Fig. 3From: Long-term slow slip events along the Nankai trough subduction zone after the 2011 Tohoku earthquake in JapanObserved horizontal detrended crustal deformation, computed deformations, and residuals in Shikoku and Kyushu obtained from our best-fitting aseismic slip model. Green arrows in the top figure indicate the observed detrended crustal deformation, while red arrows in the middle figure indicate the computed crustal deformation. Black arrows in the bottom figure indicate residuals. a–g The deformation rate and h the total crustal deformation. Thin solid lines indicate prefectural boundaries in Japan. The other nomenclature is the same for the top, middle, and bottom figures. a January 1, 2013–October 1, 2013. b October 1, 2013–May 1, 2014. c May 1, 2014–October 1, 2014. d October 1, 2014–April 1, 2015. e April 1, 2015–July 1, 2015. f July 1, 2015–February 1, 2016. g February 1, 2016–April 10, 2016. h Total detrended crustal deformation observed (top), computed (middle), and residuals (bottom) for the period between January 1, 2013, and April 10, 2016Back to article page