石油学报 ›› 2019, Vol. 40 ›› Issue (3): 268-278.DOI: 10.7623/syxb201903002

• 地质勘探 • 上一篇    下一篇

燕山地区中元古界页岩气成藏地质条件

刘静1, 周志2, 刘喜恒1, 任收麦3, 汪剑1, 王浩4, 周从安1, 刘一珉4   

  1. 1. 中国石油华北油田公司勘探开发研究院 河北任丘 062552;
    2. 中国地质调查局油气资源调查中心 北京 100083;
    3. 中国地质调查局 北京 100037;
    4. 中国地质大学(北京)地球科学与资源学院 北京 100083
  • 收稿日期:2017-12-04 修回日期:2018-11-21 出版日期:2019-03-25 发布日期:2019-03-29
  • 通讯作者: 周志,男,1983年9月生,2007年获中国地质大学(北京)石油工程专业学士学位,2010年获中国地质大学(北京)矿产普查与勘探专业硕士学位,现为中国地质调查局油气资源调查中心高级工程师,主要从事页岩油气地质研究工作。Email:zhouzhi-2008@126.com
  • 作者简介:刘静,女,1974年5月生,2004年获石油大学(华东)资源勘查工程专业本科学历,现为中国石油华北油田公司勘探开发研究院高级工程师,主要从事石油地质综合研究工作。Email:wty_ljj@petrochina.com.cn
  • 基金资助:

    中国石油华北油田公司科技项目"冀北中新元古界有利区评价及突破口选择"(HBYT-WTY-2015-JS-290)资助

Geological conditions of the Mesoproterozoic shale gas accumulation in Yanshan area,North China

Liu Jing1, Zhou Zhi2, Liu Xiheng1, Ren Shoumai3, Wang Jian1, Wang Hao4, ZHOU Cong'an1, Liu Yimin4   

  1. 1. Exploration and Development Research Institute, PetroChina Huabei Oilfield Company, Hebei Renqiu 062552, China;
    2. Oil and Gas Survey Center, China Geological Survey, Beijing 100083, China;
    3. China Geological Survey, Beijing 100037, China;
    4. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
  • Received:2017-12-04 Revised:2018-11-21 Online:2019-03-25 Published:2019-03-29

摘要:

燕山地区发育中元古界洪水庄组和下马岭组2套富有机质泥页岩,勘探程度低,页岩气资源的勘探潜力不明。对河北怀来、宽城和北京十三陵等地区开展野外地质调查,并对冀元1井、冀浅1井和京101井的中元古界黑色页岩开展岩心观察和实验分析,研究了洪水庄组和下马岭组黑色页岩的沉积相分布、有机质丰度、有机质类型、热成熟度、孔渗性和岩石矿物特征等页岩气成藏地质条件。研究表明,燕山地区洪水庄组和下马岭组的页岩厚度大、有机质含量高、热演化程度适中、生烃时间晚、受晚期构造活动破坏作用小,具备良好的页岩气成藏地质条件;河北承德-宽城一带稳定构造带为勘查洪水庄组页岩气的有利区;河北涿州-北京房山-门头沟-昌平一带和河北兰旗营子一带稳定的构造带为勘查下马岭组页岩气的有利区。

关键词: 页岩气, 成藏地质条件, 有利区, 中元古界, 燕山地区

Abstract:

Two sets of organic-rich shale are developed in Yanshan area,including Mesoproterozoic Hongshuizhuang Formation and Xiamaling Formation. Because of low exploration level,the exploration potential of these shale gas resource is unknown. Based on the field geological survey in the Huailai county and Kuancheng county of Hebei province and the Ming Tombs area of Beijing,and the observation and experimental test of Mesoproterozoic black shale cores in Wells Jiyuan-1,Jiqian-1 and Jing-101,the geological conditions of shale gas accumulation in black shale of Hongshuizhuang Formation and Xiamaling Formation are studied,including the sedimentary facies distribution,abundance and type of organic matter,thermal maturity,porosity,permeability and rock mineral features. Research result shows that the shale in Hongshuizhuang Formation and Xiamaling Formation is characterized by large thickness,high organic matter content,moderate thermal evolutionary degree,late hydrocarbon generation,little destructive effect from late tectonic activity,and favorable accumulation geological conditions. The shale gas favorable area for Hongshuizhuang Formation is in the stable tectonic zone from Chengde to Kuancheng of Hebei province; and the area for Xiamaling Formation is in the stable tectonic zone from Zhuozhou of Hebei province to Fangshan,Mentougou and Changping of Beijing,as well as in the Lanqiyingzi area of Hebei province.

Key words: shale gas, accumulation geological conditions, favorable area, Mesoproterozoic, Yanshan area

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