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Bookmark or Share- Uinta Basin - SEG WikiThe Uinta Basin is a sedimentary basin that is characterized by both conventional and unconventional plays that exist in the majority of Northeast Utah branching into parts of Western Colorado.
- Uinta Basin - WikipediaThe Uinta Basin forms a geologic structural basin, and is the source of commercial oil and gas production. Separated from the Piceance Basin by the Douglas Creek Arch, both basins formed during the Laramide Orogeny, and are bounded by the Charleston-Nebo thrust fault, the Uinta Basin boundary fault, and the Grand Hogback monocline.
- Uinta Mountains - WikipediaThe Uinta Mountains are Laramide uplifted metasedimentary rocks deposited in an intracratonic basin in southwest Laurentia during the time of the breakup of the supercontinent Rodinia.
- Uinta Basin Rail - WikipediaThe Uinta Basin Rail project is a proposed 100-mile (160 km) rail line [1] to connect the shale oil rich Uinta Basin region of eastern Utah to the national rail network. Uinta Basin oil has a wax content that requires transport in insulated containers via truck or rail rather than pipeline since the oil will solidify at room temperature. [2]
- Mysteries of the Uinta Mountains - Utah Geological SurveyLater, a normal fault developed along the reactivated suture zone that formed the northern boundary of a Neoproterozoic (770 to 740 million-year-old) basin in which thick sand, gravel, and mud accumulated—today’s Uinta Mountain Group and the core of the Uinta Mountains.
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