Academic literature on the topic 'Sedimentology'
Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles
Consult the lists of relevant articles, books, theses, conference reports, and other scholarly sources on the topic 'Sedimentology.'
Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.
You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.
Journal articles on the topic "Sedimentology"
Welch, John R., Mark T. Altaha, Garry J. Cantley, William H. Doelle, Sarah A. Herr, Morag M. Kersel, Brandi L. MacDonald, et al. "Hope in Dirt: Report of the Fort Apache Workshop on Forensic Sedimentology Applications to Cultural Property Crime, 15—19 October 2018." International Journal of Cultural Property 26, no. 02 (May 2019): 197–210. http://dx.doi.org/10.1017/s0940739119000092.
Full textEdmonds, Douglas A. "Restoration sedimentology." Nature Geoscience 5, no. 11 (November 2012): 758–59. http://dx.doi.org/10.1038/ngeo1620.
Full textFarmer, John G. "Environmental Sedimentology." Science of The Total Environment 382, no. 2-3 (September 1, 2007): 390. http://dx.doi.org/10.1016/j.scitotenv.2007.04.006.
Full textStouthamer, Esther, and Wilfried ten Brinke. "Fluvial Sedimentology." Netherlands Journal of Geosciences - Geologie en Mijnbouw 86, no. 1 (April 2007): 1. http://dx.doi.org/10.1017/s0016774600021272.
Full textChilingarian, G. V., and A. E. Gurevich. "Practical sedimentology." Journal of Petroleum Science and Engineering 14, no. 3-4 (May 1996): 257–58. http://dx.doi.org/10.1016/s0920-4105(96)90011-x.
Full textBowman, Mike. "Petroleum sedimentology." Marine and Petroleum Geology 13, no. 7 (November 1996): 858–59. http://dx.doi.org/10.1016/0264-8172(96)83698-1.
Full textChilingarian, G. V., and A. E. Gurevich. "Analytical sedimentology." Journal of Petroleum Science and Engineering 14, no. 3-4 (May 1996): 257–58. http://dx.doi.org/10.1016/0920-4105(95)00058-5.
Full textSellwood, B. "Applied sedimentology." Marine and Petroleum Geology 7, no. 2 (May 1990): 197. http://dx.doi.org/10.1016/0264-8172(90)90042-f.
Full textFörstner, Ulrich. "Environmental sedimentology." Journal of Soils and Sediments 7, no. 6 (December 2007): 431. http://dx.doi.org/10.1065/jss2007.11.263.
Full textDouglas, Ian. "Urban sedimentology." Progress in Physical Geography: Earth and Environment 9, no. 2 (June 1985): 255–80. http://dx.doi.org/10.1177/030913338500900203.
Full textDissertations / Theses on the topic "Sedimentology"
Boya, Duocastella Salvador. "El sistema deltaico de la Arenisca de Sabiñánigo y la continentalización de la cuenca de Jaca." Doctoral thesis, Universitat Autònoma de Barcelona, 2018. http://hdl.handle.net/10803/665452.
