Relevant bibliographies by topics / Bassin de San Juan

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Academic literature on the topic 'Bassin de San Juan'

Author: Grafiati
Published: 4 June 2021
Last updated: 10 February 2022

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Journal articles on the topic "Bassin de San Juan"

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Johnson, Samuel Y., Robert A. Zimmermann, Charles W. Naeser, and John T. Whetten. "Fission-track dating of the tectonic development of the San Juan Islands, Washington." Canadian Journal of Earth Sciences 23, no. 9 (September 1, 1986): 1318–30. http://dx.doi.org/10.1139/e86-127.

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The San Juan Islands of Washington State form a geologically complex province located between the north Cascades, Vancouver Island, and the Olympic Peninsula. We have obtained 53 fission-track dates from the San Juan Islands province that help constrain its late Paleozoic to early Cenozoic tectonic and sedimentary history and its relationship to neighboring geologic terranes. The San Juan Islands can be divided into two main blocks separated by the Haro fault. South of the Haro fault, complexly deformed, metamorphosed, and probably exotic early Paleozoic to early Late Cretaceous rocks form four imbricate thrust plates separated by south- and east-dipping late Early to Late Cretaceous thrust faults. Reset zircon fission-track dates indicate that thrusting may have produced an upside-down geothermal gradient in the uppermost plate, the Decatur terrane. If present, this gradient was probably produced by conductive or frictional heating associated with a now-eroded overlying thrust fault and hot thrust plate. Cretaceous thrusting in the southern San Juan Islands was accompanied by uplift and resetting of apatite fission-track dates. In contrast to correlative rocks of the southern San Juan Islands, Upper Triassic to Lower Cretaceous rocks in and north of the Haro fault zone are essentially unmetamorphosed and only broadly folded. Apatite dates from the Upper Triassic Haro Formation and the Upper Jurassic and Lower Cretaceous Spieden Group indicate they did not participate in Late Cretaceous uplift of the southern San Juan Islands. Together with their basement (the Wrangellia terrane?), these rocks probably acted as a backstop to thrusting. The synorogenic Late Cretaceous Nanaimo basin formed north of the Haro fault in front of the advancing San Juan Islands thrust system. The age of Nanaimo deposition matches uplift (apatite) dates in the southern San Juan Islands, and detrital zircons from the Nanaimo Group yield dates consistent with southern San Juan Islands sources. Burial led to resetting of apatite dates in what is probably the deeper part of the Nanaimo basin.
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Wosik, Mateusz, and Merrilee F. Guenther. "Examination of a historic collection of isolated cranial and appendicular hadrosaurid material from the lower Kirtland Formation of the San Juan Basin, New Mexico." Journal of Paleontology 90, no. 4 (July 2016): 763–70. http://dx.doi.org/10.1017/jpa.2016.75.

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AbstractThe Field Museum of Natural History collection contains several isolated hadrosaurid specimens collected by Charles H. Sternberg from the lower Kirtland Formation of the San Juan Basin, New Mexico, that have been previously overlooked. Cranial elements described herein consist of a dentary and three jugals while appendicular material is limited to two humeri and two pubes. Many of the specimens preserve taxonomically informative characters that show strong affinities with Kritosaurini but are distinct from Kritosaurus navajovius (Brown, 1910) suggesting that the saurolophine-dominated San Juan Basin diversity is greater than currently recognized. Future examination of currently unprepared material will add to our developing understanding of the ambiguous hadrosaurid diversity of the San Juan Basin.
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Cather, Steven M., Matthew T. Heizler, and Thomas E. Williamson. "Laramide fluvial evolution of the San Juan Basin, New Mexico and Colorado: Paleocurrent and detrital-sanidine age constraints from the Paleocene Nacimiento and Animas formations." Geosphere 15, no. 5 (August 14, 2019): 1641–64. http://dx.doi.org/10.1130/ges02072.1.

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Abstract Understanding the tectonic and landscape evolution of the Colorado Plateau−southern Rocky Mountains area requires knowledge of the Laramide stratigraphic development of the San Juan Basin. Laramide sediment-transport vectors within the San Juan Basin are relatively well understood, except for those of the Nacimiento and Animas formations. Throughout most of the San Juan Basin of northwestern New Mexico and adjacent Colorado, these Paleocene units are mudstone-dominated fluvial successions intercalated between the lowermost Paleocene Kimbeto Member of the Ojo Alamo Sandstone and the basal strata of the lower Eocene San Jose Formation, both sandstone-dominated fluvial deposits. For the Nacimiento and Animas formations, we present a new lithostratigraphy that provides a basis for basin-scale interpretation of the Paleocene fluvial architecture using facies analysis, paleocurrent measurements, and 40Ar/ 39Ar sanidine age data. In contrast to the dominantly southerly or southeasterly paleoflow exhibited by the underlying Kimbeto Member and the overlying San Jose Formation, the Nacimiento and Animas formations exhibit evidence of diverse paleoflow. In the southern and western part of the basin during the Puercan, the lower part of the Nacimiento Formation was deposited by south- or southeast-flowing streams, similar to those of the underlying Kimbeto Member. This pattern of southeasterly paleoflow continued during the Torrejonian in the western part of the basin, within a southeast-prograding distributive fluvial system. By Torrejonian time, a major east-northeast–flowing fluvial system, herein termed the Tsosie paleoriver, had entered the southwestern part of the basin, and a switch to northerly paleoflow had occurred in the southern San Juan Basin. The reversal of paleoslope in the southern part of the San Juan Basin probably resulted from rapid subsidence in the northeast part of the basin during the early Paleocene. Continued Tiffanian-age southeastward progradation of the distributive fluvial system that headed in the western part of the basin pushed the Tsosie paleoriver beyond the present outcrop extent of the basin. In the eastern and northern parts of the San Juan Basin, paleoflow was generally toward the south throughout deposition of the Nacimiento and the Animas formations. An important exception is a newly discovered paleodrainage that exited the northeastern part of the basin, ∼15 km south of Dulce, New Mexico. There, an ∼130-m-thick Paleocene sandstone (herein informally termed the Wirt member of the Animas Formation) records a major east-flowing paleoriver system that aggraded within a broad paleovalley carved deeply into the Upper Cretaceous Lewis Shale. 40Ar/ 39Ar dating of detrital sanidine documents a maximum depositional age of 65.58 ± 0.10 Ma for the Wirt member. The detrital sanidine grains are indistinguishable in age and K/Ca values from sanidines of the Horseshoe ash (65.49 ± 0.06 Ma), which is exposed 10.5 m above the base of the Nacimiento Formation in the southwestern part of the basin. The Wirt member may represent the deposits of the Tsosie paleoriver where it exited eastward from the basin. Our study shows that the evolution of Paleocene fluvial systems in the San Juan Basin was complex and primarily responded to variations in subsidence-related sedimentary accommodation within the basin.
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Meehan, T. J., and Robert W. Wilson. "New viverravids from the Torrejonian (Middle Paleocene) of Kutz Canyon, New Mexico and the oldest skull of the order Carnivora." Journal of Paleontology 76, no. 6 (November 2002): 1091–101. http://dx.doi.org/10.1017/s0022336000057899.

