Changes

The tectonic setting and stratigraphic section are similar to the producing trend; therefore, the [[deformation]] features of the exposed structures can be used as analogs for producing structures to the south. The numbered ridge lines in the photo provide a set of natural serial cross sections through the structures ([[:file:exploring-for-structural-traps_fig20-13.png|Figure 10]]).

The tectonic setting and stratigraphic section are similar to the producing trend; therefore, the [[deformation]] features of the exposed structures can be used as analogs for producing structures to the south. The numbered ridge lines in the photo provide a set of natural serial cross sections through the structures ([[:file:exploring-for-structural-traps_fig20-13.png|Figure 10]]).

[[:file:exploring-for-structural-traps_fig20-14.png|Figure 10]] shows structures in the upper plate of the Absaroka thrust fault on the south side of ridge line 4 in [[:file:exploring-for-structural-traps_fig20-12.png|Figure 9]]. The white [http://www.merriam-webster.com/dictionary/outcrop outcrops] in the valley in the left foreground are tightly folded Ordovician Bighorn dolomite.

[[:file:exploring-for-structural-traps_fig20-14.png|Figure 10]] shows structures in the upper plate of the Absaroka thrust fault on the south side of ridge line 4 in [[:file:exploring-for-structural-traps_fig20-12.png|Figure 9]]. The white [http://www.merriam-webster.com/dictionary/outcrop outcrops] in the valley in the left foreground are tightly folded Ordovician Bighorn [[dolomite]].

==Prospect and location==

==Prospect and location==