一维Burridge-Knopoff模型所代表的慢滑现象

H. Kawamura, Maho Yamamoto, Y. Ueda
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引用次数: 3

摘要

使用一维Burridge- Knopoff模型研究了慢滑现象,包括余震和无声地震,该模型遵循速率和状态依赖的摩擦定律。通过改变几个模型参数,这个简单的模型可以在一个框架内再现各种地震滑动,包括主震、前兆成核过程、余震和无声地震。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Slow-Slip Phenomena Represented by the One-Dimensional Burridge-Knopoff Model of Earthquakes
Slow-slip phenomena, including afterslips and silent earthquakes, are studied using a one-dimensional Burridge--Knopoff model that obeys the rate-and-state dependent friction law. By varying only a few model parameters, this simple model allows reproducing a variety of seismic slips within a single framework, including main shocks, precursory nucleation processes, afterslips, and silent earthquakes.
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