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The data can be used to map lineaments, edges of structural bodies, and faulting/fracturing which are believed to be associated with basement structure and are thought to be important contributors to hydrocarbon trapping in this northern portion of the Green River Basin. Structural highs control some of the most significant fields discovered to date, and Paleozoic sections appear to be related to deep, reactivated basement structure. In addition, there are indications that secondary porosity macrofracture trends have propagated a significant distance up into sections overlying basement faults. Therefore, zones of intersecting basement fault trends will be more prospective for increased porosity and permeability.
The survey area is immediately southwest of the Wind River Mountains and in the greater Pinedale Field area. The area trends northwest to southeast with the northern boundary including portions of Township 37N-Range 112W through T37N-R110W. The area widens to the southeast and include portions of T26N-R110W through T26N-R105W in the south. The Wind River Mountains border the survey in the east, and the outcrops provide a reference for basement correlation. The LaBarge - Big Piney Complex on the northern part of the Moxa Arch borders the survey to the west.
The acquisition specifications are as follows:
The processing and data analysis deliverables include the following: