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Characterization of the Frequency of Extreme Earthquake Events by the Generalized Pareto Distribution

机译:用广义帕累托分布表征极端地震事件的频率

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摘要

Recent results in extreme value theory suggest a new technique for statistical estimation of distribution tails (Embrechts et al., 1997), based on a limit theorem known as the Gnedenko-Pickands-Balkema-de Haan theorem. This theorem gives a natural limit law for peak-over-threshold values in the form of the Generalized Pareto Distribution (GPD), which is a family of distributions with two parameters. The GPD has been successfully applied in a number of statistical problems related to finance, insurance, hydrology, and other domains. Here, we apply the GPD approach to the well-known seismological problem of earthquake energy distribution described by the Gutenberg-Richter seismic moment-frequency law. We analyze shallow earthquakes (depth h<70 km) in the Harvard catalog over the period 1977–2000 in 12 seismic zones. The GPD is found to approximate the tails of the seismic moment distributions quite well over the lower threshold approximately M ≅ 1024 dyne-cm, or somewhat above (i.e., moment-magnitudes larger than m W =5.3). We confirm that the b-value is very different (b=2.06 ± 0.30) in mid-ocean ridges compared to other zones (b=1.00 ± 0.04) with a very high statistical confidence and propose a physical mechanism contrasting “crack-type” rupture with “dislocation-type” behavior. The GPD can as well be applied in many problems of seismic hazard assessment on a regional scale. However, in certain cases, deviations from the GPD at the very end of the tail may occur, in particular for large samples signaling a novel regime.
机译:极值理论的最新研究结果提出了一种基于分布定理的统计估计的新技术(Embrechts等,1997),其基础是称为Gnedenko-Pickands-Balkema-de Haan定理的极限定理。该定理以广义帕累托分布(GPD)的形式给出了阈值之上的峰值的自然极限定律,广义帕累托分布是具有两个参数的分布族。 GPD已成功应用于与金融,保险,水文学和其他领域有关的许多统计问题。在这里,我们将GPD方法应用于古腾堡-里希特地震矩-频率定律所描述的著名的地震能量分布地震学问题。我们分析了1977-2000年期间哈佛地区12个地震带中的浅层地震(h <70 km)。发现GPD在较低的阈值M≥1024 dyne-cm或稍高于该阈值(即大于m W = 5.3的矩幅度)下,很好地近似了地震矩分布的尾部。 )。我们确认,与其他区域(b = 1.00±0.04)相比,洋中脊的b值存在很大差异(b = 2.06±0.30),具有很高的统计置信度,并提出了与“裂缝类型”形成对比的物理机制以“位错型”行为破裂。 GPD还可以应用于区域范围内地震危险性评估的许多问题。但是,在某些情况下,可能会在尾部最末端出现与GPD的偏离,特别是对于发信号通知新模式的大样本而言。

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  • 来源
    《Pure and Applied Geophysics》 |2003年第12期|2343-2364|共22页
  • 作者

    V. F. Pisarenko; D. Sornette;

  • 作者单位

    International Institute of Earthquake Prediction Theory and Mathematical Geophysics Russian Ac. Sci. Warshavskoye sh.Institute of Geophysics and Planetary Physics and Department of Earth and Space Science University of California;

    Institute of Geophysics and Planetary Physics and Department of Earth and Space Science University of CaliforniaLaboratoire de Physique de la Matière Condensée CNRS UMR6622 Université des Sciences;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Extreme events; tail of distribution; the Generalized Pareto Distribution; seismic energy distribution;

    机译:极端事件;分布尾部;广义帕累托分布;地震能量分布;

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