西南石油大学学报(自然科学版) ›› 2016, Vol. 38 ›› Issue (6): 49-60.DOI: 10.11885/j.issn.1674-5086.2016.06.07.01

• 地质勘探 • 上一篇    下一篇

渝南-黔北五峰组-龙马溪组页岩气地质特征

康建威1,2, 余谦1, 闫剑飞1, 孙媛媛1, 戚明辉3,4   

  1. 1. 成都地质调查中心, 四川 成都 610081;
    2. 成都理工大学沉积地质研究院, 四川 成都, 610059;
    3. 页岩气评价与开采四川省重点实验室, 四川 成都 610091;
    4. 四川省煤田地质局, 四川 成都 610072
  • 收稿日期:2016-06-07 出版日期:2016-12-01 发布日期:2016-12-01
  • 通讯作者: 康建威,E-mail:best_kang@163.com
  • 作者简介:康建威,1980生,男,汉族,河南鄢陵人,博士研究生,主要从事沉积与油气地质研究。E-mail:best_kang@163.com;余谦,男,1966年生,男,汉族,四川达州人,教授级高级工程师,主要从事南方海相油气地质研究。E-mail:cdyqian@126.com;闫剑飞,1979年生,男,汉族,河南永城人,博士研究生,主要从事沉积与油气地质研究。E-mail:flyflags@126.com;孙媛媛,1980生,女,汉族,山东东营人,博士,主要从事有机地球化学,油气地质研究。E-mail:cgssunyy@163.com;戚明辉,1984生,男,汉族,浙江余姚人,硕士研究生,主要从事实验地质方面的研究工作。E-mail:13880786786@163.com
  • 基金资助:
    中国地质调查局项目(12120114071701)。

Geological Characteristics of Wufeng-Longmaxi Formations in Southern Chongqing-Northern Guizhou Area

KANG Jianwei1,2, YU Qian1, YAN Jianfei1, SUN Yuanyuan1, QI Minghui3,4   

  1. 1. Chengdu Center, China Geological Survey, Chengdu, Sichuan 610081, China;
    2. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, Sichuan 610059, China;
    3. Sichuan Key Laboratory of Shale Gas Evaluation and Exploitation, Chengdu, Sichuan 610091, China;
    4. Sichuan Coalfield Geology Bureau, Chengdu, Sichuan 610072, China
  • Received:2016-06-07 Online:2016-12-01 Published:2016-12-01

摘要: 通过大量野外露头、钻井岩芯观察,以下古生界五峰组-龙马溪组富有机质泥岩为研究对象,结合有机地化、显微薄片、X-衍射、孔渗、比表面积、扫描电镜等实验测试分析手段,综合分析了五峰组-龙马溪组页岩气基本地质特征。研究表明,在浅水陆棚-深水陆棚的沉积格局控制下,研究区富有机质页岩具有南薄北厚(10~80 m)的分布特征;富有机质页岩总体平均有机碳含量大于2.0%,为腐泥型I型干酪根,有机质成熟度程度高(Ro为0.82%~3.04%);富有机质泥岩物性特征为低孔-低渗型,发育多种微观孔隙结构。在此基础上,通过页岩气区块优选和评价,认为安场-道真向斜区具备良好的页岩气富集基础地质条件,具有良好的页岩气勘探前景。

关键词: 渝南-黔北, 下古生界, 富有机质页岩, 页岩气地质条件

Abstract: Through observation of outcrop, drilling core and the organic-rich mudstone in Wufeng-Longmaxi, and with organic geochemistry, microscopic section, X-ray diffraction, pore permeability, specific surface area, and scanning electron microscope, we analyzed the basic geological characteristics of shale gas reservoir in Wufeng-Longmaxi formation. The analysis shows that the Wufeng-Longmaxi shelf environment is the foun-dation of organic rich mud shale. The sedimentary pattern of shallow shelf and deep water shelf determines the mudstone distribution which is thin in the South(10-80 m). Deepwater mudstone average organic carbon content is greater than 2.0%, and the organic matter is of type I kerogen of sapropel type, with high degree of maturity(Ro=0:82%-3.04%). The reservoir is of low porosity and low permeability, with various micro pore structures.Through shale gas block assessment and selection, we conclude that the Anchang-Daozhensyncline area is of favorable geological conditions for shale gas enrichment and has a good prospect for shale gas exploration.

Key words: Southern Chongqing-northern Guizhou, Wufeng-Longmaxi formations, organic-rich mudstone, shale gas geological condition

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