Full textThe Jaca basin is an exceptional example of sedimentary infill of a piggyback basin. Its stratigraphic record shows the evolution from deep-marine environments during the lower Eocene until the its evolution to the transitional and terrestrial environments that represent de last stage of the basin fill during the upper Eocene-Miocene. This features, and the excellent exposure of the outcrops, allow to highlight this basin as an excellent analog in many studies related to sedimentary geology. In this thesis, a review of the delta and alluvial formations of the Jaca basin, classically defined in a descriptive sence, has been carried out in order to establish genetic depositional systems based on basin scale indicators. In order to achieve this goal a methodology based on the elaboration of a geological cartography and facies analysis has been applied, this last one, focused chiefly on the deltaic units related to the Sabiñánigo Sandstone delta system. Through the combination of both techniques, 8 depositional systems have been differentiated in the Jaca basin. Among these 8 depositional systems, the deltaic depositional ones (Bartonian to Priabonian) stand out as complex systems due the present-day lack of physical correlation in the basin between the Jaca and Fiscal sectors. From the integration of stratigraphic field data obtained in this thesis, with paleomagnetic and biostratigraphic data from the literature, it has been possible to establish an equivalence between the deltaic systems in the central Jaca sector (central part of the basin) and those of the Fiscal sector (eastern part of the basin). These equivalences allow establishing a new correlation between both sectors which allows to propose younger age range for the Fiscal units. Deltaic depositional systems analysis has been here focused in more detail on the Sabiñánigo Sandstone delta system, whose excellent quality in terms of exposure, connection and extension of its outcrops, has allowed to carry out an exhaustive facies study. Facies analysis has permitted to characterize this delta as a flood-dominated delta derived from hyperpycnal flows sourced from the north of the Jaca basin. During transgressive periods, the hyperpycnal sediments where reworked by tidal processes which developed systems of tidal bars. Synchronously, in the Fiscal sector, the upper San Felices delta system was formed as an inertia dominated delta. This system, with an eastern provenance signal, interacted with the north-derived deltas in the Jaca sector. This interaction is displayed by the recording of an eastern provenance signal in the tidal sediments, and also by the occurrence of outer shelf deposits in the southern flank of the Basa anticline. Finally, it has been possible to identify a tectonic control in the deltaic cyclicity of these systems. The deltaic system of Sabiñánigo shows growth strata which can be linked to the activity of the Otúria thrust. In the same way, the upper San Felices delta system shows growth strata in its eastern edge related to the growth of the Boltaña anticline. The active stages of each of these structures produced an alteration in the accommodation rate, generating episodes of forced transgression in the deltaic systems. In this work, the importance of detailed facies analysis is highlighted as a key tool to infer the different factors that can modify the architecture style of sedimentary systems in an active tectonic context, such as the South Pyrenean basin. In addition, this thesis presents the deltaic system of the Sabiñánigo Sandstone delta system as an excellent field analog of a flood dominated.
Speranza, Flavio Cesar. "Variabilidad paleoclimática y cambios paleoambientales en la región Chaqueña semiárida Argentina." Doctoral thesis, Universitat Autònoma de Barcelona, 2020. http://hdl.handle.net/10803/670872.
Full textLos estudios paleoclimáticos y paleoambientales del holoceno proporcionan información relevante sobre las tendencias climáticas a largo plazo necesarias para generar y probar hipótesis sobre patrones y modelos climáticos y entender los cambios ambientales recientes. Si bien hay un número creciente de este tipo de estudios en América del Sur, todavía existen extensas regiones que no cuentan con estudios detallados y de alta resolución, tal como sucede en el Chaco semiárido. El presente trabajo constituye un aporte significativo para reducir la brecha espacial de información de la variabilidad paleoclimática, la dinámica del paisaje y la transformación paleoambiental, a distintas escalas espaciales y temporales, durante los últimos siglos en la región semiárida del Chaco argentino, mediante la vinculación y articulación de una significativa cantidad y diversidad de indicadores. Se llevaron a cabo estudios fluviomorfológicos, geomorfológicos y secuencias sedimentarias mineralógicas y texturales de paleocauces en la cuenca baja del río Bermejo, principal modelador del paisaje de la llanura chaqueña semiárida; análisis de registros multiparamétricos sedimentológicos de alta resolución (litología, geoquímica, mineralogía) y palinológicos de sedimentos lacustres de Laguna Yema; construcción y análisis de cronologías de ancho de anillos de la especie arbórea Schinopsis lorentzii, ubicados en un gradiente latitudinal (Norte-Sur) en la región chaqueña semiárida de Argentina y, complementariamente, se emplearon bases de datos de estaciones meteorológicas e hidrométricas dispuestas en el área de estudio. Nuestros resultados e interpretaciones constituyen herramientas para ser empleadas en la gestión integrada de recursos hídricos en la región chaqueña semiárida, en donde la deficiencia en la disponibilidad de agua para la producción y consumo humano y las inundaciones son unas de las principales amenazas de la región. Adicionalmente, nuestro trabajo constituye un insumo para la gestión del ordenamiento ambiental y productivo del territorio, en donde el avance de la frontera agropecuaria para el desarrollo de cultivos extensivos es el principal fenómeno de cambio en la cobertura del suelo, siendo su sustentabilidad altamente dependiente de las variaciones y estacionalidad climática.
