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  5. Predicting imminence of analog megathrust earthquakes with Machine Learning: Implications for monitoring subduction zones
 
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Predicting imminence of analog megathrust earthquakes with Machine Learning: Implications for monitoring subduction zones

Author(s)
Corbi, Fabio  
Freie Universität Berlin, Department of Earth Sciences, Institute of Geological Sciences, Berlin, Germany  
Bedford, John  
Helmholtz Centre Potsdam -GFZ German Research Centre for Geosciences, Potsdam, Germany  
Sandri, Laura  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia  
Funiciello, Francesca  
Università “Roma TRE”, Dip. Scienze, Laboratory of Experimental Tectonics, Rome, Italy  
Gualandi, Adriano  
California Institute of Technology, Pasadena, CA, USA  
Rosenau, Mathias  
Helmholtz Centre Potsdam -GFZ German Research Centre for Geosciences, Potsdam, Germany  
Language
English
Obiettivo Specifico
7T. Variazioni delle caratteristiche crostali e precursori sismici
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Geophysical Research Letters  
Issue/vol(year)
4 /47 (2020)
ISSN
0094-8276
Publisher
Agu
Pages (printed)
e2019GL086615
Date Issued
April 2020
DOI
10.1029/2019GL086615
URI
https://www.earth-prints.org/handle/2122/13515
Abstract
Subduction zones are monitored using space geodesy with increasing resolution, with the aim of better capturing the deformation accompanying the seismic cycle. Here, we investigate data characteristics that maximize the performance of a machine learning binary classifier predicting slip‐event imminence. We overcome the scarcity of recorded instances from real subduction zones using data from a seismotectonic analog model monitored with a spatially dense, continuously recording onshore geodetic network. We show that a 70‐85 km wide coastal swath recording interseismic deformation gives the most important information on slip imminence. Prediction performances are mainly influenced by the alarm duration (amount of time that we consider an event as imminent), with density of stations and record length playing a secondary role. The techniques developed in this study are most likely applicable in regions of slow‐earthquakes, where stick‐slip‐like failures occur at time intervals of months to years.
Type
article
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