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Stochastic Finite Fault Modeling of Subduction Zone Earthquakes in Northeastern India

机译:印度东北俯冲带地震的随机有限断层模拟

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摘要

In this article, a stochastic finite fault source model is calibrated to estimate ground motion in northeastern India for intermediate depth events originating in the Indo-Burmese tectonic domain. A total of 47 three-component accelerograms from eight events with magnitudes ranging from M _w 4.8-6.4 are used to estimate the input source and site parameters of the finite fault source model. Key seismic parameters such as stress drop (Δσ) and site amplification function are determined from the recorded strong motion data. The obtained stress drop of the eight recorded events lies in between 105 and 165 bars.
机译:在本文中,对随机有限断层源模型进行了校准,以估计印度东北部源自印度-缅甸构造域的中间深度事件的地震动。来自八个事件的总计47个三分量加速度图,幅度范围在M_w 4.8-6.4之间,用于估计有限断层源模型的输入源和站点参数。根据记录的强运动数据确定关键的地震参数,例如应力降(Δσ)和部位放大函数。获得的八个记录事件的应力降在105至165巴之间。

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