Fractures are small cracks that occur when brittle rock is stressed to the point where it breaks. Zones of high stress frequently occur where the rock is bent the most, and therefore in places where seismic migration is most likely to be needed. Consequently, it is often important to be able to integrate seismic fracture analysis with migration. Conventional pre-and post-stack migration methods are incapable of handling azimuthal variations in amplitude. However, they can be modified to do this, and then they can be used in positioning seismic fracture attributes. Some such time-migration methods are tested on a geologically complex data set over the Manderson Field in Wyoming, USA, for which well control for the fractures in the reservoir is available. All these migrations collapse zones of apparently high fracture intensity and move them closer to significant structural features, e.g. faults. The conclusion is that these migration methods can successfully move the fracture attributes to appropriate positions.