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Letteratura scientifica selezionata sul tema "Braided fluvial"

Autore: Grafiati

Pubblicato: 21 dicembre 2024

Ultima modifica: 31 luglio 2025

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Articoli di riviste sul tema "Braided fluvial"

1

Wang, H., and X. Jia. "Selective deposition response to aeolian-fluvial sediment supply in the desert braided channel of the Upper Yellow River, China." Natural Hazards and Earth System Sciences Discussions 3, no. 2 (2015): 1269–90. http://dx.doi.org/10.5194/nhessd-3-1269-2015.

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Abstract. Rivers flow across aeolian dunes and develop braided stream channels. Both aeolian and fluvial sediment supplies regulate sediment transport and deposition in such a cross-dune braided river. Here we show a significant selective deposition in response to both aeolian and fluvial sediment supplies in the Ulan Buh desert braided channel. This selective deposition developed by the interaction between the flows and the Aeolian-fluvial sediment supplies, making the coarser sediments (> 0.08 mm) from aeolian sand supply and bank erosion to accumulate in the channel center and the finer

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2

Wang, H., X. Jia, Y. Li, and W. Peng. "Selective deposition response to aeolian–fluvial sediment supply in the desert braided channel of the upper Yellow River, China." Natural Hazards and Earth System Sciences 15, no. 9 (2015): 1955–62. http://dx.doi.org/10.5194/nhess-15-1955-2015.

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Abstract. Rivers flow across aeolian dunes and develop braided stream channels. Both aeolian and fluvial sediment supplies regulate sediment transport and deposition in such cross-dune braided rivers. Here we show a significant selective deposition in response to both aeolian and fluvial sediment supplies in the Ulan Buh desert braided channel. The Ulan Buh desert is the main coarse sediment source for this desert braided channel, and the mean percentage of the coarser (> 0.08 mm) grains on the aeolian dunes surface is 95.34 %. The lateral selective deposition process is developed by the in

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3

Sigdel, Ashok, and Tetsuya Sakai. "Sedimentary facies analysis of the fluvial systems in the Siwalik Group, Karnali River section, Nepal Himalaya, and their significance for understanding the paleoclimate and Himalayan tectonics." Journal of Nepal Geological Society 51 (December 31, 2016): 11–26. http://dx.doi.org/10.3126/jngs.v51i0.24084.

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Fluvial sediments of the Siwalik successions in the Himalayan Foreland Basin are one of the most important continental archives for the history of Himalayan tectonics and climate change during the Miocene Period. This study reanalyzes the fluvial facies of the Siwalik Group along the Karnali River, where the large paleo-Karnali River system is presumed to have flowed. The reinterpreted fluvial system comprises fine-grained meandering river (FA1), flood-flow dominated meandering river with intermittent appearance of braided rivers (FA2), deep and shallow sandy braided rivers (FA3, FA4) to grave

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Lu, Zhiyuan, Zhiliang He, Shizhong Ma, and Yu He. "Sedimentary characteristics and sand-body distributions in the Lower Permian He 8 Member, Ordos Basin, China." Interpretation 10, no. 2 (2022): T223—T236. http://dx.doi.org/10.1190/int-2021-0101.1.

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The Lower Permian He 8 Member (P1h8) in the Ordos Basin is a typical producing zone of tight lithologic gas reservoirs. Analyses of sedimentary characteristics, electrofacies, and sand-body distributions of P1h8, conducted on modern fluvial deposits, outcrops, cores, and well logs, revealed that braided rivers that developed in the Lower P1h8 and Upper P1h8 are characterized by meandering river. Within these fluvial deposits, the procedure consists of analyzing high-resolution sequence stratigraphy and sedimentary dynamics defined from calibrated logging curve signatures and depositional studi

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Ju, Xiaoyu, Xiaodong Zhao, Boyu Zhou, Ruixue Zhang, Xinyu Wu, and Dafa Guo. "Identification of Reservoir Water-Flooding Degrees via Core Sizes Based on a Drip Experiment of the Zhenwu Area in Gaoyou Sag, China." Energies 16, no. 2 (2023): 608. http://dx.doi.org/10.3390/en16020608.

