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Journal articles on the topic 'Bassin de Laragne'

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Published: 4 June 2021

Last updated: 1 February 2022

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1

Munn, L. C., and L. K. Spackman. "Soil Genesis Associated with Periglacial Ground Wedges, Laramie Basin, Wyoming." Soil Science Society of America Journal 55, no. 3 (May 1991): 772–77. http://dx.doi.org/10.2136/sssaj1991.03615995005500030023x.

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2

Reider, Richard G., Joseph M. Huss, and Timothy W. Miller. "A groundwater vortex hypothesis for mima-like mounds, Laramie Basin, Wyoming." Geomorphology 16, no. 4 (August 1996): 295–317. http://dx.doi.org/10.1016/0169-555x(95)00142-r.

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3

Zakir, Abdelali, Ahmed Chalouan, and Hugues Feinberg. "Tectono-sedimentary evolution of a fore-chain domain : example of the Habt and Sidi Mrayt basins, northwestern external Moroccan Rif ; stratigraphic precisions and tectonic modelling." Bulletin de la Société Géologique de France 175, no. 4 (July 1, 2004): 383–97. http://dx.doi.org/10.2113/175.4.383.

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Abstract In this paper, a tecto-sedimentary evolution model of the northwestern external Rif zones (Morocco) is proposed. It is based on the study of structural relationships and the biostratigraphic and sedimentologic analysis of different Tertiary syn-tectonic units. This zone shows alternating foredeep basins and anticlinal ramps with a NNW-SSE structural trend and a vergence toward the WSW. The trend of turbiditic bodies and palaeocurrent directions (from the SSE to the NNW) are parallel to the regional tectonic strike. Sidi Mrayt and El Habt basins are filled with syn-tectonic middle Eocene to middle Miocene sediments; The Habt basin is subdivided in two sub-basins: Asilah-Larache and Rirha-Gzoula. The deposits are distributed in two separated turbiditic complex, each one including a stacking of turbiditic systems. The Rirha-Gzoula and Asilah-Larache sub-basins are located in front of two anticline ridge structures made up of Upper Cretaceous and Lower Eocene material; they are respectively Boujediane and Arbaa Ayacha anticlines. The distribution of turbiditic bodies, unconformities and structural relationships within the thrusts and folds system in the northwestern external Rif indicate the progression toward the external zones of fault-propagation folds and associated basins.

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4

Reider, Richard G., Joseph M. Huss, and Timothy W. Miller. "STRATIGRAPHY, SOILS, AND AGE RELATIONSHIPS OF MIMA-LIKE MOUNDS, LARAMIE BASIN, WYOMING." Physical Geography 20, no. 1 (January 1999): 83–96. http://dx.doi.org/10.1080/02723646.1999.10642670.

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5

Mazor, E., J. I. Drever, J. Finley, P. W. Huntoon, and D. A. Lundy. "Hydrochemical implications of groundwater mixing: An example from the Southern Laramie Basin, Wyoming." Water Resources Research 29, no. 1 (January 1993): 193–205. http://dx.doi.org/10.1029/92wr01680.

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6

Prager, Steven D., J. Michael Daniels, and Scott Kelley. "Sketch-based Identification of Bench and Terrace Slope Breaks in the Laramie Basin, Wyoming." Transactions in GIS 11, no. 5 (October 2007): 703–19. http://dx.doi.org/10.1111/j.1467-9671.2007.01068.x.

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7

Martin, Renee M., Heidi Meador, Lee Bender, and Lacey Hopper. "Isolation and Characterization of 27 Novel Microsatellite Loci in Critically Endangered Wyoming Toad." Journal of Fish and Wildlife Management 10, no. 2 (September 1, 2019): 563–66. http://dx.doi.org/10.3996/042019-jfwm-029.

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Abstract Wyoming toad Anaxyrus baxteri is a federally endangered amphibian endemic to the Laramie basin in southwestern Wyoming, USA. A captive breeding program propagates A. baxteri, and the monitoring of genetic diversity in the captive stock can assist in guiding conservation measures of this species. Illumina paired-end sequencing lead to 27 species-specific polymorphic microsatellite genetic markers being developed. Across 24 samples, A. baxteri exhibited two to eight alleles per locus, and observed and expected heterozygosities per locus ranged from 0.292 to 0.958 and from 0.344 to 0.787, respectively. Tests for Hardy–Weinberg equilibrium were nonsignificant except for Abax_13 and Abax_39. These microsatellite markers will be useful for genetic monitoring to aid recovery efforts of A. baxteri captive and wild populations as well as other amphibians in the family Bufonidae.

