Fig. 8From: Geological structures controlled the rupture process of the 2011 M9.0 Tohoku-Oki earthquake in the Northeast Japan ArcQuasi-static slip rate distribution from March 11, 1996 to March 11, 2008 (Uchida and Matsuzawa 2013). The “white” regions represent the regions where there are no repeating earthquakesBack to article page