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1

Bader, Jeffrey. "Structural analysis of the Casper Mountain fault zone and area, Wyoming surrounding area, Wyoming: Implications for Laramide kinematics and structural inheritance across the Wyoming Province." Mountain Geologist 58, no. 4 (2021): 433–52. http://dx.doi.org/10.31582/rmag.mg.58.4.433.

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Casper Mountain is an E–W trending anticlinal structure that is bound on the north by the oblique-slip Casper Mountain fault. The fault is postulated to reflect preexisting Precambrian structure/fabrics that were reactivated and/or guided deformation during the Laramide orogeny. A structural analysis of the fault zone and surrounding area was conducted to confirm this hypothesis, and to garner insight into both Precambrian origins and Laramide kinematics. Surface and subsurface data for structural analysis was collected and synthesized from numerous published sources along the proposed deforma
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2

Halfen, Alan F., Glen G. Fredlund, and Shannon A. Mahan. "Holocene stratigraphy and chronology of the Casper Dune Field, Casper, Wyoming, USA." Holocene 20, no. 5 (2010): 773–83. http://dx.doi.org/10.1177/0959683610362812.

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3

Burt, R. "Ecology and Geology of the Greater Yellowstone Area." UW National Parks Service Research Station Annual Reports 33 (January 1, 2011): 229–30. http://dx.doi.org/10.13001/uwnpsrc.2011.3827.

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During the summers of 2009 and 2010 in conjunction with a long term study of small mammal community succession following the 1988 Greater Yellowstone fires undergraduate students at the University of Wyoming/ Casper College Center are provided the opportunity to engage in independent study projects associated with the small mammal work under the leadership of Dr. Scott Burt and funded by the Wyoming IDeA Networks for Biomedical Excellence (INBRE). The students enroll in Zoology 4900 for academic credit and combine laboratory work at the UW/CC Center with fieldwork conducted while in residence
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4

Kramer, Darrell L., and Thomas L. Davis. "Multicomponent VSPs for reservoir characterization South Casper Creek field, Wyoming." Leading Edge 11, no. 9 (1992): 31–35. http://dx.doi.org/10.1190/1.1436901.

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5

Herman, Jay, Guoyong Wen, Alexander Marshak, et al. "Reduction in 317–780 nm radiance reflected from the sunlit Earth during the eclipse of 21 August 2017." Atmospheric Measurement Techniques 11, no. 7 (2018): 4373–88. http://dx.doi.org/10.5194/amt-11-4373-2018.

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Abstract. Ten wavelength channels of calibrated radiance image data from the sunlit Earth are obtained every 65 min during Northern Hemisphere summer from the EPIC (Earth Polychromatic Imaging Camera) instrument on the DSCOVR (Deep Space Climate Observatory) satellite located near the Earth–Sun Lagrange 1 point (L1), about 1.5 million km from the Earth. The L1 location permitted seven observations of the Moon's shadow on the Earth for about 3 h during the 21 August 2017 eclipse. Two of the observations were timed to coincide with totality over Casper, Wyoming, and Columbia, Missouri. Since the
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6

Greifenstein, Jeremy, Rachel Shea, and John Patrick Kociolek. "A New Aulacoseira Thwaites (Bacillariophyta) Species from Wyoming, USA." Taxonomy 2, no. 2 (2022): 236–43. http://dx.doi.org/10.3390/taxonomy2020018.

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A new species, Aulacoseira wyomingensis, is described from a small seep near Casper, Wyoming, USA, using light and scanning electron microscopy, in which it was the dominant diatom taxon. Valves have large areolae that cover the valve face. Spines, when present, are short and shield-like, precluding chain formation. Unlike most members of the genus, A. wyomingensis appears to lack rimoportulae. While we assign this species to the genus Aulacoseira within the Aulacoseiraceae based on the radial nature of its valve, its cingulum composed of fine ligulate bands, and presence of a ringleiste and c
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7

Tamba, Adrian. "Garanțiile negative." Studia Universitatis Babeş-Bolyai Iurisprudentia 65, no. 4 (2021): 955–76. http://dx.doi.org/10.24193/subbiur.65(2020).4.28.

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"My work, called „Negative Pledges”, aims at some interesting legal beings. Mainly, they are used by banks. Yet, negative pledges may very well be placed in the hands of entities that are not banks; this is pointed out by, e.g., First Wyoming Bank, Casper v. Mudge. Negative pledges are encountered both in the Civil Law and the Common Law traditions. Of course, it is my view that the Romanian Civil Code embraces the so-called negative pledges, though it does not use such an expression. At the end of this paper, the abandonment of orthodoxy is highlighted: no explicit conclusions can be noticed.
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8

Snider, Kile, Matthew Ward, Bill Desing, et al. "Sanitary Sewer Interceptor Corrosion Modeling and Corrosion Control Pilot Testing at Casper, Wyoming." Proceedings of the Water Environment Federation 2014, no. 19 (2014): 4968–76. http://dx.doi.org/10.2175/193864714815942710.