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Three new species of Viverravidae (Carnivora: Miacoidea) are described: Protictis simpsoni, P. minor, and Bryanictis paulus. Holotypes and referred specimens are from the Angel Peak area, Kutz Canyon, San Juan Basin, New Mexico and are of middle Torrejonian age (middle Paleocene). The holotype of Protictis simpsoni includes a skull—the oldest known skull of the Order Carnivora. The locality is narrowly restricted stratigraphically and geographically, and specimens are better preserved than most other viverravid specimens of San Juan Basin strata.
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Nelson, Walter W., and Stephen A. Sonnenberg. "Sequence stratigraphy and regional context of the Mancos-Niobrara in the northern San Juan Basin." Mountain Geologist 58, no. 2 (April 1, 2021): 105–57. http://dx.doi.org/10.31582/rmag.mg.58.2.105.

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In the northern San Juan Basin, the Niobrara Formation is represented by the upper half of the Mancos Shale (the Smoky Hill Member and Cortez Member). This section is generally equivalent to the Niobrara Formation along the Colorado Front Range. Although the Fort Hays Limestone is absent west of Pagosa Springs, the C Chalk and B Chalk are well-expressed as two resistant bench-forming calcareous units in the northern San Juan Basin. These two calcareous units have also been established as prospective hydrocarbon targets by operators in the area. Calcareous facies equivalent to the A Chalk were not deposited in the northern San Juan Basin due to siliciclastic dilution during the regressive latter half of the Niobrara marine cycle. The overall third-order Niobrara marine cycle includes these members of the Mancos Shale: the Juana Lopez, Montezuma Valley, Smoky Hill, and Cortez members. The Smoky Hill Member sits just above the basal Niobrara unconformity in most of the study area, and the entire section also has greater thickness and siliciclastic content than its equivalent farther east along the Front Range. Several extensive outcrop locations (in and around Pagosa Springs, Piedra, and Durango, CO) along with three new cores along the CO-NM border form the foundation for sequence stratigraphic interpretation of the Niobrara marine cycle in this study. All these locations and cores were tied back to the Mancos reference section at Mesa Verde National Park established by Leckie et al. (1997) which provides detailed description and biostratigraphy for the entire Mancos Shale. Establishing and applying a sequence stratigraphic framework to any section creates consistent reference standards for communication, research, and further correlation. Comparisons of chemostratigraphic data from equivalent strata between the northern San Juan Basin and Denver-Julesburg (DJ) Basin reveal significant differences in the timing and style of source-rock deposition (and associated low-oxygen conditions). The sequence stratigraphic framework also emphasizes tremendous lateral facies changes in the basal Niobrara section (i.e., Fort Hays Limestone to Tocito Sandstone). Once refined and applied, this stratigraphic framework can be used for predicting the distribution of reservoir properties, in addition to enhancing understanding of the Niobrara marine cycle and the Western Interior Seaway.
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Lucas, Spencer G., Thomas E. Williamson, and Michael D. Middleton. "Catopsalis (Mammalia: Multituberculata) from the Paleocene of New Mexico and Utah: Taxonomy and biochronological significance." Journal of Paleontology 71, no. 3 (May 1997): 484–93. http://dx.doi.org/10.1017/s0022336000039500.

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Recently collected specimens of Catopsalis fissidens from the Torrejonian interval of the Nacimiento Formation in the San Juan Basin, New Mexico significantly augment knowledge of the morphology and dental variability of the species. This new knowledge suggests C. foliatus Cope, 1882 (=C. johnstoni Fox, 1989) is a valid Puercan species and that C. fissidens Cope, 1884a is a subjective senior synonym of C. utahensis Gazin, 1939. This latter synonymy further increases taxa shared between the Dragon Canyon local fauna of Utah and the Torrejonian fauna of the San Juan Basin, thus supporting previous inclusion of the Dragonian land-mammal “age” in the Torrejonian.
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Hart, Bruce. "Stratigraphy and hydrocarbon resources of the San Juan Basin: Lessons for other basins, lessons from other basins." Mountain Geologist 58, no. 2 (April 1, 2021): 43–103. http://dx.doi.org/10.31582/rmag.mg.58.2.43.

