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Considering the third dimension in stress-triggering of aitershocks:1993 Klamath Falls,Oregon,earthquake sequence
Author(s): 
Pages: 62-66
Year: Issue:  1
Journal: Translated World Selsmology

Abstract: 有限维断层上的倾滑产生的静态应力变化在三维情况下有很大改变。1993年的美国俄勒冈州克拉马斯福尔斯地震序列显示出位于断层外的浅源余震群具有混合的倾滑和走滑震源机制。模拟的静态应力变化与余震位置表明,用传统的二维方法观察会得出使人误解的结果。而完整的三维分析方法表明浅源右旋滑动与倾滑主震之后的局部应力扰动一致。
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