Paleoclimatic and paleoenvironmental studies of the Holocene provide relevant information regarding climatic trends in the long-term, necessaries to generate and test hypothesis on climatic patterns and models, as well as understanding recent environmental changes. While an increasing number of these type of studies are being developed in South America, there are still large regions that do not have detailed and high resolution studies, as in the case of the semi-arid Chaco. This work constitutes a significant contribution in order to reduce the spatial information gap regarding paleoclimatic variability, landscape dynamics, and paleoenvironmental transformations, at different spatial and temporal scales, during the last centuries in the semi-arid region of Argentinian Chaco, through the linkage and articulation of a significant amount and diversity of indicators. A series of studies were conducted, including fluvialmorphological, geomorphological, and textural and mineralogical sedimentary sequences in the lower basin of the Bermejo River, the main landscape modeler of the semi-arid plains in Chaco; analysis of multi-parametric sedimentological records of high-resolution (lithology, geochemistry, mineralogy) and palynological from lake sediments in Laguna Yema; construction and analysis of tree-ring width chronologies of Schinopsis lorentzii, mainly located in an altitudinal gradient (North-South) of the semi-arid Chaco region in Argentina and, as a complement, databases from meteorological and hydrometric stations arranged in the study are were also consulted. Our results and interpretations constitute tools to be employed in the integrated management of hydric resources in the semi-arid Chaco, where deficiency in water availability for production and human consumption, as well as floods, are one of the main threats in the region. In addition to that, our investigation constitutes an input for the environmental and productive management of the territory, where the advance of the agricultural border for the development of extensive crops is the main change phenomenon in soil coverage, with a sustainability highly dependent of climatic variations and seasonality.
Menezes, Priscila Melo Leal. "Análise de fácies e proveniência sedimentar em sambaquis do litoral centro-sul de Santa Catarina." Universidade de São Paulo, 2009. http://www.teses.usp.br/teses/disponiveis/44/44141/tde-19082009-102541/.
Full textThe sambaquis (also known as shell mounds or shell middens) in the Brazilian southern coast are landscape references and bear historical and scientific value. They are predominantly constituted of mollusk shells and sediments and also hold a sound presence of organic matter, piled up in different stratigraphic configurations. In this work, three sambaquis in the central-southern coast of the Santa Catarina state have been chosen as objects of study. They present two distinct configuration types: on one hand, the Carniça III and the Encantadas III, and, on the other hand, the Jabuticabeira II, which is larger and stratigraphically more complex. The proposal is to assist on the reconstruction of habits and traditions of the people who lived in this coastal area during a great part of the Holocene period (before the Portuguese navigators arrived in Brazil in 1500), and to infer their relations with the evolution of the surrounding geological environment. Two main goals have been set for this purpose: the application of facies analysis and depositional architecture in the selected sambaquis; and the investigation of the use of sediments from paleo-lagoons as their construction material. In order to achieve these goals, a multi-analytical approach has been used comprising: facies analysis; quantity evaluation of organic matter and carbonates associated with phosphates; characterization of the thick fraction in stereomicroscope; granulometry; heavy grains mineralogy; petrographic and micromorphological study of the thin section; scanning electron microscopy (SEM); and both carbon and nitrogen geochemistry and isotopy. The stratigraphy of the Carniça III and Encantada III sambaquis is composed of a sandy nucleus covered with a black organic layer full of shells and anthropic artifacts (black soil, represented as LA facies). In contrast, the Jabuticabeira II sambaqui is characterized by an assorted sequence of shell layers and thin black layers containing burial remains (funerary facies, represented as Lc) covered by black soil, and full of artifacts and burials. According to the facies analysis results, three associations have been found in this sambaqui, from bottom to top: muddy-gravel, muddy-sand and sandy-gravel. The vertical sequence of these associations reflects the progressive aggradation of the lagoon system and it establishes, thus, the relation between the sambaqui and the surrounding depositional environment. The facies associations, in any hierarchy, are limited by the thin layers in the Lc facies. The analysis of the construction materials used in the sambaquis has set their provenance in the nearest depositional features to the sites, represented by the lagoon bottom, margin and swamp for the Jabuticabeira II and Encantada III sambaquis, and by coastal lagoon barriers and superimposed wind dunes for the Carniça III site. The granulometric parameters and the heavy minerals indexes have showed control, mainly geographic, in their distribution. The analysis of phosphate components associated with the carbon and nitrogen isotopic signals shows great anthropic processing in the material which constitutes the funerary and the black soil layers found in the Jabuticabeira II sambaqui, with putrid organic matter characteristics, a probable waste from the day-by-day processing of the people who built the sambaquis. On the contrary, this kind of processing is supposed to have been much lower in the Carniça III and the Encantada III sambaquis.
