Fig. 3From: Reconsideration of the energy balance in earthquake faultingTwo independent source regions \(V_{{{\text{s0}}}}\) and \(V_{{{\text{s1}}}}\) in an elastic body \(V\) bounded by a traction-free external surface \(S_{{{\text{ex}}}}\). \(\sigma_{ij}\) represents a common stress fieldBack to article page