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This paper examines the relationships between stratigraphy and hydrocarbon production from the San Juan Basin of New Mexico and Colorado. Abundant data and the long production history allow lessons to be learned, both from an exploration and development perspective, that can be applied in other basins. Conversely, as new play types and technologies are defined and developed elsewhere, the applicability of those tools in the San Juan Basin needs to be understood for well-informed exploration and development activities to continue. The San Juan Basin is a Latest Cretaceous – Tertiary (Paleogene) structure that contains rocks deposited from the Lower Paleozoic to the Tertiary, but only the Upper Cretaceous section has significant hydrocarbon, mostly gas, production. Herein I make the case for studying depositional systems, and the controls thereon (e.g., basin development, eustasy, sediment supply), because they are the first-order controls on whether a sedimentary basin can become a hydrocarbon province, or super basin as the San Juan Basin has recently been defined. Only in the Upper Cretaceous did a suitable combination of forcing mechanisms combine to form source and reservoir rocks, and repeated transgressive-regressive cycles of the Upper Cretaceous stacked multiple successions of source and reservoir rocks in a way that leads to stacked pay potential. Because of the types of depositional systems that could develop, the source rocks were primarily gas prone, like those of other Rocky Mountain basins. Oil-prone source rocks are present but primarily restricted to episodes of peak transgression. A lack of suitable trapping mechanisms helps to explain the relative dearth of conventional oil pools. Although gas production has dropped precipitously in the past decade, driven primarily by overabundance of gas supply associated with the shale-gas boom, the combination of horizontal drilling and multi-stage hydraulic fracturing is being applied to revive oil production from some unconventional stratigraphic targets with success.
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Simmons, Nancy B. "A revision of Taeniolabis (Mammalia: Multituberculata), with a new species from the Puercan of eastern Montana." Journal of Paleontology 61, no. 4 (July 1987): 794–808. http://dx.doi.org/10.1017/s0022336000029140.

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The largest known member of the mammalian order Multituberculata is the taeniolabidid Taeniolabis, which is known from Puercan (early Paleocene) localities in northern New Mexico, Utah, Montana, and southern Saskatchewan. A locality in the Ludlow Formation of southeastern Montana has produced remains of a new species, T. lamberti n. sp., which is based on a well-preserved dentary with teeth. Isolated teeth from the Tullock Formation of northeastern Montana are referred to T. lamberti n. sp. and Taeniolabis sp.Taeniolabis triserialis, known exclusively from the San Juan Basin, New Mexico, is shown to be a junior synonym of T. taoensis. Taeniolabis sulcatus, the type species of the genus, is recognized as a nomen dubium and is synonymized with T. taoensis based on general morphology and occurrence in the same stratigraphic unit and collecting area (lower part of the Nacimiento Formation, San Juan Basin, New Mexico). The name T. taoensis is retained for this taxon in the interest of nomenclatorial stability. These synonymies limit to one the number of species of Taeniolabis recognized in the San Juan Basin, New Mexico. It is proposed that T. taoensis be designated the new type species of the genus Taeniolabis.
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Garita-Alvarado, Carlos A., and Claudia Patricia Ornelas-García. "Parallel Evolution of Allometric Trajectories of Trophic Morphology between Sympatric Morphs of Mesoamerican Astyanax (Characidae)." Applied Sciences 11, no. 17 (August 30, 2021): 8020. http://dx.doi.org/10.3390/app11178020.

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Parallel evolution of the body shape and trophic-related traits has been detected between sympatric pairs of lake-dwelling characin fishes in Mesoamerica. Here, we evaluated the variation in and the ontogenetic allometric trajectories of trophic morphology between sympatric Astyanax morphs (elongate and deep-body) in two geographic systems, Lake Catemaco (Mexico) and San Juan River basin (Nicaragua and Costa Rica). Using geometric morphometrics, we determined the shape variation and disparity in the premaxillary bone, and the patterns of allometric trajectories between morphs in each system. We found a higher differentiation and disparity in the premaxilla shape between morphs from San Juan River basin than between the Lake Catemaco ones. We found shared (parallel evolution) patterns of divergence between systems, which included allometric trajectories showing a positive correlation between the premaxilla shape and log centroid size, as well as trajectories being extended in the elongated-body morph (truncated in the deep-body morph). Regarding the unique patterns of divergence, we recovered parallel allometric trajectories between morphs from Lake Catemaco, while the San Juan River basin morphs showed divergent trajectories. Our results are congruent with the hypothesis that divergence in trophic morphology can be considered a triggering factor in the divergence in the genus Astyanax from Mesoamerica.
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Clarkson, Gerry, and Marshall Reiter. "The thermal regime of the San Juan basin since late cretaceous times and its relationship to San Juan mountains thermal sources." Journal of Volcanology and Geothermal Research 31, no. 3-4 (April 1987): 217–37. http://dx.doi.org/10.1016/0377-0273(87)90069-2.

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Dissertations / Theses on the topic "Bassin de San Juan"

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Mendoza, Ruben G. "Conquest polities of the Mesoamerican Epiclassic: Circum-Basin regionalism, A.D. 550-850." Diss., The University of Arizona, 1992. http://hdl.handle.net/10150/185780.