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In order to identify the degree of water flooding in a reservoir and to discover any remaining oil-enriched areas, in this paper, a systematic study on the water flooding of cores in obturated coring wells is carried out. With observations and testing data of the cores, based on the notion of sedimentary facies, the water-flooding degrees of 4–7 sand groups in member one of the Paleogene Sanduo Formation (E2s14–7) of the Zhenwu area in the Gaoyou Sag are determined. Overall, the results show that the study area is formed under the background of lake regression, with various sedimentary systems

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Zawri, Nurul Fahana, Abdul Hadi Abd Rahman, Numair Ahmed Siddiqui, and Norizam Md Nor. "Geomorphological evolution of the Group I fluvial system, AX field, Malay Basin." IOP Conference Series: Earth and Environmental Science 1003, no. 1 (2022): 012009. http://dx.doi.org/10.1088/1755-1315/1003/1/012009.

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Abstract The AX Field is located 167km off NNE Kerteh, Terengganu of Peninsular Malaysia, southwest of Malay Basin. This study is focused on the 3D seismic analysis of the Lower Miocene fluvio-deltaic Group I. The objective of the study is to evaluate the geomorphological evolution of fluvial succession and interpret the possible intra-basinal and extra-basinal controls on the fluvial evolution. One hundred strata slices were generated in order to evaluate the evolution of the fluvial systems within the Group I interval. Seismic attributes such as Root Mean Square (RMS), sweetness and spectral

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Sun, Yu, Xiu Li Zhang, Jin Yan Zhang, and Chen Chen. "Analysis on Grain-Size Characteristics and Sedimentary Environment of Conglomerate Reservoirs in Ying-4 Section of Xingcheng Gas Field of Songliao Basin." Advanced Materials Research 734-737 (August 2013): 286–89. http://dx.doi.org/10.4028/www.scientific.net/amr.734-737.286.

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Aimed at difficulty of conglomerate in Ying-4 Section of Xingcheng Gas Field, Songliao Basin, which it is impossible to be carried out, using routine granularity analysis methods, and the iconic grain-size analysis is carried out. According to iconic two-dimension grain-size analysis, and contacting to fundamental sedimentary characteristics of conglomerate, sedimentary environment analysis is carried out. It is thought that this area is Shallow gravel-bed braided fluvial fan deltas, to braided fluvial delta transition, which supported an important geological foundation for the next dispositio

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Liu, Yuming, Luxing Dou, Xiaoxu Ren, and Jiagen Hou. "Sedimentary characteristics of muddy deposits in sandy braided fluvial system: A case study from outcrops of the Jurassic Yungang Formation in the Datong Basin, Central China." Interpretation 8, no. 3 (2020): SM139—SM149. http://dx.doi.org/10.1190/int-2019-0174.1.

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The sandbodies within braided fluvial deposits are important reservoirs for the oil fields in China, and they usually have complex sedimentary architecture. A lot of research has been concentrated on characterizing the architecture of the sandbodies. Based on the observation that muddy deposits are commonly well preserved in fluvial deposits, we find that understanding the contact relationship between the muddy deposits and surrounding sand bodies can help characterize the depositional process of sandy braided fluvial systems. We have determined the effectiveness of this idea by characterizing

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Cui, Kunning. "Characteristics of sedimentary system evolution and sequence stratigraphy boundary of Denglouku group in Xujiaweizi fault depression, Songliao Basin." IOP Conference Series: Earth and Environmental Science 1087, no. 1 (2022): 012073. http://dx.doi.org/10.1088/1755-1315/1087/1/012073.

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Abstract In the previous studies on this area, the sequence division is relatively rough. This study has improved the precision, and the Denglouku formation is divided into 10 fourth-order sequences, with the thickness of each small layer of about 70-80m. The characteristics of each small sequence boundary are described, and three third-order, four fourth-order sequence flooding surfaces are found. The stratigraphic framework is established. From bottom to top, the base level of all strata shows decline-rise-decline, which means regression-transformation-regression. The Denglouku 1st mainly in

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Candeiro, Carlos Roberto, Rodrigo Pinto De Azevedo, and Priscila Maria Da Silva. "PRELIMINARY APPROACH ON DEPOSITIONAL ENVIRONMENTAL OF THE UBERABA FORMATION (UPPER CRETACEOUS), PEIRÓPOLIS SITE, MINAS GERAIS STATE, BRAZIL: AN INTRODUCTION." Caminhos de Geografia 8, no. 22 (2007): 81–85. http://dx.doi.org/10.14393/rcg82215625.

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The Coniacian-Santonian Uberaba Formation of Triângulo Mineiro region hás yielded a important paleofauna from fluvial and associated paleoenvironments. Although poor, fossil content are represented by invertebrates and vertebrates. The paleontological and geological data suggested that Uberaba Formation is characterized by a fluvial of a braided type.

