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前陆冲断带非对称性变形与逆冲断层运动学指向

陈书平 万华川 袁浩伟 王信棚 黄学尧

陈书平, 万华川, 袁浩伟, 等, 2022. 前陆冲断带非对称性变形与逆冲断层运动学指向. 地质力学学报, 28 (2): 182-190. DOI: 10.12090/j.issn.1006-6616.2021080
引用本文: 陈书平, 万华川, 袁浩伟, 等, 2022. 前陆冲断带非对称性变形与逆冲断层运动学指向. 地质力学学报, 28 (2): 182-190. DOI: 10.12090/j.issn.1006-6616.2021080
CHEN Shuping, WAN Huachuan, YUAN Haowei, et al., 2022. Deformation asymmetry in foreland thrust belts and the kinematic direction of the related thrust faults. Journal of Geomechanics, 28 (2): 182-190. DOI: 10.12090/j.issn.1006-6616.2021080
Citation: CHEN Shuping, WAN Huachuan, YUAN Haowei, et al., 2022. Deformation asymmetry in foreland thrust belts and the kinematic direction of the related thrust faults. Journal of Geomechanics, 28 (2): 182-190. DOI: 10.12090/j.issn.1006-6616.2021080

前陆冲断带非对称性变形与逆冲断层运动学指向

doi: 10.12090/j.issn.1006-6616.2021080
基金项目: 

国家自然科学基金 41172124

国家自然科学基金 42172138

国家重点研发计划 2017YFC0603105

中国科学院战略性先导科技专项 XDA14010306

详细信息
    作者简介:

    陈书平(1965—),男,教授,博士生导师,从事构造地质学和盆地构造分析的教学和科研工作。E-mail:csp21c@163.com

  • 中图分类号: P551

Deformation asymmetry in foreland thrust belts and the kinematic direction of the related thrust faults

Funds: 

the National Natural Science Foundation of China 41172124

the National Natural Science Foundation of China 42172138

the National Key Research and Development Plan of China 2017YFC0603105

the Strategic Priority Research Program of the Chinese Academy of Sciences XDA14010306

  • 摘要: 前陆冲断带冲断层的冲断方向一直没有得到理论解释。文中基于库伦断裂理论和造山带前陆冲断带变形的非对称性,分析了前冲断层和反冲断层的成因。变形初期将会出现两组共轭势断裂面,随后在变形非对称引起的准静力平衡条件下,两组势断裂面中所需作用力小的那组断裂面将更容易发育成冲断层,断层滑动所需作用力包括克服滑脱面摩擦力和断层面摩擦力两部分。大部分条件下,前陆区前冲断层将优先发育,但当最大主应力轴向前陆倾斜时或共轭断层交叉点在滑脱面上时,反冲断层将有可能优先发育。后缘推动力、滑脱面摩擦力和滑体形状都会决定着主应力轴的方位。上述认识能够解释包括收缩变形区、伸展变形区等断层发育的选择性。

     

  • 图  1  外力作用下初始库伦破裂方位

    Figure  1.  Initial Coulomb fractures under applied force

    图  2  共轭断裂点在中间线上且最大主应力水平时的势断层

    Figure  2.  Potential faults when both the intersection point of conjugate fractures is on the midline and the maximum principal stress is horizontal

    图  3  共轭断裂交叉点在中间线下方且最大主应力水平时的势断层方位

    Figure  3.  Potential faults when both the intersection point of conjugate fractures is beneath the midline and the maximum principal stress is horizontal

    图  4  共轭断裂交叉点在滑脱面上的势断层

    Figure  4.  Potential faults when the intersection point of conjugate fractures is on the detachment surface

    图  5  最大主应力倾斜且断层交叉点在中间线上时的势断层

    Figure  5.  Potential faults when both the intersection point of conjugate fractures is on the midline and the maximum principal stress is tilting

    图  6  前陆冲断带滑体可能的动力条件及初期断裂

    a—共轭断裂交叉点位于滑体中间线上且最大主压应力水平的动力条件;b—共轭断裂交叉点位于滑体中间线上方且最大主压应力水平的动力条件;c—共轭断裂交叉点位于滑体中间线下方且最大主压应力水平的动力条件;d—共轭断裂交叉点位于滑体中间线上且最大主压应力倾斜的动力条件

    Figure  6.  Possible geodynamic conditions and initial fractures in the foreland slipping terrane

    (a) Geodynamic conditions for both the intersection point of conjugate fractures being on the midline of the slipping terrane and the maximum principal compressive stress being horizontal; (b) Geodynamic conditions for both the intersection point of conjugate fractures being above the midline of the slipping terrane and the maximum principal compressive stress being horizontal; (c) Geodynamic conditions for both the intersection point of conjugate fractures being beneath the midline of the slipping terrane and the maximum principal compressive stress being horizontal; (d) Geodynamic conditions for both the intersection point of conjugate fractures being on the midline of the slipping terrane and the maximum principal compressive stress being tilting

    图  7  后推力倾斜及主应力水平

    P—外作用力;Fb—底面摩擦力;θ—外作用力方向与最大主压应力轴夹角; F1—断层1;F2—断层2;A1—与P作用方向平行面上的应力点;A2—与P作用方向垂直面上的应力点;σ1—水平的最大主压应力;σ3—铅直的最小主压应力

    Figure  7.  Tilting push force and horizontal principal stress

    P-Tilting applied force; Fb-Base friction; θ-Intersection angle between the applied force direction and the maximum principal stress axis; F1-Fault 1; F2-Fault 2; A1-Stress point for the plane parallel to the applied force; A2-Stress point for the plane perpendicular to the applied force; σ1-Horizontal maximum principal stress; σ3-Vertical minimum principal stress

    图  8  后推力水平及主应力倾斜

    P—水平外作用力;Fb—底面摩擦力;θ—外作用力方向与最大主压应力轴夹角;F1—断层1;F2—断层2;Β1—与P作用方向平行面上的应力点;Β2—与P作用方向垂直面上的应力点;σ1—倾斜的最大主压应力,σ3—铅直的最小主压应力

    Figure  8.  Horizontal push force and titling principal stress

    P-Horizontal applied force; Fb-Base friction; θ-Intersection angle between the applied force direction and the maximum principal stress axis; F1-Fault 1; F2-Fault 2; Β1-Stress point for the plane parallel to the applied force; Β2-Stress point for the plane perpendicular to the applied force; σ1-Tilting maximum principal stress; σ3-Vertical minimum principal stress

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  • 收稿日期:  2021-07-14
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