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Recent findings from circum-Basin central highland Mesoamerica have dramatically altered perceptions of the nature and intensity of Late Classic (A.D. 600-900) warfare in the hinterland of the Teotihuacan state. The acropolis centers of Cacaxtla, Cerro Zapotecas, Xochicalco, Teotenango, and Tula Chico, were the focus of a Late Classic pattern of Gulf lowland-central highland interactions that culminated in the militarization of circum-Basin society. The focus of this dissertation concerns a Gulf lowland-based pattern of militarized developments that enveloped highland central Mexico in the period dominated by the decline of the paramount center and polity of Teotihuacan at circa A.D. 550-850. This study seeks to demonstrate that highland central Mexico underwent a profound economic and sociopolitical transformation involving the displacement of an existing Middle Classic horizon (A.D. 400-650) commerce-based system of interregional interaction, to one structured upon a conquest-based system of inter-elite interaction. Particular attention is devoted to the examination of data bearing upon the evolution of conquest-based systems (Fox 1978); specifically, settlement patterns and mortuary data; architectural configurations; ceramic and other artifactual distributions; as well as ethnohistoric and iconographic themes documenting patterns of circum-Basin militarization. These data sources serve to demonstrate a shift toward military statecraft, human sacrifice, and a conquest-based political rhetoric in central highland Mesoamerica for the period after A.D. 550. A secondary objective of this study is to trace the proliferation and spread of Gulf lowland stylistic and sociopolitical patterns into highland central Mexico during the course of events that culminated in the militarization of circum-Basin Mesoamerica in the period after A.D. 550. It will be argued that Late Classic Gulf lowland patterns were replicated in highland contexts, and that Gulf lowland elites are implicated in this process by four primary sources of data; mainly, ethnohistory, iconography, physical anthropology, and archaeology. Finally, Zeitlin's (1982) findings on the emergence of a Gulf Coast-Isthmian exchange network are examined for implications bearing on patterns of interaction that are proposed to have dominated Late Classic highland-lowland commerce. This study concludes with a discussion of the proposed role of Gulf lowland elites, Historic Olmec, or a confederation of Oloman city-states, in the transformative process.
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Chevalier, Michel. "Analyse coûts-bénéfices et environnement : le projet d'aménagement du bassin versant de la Rivière San Juan en République dominicaine." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp05/mq20910.pdf.

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Medina, Sa´nchez Javier. "Cenozoic environmental evolution of the San Juan Raya Basin, south central Mexico." Thesis, University of Leicester, 2011. http://hdl.handle.net/2381/10290.

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This thesis was carried out to gain a better understanding of the Cenozoic environmental evolution of the San Juan Raya Basin, which is a sub-system of the Tehuacan Valley in central Mexico. The likely roles of tectonics and climate in the geomorphic processes of the basin were examined by analysing the geology, geomorphology, depositional environments, as well as other palaeo-records: palaeosols, fossils and geochemical deposits. The correlation of 11 sedimentary sections was established on the basis of 12 radiocarbon dates. A glyptodont (Xenarthra) fossil discovered as part of this study provided important palaeoenvironmental information. The first hypothesis on the Neogene evolution of the basin is put forward, indicating that this system was formed by NE faults probably since the late Miocene or later. The asymmetry of the alluvial landforms indicates that the main factor controlling the development of Pleistocene fans from the north slope was tectonics. Late Pleistocene-Holocene deposits are more widely spread and represent environmental changes since 28.5 kyr ago. Macrofossil and stable isotopes suggest a mixed vegetation and high evaporative conditions under a poorly drained basin before the Last Glacial Maximum (LGM), probably under a colder than present climate. No records are available between the LGM and the end of the Pleistocene. Higher moisture availability was inferred in the early Holocene on the basis of high deposition rates and in situ tufa, followed by periods of intense deposition during the middle Holocene. A discrete alluvial fan reveals a combination of climate and tectonics. Alluvial incision since 2.3 kyr BP coincides with the establishment of current climatic and geomorphic conditions. Late Quaternary erosion and deposition suggest that climate and tectonics have played a dominant role in controlling the geomorphic processes of this basin.
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Agrawal, Angeni. "The economic feasibility of enhanced coalbed methane recovery using CO2 sequestration in the San Juan Basin." Texas A&M University, 2003. http://hdl.handle.net/1969.1/5896.

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Carbon dioxide emissions are considered a major source of increased atmospheric CO2 levels leading towards global warming. CO2 sequestration in coal bed reservoirs is one technique that can reduce the concentration of CO2 in the air. In addition, due to the chemical and physical properties of carbon dioxide, CO2 sequestration is a potential option for substantially enhancing coal bed methane recovery (ECBM). The San Juan Fruitland coal has the most prolific coal seams in the United States. This basin was studied to investigate the potential of CO2 sequestration and ECBM. Primary recovery of methane is controversial ranging between 20-60% based on reservoir properties in coal bed reservoirs15. Using CO2 sequestration as a secondary recovery technique can enhance coal bed methane recovery up to 30%. Within the San Juan Basin, permeability ranges from 1 md to 100 md. The Fairway region is characterized with higher ranges of permeability and lower pressures. On the western outskirts of the basin, there is a transition zone characterized with lower ranges of permeability and higher pressures. Since the permeability is lower in the transition zone, it is uncertain whether this area is suitable for CO2 sequestration and if it can deliver enhanced coal bed methane recovery. The purpose of this research is to determine the economic feasibility of sequestering CO2 to enhance coal bed methane production in the transition zone of the San Juan Basin Fruitland coal seams. The goal of this research is two- fold. First, to determine whether there is a potential to enhance coal bed methane recovery by using CO2 injection in the transition zone of the San Juan Basin. The second goal is to identify the optimal design strategy and utilize a sensitivity analysis to determine whether CO2 sequestration/ECBM is economically feasible. Based on the results of my research, I found an optimal design strategy for four 160- acre spacing wells. With a high rate injection of CO2 for 10 years, the percentage of recovery can increase by 30% for methane production and it stores 10.5 BCF of CO2. The economic value of this project is $17.56 M and $19.07 M if carbon credits were granted at a price of $5.00/ton. If CO2 was not injected, the project would only give $15.55 M.
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NAVARRE, JEAN-CHRISTOPHE. "Stratigraphie genetique du groupe du mesa verde (bassin de san juan) : preservation differentielle des environnements de plaine cotiere et de littoral domine par les vagues." Rennes 1, 1995. http://www.theses.fr/1995REN10174.