Rossi, Adriana Rost. "Caracterização paleoambiental a partir dos componentes orgânicos particulados em depósitos bioturbados do Bloco Central da Jazida Carbonífera do Iruí (Cachoeira do Sul, RS)." Universidade do Vale do Rio do Sinos, 2008. http://www.repositorio.jesuita.org.br/handle/UNISINOS/2191.
Full textCoordenação de Aperfeiçoamento de Pessoal de Nível Superior
A análise integrada entre a sedimentologia e a paleoicnologia da Formação Rio Bonito e da base da Formação Palermo (bacia do Paraná) na região de Cachoeira do Sul (RS) vem demonstrando a presença de depósitos flúvio-estuarinos dominados por marés na porção inferior da Formação Rio Bonito, passando a estuarinos dominados por ondas no topo e rapidamente dando lugar a depósitos marinhos rasos (base da Formação Palermo). Visando validar e, se possível, refinar essas interpretações, foi realizada uma análise paleopalinológica de alta resolução dos depósitos bioturbados. Para tanto, foram selecionadas 26 amostras nos testemunhos de sondagem IC-07-RS, IC-44-RS, IC-03-RS e IC-12-RS, pertencentes ao bloco central da jazida carbonífera de Iruí (Cachoeira do Sul, RS), quando da análise paleoicnológica. Das amostras inicialmente coletadas, foram utilizadas para a análise paleopalinológica apenas as de natureza pelítica, de forma a homogeneizar possíveis disparidades na assembléia orgânica decorrentes de granulometri
The integrated analysis of sedimentology and paleoichnology of the Rio Bonito Formation and the lower part of Palermo Formation (Paraná Basin) in Cachoeira do Sul region (Rio Grande do Sul State, south Brazil) revealed that the Rio Bonito Formation are characterized at the base by tide-dominated fluvio-estuarine deposits, changing upward to wave-dominated estuarine deposits, which are overlapped by the shallow marine deposits of the Palermo Formation. With the aim of refine such interpretations, a high-resolution paleopalynologic analysis of the bioturbed deposits is conducted in this study. Thus, 26 samples were selected from the cores IC-07-RS, IC-44-RS, IC-03-RS and IC-12-RS, from the central area of the Iruí Quarry (Cachoeira do Sul). Only mudstones and siltstones samples were used for the paleopalynologic analysis, in order to homogenize possible disparities in the organic assemblage due to the grain-size. Paleopalynomorph and palynofacies samples were prepared following the traditional methods for Pa
Sellén, Emma. "Quaternary paleoceanography of the Arctic Ocean : A study of sediment stratigraphy and physical properties." Doctoral thesis, Stockholms universitet, Institutionen för geologi och geokemi, 2009. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-30895.
Full textAt the time of the doctoral defense, the following papers were unpublished and had a status as follows: Paper 3: In progress. Paper 4: In progress. Paper 5: In progress. Paper 6: In progress.
Tognoli, Francisco Manoel Wohnrath [UNESP]. "Estratigrafia das seqüências deposicionais do grupo Guatá, borda leste da Bacia do Paraná." Universidade Estadual Paulista (UNESP), 2006. http://hdl.handle.net/11449/102978.
