Seismic potential around the 2018 Hokkaido Eastern Iburi earthquake assessed considering the viscoelastic relaxation
Author:
Funder
Japan Society for the Promotion of Science
Publisher
Springer Science and Business Media LLC
Subject
Space and Planetary Science,Geology
Link
http://link.springer.com/content/pdf/10.1186/s40623-019-1036-4.pdf
Reference45 articles.
1. Barbot S, Fialko Y (2010) A unified continuum representation of postseismic relaxation mechanisms: semi-analytic models of afterslip, poroelastic rebound and viscoelastic flow. Geophys J Int 182(3):1124–1140. https://doi.org/10.1111/j.1365-246X.2010.04678.x
2. Barbot S, Moore JD, Lambert V (2017) Displacement and stress associated with distributed anelastic deformation in a half-space. Bull Seismol Soc Am 107(2):821–855. https://doi.org/10.1785/0120160237
3. Cho I, Kuwahara Y (2013a) Constraints on the three-dimensional thermal structure of the lower crust in the Japanese Islands. Earth Planets Space 65:855–861. https://doi.org/10.5047/eps.2013.01.005
4. Cho I, Kuwahara Y (2013b) Numerical simulation of crustal deformation using a three-dimensional viscoelastic crustal structure model for the Japanese islands under east-west compression. Earth Planet Space 65:1041–1046. https://doi.org/10.5047/eps.2013.05.006
5. Collettini C, Trippetta F (2007) A slip tendency analysis to test mechanical and structural control on aftershock rupture planes. Earth Planet Sci Lett 255:402–413. https://doi.org/10.1016/j.epsl.2007.01.001
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