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Reservoir modeling and composition simulation of primary depletion, waterflooding, and carbon dioxide flooding of a small Pennsylvanian carbonate mound complex, Anasazi field, Paradox Basin, Utah, Volume I (OFR-420)Vendor: Utah Geological SurveyBy: W. E. Culham and D. M. Lorenz This report presents the results of a comprehensive reservoir statistical modeling and oil-flow simulation engineering study of Runway field, Utah. The Runway reservoir is a deeper water bryozoan and phylloid-algal mound, found in many small fields...
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Correlation of Jurassic sediments of the Carmel and Twin Creek Formations of southern Utah using bentonitic characteristics (OFR-169)Vendor: Utah Geological SurveyB. H. Everett, B. J. Kowallis, E. H. Christiansen, and A. Deino The Jurassic Carmel Formation and Twin Creek Limestone of southern and central Utah are thought to be time equivalent deposits of marine carbonate and terrigenous sedimentary rocks that document a transgression of...
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Geology and Grand County (MP-Q)Vendor: Utah Geological SurveyBy: H. H. Doelling and others Grand County is located in the heart of the Colorado Plateaus physiographic province, ranks 9th in land area with 3,692 square miles with a population of only 8241, 20th out of 29 Utah counties (1980 census). Perhaps more...
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Geologic map of the Wales quadrangle, Juab and Sanpete Counties, Utah (MP 99-2)Vendor: Utah Geological SurveyBy: T. F. Lawton and M. P. Weiss The Wales quadrangle lies in a region of structural transition between the extended lithosphere of the Basin and Range and the moderately deformed Colorado Plateau. In Late Cretaceous time, this region was the leading edge of...
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Geology of the Sheeprock thrust sheet, central Utah - new insights (MP 98-1)Vendor: Utah Geological SurveyBy: M. Mukul and G. Mitra Proterozoic sedimentary rocks in the Sheeprock and the adjacent West Tintic Mountains in northcentral Utah were thought to be deformed and transported along the Sheeprock and Pole Canyon thrusts during the Cretaceous to early Tertiary Sevier Orogeny. Evidence...
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The Prairie Canyon Member, a new unit of the Upper Cretaceous Mancos Shale, west-central Colorado and east-central Utah (MP 97-4)Vendor: Utah Geological SurveyBy: R. D. Cole, R. G. Young and G. C. Willis For more than 30 years, surface and subsurface investigations of Upper Cretaceous strata in the southeastern Uinta Basin, southwestern Piceance Creek Basin, and along the intervening Douglas Creek arch, have documented that the...
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Outcrop study of the lower Green River Formation for reservoir characterization and hydrocarbon production enhancement in the Altamont-Bluebell field, Uinta Basin, Utah (MP 96-2)Vendor: Utah Geological SurveyBy: A. Garner and T. H. Morris In an effort to better understand the reservoir capacity and production potential of rock types in the Altamont-BluebeIl field, Uinta Basin, Utah, 850.2 meters (2789.4 ft) of continuous section of the lower Green River Formation were described...
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Collapsible soil hazard map for the southern Wasatch Front, Utah (MP 90-1)Vendor: Utah Geological SurveyBy: R. L. Owens and K. M. Rollins Soil collapse is usually associated with human activities such as irrigation, construction of canals, or disposal of wastewater that introduce water into a relatively dry environment. Although soil collapse is generally not life threatening, it can...
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Water-related geologic problems of 1983 - Utah occurrences by County (MP 89-4)Vendor: Utah Geological SurveyBy: B. N. Kaliser Twenty-four counties in Utah were surveyed in 1983-84 to compile this summary of known geological events related to the 1983 wet year. It is hoped that this summary and the one by Davis will provide a data base that is...
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Geologic consequences of the 1983 wet year in Utah (MP 88-3)Vendor: Utah Geological SurveyBy: B. N. Kaliser and J. E. Slossen Geologic consequences of the abnormally wet year of 1983 were unprecedented in number, magnitude, and geographic distribution in the l36-year history of Utah. That year was preceded by an extraordinarily wet 1982 so that antecedent moisture...