Full textAgência Nacional do Petróleo, Gás Natural e Biocombustíveis (ANP)
O Grupo Guatá foi alvo de um estudo detalhado ao longo de toda a borda leste da Bacia do Paraná. Por meio da análise e descrição seqüencial de testemunhos e integração com dados de perfis, aproximadamente 100 poços foram analisados desde o norte do Estado do Paraná até a região centro-sul de Santa Catarina. As fácies foram agrupadas em sucessões de fácies, a partir das quais foram definidos os padrões de empilhamento do tipo progradante, retrogradante e agradante, que em conjunto definem os tratos de sistemas e conseqüentemente as seqüências deposicionais. Além disso, foi realizado um estudo de integração entre sedimentologia, icnologia e geoquímica, que definiu critérios para a identificação e interpretação de superfícies com significado estratigráfico regional. Isso possibilitou correlacionar com segurança poços ao longo de toda a borda leste da Bacia do Paraná e mapear a distribuição das seqüências deposicionais de 3ª.e 4ª ordens. O arcabouço estratigráfico revelou que as seqüências são formadas pelos tratos de sistemas transgressivo e de mar alto ou apenas pelo trato de sistemas transgressivo. Notou-se também que as seqüências estão diretamente vinculadas aos principais lineamentos estruturais da bacia. Interpreta-se que as seqüências 1, 2, 3, 4 e 5 foram soerguidas ao longo de toda a borda leste da Bacia do Paraná, com sua expressão máxima na região do Arco de Ponta Grossa. Esse soerguimento gerou uma discordância angular com expressão regional sobre a qual foram depositadas as seqüências 6, 7 e 8. A seqüência 8 é marcada por subsidência entre os Alinhamentos do Rio Piquiri e São Jerônimo-Curiúva, contemporânea à deposição dos tratos de sistemas transgressivo e de trato de mar alto.
The Guatá Group was target of a detailed study along the eastern border of the Paraná Basin. Using integration of core description and well logs, approximately 100 wells were analyzed in Paraná and Santa Catarina states. Facies were grouped in facies successions, which allowed the recognition of the progradational, retrogradational and aggradational stacking patterns and, consequently, system tracts and depositional sequences. Moreover, it was performed an integration among sedimentology, ichnology and geochemistry as a way to obtain criteria for identifying and interpreting regional stratigraphic surfaces. This allowed a detailed correlation along the eastern border of Paraná Basin and the mapping of third and fourth order sequences. The stratigraphic framework has revealed sequences formed either by the transgressive and highstand system tracts or just by the transgressive one. The sequences are directly linked to the main structural linements of the basin. It is interpreted that sequences 1, 2, 3, 4 and 5 were uplifted along the eastern border of the basin, with the maximum expression in the region of the Ponta Grossa Arch. An angular unconformity was generated and sequences 6, 7 and 8 were deposited later in time. Sequence 8 was affected by subsidence between the Rio Piquiri and São Jerônimo-Curiúva linements, contemporaneous to deposition of the transgressive and highstand system tracts.
Ferreira, Manuela Pinheiro. "Geocronologia e proveniência dos sedimentos holocênicos da confluência dos rios Negro e Solimões, AM." Universidade de São Paulo, 2013. http://www.teses.usp.br/teses/disponiveis/44/44141/tde-14112013-102806/.
Full textThe Amazon river system is the largest sediment catchment basin in the world. In this context, this study aims to differentiate the sands carried by the Negro and Solimões rivers and estimate the sandy sedimentary supply derived from these two rivers to the Amazon river. Furthermore, this research also deals with temporal variations of fluvial geomorphology in the confluence area of the Negro and Solimões rivers. For this purpose, we used methods of geomorphological, facies and grain size analysis coupled with optically stimulated luminescence (OSL) sensitivity of sand fraction and OSL and 14 C dating. The sediments of the Negro river bars showed a higher percentage of sand, with mean diameter of 375,76 µm, which are dominated by quartz grains with moderate OSL sensitivity (3,06). On the other hand, sediment from bars of Solimões and Amazonas rivers are thinner, with mean diameter of 154,58 µm and 134,36 µm, respectively, high percentage of feldspar and quartz grains with low OSL sensitivity (2,49 and 2,53, respectively). The contribution of Solimões river sands (98.23%) to the Amazon river is dominant in relation to the contribution of the Negro river (1.76%). OSL sensitivity data suggest that the Negro river sediments are accommodated mainly in the Amazon River channel. The Alter of Chão Formation sandstones outcropping adjacent to the lower Negro river channel area represent the main source of sediments for this sector of the Negro river. The low compositional maturity and reduced OSL sensitivity of Solimões river sediments suggest rapid sediment transport from Andean source areas. The minimum storage time for the Negro river sand bars exposed during the dry season varies between 0,34 ± 0,04 ky and 1,7 ± 0,26 ky. The minimum storage time of sands in bars from the Solimões and Amazonas rivers ranged between 1,3 ± 0,21 ky and 11,9 ± 1,18 ky. The main construction phases of the Solimões and Amazonas rivers bars would be related to extreme precipitation events during the Holocene.
