbon migration and accumulation in the Araga graben, “multi-step” vertical hydrocarbon migration and accumulation in the Dinga faulted terrace, and the “composite” hydrocarbon migration and accumulation in the Fana transfer zone. Hydrocarbon enrichment in this basin was controlled by tectonic evolution of rift basins, that is, fault belts formed during the two stages of rifting controlled the horizontal distribution of oil and gas, while favorable reservoir-caprock assemblages in the sequences formed in the late rifting stage controlled the vertical hydrocarbon enrichment.

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