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Stresses in an overthrust sheet and propagation of thrusting: An Airy stress function solution

机译:上冲片中的应力和推力的传播:艾里应力函数解

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An Airy stress function solution is derived for the stress field in an elastic wedge‐shaped overthrust sheet subject to horizontal forces at the rear and at the front. From this stress solution the state of stress on the basal thrust (lower boundary of the sheet) is obtained. Both normal and shear stresses on the basal thrust are affected by the rear pushing and front buttressing forces and by the slopes of the upper and lower boundaries of the wedge‐shaped block. For (1) nonlinear components of external horizontal forces exerted on the vertical edges of the block and/or (2) nonzero slopes of the upper and lower boundaries the normal and shear stresses vary systematically with position along the basal thrust. The ratio of shear and normal stresses along this plane (the “frictional function” of the thrust) can be compared with the friction coefficient to determine where slippage is likely to occur. Since the frictional function is a function of position, the strength is exceeded only on part of the thrust (near the rear for most values of the parameters). The assumption of simultaneous displacement of the whole thrust sheet on the basal plane is therefore not realistic. Even simple static models such as the present one indicate that the motion on thrust faults must be envisaged in terms of progressive, consecutive “dislocation‐typ
机译:针对弹性楔形上推力片中的应力场推导了艾里应力函数解,该应力场在后部和前部受到水平力作用。从该应力解中可以得到基础推力(板材下边界)上的应力状态。基础推力的法向应力和剪切应力都受到后推力和前支撑力以及楔形块体上下边界坡度的影响。对于 (1) 施加在块体垂直边缘的外部水平力的非线性分量和/或 (2) 上下边界的非零坡度,法向应力和剪应力随沿基础推力的位置系统地变化。可以将沿该平面的剪切应力和法向应力之比(推力的“摩擦函数”)与摩擦系数进行比较,以确定可能发生滑移的位置。由于摩擦函数是位置的函数,因此仅在部分推力上超过强度(对于大多数参数值,靠近后部)。因此,整个推力片在基面上同时位移的假设是不现实的。即使是简单的静态模型,如现在的模型,也表明逆冲断层的运动必须根据渐进的、连续的“位错类型”来设想

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  • 来源
    《tectonics》 |1992年第3期|549-559|共页
  • 作者

    J. Y. Liu; G. Ranalli;

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  • 正文语种 英语
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