杨修信. 断层内闭锁区及其附近的应力分布[J]. 华北地震科学, 1990, 8(1): 30-37.
引用本文: 杨修信. 断层内闭锁区及其附近的应力分布[J]. 华北地震科学, 1990, 8(1): 30-37.
Yang Xiuxin. THE STRESS DISTRIBUTION OF THE LOCKED REGION IN THE FAULT AND ITS NEAR AREA[J]. North China Earthquake Sciences, 1990, 8(1): 30-37.
Citation: Yang Xiuxin. THE STRESS DISTRIBUTION OF THE LOCKED REGION IN THE FAULT AND ITS NEAR AREA[J]. North China Earthquake Sciences, 1990, 8(1): 30-37.

断层内闭锁区及其附近的应力分布

THE STRESS DISTRIBUTION OF THE LOCKED REGION IN THE FAULT AND ITS NEAR AREA

  • 摘要: 本文用三维有限单元法计算了在外应力场作用下,断层深部闭锁区及其附近的附加应力分布,用以模拟震源体在孕震过程中对断层两侧地质体的作用。计算结果表明,在断层因局部发生闭锁而孕育地震的过程中,断层闭锁区有着明显的应力集中,其应力值比非闭锁区高几百倍。闭锁区内的高应力分布有明显的端部效应,闭锁块体各个端部的主应力值、断层面上的正应力和剪应力值以及主应力方向,均与其内部有很大差异。对比分析断层内不同深度上的应力分布,可见深、浅部附加应力状态明显不同,并随深度增加而呈现某些有规律的变化。

     

    Abstract: In this paper the additional stress distribution of the locked region and its nearby area in the deep fault under an applied stress field has been calculated using 3-dimension finite element method in order to simulate the action of an earthquake focus to the block on both side of the fault in the course of an earthquake development. The results have shown that the stress concentration in the locked region is remarkable and their values can be hundreds times greater than that in unlocked region in the fault. The values of the principal stresses, the values of the normal and shear stress on the fault plane and the directions of principal stresses in end of locked region are greatly different from those in faults. Comparing and analysing the additional stress distributions at different depth in the fault, we can find the stress states of shllow and deep layers are different obviously and some regular changes occur with the increase of depth.

     

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