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Più fonti

Tesi sul tema "Braided fluvial"

1

Pinisetti, Moe. "Integrated numerical well test modelling in braided fluvial reservoirs." Thesis, Heriot-Watt University, 1999. http://hdl.handle.net/10399/609.

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Salas, Carlos J. "Braided fluvial architecture within a rapidly subsiding basin the Pennsylvanian Cumberland group southwest of Sand River, Nova Scotia." Thesis, University of Ottawa (Canada), 1986. http://hdl.handle.net/10393/5416.

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Reis, Adriano Domingos dos. "Análise arquitetural de depósitos fluviais da Formação Guará (Jurássico Superior-Cretáceo Inferior) na borda sudeste da Bacia do Paraná, RS, Brasil." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2016. http://hdl.handle.net/10183/133638.

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The Guará Formation (Upper Jurassic) crops out in the western portion of Rio Grande do Sul along a track with north-south orientation, of which the northern part essentially consists of fluvial deposits with paleocurrent to southwest. Despite the existence of outcrops with good vertical exposure and high lateral continuity, had not yet been carried out detailed studies of fluvial architecture of this unit. Through facies analysis, with vertical logs and lateral sections data, 9 lithofacies composing 8 architectural elements were described and interpreted. These elements are grouped in sandston

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Picco, Lorenzo. "Long period morphological dynamics in regulated braided gravel-bed rivers: comparison between Piave River (Italy) and Waitaki River (New Zealand)." Doctoral thesis, Università degli studi di Padova, 2010. http://hdl.handle.net/11577/3426981.

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Aim of this research has been to make an analysis of long and medium term morphological dynamics that may affect the regulated gravel-bed braided rivers as the Piave river (Italy) and the Waitaki river (New Zealand). The Piave river (drainage area around 4000km2), is one of the largest rivers in the north-east of Italy, the study reach is, mainly, 37 km long, and represent the intermediate course of the river within the mountain district. In addiction were been study different sub-reaches until a minimum of around 1,5 km long. The Waitaki river (drainage area around 11000 km2), is a large gr

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5

Bofill, Lucas. "From outcrop to fluid-flow : sedimentary architecture, permeability heterogeneity, and effect of sedimentary facies in fluid-flow modelling : a case study of the middle buntstandstein continental sandstones (lower triassic, eastern France)." Electronic Thesis or Diss., Strasbourg, 2024. http://www.theses.fr/2024STRAH006.

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Au fossé rhénan supérieur, dans l'est de la France, le Buntsandstein du Trias inférieur constitue un important réservoir d'eau souterraine et de saumures géothermiques riches en lithium. L'objectif scientifique de cette étude est de comprendre l'architecture de la Formation du Grès Vosgien inférieur (LGV), Buntsandstein moyen ; comment les processus sédimentologiques, à différentes échelles, génèrent des hétérogénéités significatives de perméabilité ; et l'effet de telles hétérogénéités sur les résultats de la modélisation des flux de fluides. L'étude utilise une caractérisation sédimentologiq

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Tacon, Sandrine. "Spatio-temporal analysis of braided river morphology with airborne LiDAR." Thesis, Lyon 2, 2015. http://www.theses.fr/2015LYO20054/document.

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Les rivières en tresses constituent des plaines alluviales complexes constituées d'une mosaïque d'unités correspondant à des échelles spatio-temporelles différentes. L'objectif de cette thèse a été d'utiliser des données de LiDAR aéroporté pour améliorer la connaissance des réponses morphologiques des lits en tresses à différentes échelles spatio-temporelles. Dans un premier temps, 2 levés LiDAR séquentiels ont permis de détecter les changements morphologiques d’une tresse de 7 km survenus suite à une crue de période de retour 14 ans. Ces travaux ont été réalisés sur le site du Bès, un affluen

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7

Krapf, Carmen. "Ephemeral river systems at the Skeleton Coast, NW-Namibia sedimentological and geomorphological studies on the braided river dominated Koigab Fan, the cenozoic succession in the Uniabmond area and comparative studies on fluvio-aeolian interaction between ephemeral rivers and the Skeleton Coast erg /." Doctoral thesis, [S.l. : s.n.], 2003. http://deposit.ddb.de/cgi-bin/dokserv?idn=968609740.

