Changes

Detailed analysis of the fairway proceeded using surface and subsurface data. Examples of the data used are shown below.

Detailed analysis of the fairway proceeded using surface and subsurface data. Examples of the data used are shown below.

[[:file:exploring-for-structural-traps_fig20-11.png|Figure 8]] shows a cross section across the Whitney Canyon and Ryckman Creek producing structures in the upper plate of the Absaroka thrust.

[[:file:exploring-for-structural-traps_fig20-11.png|Figure 8]] shows a [[cross section]] across the Whitney Canyon and Ryckman Creek producing structures in the upper plate of the Absaroka thrust.

[[:file:exploring-for-structural-traps_fig20-9.png|Figure 6]] shows an interpreted seismic line in the approximate location of [[:file:exploring-for-structural-traps_fig20-11.png|Figure 8]].

[[:file:exploring-for-structural-traps_fig20-9.png|Figure 6]] shows an interpreted seismic line in the approximate location of [[:file:exploring-for-structural-traps_fig20-11.png|Figure 8]].

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==

Physical models, such as those in [[:file:exploring-for-structural-traps_fig20-16.jpg|Figure 13]], that display structures similar in shape to natural, prospect-scale, thrust-related structures can provide insight on the overall geometry of the prospect and the location of zones of high strain (high [[fracture]] density?) within the structure. These insights can be useful in determining optimal well locations.

Physical models, such as those in [[:file:exploring-for-structural-traps_fig20-16.jpg|Figure 13]], that display structures similar in shape to natural, prospect-scale, thrust-related structures can provide insight on the overall geometry of the prospect and the location of zones of high strain (high [[fracture]] density?) within the structure. These insights can be useful in determining optimal well locations.

These models were constructed of originally planar layers of limestone, sandstone, and granite. They were [[Deformation|deformed]] in a pressure vessel at an effective overburden pressure of 15 × 10³ psi (1 × 10⁵ kPa). The top view is a photomicrograph of a model that simulates a thrust ramp. The bottom view simulates the hanging-wall geometry produced by movement along a series of bedding-parallel and ramp segments of a thrust fault.

These models were constructed of originally planar layers of [[limestone]], sandstone, and granite. They were [[Deformation|deformed]] in a pressure vessel at an effective overburden pressure of 15 × 10³ psi (1 × 10⁵ kPa). The top view is a photomicrograph of a model that simulates a thrust ramp. The bottom view simulates the hanging-wall geometry produced by movement along a series of bedding-parallel and ramp segments of a thrust fault.

Data on deformation mechanisms, such as fractures and how they affect reservoir properties, are obtained by integrating [http://www.merriam-webster.com/dictionary/outcrop outcrop] fracture data and laboratory estimates of fracture aperture. This integration allows for a direct calculation of fracture [[porosity]] and fracture [[permeability]] for the reservoir.

Data on deformation mechanisms, such as fractures and how they affect reservoir properties, are obtained by integrating [http://www.merriam-webster.com/dictionary/outcrop outcrop] fracture data and laboratory estimates of fracture aperture. This integration allows for a direct calculation of fracture [[porosity]] and fracture [[permeability]] for the reservoir.

[[Category:Predicting the occurrence of oil and gas traps]]  

[[Category:Predicting the occurrence of oil and gas traps]]  

[[Category:Exploring for structural traps]]

[[Category:Exploring for structural traps]]