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Estimating the earthquake occurrence rates in Corinth Gulf (Greece) through Markovian arrival process modeling

机译:通过Markovian抵达过程建模估算科林斯海湾(希腊)的地震发生率

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摘要

The Markovian Arrival Process (MAP) is applied as a candidate model to describe the time-varying earthquake activity in Corinth Gulf, Greece. To the best of our knowledge, this is the first attempt to study the earthquake temporal evolution with the specific class of MAPs. A complete catalogue is used for the earthquake temporal distribution investigation, along with data sets of different magnitude cutoffs. The study area is divided into its western and eastern subareas, and possible variations in the earthquake occurrence times were sought. Hidden states of MAPs correspond to different levels of seismicity, and hence various numbers of states are examined. Akaike and Bayes information criteria are implemented for identifying the best model, and comparison to the most known and broadly accepted theoretical interevent time distributions is provided. In all cases, the fitted MAPs with phase type distributed intearrival times outperform the models with other distributions. Important indicators of the underlying Markov process are computed, and the earthquake frequency is approximated by the counting process. The analysis demonstrates high index of burstiness for the earthquake generation in the eastern part, i.e. long quiescent periods alternate with short ones of intense seismic activity.
机译:Markovian抵达过程(地图)被应用为候选模型,以描述希腊科林斯湾的时变震动活动。据我们所知,这是第一次尝试使用特定类的地图研究地震时间演变。完整的目录用于地震时间分布调查,以及不同幅度截止的数据集。该研究区分为其西部和东部蛛网,并寻求地震发生时间的可能变化。隐藏的地图状态对应于不同级别的地震性,因此检查各种州。 Akaike和Bayes信息标准用于识别最佳模型,并提供与最着名和广泛接受的理论无线时间分布的比较。在所有情况下,具有相位类型的拟合图分布式的Intearrival时间越优于使用其他分布的模型。计算底层马尔可夫过程的重要指标,并且近似地震频率由计数过程近似。该分析表明了东部地震发生的高抗爆裂指数,即长静态时期与强烈地震活动的短暂交替。

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