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      The damage is done: Low fault friction recorded in the damage zone of the shallow Japan Trench décollement : JAPAN TRENCH DAMAGE ZONE AND FRICTION

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      Journal of Geophysical Research: Solid Earth
      Wiley-Blackwell

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          Geologically current plate motions

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            Shallow dynamic overshoot and energetic deep rupture in the 2011 Mw 9.0 Tohoku-Oki earthquake.

            Strong spatial variation of rupture characteristics in the moment magnitude (M(w)) 9.0 Tohoku-Oki megathrust earthquake controlled both the strength of shaking and the size of the tsunami that followed. Finite-source imaging reveals that the rupture consisted of a small initial phase, deep rupture for up to 40 seconds, extensive shallow rupture at 60 to 70 seconds, and continuing deep rupture lasting more than 100 seconds. A combination of a shallow dipping fault and a compliant hanging wall may have enabled large shallow slip near the trench. Normal faulting aftershocks in the area of high slip suggest dynamic overshoot on the fault. Despite prodigious total slip, shallower parts of the rupture weakly radiated at high frequencies, whereas deeper parts of the rupture radiated strongly at high frequencies.
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              Physical explanation for the displacement-length relationship of faults using a post-yield fracture mechanics model

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                Author and article information

                Journal
                Journal of Geophysical Research: Solid Earth
                J. Geophys. Res. Solid Earth
                Wiley-Blackwell
                21699313
                May 2016
                May 14 2016
                : 121
                : 5
                : 3804-3824
                Article
                10.1002/2015JB012311
                5b79171c-6135-4a22-8406-fd15ef67a1e7
                © 2016

                http://doi.wiley.com/10.1002/tdm_license_1.1

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