Martins, Patrícia Diniz. "Estimativa da concentração de sedimentos utilizando a teoria da entropia." Universidade de São Paulo, 2016. http://www.teses.usp.br/teses/disponiveis/18/18139/tde-12122016-112951/.
Full textThe concern about quality of water has been promoting the development of each day better monitoring and control techniques. As sediments transport most water contaminants, their study is fundamental. Given the large number of variables for determining sediment concentration and high costs of monitoring campaigns, it becomes necessary to develop more accessible methods which bring satisfactory practical results. Therefore, this work deals with application of the theory of entropy, a probabilistic method to determine concentration of sediments in river channels with various concentrations and particle sizes. For this purpose, it was proposed a relationship between the theory of entropy parameters in order to reduce the computational effort. The results were satisfactory at concentrations above 10 g/L with R² greater than 0.88. The calculated squared errors in this study were lower than those found when using the theory of entropy by Tsallis and the equation of Rouse, classic models for determining the sediment concentration profile. The technique was also applied to downstream and inside the Mogi reservoir. It can be observed that it is possible to apply the theory of entropy to simulate sediment concentration profile of reservoirs, since the use of the relationship between parameters facilitates calculations, reduces the number of modeled parameters and consequently the computational effort as well as better represents the variation of sediment concentration along the profile. The applicability of the proposed model and the ease of using the probabilistic method, since it does not need provide data of hydraulic bed conditions not even grain size, make it feasible.
Herries, Robert David. "Sedimentology of continental erg-margin interactions." Thesis, University of Aberdeen, 1992. http://digitool.abdn.ac.uk/R?func=search-advanced-go&find_code1=WSN&request1=AAIU045051.
Full textGodoy, Mario Duarte Pinto. "MudanÃas na sedimentaÃÃo no estuÃrio do rio Jaguaribe (CE) devido a mudanÃas nos usos do solo." Universidade Federal do CearÃ, 2011. http://www.teses.ufc.br/tde_busca/arquivo.php?codArquivo=5972.
Full textThe Jaguaribe river is the river with the biggest whatershed of Cearà and has a catchment area of 75,000 km  which occupies over 50% of the state, however, land use changes that occurred in the watershed of this river and global climate change could be causing the decrease of the depth of the estuary which can make impossible for ship to navigate in the estuary and affect the aquatic fauna. The focus of this study is the deposited sediment in islands within the estuary and the surrounding areas which were considered as possible sources of sediment to these islands. The sampling plan consisted in 6 point within the estuary of the Jaguaribe river where were taken sediment cores and further 8 points where were taken superficial sediment from the bottom of the river, from areas in the margin of the estuary and from the dune fields near the estuary. The sampling locals were chosen based on the mapping of the estuary, this mapping used images from the satellites Landsat 5, Quickbird II and Kompsat 2 and cover the period of time between the years of 1988 and 2008. This mapping showed that the existing islands in the estuary suffered great changes during this period, overall there was an increase of 31.5 hectares in the area colonized by mangrove vegetation in the islands. The period of greatest growth was the period between 1992 and 2003 where there was an increase of 6 hectares with a speed of 2.1 hectare per year. In addition to mapping was performed an estimative of sediment load from various land uses in the watershed of the lower estuary, the estimative showed that the main activities that contribute sediment to the estuary is agriculture (282,322 t / year), with the main contribution being from plantations of beans, cassava and corn. Following are the urban areas (115,076 t / year), the shrimp farms (13,475 t / year) and livestock (1,374 t / year). Unlike all the other activities found in the study area, shrimp farming is the only activity in which the sediment load is released directly into the estuary. The diameter of the sediment from the samples showed a predominance of sand on the other classes and also showed that in a same profile may be different types of sediment, with layers with large amounts of silt and clay and layers formed primarily of coarser grains, the appearance of this sediment is similar from the sediment removed from the margin of the estuary and indicates that the several areas of erosion found scattered along the margin of the river may be possible source of great importance within this context.
