Research Article

Modelling Seismically Induced Mesothermal Goldfields along the Deep-Rooted Cadillac-Larder Lake Fault, Abitibi, Canada

Figure 4

Coulomb static stress changes following the rupture of the Joannes Segment. (a) Model 1.a includes only the Cadillac-Larder Lake Fault. (b) Model 1.b includes rheological contrasts and the structural framework. (c) Model 1.c same as 1.b but with foliation fabric added as low-strength primary failing planes. Positive lobe boundaries are set at 30 kPa. The circles indicate deposits’ locations, with colours reflecting the distinct goldfields as explained in Figure 1.