Spatiotemporal Variation of Mantle Viscosity and the Presence of Cratonic Mantle Inferred From 8 Years of Postseismic Deformation Following the 2010 Maule, Chile, Earthquake

Author:

Li Shaoyang12ORCID,Bedford Jonathan1ORCID,Moreno Marcos13ORCID,Barnhart William D.2ORCID,Rosenau Matthias1ORCID,Oncken Onno1ORCID

Affiliation:

1. Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences; Potsdam Germany

2. Department of Earth and Environmental Sciences; University of Iowa; Iowa City IA USA

3. Department of Geophysics; University of Concepcion; Concepcion Chile

Funder

Deutsche Forschungsgemeinschaft

German Science Foundation (DFG)

Helmholtz graduate research school GeoSim

Chilean National Fund for Development of Science and Technology (FONDECYT)

Millennium Scientific Initiative (ICM) of the Chilean Government

Research Center for Integrated Disaster Risk Management (CIGIDEN), CONICYT/FONDAP

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference49 articles.

1. A domain decomposition approach to implementing fault slip in finite-element models of quasi-static and dynamic crustal deformation;Aagaard;Journal of Geophysical Research: Solid Earth,2013

2. Asthenosphere flow modulated by megathrust earthquake cycles;Barbot;Geophysical Research Letters,2018

3. A high-resolution, time-variable afterslip model for the 2010 Maule Mw = 8.8, Chile megathrust earthquake;Bedford;Earth and Planetary Science Letters,2013

4. Separating rapid relocking, afterslip, and viscoelastic relaxation: An application of the postseismic straightening method to the Maule 2010 cGPS;Bedford;Journal of Geophysical Research: Solid Earth,2016

5. Crustal motion north and south of the Arica deflection: Comparing recent geodetic results from the Central Andes;Bevis;Geochemistry, Geophysics, Geosystems,2000

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