Figure 5
From: Earthquake source parameters in Zagros region (Iran) from the time-evolutive P-wave displacement

Segments including large events shown in Fig. 1 with rectangles. Rupture lengths are shown as oriented projections along the strike of the causative fault (see Table 1). For the Ezgeleh earthquake, dashed rectangle shows the surface projection of the fault obtained from the Haskell model. This figure also represents the available historical events10 with yellow hexagons at each segment.