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准噶尔盆地西北缘乌夏断裂带构造特征及物理模拟实验

李萧 劳海港 胡秋媛 赵利

李萧, 劳海港, 胡秋媛, 赵利. 准噶尔盆地西北缘乌夏断裂带构造特征及物理模拟实验[J]. 石油实验地质, 2017, 39(4): 567-572. doi: 10.11781/sysydz201704567
引用本文: 李萧, 劳海港, 胡秋媛, 赵利. 准噶尔盆地西北缘乌夏断裂带构造特征及物理模拟实验[J]. 石油实验地质, 2017, 39(4): 567-572. doi: 10.11781/sysydz201704567
Li Xiao, Lao Haigang, Hu Qiuyuan, Zhao Li. Tectonic evolution and its physical simulation of Wuxia fault belt in the northwestern margin of Junggar Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(4): 567-572. doi: 10.11781/sysydz201704567
Citation: Li Xiao, Lao Haigang, Hu Qiuyuan, Zhao Li. Tectonic evolution and its physical simulation of Wuxia fault belt in the northwestern margin of Junggar Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(4): 567-572. doi: 10.11781/sysydz201704567

准噶尔盆地西北缘乌夏断裂带构造特征及物理模拟实验

doi: 10.11781/sysydz201704567
基金项目: 国家自然科学基金项目(40772132)和中国石油大学胜利学院重点科研计划项目(KY2015013)资助。
详细信息
    作者简介:

    李萧(1987—),硕士,助教,从事构造地质学研究。E-mail:136930394@qq.com。

    通讯作者:

    劳海港(1978—),博士,讲师,从事盆地构造解析研究。E-mail:haigang1609@126.com。

  • 中图分类号: TE121.2

Tectonic evolution and its physical simulation of Wuxia fault belt in the northwestern margin of Junggar Basin

  • 摘要: 依据大量地震勘探资料,对准噶尔盆地西北缘乌夏断裂带的构造特征进行了系统研究,并将其构造演化划分为碰撞前陆盆地、前陆盆地逆冲推覆、陆内拗陷逆冲褶皱、陆内拗陷抬升剥蚀和覆盖定型5个阶段。在此基础上,采用构造物理模拟实验方法对研究区典型剖面晚石炭世以来的构造演化进行了正演模拟,取得了与实际地质情况较高的吻合度。模拟结果表明,乌夏断裂带经历了由前陆盆地“前展式”逆冲向陆内拗陷“后展式”逆冲的转变。同时,实验结果进一步证实,NW-SE向挤压应力场的控制是乌夏断裂带形成、演化的根本原因,其主要受控于板块活动及造山带、边界控盆断裂的活动等关键因素。

     

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出版历程
  • 收稿日期:  2017-01-25
  • 修回日期:  2017-05-31
  • 刊出日期:  2017-07-28

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