The Kidd Creek mine, near Timmins, Ontario, Canada, is a volcanogenic sulfide deposit consisting primarily of rhyolite, basalt, diorite, ultramafics, argillite, and massive sulfides. Previous work proved the feasibility of imaging massive sulfide deposits with seismic reflections (Meng and McGaughy, 1996; Hu, 1999). Here I migrate both PP reflection and SP transmission events to image the sulphide body. I also show the benefits of applying reduced-time migration to these data.