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苏北盆地高邮凹陷基底先存断裂成因及其对新生断裂的控制

束宁凯 吴林 汪新文 郭建平

束宁凯, 吴林, 汪新文, 郭建平. 苏北盆地高邮凹陷基底先存断裂成因及其对新生断裂的控制[J]. 石油实验地质, 2017, 39(1): 8-14. doi: 10.11781/sysydz201701008
引用本文: 束宁凯, 吴林, 汪新文, 郭建平. 苏北盆地高邮凹陷基底先存断裂成因及其对新生断裂的控制[J]. 石油实验地质, 2017, 39(1): 8-14. doi: 10.11781/sysydz201701008
Shu Ningkai, Wu Lin, Wang Xinwen, Guo Jianping. Origin of pre-existing basement faults and their controls on new fault formation in Gaoyou Sag, Subei Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(1): 8-14. doi: 10.11781/sysydz201701008
Citation: Shu Ningkai, Wu Lin, Wang Xinwen, Guo Jianping. Origin of pre-existing basement faults and their controls on new fault formation in Gaoyou Sag, Subei Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(1): 8-14. doi: 10.11781/sysydz201701008

苏北盆地高邮凹陷基底先存断裂成因及其对新生断裂的控制

doi: 10.11781/sysydz201701008
基金项目: 国家科技重大专项(2011ZX05028,2011ZX05009-002)资助。
详细信息
    作者简介:

    束宁凯(1993-)女,硕士研究生,从事构造地质及油气勘探综合研究。E-mail:522345876@qq.com。

    通讯作者:

    吴林(1987-)男,博士后,从事含油气盆地分析和构造地质学研究。E-mail:19534644@sohu.com。

  • 中图分类号: TE121.2

Origin of pre-existing basement faults and their controls on new fault formation in Gaoyou Sag, Subei Basin

  • 摘要: 真武断裂和吴堡断裂是苏北盆地高邮凹陷的2条重要基底先存断裂,形成于印支期下扬子板块与华北板块的俯冲碰撞,西部走向北东东、东部走向北北东。根据区域应力场、三维地震等资料,将这2条基底断裂对南部断阶带形成和演化的控制作用分为4个阶段:(1)构造挤压期,由于下扬子区北部与华北板块东南部的碰撞,形成了一系列的冲断构造、逆冲推覆及褶皱变形;(2)构造反转期,真武断裂由逆断层反转为正断层;(3)正向裂陷期,真①断层、吴①断层继承了真武断裂分段性特点,真武断阶带、吴堡断阶带分别受真①断层、吴①断层控制强烈;(4)斜向裂陷期,真武断阶带、吴堡断阶带受基底断裂控制作用逐渐减弱,南北向张应力起主导作用。真武断阶带和吴堡断阶带存在着构造差异变形,根据基底先存断裂对新生断裂的活动方式可分为4种类型,由强至弱依次分为继承型、派生型、调节型、诱导型。研究表明,基底先存断裂是高邮凹陷南部断阶带形成演化的基础,并强烈影响着新生断裂的发育。

     

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  • 收稿日期:  2016-10-10
  • 修回日期:  2017-01-03
  • 刊出日期:  2017-01-28

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