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9

Nowak, David, Daniel Crane, Jack Stevens, Robert Hoehn, Jeffrey Walton, and Jerry Bond. "A Ground-Based Method of Assessing Urban Forest Structure and Ecosystem Services." Arboriculture & Urban Forestry 34, no. 6 (2008): 347–58. http://dx.doi.org/10.48044/jauf.2008.048.

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To properly manage urban forests, it is essential to have data on this important resource. An efficient means to obtain this information is to randomly sample urban areas. To help assess the urban forest structure (e.g., number of trees, species composition, tree sizes, health) and several functions (e.g., air pollution removal, carbon storage and sequestration), the Urban Forest Effects (UFORE) model was developed. Data collection variables and model methods are detailed and urban forest structure results are compared among 14 United States cities with average tree density ranging between 22.
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10

Tajik, Mansoureh, Karen Gottlieb, Nita Lowndes, and Gloria Stewart. "Environmental Policies, Politics, and Community Risk Perception: Case Study of Community Contamination in Casper, Wyoming." NEW SOLUTIONS: A Journal of Environmental and Occupational Health Policy 17, no. 4 (2008): 345–61. http://dx.doi.org/10.2190/ns.17.4.i.

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11

Wallace, S., and R. Kadlec. "BTEX degradation in a cold-climate wetland system." Water Science and Technology 51, no. 9 (2005): 165–71. http://dx.doi.org/10.2166/wst.2005.0311.

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A pilot-scale subsurface vertical-flow wetland system was constructed at the former BP Refinery in Casper, Wyoming in order to determine benzene, toluene, ethylbenzene and xylene (BTEX) degradation rates in a cold-climate application. The pilot system, consisting of 4 cells, each dosed at a nominal flow rate of 5.4 cubic metres per day, was operated between August and December 2002. The pilot tested the effects of wetland mulch and aeration on system performance. Areal rate constants (kA values) were calculated based on an assumed three tanks in series (3TIS). The presence of wetland sod and a
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12

Lee, Doo Sung, Veronica M. Stevenson, Phil F. Johnston, and C. E. Mullen. "Time‐lapse crosswell seismic tomography to characterize flow structure in the reservoir during the thermal stimulation." GEOPHYSICS 60, no. 3 (1995): 660–66. http://dx.doi.org/10.1190/1.1443805.

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Time‐lapse crosswell seismic tomography data, recorded with an interval of six months, indicate a strong directional thermal response in a fractured eolian sandstone reservoir at a five‐spot thermal stimulation site in the South Casper Creek oil field, Wyoming. The seismic thermal response depicted on the tomogram and in conjunction with the geological data from cores and a wireline log, reveals the multichannel flow mechanism in the reservoir formation. The three factors that control steam or heat propagation are the fractures, the directional permeability existing in the rock matrix, and the
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13

Custer, Thomas W., Christine M. Custer, Kimberly Dickerson, Kenneth Allen, Mark J. Melancon, and Larry J. Schmidt. "Polycyclic aromatic hydrocarbons, aliphatic hydrocarbons, trace elements, and monooxygenase activity in birds nesting on the North Platte River, Casper, Wyoming, USA." Environmental Toxicology and Chemistry 20, no. 3 (2001): 624–31. http://dx.doi.org/10.1002/etc.5620200323.

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14

Kugler, Anne. "Civil Procedure - Wyoming Governmental Claims Act: Back to the Future; Brown v. City of Casper, 248 P.3d 1136 (Wyo. 2011)." Wyoming Law Review 12, no. 1 (2012): 115–39. http://dx.doi.org/10.59643/1942-9916.1271.

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15

Spence, William, C. J. Langer, and George L. Choy. "Rare, large earthquakes at the Laramide deformation front—Colorado (1882) and Wyoming (1984)." Bulletin of the Seismological Society of America 86, no. 6 (1996): 1804–19. http://dx.doi.org/10.1785/bssa0860061804.

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Abstract The largest historical earthquake known in Colorado occurred on 7 November 1882. Knowledge of its size, location, and specific tectonic environment is important for the design of critical structures in the rapidly growing region of the Southern Rocky Mountains. More than one century later, on 18 October 1984, an mb 5.3 earthquake occurred in the Laramie Mountains, Wyoming. By studying the 1984 earthquake, we are able to provide constraints on the location and size of the 1882 earthquake. Analysis of broadband seismic data shows the 1984 mainshock to have nucleated at a depth of 27.5 ±
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16

Wen, Guoyong, Alexander Marshak, Si-Chee Tsay, et al. "Changes in the surface broadband shortwave radiation budget during the 2017 eclipse." Atmospheric Chemistry and Physics 20, no. 17 (2020): 10477–91. http://dx.doi.org/10.5194/acp-20-10477-2020.

