MOESM7 of Long-term slow slip events along the Nankai trough subduction zone after the 2011 Tohoku earthquake in Japan
journal contributionposted on 21.04.2017 by Shinzaburo Ozawa
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Additional file 7. (A) ∆CFS calculated from the aseismic slip for the period between January 2013 and May 2014 assuming a rigidity of 30 GPa, Poisson’s ratio of 0.25, and a friction coefficient of 0.2. The rake angle is opposite the motion of the Philippine Sea plate. The red arrows indicate the aseismic slip. (B) ∆CFS calculated from the aseismic slip for the period between July 2015 and February 2016. The nomenclature is the same as that of (A). (C) ∆CFS calculated from the total aseismic slip for the entire period in this study. Stars show the epicenters of the 1996 Hyuga-nada earthquakes. The nomenclature is the same as that of (A). ∆CFS is shown in areas adjacent to the aseismic slip area since we cannot calculate ∆CFS in aseismic slip areas.