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Forecasting strong aftershocks in earthquake clusters from northeastern Italy and western Slovenia
Physics of the Earth and Planetary Interiors ( IF 2.3 ) Pub Date : 2020-06-01 , DOI: 10.1016/j.pepi.2020.106483
S. Gentili , R. Di Giovambattista

Abstract In this study, we propose an analysis of the earthquake clusters that occurred in North-Eastern Italy and western Slovenia from 1977 to today. Given a mainshock generating alarm in the population, we are interested in forecasting if a similar magnitude earthquake will follow. We classify the earthquake clusters associated with mainshocks of magnitude Mm into two classes: if the strongest aftershock has a magnitude ≥Mm-1 (swarms or large aftershock seismic sequences) as type A, otherwise (smaller aftershocks seismic sequences) as type B. A large aftershock following a main shock can cause significant damages to already weakened buildings and infrastructures, so a timely advisory information to the civil protection is of great interest for effective decision-making. For the first time, we applied to a new catalogue a pattern recognition algorithm for cluster type forecasting that we developed for all Italy (Gentili and Di Giovambattista, 2017). Thanks to the lower completeness magnitude of the local OGS catalogue, compared to the national one, and to a new version of the algorithm, we were able to lower the threshold of the clusters mainshocks magnitude from 4.5 to 3.7. The method has been validated by rigorous statistical tests. We tested the algorithm on the 1976 highly destructive earthquake cluster (mainshock magnitude 6.5 – the strongest in the last 80 years in the region) and we retrospectively forecasted it as an A cluster. Successful results were obtained also on other three smaller earthquake clusters in 2019.

中文翻译:

预测意大利东北部和斯洛文尼亚西部地震群中的强烈余震

摘要 在这项研究中,我们对 1977 年至今发生在意大利东北部和斯洛文尼亚西部的地震群进行了分析。鉴于主震在人群中发出警报,我们有兴趣预测是否会发生类似震级的地震。我们将与 Mm 级主震相关的地震群分为两类:如果最强余震的震级≥Mm-1(群或大余震地震序列)为 A 类,否则(较小余震地震序列)为 B 类。主震后发生的大余震会对已经脆弱的建筑物和基础设施造成重大破坏,因此及时向民防部门提供咨询信息对于有效决策非常重要。首次,我们将我们为整个意大利开发的用于集群类型预测的模式识别算法应用于新目录(Gentili 和 Di Giovambattista,2017 年)。由于本地 OGS 目录的完整性低于国家目录,以及新版本的算法,我们能够将集群主震级别的阈值从 4.5 降低到 3.7。该方法已通过严格的统计测试验证。我们在 1976 年高破坏性地震群(主震 6.5 级——该地区过去 80 年来最强)上测试了该算法,我们回顾性地将其预测为 A 群。2019 年其他三个较小的地震群也取得了成功。由于本地 OGS 目录的完整度低于国家目录,以及新版本的算法,我们能够将集群主震级的阈值从 4.5 降低到 3.7。该方法已通过严格的统计测试验证。我们在 1976 年高破坏性地震群(主震 6.5 级——该地区过去 80 年来最强)上测试了该算法,我们回顾性地将其预测为 A 群。2019 年其他三个较小的地震群也取得了成功。由于本地 OGS 目录的完整度低于国家目录,以及新版本的算法,我们能够将集群主震级的阈值从 4.5 降低到 3.7。该方法已通过严格的统计测试验证。我们在 1976 年高破坏性地震群(主震 6.5 级——该地区过去 80 年来最强)上测试了该算法,我们回顾性地将其预测为 A 群。2019 年其他三个较小的地震群也取得了成功。该方法已通过严格的统计测试验证。我们在 1976 年高破坏性地震群(主震 6.5 级——该地区过去 80 年来最强)上测试了该算法,我们回顾性地将其预测为 A 群。2019 年其他三个较小的地震群也取得了成功。该方法已通过严格的统计测试验证。我们在 1976 年高破坏性地震群(主震 6.5 级——该地区过去 80 年来最强)上测试了该算法,我们回顾性地将其预测为 A 群。2019 年其他三个较小的地震群也取得了成功。
更新日期:2020-06-01
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