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Thematische Bibliographien / FLUVIAL CHARACTERISTICS

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Auswahl der wissenschaftlichen Literatur zum Thema „FLUVIAL CHARACTERISTICS“

Autor: Grafiati

Veröffentlicht am 18. Mai 2024

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Zeitschriftenartikel zum Thema "FLUVIAL CHARACTERISTICS"

1

Woronko, Barbara, Paweł Zieliński, and Robert Jan Sokołowski. "Climate evolution during the Pleniglacial and Late Glacial as recorded in quartz grain morphoscopy of fluvial to aeolian successions of the European Sand Belt." Geologos 21, no. 2 (2015): 89–103. http://dx.doi.org/10.1515/logos-2015-0005.

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Abstract We present results of research into fluvial to aeolian successions at four sites in the foreland of the Last Glacial Maximum, i.e., the central part of the “European Sand Belt”. These sites include dune fields on higher-lying river terraces and alluvial fans. Sediments were subjected to detailed lithofacies analyses and sampling for morphoscopic assessment of quartz grains. Based on these results, three units were identified in the sedimentary succession: fluvial, fluvio-aeolian and aeolian. Material with traces of aeolian origin predominate in these sediments and this enabled conclus

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2

Lin, Zhipeng, Le Chen, Jingfu Shan, Tan Zhang, Qianjun Sun, and Yiwu Wang. "A New Sequence Stratigraphic Framework of Terrestrial Fluvial." Studies in Engineering and Technology 4, no. 1 (2017): 85. http://dx.doi.org/10.11114/set.v4i1.2521.

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Currently, the recognition and research on the classification of fluvial types mainly focus on the description and results of a series of indicators, such as the plane shape and sediment characteristics. However, there is limited literacy about how to demonstrate the fluvial types from the depositional process, especially less on sequence model of inland fluvial. Thus, this paper aims o propose a new kind of sequence stratigraphic framework, which is able to reflect the fluvial processes under the perspective of sequence stratigraphy. Accordingly, we use the principle of concrete analysis for

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3

Hassan, Marwan A., Hal Voepel, Rina Schumer, Gary Parker, and Luigi Fraccarollo. "Displacement characteristics of coarse fluvial bed sediment." Journal of Geophysical Research: Earth Surface 118, no. 1 (2013): 155–65. http://dx.doi.org/10.1029/2012jf002374.

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4

Payenberg, T. H. D., and S. C. Lang. "RESERVOIR GEOMETRY OF FLUVIAL DISTRIBUTARY CHANNELS—IMPLICATIONS FOR NORTHWEST SHELF, AUSTRALIA, DELTAIC SUCCESSIONS." APPEA Journal 43, no. 1 (2003): 325. http://dx.doi.org/10.1071/aj02017.

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The exploration and development of stratigraphically trapped hydrocarbons requires detailed knowledge of the morphologies and reservoir characteristics of the stratigraphic body. Fluvial distributary channels are important exploration targets because they are typically isolated reservoirs, laterally and vertically sealed by delta plain and abandoned channel mudstone, and thus form excellent stratigraphic traps. The morphology and reservoir characteristics of fluvial distributary channels have been confused with fluvial channels in the past. Knowing the characteristics of fluvial distributary c

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5

Huang, Kai, Chunsheng Shen, Kai Kang, Libing Wang, Zhongbo Xu, and Lin Li. "Characteristics of Mudstone in Complex Fluvial Sedimentary System in Bohai L Oilfield." Earth Science Research 7, no. 2 (2018): 79. http://dx.doi.org/10.5539/esr.v7n2p79.

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Bohai L oilfield develops a complex fluvial sedimentary system, which includes many types of fluvial sedimentary facies. Based on the coring well of oil field, the distribution characteristics of mudstone are analyzed, it is shown that the mudstone has similar internal structure and can be classified into four types according to its color: gray to grayish, variegated, brown to gray-brown and khaki, the assemblage has a large gray to grayish mudstone section, large gray to grayish mudstone intercalated thin layer sandstone, gray to grayish mudstone associated with variegated (brown) mudstone, g

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6

ZHANG, Yuanfu, Xin DAI, Min WANG, and Xinxin LI. "The concept, characteristics and significance of fluvial fans." Petroleum Exploration and Development 47, no. 5 (2020): 1014–26. http://dx.doi.org/10.1016/s1876-3804(20)60113-6.

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7

Ferreira, Cesar Cardoso, Paulo César Rocha, Arnaldo Yoso Sakamoto, and Heloissa Gabriela Silva Sokolowski. "Análise Temporal da Dinâmica de Aspectos Físicos Fluviais no Rio Abobral-Pantanal-MS-BR." Revista Brasileira de Geografia Física 12, no. 7 (2020): 2672. http://dx.doi.org/10.26848/rbgf.v12.7.p2672-2684.

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O conhecimento de características geomorfológicas fluviais é de suma relevância para estudos voltados aos recursos hídricos, tanto do ponto de vista da hidráulica, da sedimentologia, como também do ponto de vista do planejamento regional. Nesse sentido, este artigo tem como objetivo individualizar e analisar sazonalmente a dinâmica fluvial do rio Abobral no Pantanal-MS situado na bacia do Alto Paraguai, compreendendo uma área composta por extensa superfície de acumulação sujeita a inundações periódicas. Para alcançar o objetivo supracitado, foram executados procedimentos divididos em quatro et

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8

Guo, Shao Lei, and Xuan Ying Guo. "The Fluvial Process of Wandering Reach in the Lower Yellow River." Applied Mechanics and Materials 438-439 (October 2013): 1309–13. http://dx.doi.org/10.4028/www.scientific.net/amm.438-439.1309.

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There are three characteristics of river channel which are wandering, transitional, bending in the Lower Yellow River. The fluvial process is complicated and variable. The channel characteristics of wandering reach was analyzed, and then based on the measured data and model test data, the formation conditions, basic characteristics and influencing factor of the fluvial process law in wandering river were analyzed. All of this can provide technical guidance and theoretical support for river regulation of the Lower Yellow River.

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9

Zheng, Dong-Yu, and Si-Xuan Wu. "Principal component analysis of textural characteristics of fluvio-lacustrine sandstones and controlling factors of sandstone textures." Geological Magazine 158, no. 10 (2021): 1847–61. http://dx.doi.org/10.1017/s0016756821000418.

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AbstractTextures are important features of sandstones; however, their controlling factors are not fully understood. We present a detailed textural analysis of fluvio-lacustrine sandstones and discuss the influences of provenance and depositional environments on sandstone textures. The upper Permian – lowermost Triassic Wutonggou sandstones in the Bogda Mountains, NW China, are the focus of this study. Sandstone thin-sections were studied by point counting and their textures were analysed using statistical and principal component analysis. Fluvial lithic, fluvial feldspathic, deltaic lithic, de

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10

Alexouli - Livaditi, A., K. Vouvalidis, G. Livaditis, and S. Pechlivanidou. "Drainage network characteristics of Athens plain at the end of the 19th century." Bulletin of the Geological Society of Greece 40, no. 4 (2007): 1513. http://dx.doi.org/10.12681/bgsg.17054.

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Kephissos River is the main fluvial system of the hydrological basin of Athens. It drains the central part of Attica and almost the entire urban area of the city of Athens. In this paper, we present the results of both the qualitative and quantitative analysis of the initial drainage network of the plain before the urbanization through the processing of digitised data with GIS software. The initial drainage network of the. basin, plotted with the use of a very detailed mosaic of maps, was constructed by German cartographers (Curtius E. and Kaupert J.) at the end of the 19' century. For the ana

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