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8

Toner, R., C. Frost, and K. Chamberlain. "Isotopic identification of natural vs. anthropogenic sources of Pb in Laramie basin groundwaters, Wyoming, USA." Environmental Geology 43, no. 5 (February 2003): 580–91. http://dx.doi.org/10.1007/s00254-002-0682-0.

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9

Peck, Dannele E., and James R. Lovvorn. "The importance of flood irrigation in water supply to wetlands in the Laramie Basin, Wyoming, USA." Wetlands 21, no. 3 (September 2001): 370–78. http://dx.doi.org/10.1672/0277-5212(2001)021[0370:tiofii]2.0.co;2.

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10

Munn, L. C. "Factors Controlling Distribution of Selenium by Geomorphic and Pedologic Processes in a Semi-Arid Environment, Laramie Basin, Wyoming." Journal American Society of Mining and Reclamation 195, no. 1 (1995): 270–83. http://dx.doi.org/10.21000/jasmr95010270.

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11

Knudson, Kelly J., and Christina Torres-Rouff. "Cultural Diversity and Paleomobility in the Andean Middle Horizon: Radiogenic Strontium Isotope Analyses in the San Pedro De Atacama Oases of Northern Chile." Latin American Antiquity 25, no. 2 (June 2014): 170–88. http://dx.doi.org/10.7183/1045-6635.25.2.170.

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Despite a long history of research, interactions between the Tiwanaku polity of the Andean Middle Horizon (ca.A.D. 500-1100) and the San Pedro de Atacama oases of northern Chile remain controversial. Here, we investigate Middle Horizon interactions through an isotopic identification of the geographic origins of individuals buried in San Pedro de Atacama cemeteries and present the largest radiogenic strontium isotope dataset generated, to date, for the Andes. For individuals in Middle Horizon San Pedro de Atacama cemeteries ofCasa Parroquial, Coyo Oriental, Coyo-3, Larache, Quitor-5, Solcor-3, Solcor Plaza, Solor-3, and Tchecar Túmulo Sur, mean tooth enamel and bone87Sr/86Sr = .70834 ± .00172 (2σ, n = 273). Overall, the mean87Sr/86Sr values from Middle Horizon San Pedro de Atacama cemeteries support the idea that interactions between Atacameños and inhabitants of other regions varied by ayllu, an Andean kin-based community structure, with some ayllus incorporating individuals with a wider variety of geographic origins than others. When our interpretations of the radiogenic strontium isotope data are contextualized with analyses of mortuary behavior and recent biodistance analyses, we argue that the San Pedro de Atacama oases appear to be have been inhabited by culturally and biologically diverse groups, rather than by large numbers of colonists from the Tiwanaku capital and the Lake Titicaca Basin.

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12

Dechesne, Marieke, Jim Cole, and Christopher Martin. "Field guide to Laramide basin evolution and drilling activity in North Park and Middle Park, Colorado." Mountain Geologist 53, no. 4 (October 2016): 283–329. http://dx.doi.org/10.31582/rmag.mg.53.4.283.

