Study on energy distributions of strong seismic events in the USCB

Agnieszka Bracławska, A. Idziak
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引用次数: 2

Abstract

Abstract The paper presents the statistical analysis of energy distribution of strong seismic shocks (energy E ≥ 105 J) occurred in the Upper Silesian Coal Basin which is one of the most seismically active mining areas in the world. In the USCB tremor epicenters do not occur uniformly throughout the whole basin but group in several regions belonging to different structural units and are separated by regions where strong shocks are not observed. The aim of the studies was to determine the modality of the energy distributions and to compare the modal types in regions of the USCB where the shocks epicenters cluster. An analysis was made for shocks with energies equal to or greater than 105 J recorded by Upper Silesian Regional Seismological Network operated by Central Mining Institute (CMI), which took place between 1987 – 2012. The analysis has proven the bimodality of seismic energy distribution in the three of five studied areas of the Upper Silesian Coal Basin. The Gumbel’s distribution II type best fit the experimental energy distribution for almost all studied tectonic units except the main syncline area, where the Gumbel’s distribution I type matched better the low-energy mode. This is due to too short time window, causing a shortage of the strongest shocks in seismic catalogue.
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USCB强震事件能量分布研究
摘要本文对世界上地震最活跃矿区之一的上西里西亚煤盆地发生的强震能量分布(能量E≥105 J)进行了统计分析。在USCB,震源并不是均匀地发生在整个盆地,而是集中在属于不同构造单元的几个区域,并被未观察到强震的区域隔开。研究的目的是确定能量分布的模态,并比较震源聚集的USCB区域的模态类型。对中央矿业研究所(CMI)运营的上西里西亚地区地震台网记录的1987 - 2012年间发生的能量等于或大于105 J的冲击进行了分析。分析证实了上西里西亚煤盆地5个研究区的3个地震能量分布具有双峰性。除了主向斜区域外,Gumbel分布II型与低能模式更匹配,几乎所有构造单元的实验能量分布与Gumbel分布II型最吻合。这是由于时间窗口太短,导致地震目录中缺乏最强的冲击。
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