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Deformation analysis of a viscoelastic half-space due to a finite and an infinite interacting faults

机译:由于有限和无限相互作用的粘弹性半空间的变形分析

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In seismically active regions the process of stress-strain accumulation near earthquake faults during aseismic period (period in between two major seismic events) has become a subject of research during the last few decades. The occurrence of multiple faults (for example Calaveras, Garlock in the neighbourhood of San Andreas fault) in seismically active region is more likely than that of a single fault (i.e. Sierra Madre fault, Raymond fault). Moreover the earthquake faults involve both the strike-slip and dip-slip faults some of which may be finite and others infinite. The way of interaction of faults with each other controls fault geometries, displacements and strains. Such phenomena encourage us to consider a model of interacting strike-slip and dip-slip faults in which a finite and an infinite interacting faults are taken to study the stress-strain accumulation in the neighbouring fault due to the movement across the other fault. The solutions for displacement, stress and strain are then found before the onset of fault slip and then superpose the effect of fault slip for both the interacting faults using Laplace transform, suitable mathematical technique of modified Green's function and Correspondence principal. The analytical results and the graphical presentations show that the velocities of both the faults movement and their inclinations have noticeable effects on displacements, stresses and strains.
机译:在地震活动区域中,在抗震期间,在抗震期间附近的应力 - 应变积累过程(两个主要地震事件之间的时期)已成为过去几十年中的研究主题。在地震活动区域中发生多个故障(例如Calaveras,在San Andreas故障附近的Garlock)比单个故障(即Sierra MadreFa错,Raymond Fault)更有可能。此外,地震缺陷涉及防撞滑动和浸渍故障,其中一些可能是有限的和其他无限的。彼此相互作用的方式控制故障几何形状,位移和菌株。这种现象鼓励我们考虑相互作用的防滑和倾倾故障的模型,其中采用有限和无限的相互作用故障来研究相邻故障中的应力 - 应变累积由于其他故障的运动。然后在发生故障滑动开始之前发现位移,应力和菌株的解决方案,然后使用LAPLACE变换,改进的绿色功能和通信校长的合适数学技术叠加故障滑动的效果。分析结果和图形介绍表明故障运动的速度及其倾斜度对位移,应力和菌株的速度显着。

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