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This two-day field trip provides an overview of the geologic history of the North Park–Middle Park area and its past and recent drilling activity. Stops highlight basin formation and the consequences of geologic configuration on oil and gas plays and development. The trip focuses on work from ongoing U.S. Geological Survey research in this area (currently part of the Cenozoic Landscape Evolution of the Southern Rocky Mountains Project funded by the National Cooperative Geologic Mapping Program). Surface mapping is integrated with perspective from petroleum exploration within the basin. The starting point is the west flank of the Denver Basin to compare and contrast the latest Cretaceous through Eocene basin fill on both flanks of the Front Range. The next stop continues on the south end of the North Park–Middle Park area, about 60 miles [95km] west from the first stop. A general clockwise loop is described by following U.S. Highway 40 from Frasier via Granby and Kremmling to Muddy Pass after which CO Highway 14 is followed to Walden for an overnight stay. On the second day after a loop north of Walden, the Continental Divide is crossed at Willow Creek Pass for a return to Granby via Highway 125. The single structural basin that underlies both physiographic depressions of North Park and Middle Park originated during the latest Cretaceous to Eocene Laramide orogeny (Tweto, 1957, 1975; Dickinson et al., 1988). It largely filled with Paleocene to Eocene sediments and is bordered on the east by the Front Range, on the west by the Park Range and Gore Range, on the north by Independence Mountain and to the south by the Williams Fork and Vasquez Mountains (Figure 1). This larger Paleocene-Eocene structural basin is continuous underneath the Continental Divide, which dissects the basin in two approximately equal physiographic depressions, the ‘Parks.’ Therefore Cole et al. (2010) proposed the name ‘Colorado Headwaters Basin’ or ‘CHB,’ rather than North Park–Middle Park basin (Tweto 1957), to eliminate any confusion between the underlying larger Paleocene-Eocene basin and the two younger depressions that developed after the middle Oligocene. The name was derived from the headwaters of the Colorado, North Platte, Laramie, Cache La Poudre, and Big Thompson Rivers which are all within or near the study area. In this field guide, we will use the name Colorado Headwaters Basin (CHB) over North Park–Middle Park basin. Several workers have described the geology in the basin starting with reports from Marvine who was part of the Hayden Survey and wrote about Middle Park in 1874, Hague and Emmons reported on North Park as part of the King Survey in 1877, Cross on Middle Park (1892), and Beekly surveyed the coal resources of North Park in 1915. Further reconnaissance geologic mapping was performed by Hail (1965 and 1968) and Kinney (1970) in the North Park area and by Izett (1968, 1975), and Izett and Barclay (1973) in Middle Park. Most research has focused on coal resources (Madden, 1977; Stands, 1992; Roberts and Rossi, 1999), and oil and gas potential (1957, all papers in the RMAG guidebook to North Park; subsurface structural geologic analysis of both Middle Park and North Park (the CHB) by oil and gas geologist Wellborn (1977a)). A more comprehensive overview of all previous geologic research in the basin can be found in Cole et al. (2010). Oil and gas exploration started in 1925 when Continental Oil's Sherman A-1 was drilled in the McCallum field in the northeast part of the CHB. It produced mostly CO2 from the Dakota Sandstone and was dubbed the ‘Snow cone’ well. Later wells were more successful finding oil and/or gas, and exploration and production in the area is ongoing, most notably in the unconventional Niobrara play in the Coalmont-Hebron area.

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13

Clausen, Eric. "Topographic Map Analysis of Laramie Range Bedrock-Walled Canyon Complex and the Goshen Hole Escarpment-Surrounded Basin, Albany and Platte Counties, Southeast Wyoming, USA." Open Journal of Geology 08, no. 01 (2018): 33–55. http://dx.doi.org/10.4236/ojg.2018.81003.

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14

Laran, Sophie, and Alexandre Gannier. "Spatial and temporal prediction of fin whale distribution in the northwestern Mediterranean Sea." ICES Journal of Marine Science 65, no. 7 (May 20, 2008): 1260–69. http://dx.doi.org/10.1093/icesjms/fsn086.

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Abstract Laran, S. and Gannier, A. 2008. Spatial and temporal prediction of fin whale distribution in the northwestern Mediterranean Sea. – ICES Journal of Marine Science, 65: 1260–1269. Understanding the distribution of the cetaceans is crucial to improving their conservation. Therefore, a prediction model of fin whale’s (Balaenoptera physalus) summer distribution was developed from data collected between May and August, in the Pelagos Mediterranean Marine Mammals Sanctuary. Explanatory variables were selected by multiple logistic regression, among several physiographic and oceanographic parameters. Depth, chlorophyll (Chl a) concentration, and sea surface temperature (SST) were selected for characterizing fin whale presence. Remote sensing imagery (Chl a and SST) was used at an 8-d resolution to capture short-term environmental variability. With the selection of a presence/absence threshold by the receiver operating characteristic curve, a correct classification of 70% (49% for presence, 85% for absence) was achieved for the initial dataset. Model reliability was also tested on an independent dataset, collected in the northwestern Basin; a correct classification of 71% (41% for presence prediction, 86% for absence prediction) was obtained. This study contributes to an understanding of where fin whales might concentrate to feed in summer. Weekly predictions of their distribution represent a valuable conservation tool in a marine protected area, for example to prevent collisions with ships.

