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Exploring the evolution of a volcanic seismic swarm: the case of the 2000 Izu Islands swarm

机译:探索火山地震群的演变:2000年伊豆群岛群的情况

摘要

The goal of this paper is to yield physical constrains onthe nature and evolution of a seismic swarm by means of aquantitative stochastic modeling of earthquakes occurrence.With this purpose, we fit different stationary andnonstationary stochastic ETAS models to the Izu Islandsseismic swarm occurred in 2000. We find that anonstationary model with background activity and p-valuevarying through time describes the observations better thanother simpler ETAS models. The coherent fluctuations ofthese parameters and of the spatio-temporal earthquakedistribution are interpreted in terms of a magma/fluidssource process that evolves through outbursts of activitysuperimposed to low frequency variations. The resultsobtained suggest that suitable nonstationary ETASmodeling can be very useful to characterize the nature ofthe swarm source, and it may provide the basis to build aquantitative tool for tracking in almost real-time theevolution of a magma/fluids source.
机译:本文的目的是通过地震发生的定量随机建模来对地震群的性质和演化产生物理约束。为此,我们将2000年发生的伊豆群岛地震群拟合为不同的平稳和非平稳随机ETAS模型。发现具有背景活动和p值随时间变化的非平稳模型比其他更简单的ETAS模型更好地描述了观测结果。这些参数和时空地震分布的相干波动是通过岩浆/流体源过程来解释的,该过程是通过活动爆发叠加低频变化而演变而来的。获得的结果表明,合适的非平稳ETAS模型对于表征群源的性质可能非常有用,并且可以为构建定量工具以跟踪岩浆/流体源的几乎实时演化提供基础。

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