复杂构造背景区页岩气富集条件研究——以大巴山前缘地区为例

康建威; 林小兵; 余谦; 田景春; 门玉澎; 闫剑飞; 林家善; 孙媛媛

doi:10.11781/sysydz201704437

复杂构造背景区页岩气富集条件研究——以大巴山前缘地区为例

doi: 10.11781/sysydz201704437

1.
成都理工大学沉积地质研究院, 成都 610059
2. 成都地质调查中心, 成都 610081

基金项目: 中国地质调查局“四川盆地下古生界海相页岩气基础地质调查”（DD20160176）和重庆市国土资源和房屋管理局“重庆富有机质页岩沉积特征与储层评价研究”（渝地调设审字[2013]032号）资助。

详细信息

作者简介:
康建威(1980—),男,在读博士,工程师,从事沉积与油气地质研究。E-mail:best_kang@163.com。

通讯作者:
林小兵(1980—),博士,讲师,从事沉积地质学的教学与科研工作。E-mail:linxiaobing07@cdut.cn。

中图分类号: TE132.2
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出版历程
- 收稿日期: 2017-03-06
- 修回日期: 2017-06-10
- 刊出日期: 2017-07-28

Shale gas enrichment conditions in complex geological structure areas: A case study in the front margin of Daba Mountain

1.
Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu, Sichuan 610059, China
2. Chengdu Center, China Geological Survey, Chengdu, Sichuan 610081, China

摘要

摘要: 通过大巴山前缘地区五峰—龙马溪组富有机质泥岩的野外露头、钻井、岩心等资料的研究，对一系列岩石样品进行了显微薄片、扫描电镜、有机地化、孔渗性、比表面积、含气性解析等多项实验测试分析，对五峰—龙马溪组页岩气的富集条件进行了综合研究。结果表明：大巴山前缘地区富有机质泥岩总体处在浅水—深水陆棚沉积环境下，其沉积厚度在40~70 m左右，平均有机碳含量大于2%；有机质类型为腐泥型Ⅰ型干酪根，有机质成熟度多数为0.82%~3.04%，达到高—过成熟阶段；低渗透—低孔特征，并发育多种微观空隙结构。典型钻井解剖分析认为，页岩气保存条件是该区富集条件中最为关键的因素；未被断裂破坏的箱状背斜是最为有利的构造保存条件。
- 富有机质泥岩 /
- 页岩气富集条件 /
- 构造复杂区 /
- 五峰—龙马溪组 /
- 大巴山前缘
Abstract: A series of investigations on both outcrops and drilling cores from the front edge of Daba Mountain were carried out. Organic-rich mudstones collected from the Wufeng-Longmaxi formations in Fengjie-Kaixian-Baiquan-Manyue areas were sampled and analyzed. Information was obtained from thin sections and Scanning Electron Microscopy (SEM), and some relevant laboratory tests including organic geochemistry, X-ray diffraction, He-porosity and permeability and Specific Surface Area were made to summarize the basic geological conditions of Wufeng-Longmaxi formations in the study area. The results show that the organic-rich mudstones in the front edge of Daba Mountain were probably formed in a shallow to deep shelf during the Late Ordovician-Early Silurian. The thicknesses of these mudstones range 40-70 m, and the average total organic carbon (TOC) content is more than 2%. The kerogen mainly shows characteristics of type Ⅰ. The thermal maturity of mudstones ranges 0.82%-3.04%, indicating a high to over mature stage. Additionally, the features of low permeability and low porosity as well as several types of pore microstructures were observed in these mudstones. The analyses of typical wells indicate that the preservation of shale gas is a key element for hydrocarbon accumulation. The well-preserved box-shaped anticlines are most favorable for shale gas preservation.
- organic-rich mudstone /
- shale gas preservation condition /
- complex geological structure area /
- Wufeng-Longmaxi formations /
- front margin of Daba Mountain

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