用 DPS 拓扑过滤算法分析地震事件的空间聚类:贝加尔湖地区

A. K. Nekrasova, A. S. Agayan, V. G. Kossobokov
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引用次数: 0

摘要

本文介绍了应用离散完美集(DPS)拓扑过滤算法分析贝加尔湖地区地震震中空间聚类的结果。研究利用了俄罗斯科学院地球物理勘测贝加尔湖分部地震网络记录的 1964 年至 2018 年期间北纬 48°、58°和东经 99°、122°范围内的地震数据。在以下情况下获得了聚类特征:(i) 1989 年至 2018 年的记录期间,DPS 算法参数不同,地震事件的最小能量等级 KР 分为四级;(ii) 1964 年至 2018 年的六个不重叠时间段,地震事件的能量等级 KР ≥ 8.6,DPS 算法参数固定。从 1964 年到 2018 年聚类参数的动态变化可以说明该地区地震机制的多变性。具体而言,已识别震中群区域的线性大小从约一千公里减小到几十公里,这可能表明与 1964 年至 1997 年期间相比,贝加尔湖地区的地震机制在 20 世纪 90 年代末和 21 世纪初发生了重大变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Analysis of Spatial Clustering of Seismic Events by the DPS Topological Filtering Algorithm: Lake Baikal Region
The paper presents the results of applying the Discrete Perfect Set (DPS) topological filtering algorithm to analyze the spatial clustering of seismic epicenters in the Lake Baikal region. The study utilizes earthquake data recorded by the seismic network of the Baikal Branch of the Geophysical Survey of the Russian Academy of Sciences within the latitude range 48°N, 58°N and longitude range of 99°E, 122°E for the period from 1964 to 2018. Clustering characteristics are obtained for (i) the recording period from 1989 to 2018 with varying parameters of the DPS algorithm and four levels of the minimum energy class KР of seismic events and (ii) six non-overlapping time intervals from 1964 to 2018 and seismic events of energy class KР ≥ 8.6 with fixed parameters of the DPS algorithm. The dynamics of the clustering parameters from 1964 to 2018 may characterise the variability of the seismic regime of the region. Specifically, the decrease in the linear size of the areas of identified epicenter groups from about a thousand km to tens km may indicate a significant change in the seismic regime of the Lake Baikal region at the end of the 1990s and the beginning of the 2000s compared to the period between 1964 and 1997.
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