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Статті в журналах з теми "Sedimentation and deposition – Uinta Mountains"
Munroe, Jeffrey S., Emily C. Attwood, Samuel S. O'Keefe, and Paul J. M. Quackenbush. "Eolian deposition in the alpine zone of the Uinta Mountains, Utah, USA." CATENA 124 (January 2015): 119–29. http://dx.doi.org/10.1016/j.catena.2014.09.008.
Повний текст джерелаWebb, Casey, Michael Jensen, Bart Kowallis, Eric Christiansen, Douglas Sprinkel, and Sam Hudson. "Stratigraphic relationships of the Eocene Duchesne River Formation and Oligocene Bishop Conglomerate, northeastern Utah—pulsed sedimentary response to rollback of the subducted Farallon slab." Geology of the Intermountain West 9 (September 14, 2022): 153–79. http://dx.doi.org/10.31711/giw.v9.pp153-179.
Повний текст джерелаMunroe, Jeffrey S., Ryan McElroy, Sam O'Keefe, Andrew Peters, and Luna Wasson. "Holocene records of eolian dust deposition from high‐elevation lakes in the Uinta Mountains, Utah, USA." Journal of Quaternary Science 36, no. 1 (September 22, 2020): 66–75. http://dx.doi.org/10.1002/jqs.3250.
Повний текст джерелаCarson, Eric C. "Hydrologic modeling of flood conveyance and impacts of historic overbank sedimentation on West Fork Black's Fork, Uinta Mountains, northeastern Utah, USA." Geomorphology 75, no. 3-4 (May 2006): 368–83. http://dx.doi.org/10.1016/j.geomorph.2005.07.022.
Повний текст джерелаCorbett, Lee B., and Jeffrey S. Munroe. "Investigating the influence of hydrogeomorphic setting on the response of lake sedimentation to climatic changes in the Uinta Mountains, Utah, USA." Journal of Paleolimnology 44, no. 1 (January 13, 2010): 311–25. http://dx.doi.org/10.1007/s10933-009-9405-9.
Повний текст джерелаDalrymple, R. W., and G. M. Narbonne. "Continental slope sedimentation in the Sheepbed Formation (Neoproterozoic, Windermere Supergroup), Mackenzie Mountains, N.W.T." Canadian Journal of Earth Sciences 33, no. 6 (June 1, 1996): 848–62. http://dx.doi.org/10.1139/e96-064.
Повний текст джерелаTabet, David. "Boron in the strata and waters of the Eocene Green River and Uinta Formations, Uinta Basin, Utah." Geosites 50 (September 1, 2022): 1–30. http://dx.doi.org/10.31711/ugap.v50i.111.
Повний текст джерелаPisarska-Jamroży, Małgorzata, Katarzyna Machowiak, and Dariusz Krzyszkowski. "Sedimentation style of a Pleistocene kame terrace from the Western Sudety Mountains, S Poland." Geologos 16, no. 2 (June 1, 2010): 101–10. http://dx.doi.org/10.2478/v10118-009-0008-8.
Повний текст джерелаClark, Peter U., Susan K. Short, Kerstin M. Williams, and John T. Andrews. "Late Quaternary chronology and environments of Square Lake, Torngat Mountains, Labrador." Canadian Journal of Earth Sciences 26, no. 10 (October 1, 1989): 2130–44. http://dx.doi.org/10.1139/e89-179.
Повний текст джерелаMCLOUGHLIN, STEPHEN, and ANDREW N. DRINNAN. "Fluvial sedimentology and revised stratigraphy of the Triassic Flagstone Bench Formation, northern Prince Charles Mountains, East Antarctica." Geological Magazine 134, no. 6 (November 1997): 781–806. http://dx.doi.org/10.1017/s0016756897007528.
Повний текст джерелаДисертації з теми "Sedimentation and deposition – Uinta Mountains"
Hamilton, Doann M. "Sediment Yield Analysis of Reservoir #1, Bull Run Watershed, West Cascade Mountains, Oregon." PDXScholar, 1994. https://pdxscholar.library.pdx.edu/open_access_etds/4838.
Повний текст джерелаOwens, Philip Neil. "Lake sediment-based sediment yields and erosion rates in the Coast Mountains, British Columbia." Thesis, University of British Columbia, 1990. http://hdl.handle.net/2429/29695.
Повний текст джерелаArts, Faculty of
Geography, Department of
Graduate
Davis, Nathan Robert. "Sequence Stratigraphy of the Lower Pennsylvanian (Bashkirian, Morrowan) Round Valley Limestone, Split Mountain Anticline (Dinosaur National Monument) and in the Eastern Uinta Mountains, Utah." BYU ScholarsArchive, 2010. https://scholarsarchive.byu.edu/etd/2377.
Повний текст джерелаHopkins, Chelsea Elizabeth. "Beryllium-10 derived erosion rates from the Hangay Mountains, Mongolia: landscape evolution in a periglacially-dominated continental interior." Thesis, Georgia Institute of Technology, 2012. http://hdl.handle.net/1853/45799.