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L'un des problemes majeurs de la geologie sedimentaire est d'expliquer la nature de l'enregistrement sedimentaire et les relations espace-temps a l'interieur des sediments, c'est-a-dire la preservation d'un paysage au cours des temps geologiques. Le groupe du mesa verde du bassin de san juan (new-mexico, usa) est un domaine privilegie pour comprendre la preservation differentielle de milieux de sedimentation distincts, a differentes echelles de temps. Le groupe du mesa verde (cretace superieur) comprend des cycles stratigraphiques de trois ordres. Ils enregistrent les oscillations du niveau de base qui traduisent, a differentes echelles, les variations du rapport accommodation/flux sedimentaire. Les geometries de ces cycles et notamment les relations entre les domaines de plaine cotiere et littoraux ont ete reconstituees. (1) les unites genetiques sont les plus petits cycles de variation du niveau de base identifiables. Ce sont des cycles haute frequence dont la duree est estimee de 50 000 a 100 000 ans. (2) les groupements d'unites genetiques correspondent aux cycles de 250 000 a 500 000 ans de moyenne frequence. Ils sont formes de l'empilement d'unites genetiques. (3) l'empilement des groupements d'unites genetiques met en evidence un cycle basse frequence (3-4 ma de duree). La preservation des littoraux et de la plaine cotiere du groupe du mesa verde s'exprime differemment selon: (1) la position des milieux de sedimentation dans une phase de chute ou de montee du niveau de base d'une meme entite stratigraphique (unite genetique ou groupement d'unites genetiques). Ce type de preservation differentielle est appele le partitionnement facietal (facies differentiation). Il correspond a une variation complete ou partielle des associations de facies entre la phase de chute et de montee d'un meme cycle de niveau de base. Dans le cas de cette etude, en domaine littoral, les facies domines par l'action des vagues se preservent en phase de chute du niveau de base, les facies tidaux se deposent en phase de montee du niveau de base. En domaine de plaine cotiere, les ceintures de chenaux amalgames, au-dessus d'une surface de discordance correspondent a un demi-cycle de montee du niveau de base. Le demi-cycle de chute du niveau de base est represente par le depot du complexe d'epandage de crevasses et par la formation d'une surface d'erosion ou d'une surface de discontinuite. (2) selon la position des milieux de sedimentation par rapport au cycle de niveau de base de duree superieure (groupement d'unites genetiques, cycle de basse frequence). Ce type de preservation differentielle est l'effet de la distorsion des cycles superposes et du partitionnement volumetrique (volumetric partitioning) des sediments. (a) en periode de chute du niveau de base de basse frequence, les sediments sont transportes et deposes jusqu'au littoral, au dela de la plaine cotiere. Le domaine littoral est le lieu de la preservation des sediments et les facies de plaine cotiere sont reduits. (b) en periode de montee du niveau de base de basse frequence, l'accomodation est creee progressivement dans la direction du continent. Les sediments se deposent alors en milieu de plaine cotiere. Les domaines littoraux sont progressivement depourvus de sediments siliciclastiques. Les caracteristiques de l'enregistrement sedimentaire dependent des variations d'accomodation. Ces variations conditionnent l'expression des facies et donc leurs caracteres petrophysiques. Elles definissent les attributs sedimentaires et stratigraphiques. Il s'agit par exemple des proprietes du shoreface ou des chenaux de plaine cotiere en fonction de leur position stratigraphique. Ce sont des elements indispensables pour predire qualitativement et quantitativement la geometrie des reservoirs
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Santarelli, Brunella. "Technological Analysis of Pueblo I Lead Glazed Ceramics from the Upper San Juan Basin, Colorado (ca.700-850 CE)." Diss., The University of Arizona, 2015. http://hdl.handle.net/10150/578888.

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The production of lead glaze paints has intrigued Southwestern archaeologists since the 1930s, and significant efforts have been dedicated to the study of this technology by researchers interested in the Pueblo IV (ca. 1275-1400 CE) glazes. In this dissertation I explore the technology of production of the earliest glaze paints produced in the Southwest: the Pueblo I (ca. 700-850 CE) glaze paints from the Upper San Juan. These glaze paints were produced nearly 500 years before the later and well studied Pueblo IV glaze paints, and these technologies represent two separate, independent instances of invention of glaze technology in the prehistoric Southwest. The unique aspect of prehistoric Southwestern glazes is that they were developed as paints, thus serving as decorations. Glaze paints are culturally and technologically significant because it is in the production of the paint that potters are innovating and experimenting with materials. This dissertation presents evidence for a patterned technological behavior in the production of Pueblo I glaze paints - while there is no evidence of specialization, there is evidence for shared technological knowledge regarding other aspects of production. The lack of control over the variability in visual appearance as related to the variability in compositions indicates that it is unlikely that any differences in composition represent intentional technological choices; therefore, Pueblo I potters were not using standardized recipes in the production of glaze paints. I argue that potters were aware of the effect of applying a lead-based paint to the ceramic, thus indicating intentionality, but could not control all of the variables that are involved in the production of a ceramic ware. To understand the mechanisms of invention, and later abandonment, of this technology, I looked for clues in the history of ceramic production in the area, and coupled it with a study of the social and environmental constraints placed on the production. My research suggests that the production of the Pueblo I glaze paints, while not as specialized and widespread as that of the later glaze paints, is a significant technological component of the sequence of ceramic production in the Southwest.
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Yuvaraj, Senthil Velan. "Use of Architectural Element Analysis to Interpret the Depositional Environment and Reservoir Characteristics of the Pictured Cliffs Sandstone, Northern San Juan Basin, Colorado." Bowling Green State University / OhioLINK, 2010. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1287590931.

