The study is complete except for the formal write-up and some core observations. For example, the proof for the seismogenic initiation of a polygonal fault system is complete. For this, a 5 square mile 3-D seismic dataset encompassing 25 vertical wells from Success, western Saskatchewan was analyzed. These seismic data were graciously provided by Andrew Dyke at TGS Canada Inc.
We will post visually pleasing images here from time-to-time. The adjacent image is from eastern Saskatchewan: