Fig. 10From: Dynamics of a fault model with two mechanically different regionsGround displacement produced by afterslip following the 2011 Tohoku-Oki earthquake, according to the model. a Horizontal component; b vertical component \(u_3\). The rectangle is the projection of the weak fault region on the Earth’s surface, and the dashed segment is the fault trace. The \(x_1\) and \(x_2\) axes are parallel to the strike direction of the fault and to the direction normal to strike, respectively. Distances are measured in units of the half-side of the fault along the strike direction, namely \(L = 200\) kmBack to article page