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Stress inversion from focal mechanism solution of Bam earthquake aftershocks (Iran, 2003)

机译:巴姆地震余震震源机制解的应力反演(伊朗,2003年)

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Conventional inversion methods for in situ stress determination from fault slip data obtained from focal mechanism solutions, define the optimum stress as the maximum point of the object function. In this research, object functions are computed for a mesh of principal stress directions and stress ratios for fault slip data obtained from fault plane solution for aftershocks of Bam Earthquake in Iran, in 2003. Several stress state possibilities are found with close values of object function. To overcome this problem, a method is introduced in which the stress states with less than 5 percent difference with maximum value of the object function are selected and categorized according to their stress ratio. Significant stress states for each category are identified as high concentrated loci of principal stresses. The results obtained in this method are compared with results obtained from multiple inverse method which shows a close agreement.
机译:根据从震源机制解获得的断层滑动数据来确定地应力的常规反演方法将最佳应力定义为目标函数的最大点。在这项研究中,针对主应力方向和应力比的网格计算了目标函数,该网格是从2003年伊朗巴姆地震余震的断层平面解中获得的断层滑移数据。发现了一些应力状态可能性,它们与目标函数的值接近。为了克服这个问题,引入了一种方法,其中选择与目标函数的最大值相差小于5%的应力状态,并根据它们的应力比进行分类。每个类别的显着应力状态被确定为主应力的高集中位点。将这种方法获得的结果与从多重逆方法获得的结果进行比较,结果显示出非常好的一致性。

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