Fig. 9From: Crustal deformation associated with the 2016 Kumamoto Earthquake and its effect on the magma system of Aso volcanoDifferential stress (S-DIF) and maximum (S-MAX) and minimum (S-MIN) principal stresses loaded on the surface of magma system by the movement of the seismic faults (F1, F2, F3, and F4) of the 2016 Kumamoto Earthquake, viewed from the southwest (a) and northeast (d). Thin lines indicate the axes of maximum and minimum principal stress, respectivelyBack to article page