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PICCO, LORENZO. "Long period morphological dynamics in regulated braided gravel-bed rivers: comparison between Piave River (Italy) and Waitaki River (New Zealand)." Doctoral thesis, 2010. http://hdl.handle.net/11577/3033851.

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Obbiettivo della presente ricerca è quello di eseguire un’analisi di lungo e medio periodo sulla dinamica della morfologia fluviale riguardante fiumi a canali intrecciati a fondo ghiaioso, sottoposti a regolazione dei regimi idrici, come il fiume Piave (Italia) e il fiume Waitaki (Nuova Zelanda). Il fiume Piave (area del bacino di circa 4000 km2), è uno dei principali fiumi del nord-est d’Italia; il tratto analizzato ha una lunghezza di circa 37 km e si trova nella parte centrale del bacino montano. Inoltre, sono stati studiati diversi sottotratti fino ad un minimo di 1.5 km di lunghezza. Il f

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Krapf, Carmen [Verfasser]. "Ephemeral river systems at the Skeleton Coast, NW-Namibia : sedimentological and geomorphological studies on the braided river dominated Koigab Fan, the cenozoic succession in the Uniabmond area and comparative studies on fluvio-aeolian interaction between ephemeral rivers and the Skeleton Coast erg / vorgelegt von Carmen Krapf." 2003. http://d-nb.info/968609740/34.

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Libri sul tema "Braided fluvial"

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E&G Quaternary Science Journal Vol. 60 No 4: Quaternary landscape evolution in the Peribaltic region. Geozon Science Media, 2011.

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Capitoli di libri sul tema "Braided fluvial"

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Surian, Nicola. "Fluvial Processes in Braided Rivers." In Rivers – Physical, Fluvial and Environmental Processes. Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-17719-9_15.

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Ashmore, P., and J. T. Gardner. "Unconfined Confluences in Braided Rivers." In River Confluences, Tributaries and the Fluvial Network. John Wiley & Sons, Ltd, 2008. http://dx.doi.org/10.1002/9780470760383.ch7.

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Gardiner, Scott, David V. Thomas, E. Dale Bowering, and Larry S. McMinn. "A Braided Fluvial Reservoir, Peco Field, Alberta, Canada." In Casebooks in Earth Sciences. Springer New York, 1990. http://dx.doi.org/10.1007/978-1-4613-8988-0_3.

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Surian, Nicola, and Alessandro Fontana. "The Tagliamento River: The Fluvial Landscape and Long-Term Evolution of a Large Alpine Braided River." In World Geomorphological Landscapes. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-26194-2_13.

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Momin, Hassan, and Gorky Chakraborty. "Missing Fluvio-Social Dynamics of a Braided River: A Study on a Select Stretch of the Brahmaputra in Assam." In Indigeneity, Development and Sustainability. Springer Nature Singapore, 2024. http://dx.doi.org/10.1007/978-981-97-1436-0_12.

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"Braided Fluvial Reservoirs." In Oil Field Production Geology. American Association of Petroleum Geologists, 2009. http://dx.doi.org/10.1306/13161222m913372.

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Ball, Leslie, Michael Boebé, Peter Sadler, Patrick Corbett, and Jonathan Lewis. "Permeability Prediction in a Braided Fluvial Reservoir." In The Geology of Sirt Basin. Elsevier, 1996. https://doi.org/10.1016/b978-044482403-5/50053-0.

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MAIZELS, JUDITH K. "LARGE-SCALE FLOOD DEPOSITS ASSOCIATED WITH THE FORMATION OF COARSE-GRAINED, BRAIDED TERRACE SEQUENCES." In Recent Developments in Fluvial Sedimentology. SEPM (Society for Sedimentary Geology), 1987. http://dx.doi.org/10.2110/pec.87.39.0135.

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Mcvey, R., B. Rumsby, and J. Brasington. "The potential for high resolution fluvial archives in braided rivers." In River Basin Sediment Systems - Archives of Environmental Change. Taylor & Francis, 2001. http://dx.doi.org/10.1201/9781439824672.ch16.

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KINGSLEY, CHARLES S. "FACIES CHANGES FROM FLUVIAL CONGLOMERATE TO BRAIDED SANDSTONE OF THE EARLY PROTEROZOIC ELDORADO FORMATION, WELKOM GOLDFIELD, SOUTH AFRICA." In Recent Developments in Fluvial Sedimentology. SEPM (Society for Sedimentary Geology), 1987. http://dx.doi.org/10.2110/pec.87.39.0359.