Books on the topic "Sedimentology"
Chamley, Hervé. Sedimentology. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-75565-1.
Full textMaurice, Renard, ed. Sedimentology. Lisse: A.A. Balkema, 2002.
Find full textCojan, Isabelle. Sedimentology. Lisse: Balkema, 2000.
Find full textLewis, Douglas W., and David McConchie. Practical Sedimentology. Boston, MA: Springer US, 1994. http://dx.doi.org/10.1007/978-1-4615-2634-6.
Full textLewis, Douglas W., and David McConchie. Analytical Sedimentology. Boston, MA: Springer US, 1994. http://dx.doi.org/10.1007/978-1-4615-2636-0.
Full textChamley, Hervé. Clay Sedimentology. Berlin, Heidelberg: Springer Berlin Heidelberg, 1989. http://dx.doi.org/10.1007/978-3-642-85916-8.
Full textDavid, McConchie, ed. Analytical sedimentology. New York: Chapman & Hall, 1994.
Find full textChris, Perry, and Taylor Kevin, eds. Environmental sedimentology. Malden, MA: Blackwell Pub., 2007.
Find full textW, Tillman Roderick, Weber K. J, and Society of Economic Paleontologists and Mineralogists., eds. Reservoir sedimentology. Tulsa, Okla., U.S.A: Society of Economic Paleontologists and Mineralogists, 1987.
Find full textZimmerle, Winfried. Petroleum sedimentology. Dordrecht: Kluwer Academic Publishers, 1995.
Find full textBook chapters on the topic "Sedimentology"
Adelsberger, Katherine A. "Sedimentology." In Encyclopedia of Geoarchaeology, 764–72. Dordrecht: Springer Netherlands, 2016. http://dx.doi.org/10.1007/978-1-4020-4409-0_160.
Full textLiu, Zhifei, Wei Huang, Jianru Li, Pinxian Wang, Rujian Wang, Kefu Yu, and Jianxin Zhao. "Sedimentology." In The South China Sea, 171–295. Dordrecht: Springer Netherlands, 2009. http://dx.doi.org/10.1007/978-1-4020-9745-4_4.
Full textPande, Chaitanya B. "Sedimentology." In Geology, Petrography and Geochemistry of Basaltic Rock in Central India, 151–87. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-30574-0_5.
Full textLewis, Douglas W., and David McConchie. "Borehole Sedimentology." In Analytical Sedimentology, 182–97. Boston, MA: Springer US, 1994. http://dx.doi.org/10.1007/978-1-4615-2636-0_10.
Full textCosta, Pedro J. M., and S. Dawson. "Tsunami Sedimentology." In Encyclopedia of Complexity and Systems Science, 1–17. Berlin, Heidelberg: Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-642-27737-5_646-1.
Full textCosta, Pedro J. M., and S. Dawson. "Tsunami Sedimentology." In Complexity in Tsunamis, Volcanoes, and their Hazards, 135–51. New York, NY: Springer US, 2021. http://dx.doi.org/10.1007/978-1-0716-1705-2_646.
Full textChamley, Hervé. "Origin of Sedimentary Components." In Sedimentology, 1–45. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-75565-1_1.
Full textChamley, Hervé. "Properties of Sedimentary Particles." In Sedimentology, 47–59. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-75565-1_2.
Full textChamley, Hervé. "Deposition of Sediments." In Sedimentology, 61–103. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-75565-1_3.
Full textChamley, Hervé. "From Sediment to Sedimentary Rock." In Sedimentology, 105–30. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-75565-1_4.
Full textConference papers on the topic "Sedimentology"
Shugar, Dan H. "ROCK AVALANCHE SEDIMENTOLOGY AND GEOMORPHOLOGY." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-299195.
