A considerable amount of orebodies, especially rich ores at home and abroad, were discovered at the tectonic intersections of different strikes, features, types, scales or phases. The scales, features, phases and active sequence of the structures, as well as their close relationships with the magmatic activities defined the type and the size of the orebodies. With several cases located at these intersections and the authors′years of prospecting practice, this paper points out that orebodies, especially rich orebodies tend to form at the intersections, which would provide reference for geological prospecting. |