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We investigated aseismic slip in Shikoku and Kyushu islands using GNSS data and found out that Bungo, northern Miyazaki, and southern Miyazaki slow slips were occurring. The top figure shows the estimated aseismic slips with arrows indicating aseismic slip vectors. The two different rupture processes from 2013 to 2015 and from 2015 to 2016 may be an important clue toward understanding subduction tectonics in southwest Japan.

Long-term slow slip events along the Nankai trough subduction zone after the 2011 Tohoku earthquake in Japan