古地理学报 ›› 2020, Vol. 22 ›› Issue (2): 235-250. doi: 10.7605/gdlxb.2020.02.074

• 岩相古地理学及沉积学 • 上一篇    下一篇

四川盆地震旦系灯影组不同古地理环境下丘滩储集体的差异性*

徐哲航1,2, 兰才俊1,2, 郝芳3, 陈浩如4, 杨伟强1,2, 马肖琳2,5, 邹华耀1,2   

  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 中国石油大学(华东)地球科学与技术学院,山东青岛 266580;
    4 中国地质大学(武汉)资源学院,湖北武汉 430074;
    5 中国海洋石油南海东部石油管理局,广州深圳 518067
  • 收稿日期:2019-07-15 修回日期:2019-12-01 出版日期:2020-04-01 发布日期:2020-03-30
  • 通讯作者: 邹华耀,男,1963年生,教授,博士生导师,主要从事油气成藏机理教学与科研工作。E-mail: huayaozou@cup.edu.cn。
  • 作者简介:徐哲航,男,1993年生,博士研究生,主要从事四川盆地碳酸盐岩储层研究。E-mail: xuzhehang93@outlook.com。
  • 基金资助:
    *中国科学院战略性先导科技专项(A类)(编号:XDA14010306),国家自然科学基金项目(编号:U1663210),国家科技重大专项(编号:2017ZX05005-003-003)共同资助

Difference of mound-bank complex reservoir under different palaeogeographic environment of the Sinian Dengying Formation in Sichuan Basin

Xu Zhe-Hang1,2, Lan Cai-Jun1,2, Hao Fang3, Chen Hao-Ru4, Yang Wei-Qiang1,2, Ma Xiao-Lin2,5, Zou Hua-Yao1,2   

  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 School of Geosciences,China University of Petroleum(East China),Qingdao 266580,China;
    4 Faculty of Earth Resources,China University of Geosciences(Wuhan),Wuhan 430074,China;
    5 CNOOC Nanhai East Petroleum Bureau,Shenzhen 518067,China
  • Received:2019-07-15 Revised:2019-12-01 Online:2020-04-01 Published:2020-03-30
  • Contact: Zou Hua-Yao,born in 1963,professor,is mainly engaged in petroleum generation and accumulation. E-mail: huayaozou@cup.edu.cn.
  • About author:Xu Zhe-Hang,born in 1993,Ph.D. candidate,is mainly engaged in carbonate reservoir in the Sichuan Basin. E-mail: xuzhehang93@outlook.com.
  • Supported by:
    Co-funded by the Strategic Priority Research Program of the Chinese Academy of Sciences(No. XDA14010306),the National Natural Science Foundation of China(No. U1663210)and the National Science and Technology Major Project(No.2017ZX05005-003-003)

摘要: 四川盆地震旦系灯影组丘滩沉积体广泛发育,具有很好的储集价值。基于露头勘查与岩心观测获取的资料,通过薄片鉴定、孔隙度、渗透率测试等方法分析丘滩储集体的储集性能。结果表明,由于震旦纪末期绵阳—长宁裂陷槽的发育影响了灯二段与灯四段碳酸盐岩台地相带展布,导致形成不同的古地理环境,目前可识别出高能环境、过渡环境、低能环境下发育的丘滩岩石类型,即以胡家坝剖面灯四段为代表的并进型丘滩多沉积高能环境岩石类型,以杨坝剖面灯二段为代表的追补型丘滩多沉积过渡环境岩石类型,以福成剖面灯四段为代表的饥饿型丘滩多沉积低能环境岩石类型。通过分析3种丘滩类型的储集空间与经历的准同生期成岩作用,并比较它们的物性特征,认为并进型丘滩体为最好的储集层。该研究成果有助于寻找优质储集层的发育位置,进而为四川盆地灯影组油气勘探提供参考。

关键词: 古地理环境, 丘滩复合体, 微生物岩, 碳酸盐岩储集层, 震旦系, 灯影组, 四川盆地

Abstract: The mound-bank deposits of the Dengying Formation of the Sinian System are well developed in Sichuan Basin,with good reservoir value. Based on outcrop and core observation,thin section observation,porosity and permeability of samples test,we analyzed the reservoir quality of different mound-bank complexes. During the terminal of Sinian Period,development of the Mianyang-Changning rift affected distribution of sedimentary facies of the 2nd and the 4th Members of Dengying Formation,forming different palaeogeographic units. The high-energy environment,transition environment and low-energy environment of the mound-bank complex rock types are identified,and their reservoir quality is different. The keep-up platform margin mound-bank complex,which is represented by Hujiaba section in the 4th Member of the Dengying Formation mainly deposited high-energy zone rock types. The catch-up platform margin mound-bank complex,which is represented by Yangba section in the 2nd Member of the Dengying Formation,mainly deposited transform zone rock types. The give-up platform interior mound-bank complex,which is represented by Fucheng section in the 4th Member of the Dengying Formation mainly deposited low-energy zone rock types. By comparing reservoir characteristics of three types of mound-bank complex,it is found that the keep-up platform margin mound-bank complex is the‘Sweet spots’ of the Dengying Formation in the Sichuan Basin. The above studies are conducive to find the‘Sweet spots’ of the Sinian Dengying Formation in the Sichuan Basin.

Key words: palaeogeographic environment, mound-bank complex, microbialite, carbonate reservoir, Sinian, Dengying Formation, Sichuan Basin

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