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Geology and Antelope Island State Park, Utah (MP 88-2)Vendor: Utah Geological SurveyBy: H. H. Doelling and others Antelope Island is located in the southeast corner of Great Salt lake and is the largest of its islands. It is a little over 40 square miles in size, with a length of 15 miles in a north-south...
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Mineral fuels and associated energy resources (MP 87-2)Vendor: Utah Geological SurveyBy: M. R. SmithUtah has valuable and abundant natural energy resources which include oil and natural gas, coal, uranium, gilsonite, geothermal hot water and steam, oil shale, tar sand, and methane. The locations of important energy resources are shown on the brochure map. At...
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Ground-water sensitivity and vulnerability to pesticides, the southern Sevier Desert and Pahvant Valley, Millard County, Utah (MP 03-1)Vendor: Utah Geological SurveyBy: M. Lowe and I. D. Sanderson The U.S. Environmental Protection Agency has recommended that states develop Pesticide Management Plans for four agricultural chemicals - alachlor, atrazine, metolachlor, and simazine - used in Utah as herbicides in the production of corn and sorghum, and...
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Deterministic maximum peak bedrock acceleration maps for Utah (MP 02-11)Vendor: Utah Geological SurveyBy: M. W. Halling, J. R. Keaton, L. R. Anderson, and W. Kohler Maximum ground motion maps for the State of Utah were prepared for the Utah Department of Transportation to provide context for probabilistic ground motion maps. Deterministic procedures were used to prepare...
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Southwestern Utah coal fields: Alton, Kaiparowits Plateau and Kolob-Harmony (MO-1)Vendor: Utah Geological SurveyEdited By: H. H. Doelling and R. L. Graham This publication covers information regarding the Southwestern Utah coal fields, and is the first in a three part series of publications. The text is subdivided into coal fields, area and quadrangle; geographical data, geology, mines...
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Landslide maps of Utah (M-246dm)Vendor: Utah Geological SurveyBy: A. H. Elliot and K. M. Harty Significant economic losses are associated with landslides, and Utah has numerous landslides and landslide-prone geologic units. Exposure to landslide hazards increases as development expands onto hillsides and other landslide-prone areas. To improve the understanding of landslides...
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Uranium and Vanadium map of Utah (M-215dm)Vendor: Utah Geological SurveyBy: R. W. Gloyn, R. L. Bon, S. I. Wakefield, and K. KrahulecThe Uranium and Vanadium Map of Utah depicts the areas throughout the state where uranium and vanadium are located. Information on this map includes: permitted uranium/vanadium mine, past producers, prospect/occurrence, uranium as...
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Map of recharge and discharge areas for the principal valley-fill aquifer, Sanpete Valley, Sanpete County, Utah (M-174)Vendor: Utah Geological SurveyBy: N. P. Snyder and M. Lowe The most important source of drinking water in Sanpete County is ground water from the principal valley-fill aquifer in Sanpete Valley. In this study we mapped recharge and discharge areas for the principal aquifer to aid in...
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The radon-hazard-potential map of Utah (M-149)Vendor: Utah Geological SurveyBy: B. D. Black Radon is a naturally occurring radioactive gas formed by the decay of uranium which can be found in small concentrations in nearly all geologic materials. When radon is inhaled, its decay products are a significant cause of lung cancer. Radon...
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Effect of geothermal drawdown on sustainable development, Newcastle area, Iron County, Utah (C-97)Vendor: Utah Geological SurveyBy: R. E. Blackett, H. P. Ross, and C. B. Forster Discovered in 1975 by local farmers, the Newcastle geothermal resource has developed slowly. Pumping of geothermal water from the unconfined aquifer for space heating, mainly for commercial greenhouses, began in the early 1980s,...
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