Fig. 3From: Long-term slow slip events along the Nankai trough delayed by the 2016 Kumamoto earthquake, JapanDetrended crustal deformation (black arrows) and computation from our optimal model (white arrows). a–h Horizontal displacements. a April 1, 2018–June 1, 2018. b June 1, 2018–August 1, 2018. c August 1, 2018–October 1, 2018. d October 1, 2018–December, 1, 2018. e December 1, 2018–February 1, 2019. f February 1, 2019–April 1, 2019. g April 1, 2019–June 1, 2019. h June 1, 2019–August 1, 2019. i–p Vertical displacements for the periods corresponding to a–h. The color shows the computed vertical displacements, while solid arrows indicate observationsBack to article page