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15

Marlow, Clayton, and Sarah Summerford. "Impact of Irrigation Cessation on Wetland Communities within the Elk Ranch, Grand Teton National Park, Moose, Wyoming." UW National Parks Service Research Station Annual Reports 30 (January 1, 2006): 46–50. http://dx.doi.org/10.13001/uwnpsrc.2006.3643.

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Riparian ecology research in Arizona and California has documented the likelihood of a subsurface linkage between irrigation, especially flood-irrigation, and riparian function (Smith et al. 1989; Stromberg et al. 1996). Initial groundwater monitoring results from rural New Mexico indicate water tables rose 1 to 2m after the onset of field irrigation and subsurface flow paths towards the Rio Grande River developed soon after (Fernald et al. 2008). Results from a study of wetlands in southeastern Wyoming suggest that declining flood-irrigation levels would lead to a reduction in the total area of wetlands and related areas of wetland vegetation types in the Laramie Basin (Peck and Lovvorm 2001). Stringham et al. (1998) have reported further evidence for a linkage between irrigation and riparian function. These Oregon researchers noted lower water temperatures in stream reaches receiving subsurface return flows from irrigated hayfields than similar reaches flowing through non-irrigated lands. This information is timely because Grand Teton National Park (GTNP) managers have begun an evaluation of historic irrigation operations within the Park and are endeavoring to learn how cessation of flood irrigation will affect Park wetlands. The historically irrigated hayfields at the Elk Ranch provide an opportunity to address the Park Service's informational needs through identification of vegetation composition, soil physical characteristics and groundwater patterns associated with irrigated and naturally occurring wetlands. Successful description of patterns unique to natural wetlands will provide an avenue for predicting which Park wetlands would remain functional should irrigation efforts be brought to a close. Development of criteria for identifying naturally occurring wetlands could also serve as a basis for identifying areas for wetland mitigation and rehabilitation elsewhere in GTNP and the mountain valleys of the Northern Rocky Mountains.

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16

Lasaki, Gbolahan O., Richard Martel, and John L. Fahy. "Numerical Simulation of Combined Reverse Combustion and Steamflooding for Oil Recovery in a Utah Tar Sand." Society of Petroleum Engineers Journal 25, no. 02 (April 1, 1985): 227–34. http://dx.doi.org/10.2118/11159-pa.