Повний текст джерелаAnderson, Alvin D. "Geology of the Phil Pico Mountain Quadrangle, Daggett County, Utah, and Sweetwater County, Wyoming." Diss., CLICK HERE for online access, 2008. http://contentdm.lib.byu.edu/ETD/image/etd2384.pdf.
Повний текст джерелаMoragas, Rodriguez Mar. "Multidisciplinary characterization of diapiric basins integrating field examples, numerical and analogue modelling: Central High Atlas Basin (Morocco)." Doctoral thesis, Universitat de Barcelona, 2017. http://hdl.handle.net/10803/436892.
Повний текст джерелаLa discriminació entre processos associats a tectònica extensiva i a tectònica salina es problemàtica; especialment en conques diapíriques extensives invertides com és el cas del Alt Atles Central de Marroc (CHA). L’objectiu d’aquesta tesis és analitzar i entendre els processos que interaccionaren a la conca diapírica del CHA durant el rift Juràssic i el subseqüent període post rift, utilitzant una metodologia multidisciplinària que integra treball de camp, models analògics i models numèrics. S’han estudiat dos dominis de la conca: no diapiric i diapiric (diapirisme durant el Juràssic Inferior i Mitjà). Els models analògics mostren que progradacions longitudinals i transversals i el moment quan s’inicien tenen un gran impacte en la migració dels nivells dúctils, en el mode de creixement diapiric i les seves variacions laterals. Els models amb compressió post-diapírica mostren que dita compressió produeix la reducció progressiva de l’amplada de les estructures diapíriques fins al seu tancament complet, així com a un increment dels cabussaments dels flancs com s’ha observat a les zones d’estudi. Les corbes de subsidència varien segons el domini analitzat. El domini no diapiric es caracteritza per un període llarg de baixes taxes de subsidència tectònica i total (0.06 i 0.08 mma-1). El domini diapiric registra taxes de subsidència tectònica i total fins a un ordre de magnitud majors que en el domini no diapiric (0.23 i 0.90 mma-1) i una migració dels depocentres subsidents. La subsidència del domini diapiric s’interpreta, durant el rift Juràssic Inferior, com una combinació d’activitat de falles normals i migració salina, sent aquesta darrera la predominant durant la fase post-extensiva i emmascarant el patró de subsidència esperat en un estadi de transició rift-post rift. Per primera vegada, es presenta la geohistòria de la part central del CHA. Els models tèrmics emprats per a la seva construcció, avaluats amb 27 noves dades de reflectància de vitrinites de la zona d’estudi, suggereixen una evolució post-Juràssic Mitjà caracteritzada per un període llarg de baixa subsidència que hauria enterrat la regió entre 1200-2400 m, en comptes de una complexa historia que inclouria diversos esdeveniments d’exhumació com s’ha enregistrat en altres zones del Alt Atles Marroquí.
Adams, Rebecca Kavage. "The form and function of headwater streams based on field and modeling investigations in the Southern Appalachian mountains /." 2002. http://scholar.lib.vt.edu/theses/available/etd-12172002-111512.
Повний текст джерелаUroza, Carlos Alberto 1966. "Processes and architectures of deltas in shelf-break and ramp platforms : examples from the Eocene of West Spitsbergen (Norway), the Pliocene paleo-Orinoco Delta (SE Trinidad), and the Cretaceous Western Interior Seaway (S. Wyoming & NE Utah)." 2008. http://hdl.handle.net/2152/18217.
Повний текст джерелаtext
Welke, Bethany. "Double dating detrital zircons in till from the Ross Embayment, Antarctica." Thesis, 2014. http://hdl.handle.net/1805/4450.
Повний текст джерелаU/Pb and (U-Th)/He (ZHe) dating of detrital zircons from glacial till samples in the Ross Embayment, Antarctica records cooling after the Ross/Pan-African orogeny (450-625 Ma) followed by a mid-Jurassic to mid-Cretaceous heating event in the Beacon basin. Zircons were extracted from till samples from heads of major outlet glaciers in East Antarctica, one sample at the mouth of Scott Glacier, and from beneath three West Antarctic ice streams. The Ross/Pan-African U/Pb population is ubiquitous in these Antarctic tills and many Beacon Supergroup sandstones, thus 83 grains were analyzed for ZHe to subdivide this population. Two ZHe age populations are evident in East Antarctic tills, with 64% of grains 115-200 Ma and 35% between 200-650 Ma. The older population is interpreted to be associated with the Ross/Pan-African orogeny including cooling of the Granite Harbour Intrusives and/or exhumation of the older basement rocks to form the Kukri Peneplain. The lag time between zircon U/Pb, ZHe and 40Ar/39Ar ages from K-bearing minerals show cooling over 200 My. Grains in East Antarctic tills with a ZHe age of 115-200 Ma likely reflects regional heating following the breakup of Gondwana from the Ferrar dolerite intrusions, subsidence within the rift basin, and a higher geothermal gradient. Subsequent cooling and/or exhumation of the Transantarctic Mountains brought grains below the closure temperature over a span of 80 My. This population may also provide a Beacon Supergroup signature as most of the tills with this age are adjacent to nunataks mapped as Beacon Supergroup and contain an abundance of vi Beacon pebbles within the moraine. Nine zircons grains from three Beacon Supergroup sandstones collected from moraines across the Transantarctic Mountains yield ages from 125-180 Ma. West Antarctic tills contain a range of ZHe ages from 75-450 Ma reflecting the diverse provenance of basin fill from East Antarctica and Marie Byrd Land. ZHe and U/Pb ages <105 Ma appear to be distinctive of West Antarctic tills. The combination of U/Pb, ZHe and 40Ar/39Ar analyses demonstrates that these techniques can be used to better constrain the tectonic evolution and cooling of the inaccessible subglacial source terrains beneath the Antarctic Ice Sheet.