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Atti di convegni sul tema "Braided fluvial"

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Toro-Rivera, M. L. E., P. W. M. Corbett, and George Stewart. "Well Test Interpretation in a Heterogeneous Braided Fluvial Reservoir." In European Petroleum Conference. Society of Petroleum Engineers, 1994. http://dx.doi.org/10.2118/28828-ms.

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Ettema, R., D. Armstrong, C. Thornton, S. Hughes, and S. Abt. "Hydraulic modeling of braided channels self-formed in an alluvial plain." In The International Conference On Fluvial Hydraulics (River Flow 2016). CRC Press, 2016. http://dx.doi.org/10.1201/9781315644479-176.

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Taylor, D., D. Hodgetts, J. Redfern, and J. Richardson. "Quantification and Prediction of Braided Fluvial Systems Using Digital Outcrop Models." In 80th EAGE Conference and Exhibition 2018. EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201801689.

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Biswas, Robin, A. Yorozuya, and S. Egashira. "Monitoring of sandbars migration process in mega-sized braided river using MODIS." In The International Conference On Fluvial Hydraulics (River Flow 2016). CRC Press, 2016. http://dx.doi.org/10.1201/9781315644479-99.

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Li, S. L., and X. H. Yu. "The Response of Architectural Elements to Sequence Stratigraphy in Braided Fluvial System." In Saint Petersburg 2012. EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20143720.

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Unsworth, C., A. Nicholas, P. Ashworth, et al. "Using bedform migration and orientation to infer sediment transport pathways in a sandy braided river." In The International Conference On Fluvial Hydraulics (River Flow 2016). CRC Press, 2016. http://dx.doi.org/10.1201/9781315644479-180.

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Becker, Mauro R., Larry W. Lake, and Noel Tyler. "Fractal Properties of Braided Fluvial Deposits for Characterization and Simulation of Reservoir Heterogeneity." In Latin American and Caribbean Petroleum Engineering Conference. Society of Petroleum Engineers, 1997. http://dx.doi.org/10.2118/38951-ms.

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Labourdette, R., and R. Jones. "Characterisation of Fluvial Architectural Elements Using a Three Dimensional Outcrop Dataset – Escanilla Braided System." In 69th EAGE Conference and Exhibition incorporating SPE EUROPEC 2007. European Association of Geoscientists & Engineers, 2007. http://dx.doi.org/10.3997/2214-4609.201401722.

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Davies, D. K., B. P. J. Williams, and R. K. Vessell. "Models for Meandering and Braided Fluvial Reservoirs With Examples From the Travis Peak Formation, East Texas." In SPE Annual Technical Conference and Exhibition. Society of Petroleum Engineers, 1992. http://dx.doi.org/10.2118/24692-ms.

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Zhongbo, Xu, Huang Kai, Shen Chunsheng, et al. "Architecture Characterization of Sandy Braided Fluvial Reservoir: A Case Study of P Oilfield (Neogene), Bohai Offshore, China." In SPE Annual Technical Conference and Exhibition. Society of Petroleum Engineers, 2015. http://dx.doi.org/10.2118/174886-ms.

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Rapporti di organizzazioni sul tema "Braided fluvial"

1

Devaney, J. R., and P. W. Fralick. Regional sedimentology of the Namewaminikan group, northern Ontario: archean fluvial fans, braided rivers, deltas, and an aquabasin. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/120237.

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Ambrose, William A., Tucker F. Hentz, Harold Rogers, and David L. Carr. Regional and Local Variability in Lowstand Valley Fill and Deltaic Deposits in the Tannehill Sandstone (Cisco Group), Eastern Shelf of the Permian Basin. University of Texas at Austin, Bureau of Economic Geology, 2024. https://doi.org/10.23867/ri0290d.

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Lowstand valley fill and shelf-edge deltaic deposits in the Tannehill sandstone (Wolfcampian Cisco Group) in the Eastern Shelf of the Permian Basin are major targets for oil and gas exploration. The most-productive trends link coarse-grained alluvial systems in Baylor County to shelf-edge and upper-slope deepwater systems in Dickens County. Depositional axes in the Tannehill sandstone in the updip (eastern) facies tract in Wichita, Archer, Clay, and Montague Counties, proximal to sediment source areas in the Ouachita fold belt and the Arbuckle Mountains, contain 40 to 80 ft (12–24 m) of net sa

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