Estimating Magnitude Completeness in Earthquake Catalogs: A Comparative Study of Catalog-Based Methods

IF 4.1 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Xinyi Wang, Jiawei Li, Ao Feng, Didier Sornette
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引用次数: 0

Abstract

Without careful attention to the earthquake catalog completeness, claims of novel discoveries or forecasting skills lack credibility. Estimating the completeness magnitude (Mc) is therefore a critical step in seismological analysis. Among the available techniques, catalog-based methods are the most accessible and widely adopted, and they also often form the basis for more sophisticated techniques. However, current frameworks for evaluating methods do not provide a standardized strategy for generating synthetic catalogs that are independent of any specific Mc estimation technique. An effective evaluation framework should also allow for the simulation of data sets with spatially and temporally varying Mc values. In this study, we introduce a robust evaluation framework specifically designed to benchmark catalog-based Mc estimation methods, including six established and three newly proposed methods, under realistic and controlled simulation conditions. The proposed methods are evaluated on both simulated data sets, with homogeneous and heterogeneous Mc distributions, and on real-world earthquake catalogs from China, California, and New Zealand. In the synthetic tests, The traditional method MBS-WW and two new methods, BSReLU and especially AEReLU, consistently deliver reliable Mc estimates, provided the data are sufficiently dense and well-resolved. Among them, AEReLU demonstrates superior accuracy and adaptability, particularly under challenging conditions. When applied to six empirical catalogs, AEReLU produces the most robust and physically meaningful Mc estimates. Its predicted Mc values closely align with known regional completeness thresholds (e.g., Mc ≈ 1.8) and remain stable across diverse tectonic environments. Moreover, AEReLU yields consistent b-values and reveals spatial variations in the asymmetry parameter β, which captures differences in how detection completeness converges below and above Mc, reflecting region-specific patterns of seismicity and catalog incompleteness. Unlike traditional methods that impose a sharp Mc cut-off, BSReLU and AEReLU adopt a probabilistic framework that models the smooth transition in detection likelihood from zero to one as magnitude increases. This formulation better reflects the gradual shift from incomplete to complete reporting, effectively overcoming the limitations of step-function-based models. By rigorously comparing these methods, the present study not only identifies the contexts in which each is most suitable but also enhances our understanding of seismicity, earthquake forecasting, and hazard assessment, underscoring the critical role of data completeness in all such analyses.

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地震目录中震级完整性的估计:基于目录方法的比较研究
如果不认真注意地震目录的完整性,声称有新发现或预报技能就缺乏可信度。因此,完整震级(Mc)的估计是地震分析中的一个关键步骤。在现有的技术中,基于目录的方法是最容易获得和被广泛采用的,它们也经常构成更复杂技术的基础。然而,目前评估方法的框架并没有提供一个标准化的策略来生成独立于任何特定Mc估计技术的合成目录。有效的评估框架还应允许模拟具有空间和时间变化的Mc值的数据集。在这项研究中,我们引入了一个专门设计的鲁棒评估框架,以基准基于目录的Mc估计方法,包括六种已建立的方法和三种新提出的方法,在现实和可控的仿真条件下。本文在具有均匀和非均匀Mc分布的模拟数据集以及来自中国、加利福尼亚和新西兰的真实地震目录上对所提出的方法进行了评估。在综合测试中,传统方法MBS-WW和两种新方法BSReLU,特别是AEReLU,在数据足够密集和分辨率良好的情况下,始终能够提供可靠的Mc估计。其中,AEReLU表现出卓越的精度和适应性,特别是在具有挑战性的条件下。当应用于六个经验目录时,AEReLU产生最稳健和物理上有意义的Mc估计。预测的Mc值与已知的区域完备性阈值(如Mc≈1.8)接近,在不同构造环境下保持稳定。此外,AEReLU得到一致的b值,并揭示了不对称参数β的空间变化,该参数捕获了探测完整性在Mc以下和Mc以上收敛的差异,反映了地震活动和目录不完整性的区域特定模式。与传统方法施加尖锐的Mc截止值不同,BSReLU和AEReLU采用概率框架,随着震级的增加,检测可能性从0到1的平滑过渡建模。这种表述更好地反映了从不完整报告到完整报告的逐渐转变,有效地克服了基于阶梯函数的模型的局限性。通过严格比较这些方法,本研究不仅确定了每种方法最适合的环境,而且还增强了我们对地震活动性、地震预报和危害评估的理解,强调了数据完整性在所有这些分析中的关键作用。
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来源期刊
Journal of Geophysical Research: Solid Earth
Journal of Geophysical Research: Solid Earth Earth and Planetary Sciences-Geophysics
CiteScore
7.50
自引率
15.40%
发文量
559
期刊介绍: The Journal of Geophysical Research: Solid Earth serves as the premier publication for the breadth of solid Earth geophysics including (in alphabetical order): electromagnetic methods; exploration geophysics; geodesy and gravity; geodynamics, rheology, and plate kinematics; geomagnetism and paleomagnetism; hydrogeophysics; Instruments, techniques, and models; solid Earth interactions with the cryosphere, atmosphere, oceans, and climate; marine geology and geophysics; natural and anthropogenic hazards; near surface geophysics; petrology, geochemistry, and mineralogy; planet Earth physics and chemistry; rock mechanics and deformation; seismology; tectonophysics; and volcanology. JGR: Solid Earth has long distinguished itself as the venue for publication of Research Articles backed solidly by data and as well as presenting theoretical and numerical developments with broad applications. Research Articles published in JGR: Solid Earth have had long-term impacts in their fields. JGR: Solid Earth provides a venue for special issues and special themes based on conferences, workshops, and community initiatives. JGR: Solid Earth also publishes Commentaries on research and emerging trends in the field; these are commissioned by the editors, and suggestion are welcome.
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