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Maurer, Joshua Thomas. "Reinterpretation of the Ignacio and Elbert Formations as an Incised Valley Fill Using Facies Analysis and Sequence Stratigraphy; San Juan Basin, Southwest Colorado." Bowling Green State University / OhioLINK, 2012. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1342967247.

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Eckersley, Jaclyn Marie. "The Beef Basin Occupation as an Extension of the Northern San Region: An In-Depth Analysis of the Ceramics in Beef Basin, Utah." BYU ScholarsArchive, 2018. https://scholarsarchive.byu.edu/etd/7061.

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This paper is a summary of the methods and key results of my analysis of 7,997 sherds from 14 sites in Beef Basin, Utah. I discuss physical attributes of the collection, the results of mean ceramic dating, the results of neutron activation analysis, and the results of refiring a sample of nips in an oxidizing atmosphere. I briefly summarize the architecture at each site , as well as possible Fremont cultural material found in and near Beef Basin. I conclude that Beef Basin was likely occupied in the early Pueblo III period and that the occupation was sudden and brief. I determined that paste color can be used as a general indicator of clay procurement locale north of the Abajo Mountains, just as it is in the Comb Ridge vicinity (Glowacki et al. 2015), that there was ceramic production in Beef Basin using local materials, and that the people of Beef Basin had similar connections as, or connections with the east of the Comb Ridge area, as evinced by similar sources for light-paste ceramics found in both areas.
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Granjeon, Didier. "Modélisation stratigraphique déterministe : conception et applications d'un modèle diffusif 3d multilithologique." Phd thesis, Université Rennes 1, 1996. http://tel.archives-ouvertes.fr/tel-00648827.

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Les progrès récents en géologie, et en particulier en stratigraphie génétique, ont permis de mieux appréhender l'étude du remplissage sédimentaire des bassins sur des échelles de temps de quelques centaines de milliers à dizaines de millions d'années, et d'espace de l'ordre de la dizaine à la centaine de kilomètres. Le but de notre travail est la conception d'un modèle déterministe numérique permettant la simulation de ce remplissage sédimentaire. Trois types de modélisation sont actuellement développées : les modèles géométriques, diffusifs et particulaires. Parmi ces approches, nous avons retenu l'approche diffusive, seule approche permettant la simulation du remplissage des bassins sédimentaires aux échelles de temps et d'espace envisagées. Nous avons ainsi conçu un modèle diffusif, baptisé Dionisos (Diffusion Oriented - Normal and Inverse - Simulation Of Sedimentation). L'étude de lois utilisées en mécanique des fluides et de leurs enregistrements dans les sédiments sur de grandes échelles de temps et d'espace nous a permis de concevoir une équation de diffusion reliant le flux de sédiments, s'écoulant en chaque point du bassin, à la pente (énergie de l'écoulement de l'eau), au flux d'eau (capacité de transport de l'eau) et à un coefficient de diffusion (efficacité du transport). Afin de simuler le transport de plusieurs lithologies, nous avons de plus défini une couche superficielle d'altération au sein de laquelle s'effectue l'ensemble de ce transport. Les applications de ce modèle diffusif sur des cas théoriques et sur des cas réels ont montré que ce modèle restitue les implications des concepts de la stratigraphie génétique (partitionnement volumétrique et distorsion des unités génétiques) et les géométries sédimentaires observées. Le modèle est ainsi physiquement et géologiquement cohérent. Ces applications du modèle Dionisos ont de plus illustré différents retours possibles vers les informations géologiques, tant au niveau des cas théoriques (relation entre bathymétrie et sablosité, évolution de la pente du littoral, ... ) qu'au niveau des cas réels (affinement de la définition des bathymétries, ... ). Malgré ces résultats encourageants, il reste cependant différents points à tester, améliorer ou développer, tels que la prise en compte de la dérive littorale et des écoulements turbiditiques, ainsi que la production des carbonates. Ainsi, couplé avec des modèles tectoniques, le modèle Dionisos devrait permettre de mieux appréhender l'influence à diverses échelles des processus tectoniques sur la sédimentation.
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Books on the topic "Bassin de San Juan"

1

Vivian, R. Gwinn. The Chacoan prehistory of the San Juan Basin. San Diego: Academic Press, 1990.

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United States. Bureau of Land Management. San Juan Field Office. Draft environmental impact statement: Northern San Juan Basin coal bed methane project. Durango, Colo: U.S. Dept. of Interior, Bureau of Land Management, San Juan Field Office, 2004.

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Huffman, A. C. Petroleum geology and hydrocarbon plays of the San Juan Basin petroleum province. [Reston, Va.?]: U.S. Geological Survey, 1987.

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Huffman, A. C. Petroleum geology and hydrocarbon plays of the San Juan Basin petroleum province. [Reston, Va.?]: U.S. Geological Survey, 1987.

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Howe, Wesley M. From basin to peak: An explorer's companion to the Colorado-New Mexico San Juan Basin. Lubbock, Tex: Texas Tech University Press, 1998.

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M, Condon Steven. Revisions of Middle Jurassic nomenclature in the southeastern San Juan basin, New Mexico. [Washington]: U.S. G.P.O., 1989.

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Criteria, ECOS Management. Air quality studies in the San Juan Basin coal region: Final technical report. [Santa Fe, N.M.]: Bureau of Land Managment, New Mexico State Office, 1986.

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Nickelson, Howard B. One hundred years of coal mining in the San Juan Basin, New Mexico. Socorro: New Mexico Bureau of Mines & Mineral Resources, 1988.

