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Planar seismic source characterization models developed for probabilistic seismic hazard assessment of Istanbul

机译:为伊斯坦布尔的概率地震危害评估开发了平面地震源特征模型

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This contribution provides an updated planar seismic source characterization (SSC) model to be used in the probabilistic seismic hazard assessment (PSHA) for Istanbul. It defines planar rupture systems for the four main segments of the North Anatolian fault zone (NAFZ) that are critical for the PSHA of Istanbul: segments covering the rupture zones of the 1999 Kocaeli and Düzce earthquakes, central Marmara, and Ganos/Saros segments. In each rupture system, the source geometry is defined in terms of fault length, fault width, fault plane attitude, and segmentation points. Activity rates and the magnitude recurrence models for each rupture system are established by considering geological and geodetic constraints and are tested based on the observed seismicity that is associated with the rupture system. Uncertainty in the SSC model parameters (e.g., b?value, maximum magnitude, slip rate, weights of the rupture scenarios) is considered, whereas the uncertainty in the fault geometry is not included in the logic tree. To acknowledge the effect of earthquakes that are not associated with the defined rupture systems on the hazard, a?background zone is introduced and the seismicity rates in the background zone are calculated using smoothed-seismicity approach. The state-of-the-art SSC model presented here is the first fully documented and ready-to-use fault-based SSC model developed for the PSHA of Istanbul.
机译:该贡献提供了更新的平面地震源表征(SSC)模型,用于用于伊斯坦布尔的概率地震危害评估(PSHA)。它为北安纳托利亚故障区(NAFZ)的四个主要部分定义了平面破裂系统,这对于伊斯坦布尔的PSHA至关重要:涵盖了1999年Kocaeli和Düzce地震,中央马尔马拉和Ganos / Saros段的破裂区。在每个破裂系统中,源几何形状在故障长度,故障宽度,故障平面姿态和分割点方面定义。通过考虑地质和大地测量约束来建立每个破裂系统的活动速率和每个破裂系统的幅度复制模型,并且基于与破裂系统相关的观察到的地震来测试。考虑SSC模型参数的不确定性(例如,B?值,最大幅度,滑移速率,破裂方案的权重),而故障几何中的不确定性不包括在逻辑树中。为了承认地震的效果与危险的定义破裂系统没有相关的地震,介绍了背景区域,并且使用平滑地震性方法计算背景区域中的地震率。此处提供的最先进的SSC模型是为伊斯坦布尔PSHA开发的第一个完全记录和即用的基于故障的SSC模型。

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