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

机译:通过马尔可夫到达过程建模估算科林斯湾(希腊)的地震发生率

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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:马尔可夫到达过程(MAP)被用作描述希腊科林斯湾随时间变化的地震活动的候选模型。据我们所知,这是首次尝试使用特定类别的MAPs研究地震的时间演变。完整的目录与不同震级的数据集一起用于地震时空分布调查。研究区域分为西部和东部两个子区域,并探讨了地震发生时间的可能变化。 MAP的隐藏状态对应于不同的地震活动级别,因此要检查各种状态。实施了Akaike和Bayes信息标准以识别最佳模型,并与最著名和广为接受的理论事件间隔时间进行了比较。在所有情况下,具有相位类型分布的到达时间的拟合MAP均优于具有其他分布的模型。计算了潜在的马尔可夫过程的重要指标,并通过计数过程估算了地震频率。分析表明,东部地区地震的爆发性指数很高,即较长的静止期与较短的剧烈地震活动交替出现。

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