A Transient in Surface Motions Dominated by Deep Afterslip Subsequent to a Shallow Supershear Earthquake: The 2018 Mw7.5 Palu Case

Abstract The 2018 Mw7.5 Palu earthquake is a remarkable strike‐slip event due to its nature as a shallow supershear fault rupture across several segments and a destructive tsunami that followed coseismic deformation. GPS offsets in the wake of the 2018 earthquake display a transient in the surface m...

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Main Authors: N. Nijholt, W. J. F. Simons, J. Efendi, D. A. Sarsito, R. E. M. Riva
Format: Article
Language:English
Published: Wiley 2021-04-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
Online Access:https://doi.org/10.1029/2020GC009491
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author N. Nijholt
W. J. F. Simons
J. Efendi
D. A. Sarsito
R. E. M. Riva
author_facet N. Nijholt
W. J. F. Simons
J. Efendi
D. A. Sarsito
R. E. M. Riva
author_sort N. Nijholt
collection DOAJ
description Abstract The 2018 Mw7.5 Palu earthquake is a remarkable strike‐slip event due to its nature as a shallow supershear fault rupture across several segments and a destructive tsunami that followed coseismic deformation. GPS offsets in the wake of the 2018 earthquake display a transient in the surface motions of northwest Sulawesi. A Bayesian approach identifies (predominantly aseismic) deep afterslip on and below the coseismic rupture plane as the dominant physical mechanism causing the cumulative, postseismic, surface displacements whereas viscous relaxation of the lower crust and poro‐elastic rebound contribute negligibly. We confirm a correlation between shallow supershear rupture and postseismic surface transients with afterslip activity in the zone below an interseismically locked fault plane where the slip rate tapers from zero to creeping.
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spelling doaj.art-4acf30b6a3204ecf8c881ea78a517c892023-11-03T16:55:42ZengWileyGeochemistry, Geophysics, Geosystems1525-20272021-04-01224n/an/a10.1029/2020GC009491A Transient in Surface Motions Dominated by Deep Afterslip Subsequent to a Shallow Supershear Earthquake: The 2018 Mw7.5 Palu CaseN. Nijholt0W. J. F. Simons1J. Efendi2D. A. Sarsito3R. E. M. Riva4Department of Geoscience and Remote Sensing Faculty of Civil Engineering and Geosciences Delft University of Technology Delft The NetherlandsDepartment of Space Engineering Faculty of Aerospace Engineering Delft University of Technology Delft The NetherlandsBIG (Badan Informasi Geospasial/Geospatial Information Agency) Java IndonesiaFaculty of Earth Sciences and Technology ITB (Institut Teknologi Bandung/Institute of Technology Bandung) Geodesy Research Group Bandung IndonesiaDepartment of Geoscience and Remote Sensing Faculty of Civil Engineering and Geosciences Delft University of Technology Delft The NetherlandsAbstract The 2018 Mw7.5 Palu earthquake is a remarkable strike‐slip event due to its nature as a shallow supershear fault rupture across several segments and a destructive tsunami that followed coseismic deformation. GPS offsets in the wake of the 2018 earthquake display a transient in the surface motions of northwest Sulawesi. A Bayesian approach identifies (predominantly aseismic) deep afterslip on and below the coseismic rupture plane as the dominant physical mechanism causing the cumulative, postseismic, surface displacements whereas viscous relaxation of the lower crust and poro‐elastic rebound contribute negligibly. We confirm a correlation between shallow supershear rupture and postseismic surface transients with afterslip activity in the zone below an interseismically locked fault plane where the slip rate tapers from zero to creeping.https://doi.org/10.1029/2020GC009491afterslipBayesian inferenceGPSpostseismic deformationstrike‐slip faultSulawesi
spellingShingle N. Nijholt
W. J. F. Simons
J. Efendi
D. A. Sarsito
R. E. M. Riva
A Transient in Surface Motions Dominated by Deep Afterslip Subsequent to a Shallow Supershear Earthquake: The 2018 Mw7.5 Palu Case
Geochemistry, Geophysics, Geosystems
afterslip
Bayesian inference
GPS
postseismic deformation
strike‐slip fault
Sulawesi
title A Transient in Surface Motions Dominated by Deep Afterslip Subsequent to a Shallow Supershear Earthquake: The 2018 Mw7.5 Palu Case
title_full A Transient in Surface Motions Dominated by Deep Afterslip Subsequent to a Shallow Supershear Earthquake: The 2018 Mw7.5 Palu Case
title_fullStr A Transient in Surface Motions Dominated by Deep Afterslip Subsequent to a Shallow Supershear Earthquake: The 2018 Mw7.5 Palu Case
title_full_unstemmed A Transient in Surface Motions Dominated by Deep Afterslip Subsequent to a Shallow Supershear Earthquake: The 2018 Mw7.5 Palu Case
title_short A Transient in Surface Motions Dominated by Deep Afterslip Subsequent to a Shallow Supershear Earthquake: The 2018 Mw7.5 Palu Case
title_sort transient in surface motions dominated by deep afterslip subsequent to a shallow supershear earthquake the 2018 mw7 5 palu case
topic afterslip
Bayesian inference
GPS
postseismic deformation
strike‐slip fault
Sulawesi
url https://doi.org/10.1029/2020GC009491
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