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.

(a)

(b)

(c)