GPS constraints on deformation in northern Central America from 1999 to 2017, Part 1 – Time-dependent modelling of large regional earthquakes and their post-seismic effects
Autor: | Hélène Lyon-Caen, Douglas Hernández, Vladimir Kostoglodov, Manuel Rodriguez Maradiaga, Pierre Briole, Alejandra Staller, S. E. Graham, A. P. Ellis, Omar Flores, Niel Lord, Robert McCaffrey, Marco Guzmán-Speziale, E. Molina, Peter LaFemina, Robert D. Rogers, Cécile Lasserre, Charles DeMets, Jeffrey Rivera, Beatriz Cosenza |
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Přispěvatelé: | Department of Geosciences, University of Wisconsin-Madison, Laboratoire de géologie de l'ENS (LGE), Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS Paris)-École normale supérieure - Paris (ENS Paris), Universidad San Carlos, Department of Environmental, Earth and Ocean Sciences [Boston] (EEOS), University of Massachusetts [Boston] (UMass Boston), University of Massachusetts System (UMASS)-University of Massachusetts System (UMASS), Centro de Geociencias [Queretaro], Universidad Nacional Autónoma de México (UNAM), Instituto de Geofísica, Pennsylvania State University (Penn State), Penn State System-Penn State System, Institut des Sciences de la Terre (ISTerre), Université Grenoble Alpes (UGA)-Centre National de la Recherche Scientifique (CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-PRES Université de Grenoble-Institut de recherche pour le développement [IRD] : UR219-Institut national des sciences de l'Univers (INSU - CNRS)-Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR)-Université Joseph Fourier - Grenoble 1 (UJF), Universidad Nacional Autónoma de Honduras, Department of Geology [Portland], Portland State University [Portland] (PSU), Universidad Mariano Galvez, California State University [Stanislaus], Universidad Politécnica de Madrid (UPM), Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement [Lyon] (LGL-TPE), École normale supérieure - Lyon (ENS Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-École normale supérieure - Lyon (ENS Lyon), Laboratoire de géologie de l'ENS (LGENS), École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL), Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR)-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 Grenoble Alpes [2016-2019] (UGA [2016-2019]), Universidad Nacional Autónoma de Honduras (UNAH), École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS-PSL), Universidad Nacional Autónoma de México = National Autonomous University of Mexico (UNAM), Penn State Department of Geosciences |
Jazyk: | angličtina |
Rok vydání: | 2018 |
Předmět: |
010504 meteorology & atmospheric sciences
Satellite geodesy Space geodetic surveys [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] Earthquake prediction Slip (materials science) 010502 geochemistry & geophysics 01 natural sciences Mantle (geology) Geochemistry and Petrology Middle america ComputingMilieux_MISCELLANEOUS 0105 earth and related environmental sciences [SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonics Seismic cycle business.industry Geodetic datum Central America Geodesy Geophysics Transient deformation Trench Global Positioning System business Geology |
Zdroj: | Geophysical Journal International Geophysical Journal International, Oxford University Press (OUP), 2018, 214 (3), pp.2177-2194. ⟨10.1093/gji/ggy249⟩ Geophysical Journal International, 2018, 214 (3), pp.2177-2194. ⟨10.1093/gji/ggy249⟩ |
ISSN: | 0956-540X 1365-246X |
DOI: | 10.1093/gji/ggy249⟩ |
Popis: | International audience; We use continuous and campaign measurements from 215 GPS sites in northern Central America and southern Mexico to estimate coseismic and afterslip solutions for the 2009 M w = 7.3 Swan Islands fault strike-slip earthquake and the 2012 M w = 7.3 El Salvador and M w = 7.4 Guatemala thrust-faulting earthquakes on the Middle America trench. Our simultaneous , time-dependent inversion of more than 350 000 daily GPS site positions gives the first jointly consistent estimates of the coseismic slips for all three earthquakes, their combined time-dependent post-seismic effects and secular station velocities corrected for both the co-seismic and post-seismic deformation. Our geodetic slip solutions for all three earthquakes agree with previous estimates that were derived via static coseismic-offset modelling. Our time-dependent model, which attributes all transient post-seismic deformation to earthquake afterslip, fits nearly all of the continuous GPS site position time-series within their several-millimetre position noise. Afterslip moments for the three earthquakes range from 35 to 140 per cent of the geodetic coseismic moments, with the largest afterslip estimated for the 2012 El Salvador earthquake along the weakly coupled El Salvador trench segment. Forward modelling of viscoelastic deformation triggered by all three earthquakes for a range of assumed mantle and lower crustal viscosities suggests that it accounts for under 20 per cent of the observed post-seismic deformation and possibly under 10 per cent. Our results thus point to afterslip as the primary and perhaps dominant mode of post-seismic deformation for these C The Author(s) |
Databáze: | OpenAIRE |
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