Data Publication

Model output for the paper "Offshore landward motion shortly after a subduction earthquake implies rapid relocking of the shallow megathrust"

Mario D'Acquisto

Utrecht University

(2022)

Descriptions

This repository contains the relevant data (part of numerical model output) used to plot the figures in the main body of the manuscript entitled "Offshore landward motion shortly after a subduction earthquake implies rapid relocking of the shallow megathrust", by Mario D'Acquisto and Rob Govers. Paper abstract: "Geodetic observations after large subduction earthquakes reflect multiple postseismic processes, including megathrust relocking. What the timing of relocking is, and how well observations constrain it, is unclear. It has been inferred to explain some observed landward motion that occurs within months. It has also been considered unable to explain other, greater landward motion, including off the coast of Japan beginning weeks after the 2011 Tohoku earthquake, which is attributed to postseismic relaxation. We use generic, 3D numerical models to show that relocking, particularly of the shallow interface, is needed for postseismic relaxation to produce landward motion on the tip of the overriding plate. We argue that this finding is consistent with previous simulations that implicitly relock the megathrust where afterslip is not included, that the Tohoku megathrust thus relocked within less than two months of the earthquake, and that the shallow megathrust probably behaves as a true, unstably sliding asperity." The model consists of a three-dimensional (3D) finite element method (FEM) simulation of the megathrust earthquake cycle with two fully elastic plates and Maxwell viscoelastic mantle. The software used to perform the simulations and extract the model output in the files stored here was GTECTON (Govers & Wortel, 1993, 2005; Govers et al., 2018), version 2021.0. The software used to generate the relevant figures in the paper from the data was Generic Mapping Tools (GMT) (Wessel et al., 2019) version 6.4.0. Each directory corresponds to a different model. The meaning of each model name, as well as the meaning of the file name and the internal data format of the files, are specified in the readme file (readme.txt). All files are plain text files. For more information regarding the goals, model features, and output, please refer to the paper. Contact person: Mario D'Acquisto - m.dacquisto@uu.nl

Keywords


Originally assigned keywords
FOS: Earth and related environmental sciences
numerical modeling
megathrust relocking
earthquake cycle
postseismic relaxation
surface velocities
offshore displacement
geophysics
tectonics
satellite geodesy
GTECTON
Generic Mapping Tools

Corresponding MSL vocabulary keywords
tectonic plate boundary

MSL enriched keywords
tectonic plate boundary
convergent tectonic plate boundary
subduction
subducting plate interface
tectonic deformation structure
tectonic fault
thrust fault
Measured property
stress relaxation

Metadata


MSL enriched sub domains

rock and melt physics

Resource Type

Research Data


Source


Source publisher

Utrecht University

DOI

10.24416/uu01-ss41uk

Creators

Mario D'Acquisto
Personal
Utrecht University

Contributors

D'Acquisto, Mario
Personal
Utrecht University
Govers, Rob
Personal
Utrecht University

Citation

D'Acquisto, M. (2022). Model output for the paper "Offshore landward motion shortly after a subduction earthquake implies rapid relocking of the shallow megathrust" (Version 1.0) [Data set]. Utrecht University. https://doi.org/10.24416/UU01-SS41UK


Dates

Issued 2022-10-07T15:32:02
Updated 2024-07-12T11:10:11
Collected 2022-03-05/2022-01-08

Language

en


Funding References

Funder Name NWO

Rights

Name Open - freely retrievable
URI info:eu-repo/semantics/openAccess
Name Creative Commons Attribution 4.0 International
URI https://creativecommons.org/licenses/by/4.0/legalcode
Identifier cc-by-4.0
Identifier Scheme SPDX
Scheme URI https://spdx.org/licenses/

Locations


Geo location(s)

Tohoku, Japan