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鄂尔多斯盆地东部高家堡地区下古生界断裂分层变形特征及形成机制

陈平 李明瑞 李维 强敏 路鹏程 于小伟 韩伟

陈平, 李明瑞, 李维, 强敏, 路鹏程, 于小伟, 韩伟. 鄂尔多斯盆地东部高家堡地区下古生界断裂分层变形特征及形成机制[J]. 石油实验地质, 2024, 46(3): 542-552. doi: 10.11781/sysydz202403542
引用本文: 陈平, 李明瑞, 李维, 强敏, 路鹏程, 于小伟, 韩伟. 鄂尔多斯盆地东部高家堡地区下古生界断裂分层变形特征及形成机制[J]. 石油实验地质, 2024, 46(3): 542-552. doi: 10.11781/sysydz202403542
CHEN Ping, LI Mingrui, LI Wei, QIANG Min, LU Pengcheng, YU Xiaowei, HAN Wei. Characteristics and formation mechanism of stratified deformation of Lower Paleozoic faults in Gaojiapu area, eastern Ordos Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2024, 46(3): 542-552. doi: 10.11781/sysydz202403542
Citation: CHEN Ping, LI Mingrui, LI Wei, QIANG Min, LU Pengcheng, YU Xiaowei, HAN Wei. Characteristics and formation mechanism of stratified deformation of Lower Paleozoic faults in Gaojiapu area, eastern Ordos Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2024, 46(3): 542-552. doi: 10.11781/sysydz202403542

鄂尔多斯盆地东部高家堡地区下古生界断裂分层变形特征及形成机制

doi: 10.11781/sysydz202403542
基金项目: 

中国石油科学研究与技术开发项目“海相碳酸盐岩重点领域综合地质研究与高效勘探关键技术攻关” 2022KT0103

详细信息
    作者简介:

    陈平(1995—),男,硕士,工程师,从事构造地质学研究。E-mail:243801601@qq.com

  • 中图分类号: TE121.2

Characteristics and formation mechanism of stratified deformation of Lower Paleozoic faults in Gaojiapu area, eastern Ordos Basin

  • 摘要: 近年来,鄂尔多斯盆地奥陶系马家沟组五段以深地层相继取得勘探突破,揭示了其巨大的勘探潜力。随着高精度三维地震资料的部署以及油气勘探的深入,断裂对马五段以深气藏的控制作用越发凸显。基于高精度三维地震资料,在系统刻画高家堡地区断裂几何学特征的基础上,解剖断裂典型构造样式,建立断裂形成演化模式,并结合钻井试气资料探讨断裂对马五段以深气藏差异富集的控制作用。研究取得了以下认识:鄂尔多斯盆地高家堡地区下古生界断裂具有明显的分层变形特征,盆地内马三段、马五段两套膏盐岩是造成断裂分层的主要原因之一;高家堡地区下古生界主要发育具有压扭性质的走滑断裂和逆冲断裂;通过对高家堡地区地层构造形态及断裂样式的研究,推测燕山构造运动是对加里东构造运动形成的断裂影响最大的一期后期改造运动;高家堡地区地层构造隆升期与油气充注期耦合,断裂具有改善储层、沟通源岩、控制圈闭等多重作用。

     

  • 图  1  鄂尔多斯盆地东部高家堡地区研究区位置(a)和盆地中东部下奥陶统地层柱状图(b)

    Figure  1.  Regional location of study area (a) in Gaojiapu area in eastern Ordos Basin and histogram of Lower Ordovician of central and eastern Ordos Basin (b)

    图  2  鄂尔多斯盆地东部高家堡地区多层系顺层相干及断裂平面展布

    Figure  2.  Coherence and fault plane layout of multilayer system in Gaojiapu area, eastern Ordos Basin

    图  3  鄂尔多斯盆地东部高家堡地区典型地震剖面

    剖面位置见图 2

    Figure  3.  Typical seismic profile of Gaojiapu area, eastern Ordos Basin

    图  4  鄂尔多斯盆地东部高家堡地区下古生界断裂构造样式

    Figure  4.  Fault structure pattern of Lower Paleozoic in Gaojiapu area, eastern Ordos Basin

    图  5  鄂尔多斯盆地东部高家堡地区下古生界断裂分层模式

    Figure  5.  Stratification model of Lower Paleozoic faults in Gaojiapu area, eastern Ordos Basin

    图  6  鄂尔多斯盆地东部高家堡地区下伏凸起带活动性

    Figure  6.  Activity of underlying uplift zone in Gaojiapu area, eastern Ordos Basin

    图  7  鄂尔多斯盆地东部高家堡地区奥陶系马家沟组四段底断裂活动性

    Figure  7.  Activity of bottom faults of fourth member of Ordovician Majiagou Formation in Gaojiapu area, eastern Ordos Basin

    图  8  鄂尔多斯盆地东部高家堡地区断裂与构造分层结构

    Figure  8.  Fault and stratified structure of Gaojiapu area, eastern Ordos Basin

    图  9  鄂尔多斯盆地东部高家堡地区加里东期断裂形成演化及后期改造立体模式

    Figure  9.  Stereoscopic model of Caledonian fault formation and evolution and late reconstruction in Gaojiapu area, eastern Ordos Basin

    图  10  鄂尔多斯盆地东部高家堡地区米探1井与米探2井油藏剖面

    Figure  10.  Reservoir profiles of wells Mitan 1 and Mitan 2 in Gaojiapu area, eastern Ordos Basin

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出版历程
  • 收稿日期:  2023-06-25
  • 修回日期:  2024-03-29
  • 刊出日期:  2024-05-28

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