Item talk:Q57182

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     "name": "Structure contour and overburden maps of the Niobrara interval of the Upper Cretaceous Cody Shale in the Wind River Basin, Wyoming",
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     "abstract": "The Wind River Basin in central Wyoming is one of many structural and\u00a0sedimentary basins that formed in the Rocky Mountain foreland during\u00a0the Laramide orogeny. The basin is bounded by the Washakie, Owl Creek, and southern Bighorn uplifts on the north, the Casper arch on the east,\u00a0the Granite Mountains uplift on the south, and Wind River uplift on\u00a0the west.The first commercial oil well in Wyoming was drilled at Dallas dome\u00a0near an oil seep along the southwestern edge of the Wind River Basin\u00a0in 1884. Since then, many important conventional oil and gas fields,\u00a0that produce from reservoirs ranging in age from Mississippian through\u00a0Tertiary, have been discovered in this basin. In addition, an extensive\u00a0unconventional (continuous) overpressured basin-centered gas\u00a0accumulation has been identified in Cretaceous and Tertiary strata in\u00a0the deeper parts of the basin. It has been suggested that various Upper\u00a0Cretaceous marine shales, including the Cody Shale, are the principal\u00a0hydrocarbon source rocks for many of these accumulations. With recent\u00a0advances in horizontal drilling and multistage fracture stimulation,\u00a0there has been an increase in exploration and completion of wells in\u00a0equivalent marine shales in other Rocky Mountain Laramide basins that\u00a0were traditionally thought of only as hydrocarbon source rocks.\u00a0The maps presented in this report were constructed as part of a project\u00a0carried out by the U.S. Geological Survey to characterize the geologic\u00a0framework of potential undiscovered continuous (unconventional) oil\u00a0and gas resources of the Niobrara interval of the Upper Cretaceous Cody\u00a0Shale in the Wind River Basin in central Wyoming.",
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