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Abstract This paper presents the design of the U.S. DOE Laramie Energy Technology Center's (LETC) Project TS-4, which involves numerical simulation of both in-situ reverse combustion and steamflooding. The simulator showed that the combustion could be limited and contained in a middle 10-ft [3-m] interval with a correlatable High-permeability streak within the 65-ft [20-m] pay zone of the upper Rimrock tar sand formation in Northwest Asphalt Ridge, Uintah County, UT. A high-transmissibility path was necessary to obtain adequate injectivity and sustain a stable reverse combustion. Combustion "echoes" developed and the front changed into a forward mode as the formation pressure increased and at very low air-injection rates. Oil recovery by steam injection was accelerated in a formation preheated by a reverse combustion. Introduction In 1973 LETC began a series of projects aimed at identifying feasible oil recovery techniques for the large deposits of tar sands in the U.S. Two previous combustion experiments have been reported by LETC: Land et al previous combustion experiments have been reported by LETC: Land et al reported the LETC TS-1C, and Johnson et al reported the LETC TS-2C. Both of these were conducted in the Northwest Asphalt Ridge tar sand deposit (T4S-R20E), in Uintah County, in 1975 and 1977, respectively. These were followed by a steamflood experiment, LETC TS-1S, in 1980 in the same area. Analysis of this steamflood experiment indicated that only 18.5% of the original oil in place (OOIP) was mobilized because of poor communication between the injector and the producers. It was clear at this point that the producers had to be stimulated to improve the oil mobility around the wellbores. Steam soaking was considered but discarded because of the lack of adequate reservoir pressure. Since LETC had been successful with its previous use of combustion, the use of reverse combustion to preheat the previous use of combustion, the use of reverse combustion to preheat the producers and possibly the entire sand was considered. A reverse producers and possibly the entire sand was considered. A reverse combustion is preferred to forward combustion because it eliminates the problem of plugging. Project TS-4, therefore, involves a combination of problem of plugging. Project TS-4, therefore, involves a combination of in-situ reverse combustion and steamflooding. The site selected for the test is about 200 ft [61 m] southeast of the location of the LETC TS-1S experiment. The project targets the 65-ft [20-m] pay zone of the upper Rimrock tar sand formation rather than the lower Rimrock targeted in all previous experiments. The sand is well confined and fairly continuous with previous experiments. The sand is well confined and fairly continuous with varying levels of shaliness. The formation bitumen saturation is about 80% compared with 35 to 65% in the lower Rimrock. The permeability of the unextracted core is less than 1 md in some parts and generally one or two orders of magnitude less than that of the lower Rimrock. Preliminary field tests ordinarily showed very poor injectivity without fracturing the formation. The in-situ reverse combustion is intended to preheat the formation rapidly before steamflooding the entire formation. It is confined to a 10ft [3-m] interval that includes a correlatable high-permeability streak to limit the air requirement. It also is expected that good communication can be established between the injector and producers while reducing the oil viscosity and, thus, improving the mobility of the oil. This paper reports a simulation study evaluating the feasibility of this project on a commercial scale and presents a conceptual study of the experiment using a numerical simulator previously described by Coats. Owing to the recent defederalization of LETC, the planned field test for Project TS-4 now has been abandoned. Geology The Northwest Asphalt Ridge is located at T4S-R20E in the Uintah Basin, Uintah County, UT. The geology of this area is described in a greater detail by Campbell and Ritzma. The ridge is separated from the major Asphalt Ridge by a northeast-trending fault. The strata dip southwesterly from about 9 to 350 Average dip angle at the TS-4 location is about 28. The Rimrock sandstone is a member of the Late Cretaceous Mesaverde formation. The other member of the group in this location is the Asphalt Ridge sandstone. Both are of marine origin and oil impregnated. The Rimrock sandstone is unconformably overlain by Tertiary Duchesne River formation of continental origin. It is underlain by the Asphalt Ridge sandstone and separated from it by a thin tongue of Mancos shale. SPEJ p. 227

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17

Randi S. Martinsen. "Cretaceous Stratigraphy, Laramie Basin, Southeastern Wyoming: ABSTRACT." AAPG Bulletin 74 (1990). http://dx.doi.org/10.1306/20b22ca1-170d-11d7-8645000102c1865d.

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18

ROBERTS, STEPHEN B., and NEIL S. FI. "ABSTRACT: Coal-bed Methane Potential In The Laramie Formation, Greater Wattenberg Area, Denver Basin, Colorado: Just Wishful Thinking?" AAPG Bulletin 84 (2000). http://dx.doi.org/10.1306/a9673e32-1738-11d7-8645000102c1865d.

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19

Laura L. Wray1, Nicole V. Koenig1,. "ABSTRACT: Preliminary Assessment of Coalbed Methane Potential of the Low Rank Denver and Laramie Formation Coals, Denver Basin, Colorado." AAPG Bulletin 86 (2002). http://dx.doi.org/10.1306/3fef5121-1741-11d7-8645000102c1865d.

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20

Donald S. Stone (2). "Structure and Kinematic Genesis of the Quealy Wrench Duplex: Transpressional Reactivation of the Precambrian Cheyenne Belt in the Laramie Basin, Wyoming." AAPG Bulletin 79 (1995). http://dx.doi.org/10.1306/7834d4cc-1721-11d7-8645000102c1865d.

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21

Donald S. Stone. "Structure and Kinematic Genesis of the Quealy Wrench Fault Duplex: Product of Laramide Reactivation of Precambrian Shear Zones of the Cheyenne Belt in the Laramie Basin, Wyoming: ABSTRACT." AAPG Bulletin 78 (1994). http://dx.doi.org/10.1306/8d2b0fd0-171e-11d7-8645000102c1865d.

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