川东南綦江地区基底走滑断裂特征及控藏意义

刘海涛, 石司宇, 李让彬. 2025. 川东南綦江地区基底走滑断裂特征及控藏意义. 沉积与特提斯地质, 45(2): 424-433. doi: 10.19826/j.cnki.1009-3850.2025.02005
引用本文: 刘海涛, 石司宇, 李让彬. 2025. 川东南綦江地区基底走滑断裂特征及控藏意义. 沉积与特提斯地质, 45(2): 424-433. doi: 10.19826/j.cnki.1009-3850.2025.02005
LIU Haitao, SHI Siyu, LI Rangbin. 2025. Basement strike-slip faults in the Qijiang area, southeastern Sichuan, and their signficance in reservoir control. Sedimentary Geology and Tethyan Geology, 45(2): 424-433. doi: 10.19826/j.cnki.1009-3850.2025.02005
Citation: LIU Haitao, SHI Siyu, LI Rangbin. 2025. Basement strike-slip faults in the Qijiang area, southeastern Sichuan, and their signficance in reservoir control. Sedimentary Geology and Tethyan Geology, 45(2): 424-433. doi: 10.19826/j.cnki.1009-3850.2025.02005

川东南綦江地区基底走滑断裂特征及控藏意义

  • 基金项目: 国家自然科学基金企业创新发展联合基金项目“海相深层油气富集机理与关键工程技术基础研究(U19B6003);中国石化科技部重点科技项目“四川盆地走滑断裂带成因及控藏机制研究”(P20062-3);中国石化股份项目“四川盆地及周缘资源评价”(P23221)
详细信息
    作者简介: 刘海涛(1985—),女,硕士,工程师,主要从事海相碳酸盐岩、断裂特征及控储控藏等相关研究工作。E-mail:407072733@qq.com
  • 中图分类号: P618.13

Basement strike-slip faults in the Qijiang area, southeastern Sichuan, and their signficance in reservoir control

  • 川东南綦江地区的油气勘探已经证实,基底走滑断裂对油气成藏具有重要的控制作用。本文基于对最新获取的三维地震资料的解译,对基底走滑断裂进行精细刻画,分析其形成和演化对油气成藏的控制作用。研究表明,綦江地区基底走滑断裂呈负花状、单条陡立状和多条陡立平行状三种剖面样式,平面上主要呈线性构造、近平行构造、雁列式构造和走滑双重构造等组合样式。基底断裂的走滑拉分强度与东吴期的古地貌高差共同控制岩溶储层的发育,主要表现为3种类型:沿不整合面的表生岩溶、隔水层之上与断裂走向强相关的顺层岩溶,以及与基底断面相关的断裂岩溶。这3类岩溶是川东南綦江地区形成碳酸盐岩优质储层的关键。东吴期活化并开启的基底断裂沟通上下烃源岩层,为茅口组油气藏的运移提供了良好通道。位于綦江地区西南部的栗子–石龙峡地区整体处于岩溶斜坡有利带,靠近基底走滑断裂,规模岩溶储层发育,同时断裂在东吴期活化沟通源岩,盖层相对稳定,为油气勘探有利区。

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  • 图 1  川东南綦江地区位置图(a)与地层综合柱状图(b)

    Figure 1. 

    图 2  綦江地区走滑断裂典型剖面特征与平面分布图

    Figure 2. 

    图 3  綦江地区基底断裂活动强度分析图

    Figure 3. 

    图 4  基底断裂对下二叠统岩溶储层发育模式的控制作用示意图

    Figure 4. 

    图 5  綦江地区及周缘二叠系茅口组天然气甲烷、乙烷碳同位素图

    Figure 5. 

    图 6  綦江地区有利区带综合评价图

    Figure 6. 

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出版历程
收稿日期:  2024-10-21
修回日期:  2024-12-18
录用日期:  2025-01-21
刊出日期:  2025-06-20

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