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United States. Bureau of Land Management. Montrose District. Record of decision for San Juan-San Miguel resource management plan and final environmental impact statement. Montrose, Colo: The District, 1985.

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Pawlewicz, M. J. Vitrinite reflectance values of coal from drill-hole cuttings, San Juan Basin, New Mexico. Denver, CO: U.S. Geological Survey, 1991.

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Book chapters on the topic "Bassin de San Juan"

1

Stone, William J. "Hydrology of the San Juan Basin." In Coal, Uranium, and Oil and Gas in Mesozoic Rocks of the San Juan Basin: Anatomy of a Giant Energy‐Rich Basin: Sandia Mountains to Mesita, New Mexico June 30–July 7, 1989, 39–41. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft120p0039.

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Fassett, James E. "Coal resources of the San Juan Basin." In Coal, Uranium, and Oil and Gas in Mesozoic Rocks of the San Juan Basin: Anatomy of a Giant Energy‐Rich Basin: Sandia Mountains to Mesita, New Mexico June 30–July 7, 1989, 19–26. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft120p0019.

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Huffman, A. Curtis. "Petroleum geology of the San Juan Basin." In Coal, Uranium, and Oil and Gas in Mesozoic Rocks of the San Juan Basin: Anatomy of a Giant Energy‐Rich Basin: Sandia Mountains to Mesita, New Mexico June 30–July 7, 1989, 33–38. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft120p0033.

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Finch, W. I., and V. T. McLemore. "Uranium geology and resources of the San Juan Basin." In Coal, Uranium, and Oil and Gas in Mesozoic Rocks of the San Juan Basin: Anatomy of a Giant Energy‐Rich Basin: Sandia Mountains to Mesita, New Mexico June 30–July 7, 1989, 27–32. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft120p0027.

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Gimenez, Juan Carlos, Emilio Juan Lentini, and Alicia Fernández Cirelli. "Forecasting Streamflows in the San Juan River Basin in Argentina." In Water and Sustainability in Arid Regions, 261–74. Dordrecht: Springer Netherlands, 2009. http://dx.doi.org/10.1007/978-90-481-2776-4_16.

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Ridgley, Jennie. "Introduction to the geology and geography of the San Juan Basin." In Coal, Uranium, and Oil and Gas in Mesozoic Rocks of the San Juan Basin: Anatomy of a Giant Energy‐Rich Basin: Sandia Mountains to Mesita, New Mexico June 30–July 7, 1989, 9–12. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft120p0009.

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Lucas, Spencer G. "Vertebrate biochronology of the Cretaceous-Tertiary boundary, San Juan Basin, New Mexico." In Coal, Uranium, and Oil and Gas in Mesozoic Rocks of the San Juan Basin: Anatomy of a Giant Energy‐Rich Basin: Sandia Mountains to Mesita, New Mexico June 30–July 7, 1989, 47–51. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft120p0047.

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Ginesta Torcivia, Carla E., and Natalia N. Ríos López. "Preliminary Morphometric Analysis: Río Talacasto Basin, Central Precordillera of San Juan, Argentina." In Advances in Geomorphology and Quaternary Studies in Argentina, 158–68. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-22621-3_8.

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Condon, Steven M., and A. Curtis Huffman. "Mesozoic and Cenozoic structure and stratigraphy of the San Juan Basin: An overview." In Coal, Uranium, and Oil and Gas in Mesozoic Rocks of the San Juan Basin: Anatomy of a Giant Energy‐Rich Basin: Sandia Mountains to Mesita, New Mexico June 30–July 7, 1989, 13–18. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft120p0013.

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Megale, Teresa. "L’ombra di Don Juan Tenorio sulla scena barocca partenopea: indizi d’archivio e canoni drammaturgici." In Studi e saggi, 205–18. Florence: Firenze University Press, 2020. http://dx.doi.org/10.36253/978-88-5518-150-1.13.

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This paper highlights archival evidence and dramaturgic mythemes in order to reconsider the historiographical issues related to the XVIIth-century theatrical reception of El burlador de Sevilla y convidado de piedra outside of Spain. Among the crossroads of theatrical practices alive in XVIIth-century Naples, Don Juan underwent a rapid process of assimilation and transformation. The chronology of its Neapolitan debut at the Teatro di San Bartolomeo is re-examined in this paper, while unfolding some new and possible scenarios interweaving history and dramaturgy, the stage and the historical political events of the Kingdom of Naples during the first decades of the XVIIth century. This study examines the Mediterranean basis consolidating the myth of Don Juan – the character with «feet made of wind» (Garboli) – and defining its dramaturgic status all around Europe.
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Conference papers on the topic "Bassin de San Juan"

1

Estrada, Erick, Neale Russell Roberts, Leen Weijers, Thomas Gerald Riebel, and Steven Duane Logan. "Fracture Mapping in the San Juan Basin." In SPE Annual Technical Conference and Exhibition. Society of Petroleum Engineers, 2009. http://dx.doi.org/10.2118/124673-ms.

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Palmer, I. D., and G. M. Kutas. "Hydraulic Fracture Height Growth in San Juan Basin Coalbeds." In Low Permeability Reservoirs Symposium. Society of Petroleum Engineers, 1991. http://dx.doi.org/10.2118/21811-ms.

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Yale, D. P., M. K. Strubhar, and A. W. El Rabaa. "Determination of Hydraulic Fracture Direction, San Juan Basin, New Mexico." In SPE Production Operations Symposium. Society of Petroleum Engineers, 1993. http://dx.doi.org/10.2118/25466-ms.

