Dynamics of a fault model with two mechanically different regions
Author:
Publisher
Springer Science and Business Media LLC
Subject
Space and Planetary Science,Geology
Link
http://link.springer.com/content/pdf/10.1186/s40623-017-0731-2.pdf
Reference48 articles.
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3. Barbot S, Fialko Y, Bock Y (2009) Postseismic deformation due to the $$M_w$$ M w 6.0 2004 Parkfield earthquake: stress-driven creep on a fault with spatially variable rate-and-state friction parameters. J Geophys Res 114:B07405. doi: 10.1029/2008JB005748
4. Belardinelli ME, Bonafede M (1995) Post-seismic stress evolution for a strike-slip fault in the presence of a viscoelastic asthenosphere. Geophys J Int 123:744–756. doi: 10.1111/j.1365-246X.1995.tb06887.x
5. Bletery Q, Sladen A, Delouis B, Vallée M, Nocquet J-M, Rolland L, Jiang J (2014) A detailed source model for the $$M_w$$ M w 9.0 Tohoku-Oki earthquake reconciling geodesy, seismology, and tsunami records. J Geophys Res Solid Earth 119:7636–7653. doi: 10.1002/2014JB011261
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