Figure 7
From: A long-term slow slip event from 1996 to 1997 in the Kii Channel, Japan
Spatiotemporal distribution of long-term slow slip events along the Nankai Trough. Dots represent the epicenters of low-frequency earthquakes from January 2006 to December 2010. The gray rectangle indicates the investigation period using leveling and sea-level data (Kobayashi and Yamamoto 2011; Kobayashi 2012; Kobayashi 2013). T: Tokai (Kobayashi and Yoshida 2004; Yamamoto et al. 2005; Suito and Ozawa 2009). KP: Kii Peninsula (Kobayashi 2013). KC: Kii Channel (this study). S1: central Shikoku (Kobayashi 2012). S2: western Shikoku (Kobayashi 2010). B: Bungo Channel (Hirose et al. 1999; Kobayashi and Yamamoto 2011; Ozawa et al. 2013). H: Hyuga-nada (Yarai and Ozawa 2013).