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    赵力彬, 陈冬霞, 冯建伟, 梁骁, 杨学君, 2026. 天山及南缘新生代旋扭构造体系特征及应力场演化. 地球科学. doi: 10.3799/dqkx.2026.099
    引用本文: 赵力彬, 陈冬霞, 冯建伟, 梁骁, 杨学君, 2026. 天山及南缘新生代旋扭构造体系特征及应力场演化. 地球科学. doi: 10.3799/dqkx.2026.099
    Zhao Libin, Chen Dongxia, Feng Jianwei, Liang Xiao, Yang Xuejun, 2026. Characteristics and stress field evolution of the Cenozoic rotational shear tectonic system in the Tianshan Mountains and its southern margin. Earth Science. doi: 10.3799/dqkx.2026.099
    Citation: Zhao Libin, Chen Dongxia, Feng Jianwei, Liang Xiao, Yang Xuejun, 2026. Characteristics and stress field evolution of the Cenozoic rotational shear tectonic system in the Tianshan Mountains and its southern margin. Earth Science. doi: 10.3799/dqkx.2026.099

    天山及南缘新生代旋扭构造体系特征及应力场演化

    doi: 10.3799/dqkx.2026.099
    基金项目: 

    中石油重大项目(No.2023ZZ14YJ03).

    详细信息
      作者简介:

      赵力彬(1979-),男,正高级工程师,博士研究生,主要从事油气田开发,E-mail:zhaolb-tlm@petrochina.com.cn,ORCID: 0009-0002-8409-9281

      通讯作者:

      陈冬霞,E-mail:lindachen@cup.edu.cn

    • 中图分类号: P618.31

    Characteristics and stress field evolution of the Cenozoic rotational shear tectonic system in the Tianshan Mountains and its southern margin

    • 摘要: 天山作为典型的对称型新生代板内复活型造山带,针对新生代以来构造动力学机制及与南缘前陆冲断带耦合模式的科学难题,本文基于最新地质地球物理资料和露头调研,以地质力学理论为指导,认为天山南缘柯坪-库车地区的新生代断裂系统呈帚状向西撒开,属旋扭构造体系,而非简单逆冲-推覆构造。通过建立大变形弹塑性有限元(FEM)模型,从四维演化的角度模拟了新生代以来,在印度-欧亚板块碰撞的远程效应下,塔里木板块发生被动顺时针旋转,并激发了西天山深部壳幔活动,进而控制了天山及南缘造山带由西向东的递进形成与旋扭构造的发育。该旋扭运动在盆山边界及大型断裂周缘控制形成了多个油气富集带,展现出广阔的勘探前景。

       

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