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Simulation of finite fault hybrid source models for theM(w)6.6 Jiuzhaigou, China, earthquake

机译:M(w)6.6九寨沟地震有限断层混合源模型仿真

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摘要

A hybrid source model for theM(w)6.6 Jiuzhaigou earthquake, China, based on the finite fault is established. The global parameters are estimated mainly according to the regional seismic structure, crustal structure, seismicity, and semi-empirical calibration laws. The local parameters are divided into two parts: the asperity part describing the deterministic slip and thek-square model describing the random slip. The source models are generated by 30 groups of simulation and are compared with those retrieved by other scholars. The results show that this method can be used as an effective approach to predict seismic source models.
机译:建立了基于有限断层的中国M(w)6.6九寨沟地震混合震源模型。主要根据区域地震结构、地壳结构、地震活动和半经验校准规律对全局参数进行估计。局部参数分为两部分:描述确定性滑移的粗糙度部分和描述随机滑移的平方模型。源模型由30组模拟生成,并与其他学者检索到的模型进行比较。结果表明,该方法可作为预测地震源模型的有效方法。

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