The Cretaceous Cadotte Sandstone limit is taken from Leckie et al. Well control diminishes along the course of the Peace River, related to present-day erosion. Figure 3.7 Dunvegan and Belloy gas fields. Structure map on the Mississippian Debolt Formation. The Dunvegan Fault is approximately coincident with the northeast limit of the Ksituan magnetically positive arc.
Tops are from a variety of sources and can be used only in a regional context.
Figure 3.8 Dunvegan seismic section. Displacement of Devonian Wabamun is 60 ms. Figure 3.10 Burial history curves and Phanerozoic isopach map. No profile is decompacted. Locations are indicated by letters on the accompanying Phanerozoic map.