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Abstract. While solar eclipses are known to greatly diminish the visible radiation reaching the surface of the Earth, less is known about the magnitude of the impact. We explore both the observed and modeled levels of change in surface radiation during the eclipse of 2017. We deployed a pyranometer and Pandora spectrometer instrument to Casper, Wyoming, and Columbia, Missouri, to measure surface broadband shortwave (SW) flux and atmospheric properties during the 21 August 2017 solar eclipse event. We performed detailed radiative transfer simulations to understand the role of clouds in spectral
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17

Nesbitt, Sterling J., John M. Zawiskie, and Robert M. Dawley. "The osteology and phylogenetic position of the loricatan (Archosauria: Pseudosuchia) Heptasuchus clarki, from the ?Mid-Upper Triassic, southeastern Big Horn Mountains, Central Wyoming (USA)." PeerJ 8 (October 27, 2020): e10101. http://dx.doi.org/10.7717/peerj.10101.

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Loricatan pseudosuchians (known as “rauisuchians”) typically consist of poorly understood fragmentary remains known worldwide from the Middle Triassic to the end of the Triassic Period. Renewed interest and the discovery of more complete specimens recently revolutionized our understanding of the relationships of archosaurs, the origin of Crocodylomorpha, and the paleobiology of these animals. However, there are still few loricatans known from the Middle to early portion of the Late Triassic and the forms that occur during this time are largely known from southern Pangea or Europe. Heptasuchus
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18

Burch, D. N., and R. M. Cluff. "A Volumetric Analysis of Almond Formation (Cretaceous, Mesaverde Group) Gas Production in the Coal Gulch-Echo Springs Standard Draw Field Complex, Washakie Basin, Southwest Wyoming." SPE Reservoir Evaluation & Engineering 1, no. 04 (1998): 328–37. http://dx.doi.org/10.2118/50995-pa.

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This paper (SPE 50995) was revised for publication from paper SPE 38368, first presented at the 1997 SPE Rocky Mountain Regional Meeting, Casper, Wyoming, 18-21 May. Original manuscript received for review 18 June 1997. Revised manuscript received 27 April 1998. Paper peer approved 1 June 1998. Summary The Coal Gulch-Echo Springs-Standard Draw field complex is one of the largest commercial gas accumulations in the Rocky Mountain region with over 1 Tcf of gas of recoverable reserves. Gas is produced from both the Upper Almond barrier bar and shoreline sandstones at the top of the Mesaverde Grou
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19

Smith, Michael B. "Stimulation Design for Short, Precise Hydraulic Fractures." Society of Petroleum Engineers Journal 25, no. 03 (1985): 371–79. http://dx.doi.org/10.2118/10313-pa.

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Abstract This report discusses the philosophy, design, and implementation of small, precise, hydraulic fracture stimulations as applied in a micellar pilot in Salt Creek field, located in central Wyoming. Wellbore damage and relatively low permeability were resulting in low injection/withdrawal rates in the 1-acre [4046-M ] pilot in this field. Unchanged, these low rates would extend the pilot life by an unacceptable amount and also result in oil production rates too small for meaningful analysis. Accordingly, the decision was made to fracturestimulate the pilot wells on the basis of reservoir
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20

Waller, Aaron, Donald McLeod, and David Taylor. "Conservation Opportunities for Securing In-Stream Flows in the Platte River Basin: A Case Study Drawing on Casper, Wyoming’s MunicipalWater Strategy." Environmental Management 34, no. 5 (2004): 620–33. http://dx.doi.org/10.1007/s00267-003-0154-7.

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21

"Casper, Wyoming." Raven: A Journal of Vexillology 9 (2002): 60–61. http://dx.doi.org/10.5840/raven2002/20039/1025.

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22

Arthur E. Burford. "Comparison of East and West Plunge Areas of Casper Mountain, Wyoming: ABSTRACT." AAPG Bulletin 70 (1986). http://dx.doi.org/10.1306/948866b4-1704-11d7-8645000102c1865d.

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23

JOHNSTON, PHIL, DOO-SUNG LEE, and F. "Seismic Monitoring of a Steamflood at South Casper Creek Oil Field, Wyoming." AAPG Bulletin 75 (1991). http://dx.doi.org/10.1306/20b23791-170d-11d7-8645000102c1865d.

