“…In Sweden, initial successful imaging of faults and fracture zones within Precambrian crystalline rocks was driven by experimental surveys for mineral exploration and the characterization of radioactive waste storage sites (e.g., Juhlin et al, 1991;Juhlin, 1995). This early successful high-resolution seismic reflection work by Juhlin et al (1991), allowing imaging of fracture zones and lithological contrasts (Figure 13), paved the way for two larger projects in Sweden to study large-scale structures hosting mineral deposits, namely GEORANGE3D (e.g., Malehmir et al, 2006Malehmir et al, , 2007Malehmir et al, , 2009aMalehmir et al, , 2009bTryggvason et al, 2006;Hübert et al, 2009) and VINNOVA4D (Dehghannejad et al, 2010(Dehghannejad et al, , 2012a(Dehghannejad et al, , 2012bSkyttä et al, 2010;Bauer et al, 2011). These projects were of a multidisciplinary nature and allowed the construction of a 3D geologic model of a major mining district of northern Sweden.…”