Non-Stationary Crustal Deformation around the Bungo Channel
Non-stationary crustal deformation was detected around the Bungo Channel. It began in the summer of 2014 and is almost stagnant at present.
Upper figure: Horizontal deformation vectors (non-stationary component)
Lower figure: Graphs of time series (non-stationary component)
Geospatial Information Authority of Japan
[Evaluation of Seismic Activities for February 2015 (March 10, 2015)]