Книги з теми "Sedimentation and deposition – Uinta Mountains"
Nichols, K. M. Petrology and depositional setting of Mississippian rocks associated with an anoxic events at Samak, western Uinta Mountains, Utah.: Petrology and significance of a Mississippian (Osagean-Meramecian) anoxic event, lakeside mountains, northwestern Utah. Denver, CO: U.S. Geological Survey, 1992.
Знайти повний текст джерелаNichols, K. M. Petrology and depositional setting of Mississippian rocks associated with an anoxic event at Samak, western Uinta Mountains, Utah ; Petrology and significance of a Mississippian (Osagean-Meramecian) anoxic event, Lakeside Mountains, northwestern Utah. Washington, D.C: U.S. G.P.O., 1991.
Знайти повний текст джерелаWardlaw, Bruce R. Conodont biostratigraphy of the Permian Road Canyon Formation, Glass Mountains, Texas. [Washington]: U.S. G.P.O., 1990.
Знайти повний текст джерелаAitken, J. D. The Ice Brook Formation and post-Rapitan, Late Proterozoic glaciation, Mackenzie Mountains, Northwest Territories. [Ottawa]: Energy, Mines and Resources Canada, 1991.
Знайти повний текст джерелаMcCartan, Lucy. Petrology and sedimentology of the Horlick Formation (Lower Devonian), Ohio Range, Transantarctic Mountains. [Washington, D.C.]: U.S. G.P.O., 1987.
Знайти повний текст джерелаMcCartan, Lucy. Petrology and sedimentology of the Horlick Formation (Lower Devonian), Ohio Range, Transantarctic Mountains. Washington, DC: U.S. Geological Survey, 1987.
Знайти повний текст джерелаKrajewski, Marcin. Facies, microfacies and development of the Upper Jurassic-Lower Creataceous of the Crimean carbonate platform from the Yalta and Aj-Petri massifs (Crimea Mountains, southern Ukraine) =: Wykształcenie facjalne i mikrofacjalne oraz rozwój platformy węglowej Gór Krymskich na przykładzie masywów Jałtańskiego i Aj-Petri (górna jura- dolna kreda, Góry Krymskie, południowa Ukraina). Kraków: AGH University of Science and Technology Press, 2010.
Знайти повний текст джерелаMustard, P. S. Rift-related volcanism, sedimentation, and tectonic setting of the Mount Harper Group, Ogilvie Mountains, Yukon Territory. Ottawa: Geological Survey of Canada, 1997.
Знайти повний текст джерелаEvolution of sedimentary basins--Uinta and Piceance basins. [Washington]: U.S. G.P.O., 1987.
Знайти повний текст джерелаGygi, Reinhart A. Quantitative Geology of Late Jurassic Epicontinental Sediments in the Jura Mountains of Switzerland. Birkhäuser, 2012.
Знайти повний текст джерелаЧастини книг з теми "Sedimentation and deposition – Uinta Mountains"
Bruhn, R. L., M. D. Picard, and J. S. Isby. "Tectonics and Sedimentology of Uinta Arch, Western Uinta Mountains, and Uinta Basin." In Paleotectonics and sedimentation in the Rocky Mountain Region, United States. American Association of Petroleum Geologists, 1986. http://dx.doi.org/10.1306/m41456c16.
Повний текст джерелаТези доповідей конференцій з теми "Sedimentation and deposition – Uinta Mountains"
Moser, Katrina A., Elizabeth J. Hundey, Shirley Ngai, Maria Eloisa Sia, and Fred J. Longstaffe. "INSIGHTS INTO THE EFFECTS OF CLIMATE CHANGE AND ATMOSPHERIC DEPOSITION ON LAKES IN THE UINTA MOUNTAINS, UT USING A VARIETY OF PALEOLIMNOLOGICAL TECHNIQUES." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272846.
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