2022
DOI: 10.1029/2021jb023254
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An Adaptable Random Forest Model for the Declustering of Earthquake Catalogs

Abstract: The simplest classification of earthquakes breaks down the total seismicity rate into two categories: background events generated by long-term, large-scale tectonic forcings, and aftershocks directly triggered by a background event or another aftershock. Physically speaking, classifying earthquakes in these two categories is not firmly accurate. However, isolating the background seismicity from the aftershocks, which we will refer to as catalog declustering, is crucial for a wide range of studies, such as the … Show more

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Cited by 22 publications
(11 citation statements)
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References 83 publications
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“…Steinmann et al (2022) proposes a hierarchical clustering strategy to classify noise and seismicity based on the deep scattering spectrum of the seismic data. Aden-Antoniow et al (2022) compresses the seismic information into a low-dimensional latent space using an autoencoder before these latent vectors are clustered to identify seismicity from different sources.…”
Section: Earthquake Data Applicationsmentioning
confidence: 99%
See 1 more Smart Citation
“…Steinmann et al (2022) proposes a hierarchical clustering strategy to classify noise and seismicity based on the deep scattering spectrum of the seismic data. Aden-Antoniow et al (2022) compresses the seismic information into a low-dimensional latent space using an autoencoder before these latent vectors are clustered to identify seismicity from different sources.…”
Section: Earthquake Data Applicationsmentioning
confidence: 99%
“…Aden‐Antoniow et al. (2022) compresses the seismic information into a low‐dimensional latent space using an autoencoder before these latent vectors are clustered to identify seismicity from different sources.…”
Section: Highlightsmentioning
confidence: 99%
“…The parent can be identified as the nearest neighbor using the proximity function of the spatio-temporal metric based on the Gutenberg-Richter law [7], which relates the magnitude and frequency of aftershocks, and modified Omori's law [13,18,19], which relates the time after the mainshock and occurrence rate of aftershocks. This metric follows a bimodal distribution related to the background seismicity and aftershocks, and methods to obtain two separate distributions are being actively studied [1]. Furthermore, the correlation metric is promising because it resembles the epidemic-type aftershock sequence model.…”
Section: Link-based Declusteringmentioning
confidence: 99%
“…We may cite for instance those based on the Epidemic Type Aftershock Sequence (ETAS) model (Iacoletti et al, 2022;Zhang & Huang, 2022;Mizrahi et al, 2022;Field et al, 2021Field et al, , 2022Hainzl, 2022), on nearest-neighbour distances (Zaliapin et al, 2008;Zhuang et al, 2002) or on supervised machine learning (Aden-Antoniow et al, 2022;Pavez O & Estay H, 2021;Seydoux et al, 2020). The reason why there are so many methods is that each of them takes into account new or additional statistical and/or physical features that are assumed to better describe the behaviour of earthquakes in the specific seismotectonic context for which they are applied (Zaliapin & Ben-Zion, 2021).…”
Section: Introductionmentioning
confidence: 99%