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Dube, H. G., G. E. Christiansen, J. H. Frantz, N. R. Fairchild, A. J. Olszewski, W. K. Sawyer, and J. R. Williamson. "The Lewis Shale, San Juan Basin: What We Know Now." In SPE Annual Technical Conference and Exhibition. Society of Petroleum Engineers, 2000. http://dx.doi.org/10.2118/63091-ms.

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Parihar, Prannay, Russell Warner, James Micikas, Lianne Armpriester, James Anderson, and Elizabeth Zuluaga. "Infill Drilling Opportunity in Fruitland Coal, San Juan Basin, Colorado." In SPE Low Perm Symposium. Society of Petroleum Engineers, 2016. http://dx.doi.org/10.2118/180247-ms.

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BOUKALOVÁ, ZUZANA, JAN TĚŠITEL, and ZBYNEK KŘIVÁNEK. "THE CONTRIBUTION OF CLIMATE SERVICES TO SUSTAINABLE WINE PRODUCTION IN SAN JUAN, ARGENTINA." In RIVER BASIN MANAGEMENT 2017. Southampton UK: WIT Press, 2017. http://dx.doi.org/10.2495/rbm170031.

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A. Azeglio, Edgardo, Mario E. Gimenez, and Antonio Introcaso. "A 3D Gravimetric Model Of Las Salinas Basin, San Juan, Argentina." In 11th International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 2009. http://dx.doi.org/10.3997/2214-4609-pdb.195.1424_evt_6year_2009.

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Cummings, S. G. "Natural Gas Drilling Methods and Practice: San Juan Basin, New Mexico." In SPE/IADC Drilling Conference. Society of Petroleum Engineers, 1987. http://dx.doi.org/10.2118/16167-ms.

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Cox, D. O., S. H. Stevens, D. G. Hill, and R. A. McBane. "Water Disposal From Coalbed Methane Wells in the San Juan Basin." In SPE Annual Technical Conference and Exhibition. Society of Petroleum Engineers, 1993. http://dx.doi.org/10.2118/26384-ms.

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Azeglio, Edgardo A., Mario E. Gimenez, and Antonio Introcaso. "A 3D Gravimetric model of Las Salinas basin, San Juan, Argentina." In 11th International Congress of the Brazilian Geophysical Society & EXPOGEF 2009, Salvador, Bahia, Brazil, 24-28 August 2009. Society of Exploration Geophysicists and Brazilian Geophysical Society, 2009. http://dx.doi.org/10.1190/sbgf2009-156.

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Reports on the topic "Bassin de San Juan"

1

Martha Cather, Robert Lee, Robert Balch, Tom Engler, Roger Ruan, and Shaojie Ma. Petrophysical Analysis and Geographic Information System for San Juan Basin Tight Gas Reservoirs. Office of Scientific and Technical Information (OSTI), October 2008. http://dx.doi.org/10.2172/966368.

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K. A. M. Gasem, R. L. Robinson, and S. R. Reeves. Adsorption of Pure Methane, Nitrogen, and Carbon Dioxide and Their Mixtures on San Juan Basin Coal. Office of Scientific and Technical Information (OSTI), March 2002. http://dx.doi.org/10.2172/923254.

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M Gasem, K., R. Robinson, and S. Reeves. Adsorption of Pure Methane, Nitrogen, and Carbon Dioxide and Their Mixtures on San Juan Basin Coal. Office of Scientific and Technical Information (OSTI), March 2002. http://dx.doi.org/10.2172/923253.

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Varney, Peter J. Sequence Stratigraphy of the Dakota Sandstone, Eastern San Juan Basin, New Mexico, and its Relationship to Reservoir Compartmentalization. Office of Scientific and Technical Information (OSTI), April 2002. http://dx.doi.org/10.2172/793620.

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Jason Heath, Brian McPherson, and Thomas Dewers. Natural Tracers and Multi-Scale Assessment of Caprock Sealing Behavior: A Case Study of the Kirtland Formation, San Juan Basin. Office of Scientific and Technical Information (OSTI), March 2011. http://dx.doi.org/10.2172/1025536.

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LORENZ, JOHN C., and SCOTT P. COOPER. Tectonic Setting and Characteristics of Natural Fractures in Mesaverde and Dakota Reservoirs of the San Juan Basin, New Mexico and Colorado. Office of Scientific and Technical Information (OSTI), January 2001. http://dx.doi.org/10.2172/776356.

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Reeves, Scott, and Randy Billingsley. Application of Advanced Exploration Technologies for the Development of Mancos Formation Oil Reservoirs, Jicarilla Apache Indian Nation, San Juan Basin, New Mexico. Office of Scientific and Technical Information (OSTI), September 2002. http://dx.doi.org/10.2172/800801.

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Pat Fort and Don L. Hanosh. USING CABLE SUSPENDED SUBMERSIBLE PUMPS TO REDUCE PRODUCTION COSTS TO INCREASE ULTIMATE RECOVERY IN THE RED MOUNTAIN FIELD IN SAN JUAN BASIN REGION. Office of Scientific and Technical Information (OSTI), November 2003. http://dx.doi.org/10.2172/823011.

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Don L. Hanosh. USING CABLE SUSPENDED SUBMERSIBLE PUMPS TO REDUCE PRODUCTION COSTS TO INCREASE ULTIMATE RECOVERY IN THE RED MOUNTAIN FIELD IN SAN JUAN BASIN REGION. Office of Scientific and Technical Information (OSTI), January 2004. http://dx.doi.org/10.2172/824489.

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Don L. Hanosh. Using Cable Suspended Submersible Pumps to Reduce Production Costs to Increase Ultimate Recovery in the Red Mountain Field of the San Juan Basin Region. Office of Scientific and Technical Information (OSTI), August 2006. http://dx.doi.org/10.2172/902834.

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