Full textZeng, Hongliu, John A., Katherine G. Jackson, and Bingheng Yuan. "Seismic sedimentology: Concepts and challenges." In Beijing 2009 International Geophysical Conference and Exposition. Society of Exploration Geophysicists, 2009. http://dx.doi.org/10.1190/1.3603805.
Full textHurst, A., B. Cronin, and C. Ball. "Seismic Sedimentology of a Submarine Channel System." In 62nd EAGE Conference & Exhibition. European Association of Geoscientists & Engineers, 2000. http://dx.doi.org/10.3997/2214-4609-pdb.28.x7.
Full textPalaparthi, Jyothirmayi, and Tiffany Roberts Briggs. "INFLUENCE OF SEDIMENTOLOGY ON BEACH SUBSTRATE TEMPERATURES." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-357959.
Full textGorbovskaia, O. A., S. V. Parnachev, B. V. Belozerov, and A. S. Bochkov. "Optimization of Core Sampling Program for Selected Sedimentology." In 6th Saint Petersburg International Conference and Exhibition. Netherlands: EAGE Publications BV, 2014. http://dx.doi.org/10.3997/2214-4609.20140246.
Full textMijnssen, F. C. J., K. J. Weber, F. J. T. Floris, and E. F. Kaasschieter. "Relating Sedimentology to Production Behaviour In Deltaic Rocks." In European Petroleum Conference. Society of Petroleum Engineers, 1990. http://dx.doi.org/10.2118/20946-ms.
Full textYal Khattab, N. F. N. "Sedimentology of Semanggol Formation at Pokok Sena, Kedah." In EAGE-GSM 2nd Asia Pacific Meeting on Near Surface Geoscience and Engineering. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201900407.
Full textMallet, J. L., and A. Shtuka. "Stratigraphic inversion integrating wells, seismic & sedimentology data." In SEG Technical Program Expanded Abstracts 1997. Society of Exploration Geophysicists, 1997. http://dx.doi.org/10.1190/1.1885736.
Full textLiu, Lihui, Bin Li, and Handong Zhu. "Application of seismic sedimentology in turbidite fan's study." In Beijing 2009 International Geophysical Conference and Exposition. Society of Exploration Geophysicists, 2009. http://dx.doi.org/10.1190/1.3603682.
Full textHAUPTMAN, LEANNE, and TIFFANY ROBERTS BRIGGS. "GEOMORPHOLOGY AND SEDIMENTOLOGY INFLUENCES ON SEA TURTLE HABITAT." In Coastal Sediments 2023. WORLD SCIENTIFIC, 2023. http://dx.doi.org/10.1142/9789811275135_0019.
Full textReports on the topic "Sedimentology"
Jenner, K. A., and S. M. Blasco. Sedimentology. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132220.
Full textGirard, I., R. A. Klassen, and R. R. Laframboise. Sedimentology Laboratory manual, Terrain Sciences Division. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2004. http://dx.doi.org/10.4095/216141.
Full textCragin, Melissa. Carbonate Sedimentology - University of Illinois Urbana-Champaign. Purdue University Libraries, October 2009. http://dx.doi.org/10.5703/1288284315001.
Full textRicketts, B. D. Sedimentology of the Lower Bowser Lake Group, B.c. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131225.
Full textWaldron, J. W. F., and L. R. Jensen. Sedimentology of the Goldenville formation, eastern shore, Nova Scotia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/120314.
Full textHiggs, R. Cretaceous and Tertiary sedimentology, Queen Charlotte Islands, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/122718.
Full textYeager, Kevin M. Floodplain sedimentology and sediment accumulation assessment – Savannah River Site. Office of Scientific and Technical Information (OSTI), January 2016. http://dx.doi.org/10.2172/1234549.
Full textSyvitski, J. P. M., and D. B. Praeg. Sedimentology of Arctic fjords experiment: data report, volume 3. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/130318.
Full textSyvitski, J. P. M., C. T. Schafer, K. W. Asprey, F. J. Hein, G D Hodge, and R. Gilbert. Sedimentology of Arctic fjords experiment: PA-85-062 expedition report. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/130052.
Full textRiediger, C. L., and J. C. Harrison. Stratigraphy and sedimentology of the Canyon Fiord formation, Melville Island. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/194019.
Full text