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24

Kenkmann, Thomas, Louis Müller, Allan Fraser, Doug Cook, Kent Sundell, and Auriol S. P. Rae. "Secondary cratering on Earth: The Wyoming impact crater field." GSA Bulletin, February 11, 2022. http://dx.doi.org/10.1130/b36196.1.

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A large number of small impact structures have been discovered in Wyoming, USA, and we raise the question of how this accumulation occurred. We document 31 crater structures of 10−70 m diameter with corresponding shock features but missing meteorite relics. All craters occur along the outcrops of the uppermost Permo-Pennsylvanian Casper Sandstone Formation and are ∼280 m.y. old. Their spatial arrangement shows clusters and ray-like alignments. Several craters have elliptical crater morphologies that allow the reconstruction of impact trajectories. The radial arrangement of the trajectories ind
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25

DAVIS, THOMAS L., ROBERT D. BENSON,. "Reservoir Characterization by Multicomponent 3-D Seismic Imaging, South Casper Creek Field, Wyoming." AAPG Bulletin 76 (1992). http://dx.doi.org/10.1306/f4c8fffc-1712-11d7-8645000102c1865d.

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26

BENSON, ROBERT D., THOMAS L. DAVIS,. "3-D Multicomponent Seismic Reservoir Characterization of South Casper Creek Field, Natrona County, Wyoming." AAPG Bulletin 77 (1993). http://dx.doi.org/10.1306/d9cb51dd-1715-11d7-8645000102c1865d.

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27

COLE, REX D., Unocal Corporation, B. "Reservoir Characterization of Tensleep Sandstone (Pennsylvanian-Permian), South Casper Creek Field, Natrona County, Wyoming." AAPG Bulletin 76 (1992). http://dx.doi.org/10.1306/f4c8ffe8-1712-11d7-8645000102c1865d.

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28

STONE, DONALD S. "Abstract: Geology of the Cloud Creek Impact Structure on the Casper Arch, Central Wyoming ." AAPG Bulletin 83 (1999). http://dx.doi.org/10.1306/e4fd303b-1732-11d7-8645000102c1865d.

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29

Rex D. Cole, Christopher E. Mullen. "Reservoir Characterization of Tensleep Sandstone (Pennsylvanian-Permian), South Casper Creek Field, Natrona County, Wyoming: ABSTRACT." AAPG Bulletin 74 (1990). http://dx.doi.org/10.1306/20b229c7-170d-11d7-8645000102c1865d.

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30

Singer, Brad S., Brian R. Jicha, David Sawyer, Ireneusz Walaszczyk, Robert Buchwaldt, and Jorg Mutterlose. "Geochronology of late Albian−Cenomanian strata in the U.S. Western Interior." GSA Bulletin, December 10, 2020. http://dx.doi.org/10.1130/b35794.1.

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Since the publication of 40Ar/39Ar dates from Cretaceous bentonites in the Western Interior Basin by J.D. Obradovich in 1993 and in Japan by J.D. Obradovich and colleagues in 2002, improvements in the 40Ar/39Ar method have included a shift to astronomically calibrated ages for standard minerals and development of a new generation of multi-collector mass spectrometers. Thus, the 40Ar/39Ar chronometer can yield results that are synchronous with U-Pb zircon dates and astrochronologic age models for Cretaceous strata. Ages determined by Obradovich have ± 2σ analytical uncertainties of ± 400 ka (ex
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31

Philipp C. Molzer, Eric A. Erslev (. "Oblique Convergence During Northeast-Southwest Laramide Compression Along the East-West Owl Creek and Casper Mountain Arches, Central Wyoming." AAPG Bulletin 79 (1995). http://dx.doi.org/10.1306/7834d4d6-1721-11d7-8645000102c1865d.

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32

David A. Moore. "Tensleep, Minnelusa, and Casper Formations, Wyoming and Adjacent States: Study of Permian-Pennsylvanian Oil Occurrence and Oil Gravity Distribution: ABSTRACT." AAPG Bulletin 70 (1986). http://dx.doi.org/10.1306/94886849-1704-11d7-8645000102c1865d.

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33

Donald S. Stone1. "Morphology of the Casper Mountain uplift and related, subsidiary structures, central Wyoming: Implications for Laramide kinematics, dynamics, and crustal inheritance." AAPG Bulletin 86 (2002). http://dx.doi.org/10.1306/61eedcba-173e-11d7-8645000102c1865d.

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34

"Briefs." Campus Security Report 21, no. 9 (2024): 2–5. https://doi.org/10.1002/casr.31344.

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Sorority, fraternity members charged in student drowning Wyoming Board of Trustees nixes expanded concealed carry on campus Suspected killer of student found guilty of murder 56 students found blindfolded in basement in potential hazing incident
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