Clustering earthquake signals and background noises in continuous seismic data with unsupervised deep learning

International audience The continuously growing amount of seismic data collected worldwide is outpacing our abilities for analysis, since to date, such datasets have been analyzed in a human-expert-intensive, supervised fashion. Moreover, analyses that are conducted can be strongly biased by the sta...

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Bibliographic Details
Published in:Nature Communications
Main Authors: Seydoux, Léonard, Balestriero, Randall, Poli, Piero, Hoop, Maarten de, Campillo, Michel, Baraniuk, Richard
Other Authors: Institut des Sciences de la Terre (ISTerre), Institut national des sciences de l'Univers (INSU - CNRS)-Institut de recherche pour le développement IRD : UR219-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Gustave Eiffel-Université Grenoble Alpes (UGA), Rice University Houston, ANR-19-P3IA-0003,MIAI,MIAI @ Grenoble Alpes(2019)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2020
Subjects:
Online Access:https://hal.univ-grenoble-alpes.fr/hal-02929377
https://hal.univ-grenoble-alpes.fr/hal-02929377/document
https://hal.univ-grenoble-alpes.fr/hal-02929377/file/Preprint2_Seydoux_et_al.pdf
https://doi.org/10.1038/s41467-020-17841-x
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Summary:International audience The continuously growing amount of seismic data collected worldwide is outpacing our abilities for analysis, since to date, such datasets have been analyzed in a human-expert-intensive, supervised fashion. Moreover, analyses that are conducted can be strongly biased by the standard models employed by seismologists. In response to both of these challenges, we develop a new unsupervised machine learning framework for detecting and clustering seismic signals in continuous seismic records. Our approach combines a deep scattering network and a Gaussian mixture model to cluster seismic signal segments and detect novel structures. To illustrate the power of the framework, we analyze seismic data acquired during the June 2017 Nuugaatsiaq, Greenland landslide. We demonstrate the blind detection and recovery of the repeating precursory seismicity that was recorded before the main landslide rupture, which suggests that our approach could lead to more informative forecasting of the seismic activity in seismogenic areas.