Fig. 4From: Temporal gravity anomalies observed in the Tokai area and a possible relationship with slow slipsThe poroelastic model. a The rate for gravity change at 3 years after the onset of the LSSE for model B. b The same as in (a) but for the pressure increment. c A model configuration. The dip angle is assumed to be constant with depth. d The pressure increment along the X-axis for model B. The blue and red curves represent the steady-state solution (the left vertical axis) and the pressure change in 3 years from the onset of the LSSE (the right vertical axis), respectivelyBack to article page