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Stress Distribution in the Vicinity of Right Strike-Slip Fault, a Numerical Approach

机译:右走滑断层附近的应力分布,一种数值方法

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摘要

When fault exist in the formation, the local stressesin the shallow depth will be affected by presence of slip ordisplacement on fault and topography If the trace of fault is notstraight, the stress distribution near fault become morecomplicated. This feature is studied numerically using boundaryelement method. Related to this problem, a numerical procedure of2 and 3 dimensional coupled fictitious stress method anddisplacement discontinuity method which takes joint element intoconsideration is adopted. A sinusoidal fault trace is used tomodelize the non-straight strike-slip fault in 2 dimensions, while asinusoidal fault plane buried in the middle of symmetrical valley isused as numerical model study in 3 dimensions. This model is thenapplied to the Mozumi Sukenobe fault as field case study. Ourfinding on local stress near fault is consistent with fieldmeasurement. If the far field stress is defined in proportion todepth, our finding also predicts that the applied far field stress inthe Mozumi Sukenobe fault is in compression with ?Ho oriented at-40°from fault strike and the magnitudes of far field stresscomponents are ?vo≈?gh, ?HO≈0.74?vo and ?ho≈0.5?vo.
机译:当地层中存在断层时,浅层深度的局部应力会受到断层和地形上的滑动或位移的影响。如果断层的轨迹不平直,则断层附近的应力分布会变得更加复杂。使用边界元方法对该特征进行了数值研究。与此相关的是,采用了考虑连接单元的二维和三维耦合虚拟应力法和位移不连续法的数值程序。正弦断层轨迹用于二维非直线走滑断层的建模,而埋在对称谷中间的非正弦断层平面则用于三维模型研究。然后将该模型应用到Mozumi Sukenobe断层,作为现场案例研究。我们对断层附近局部应力的发现与现场测量是一致的。如果将远场应力定义为与深度成比例,我们的发现还可以预测,在Mozumi Sukenobe断层中施加的远场应力处于压缩状态,从断层走向向Ho定向为?°,远场应力分量的大小为?vo≈ gh,HO≈0.74vo和ho≈0.5vo。

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