Relevant bibliographies by topics / Sedimentological

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Sedimentological'

Author: Grafiati
Published: 4 June 2021
Last updated: 31 January 2023

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Journal articles on the topic "Sedimentological"

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SMEESTERS, An, Philippe MUCHEZ, and Luc HANCE. "Sequence stratigraphical study of the Tournaisian strata in Belgium and Southern China." Geologica Belgica 3, no. 3-4 (October 1, 2001): 285–307. http://dx.doi.org/10.20341/gb.2014.034.

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Strata of late Devonian and Tournaisian age in Belgium and Southern China were studied sedimentologically. This detailed study integrated into a biostratigraphical framework, based on foraminiferal zonation, allowed the construction of a sequence stratigraphical model for both areas. Based on these models a correlation on the scale of third order sequences between these two widely separated depositional environments can be made. This indicates the eustatic nature of the sea-level changes that caused the sedimentological changes during the Tournaisian.
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Nenadic, Drazenko, Vladimir Simic, and Slobodan Knezevic. "Stratigraphical and Lithological characteristics of Preloess sediments in Eastern Srem, Serbia." Annales g?ologiques de la Peninsule balkanique, no. 64 (2002): 53–62. http://dx.doi.org/10.2298/gabp0264053n.

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In the area of Eastern Srem Pleistocene sediments cover large territories. Their facial diversity and very complex interrelations of lithological units are one of the important features of this part of the Pannonian basin. Study of stratigraphic, lithologic, sedimentologic and mineralogic characteristics of these deposits from boreholes in Zemun, Indjija, Cortanovci and Ruma led to conclusion that the interaction of tectonic and climatic changes, as well as difference in sedimentological environments, caused formation of genetically different lithostratigraphic units.
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Begma, D. S., and V. A. Belkina. "LITOLOGICAL CHARACTERISTIC OF ONE OF LAYERS OF UPPERJURASSIC SEDIMENTS OF THE T FIELD." Oil and Gas Studies, no. 4 (September 1, 2017): 7–13. http://dx.doi.org/10.31660/0445-0108-2017-4-7-13.

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The relevance of the discussed issue is predetermined by the fact that almost all geological issues are solved on the basis of the models, which accuracy increases considerably, when using sedimentological component. Sedimentological factors control the conditions of formation, placement and quality of a reservoir and caps. It means that consideration of sedimentological models increases the efficiency of exploration for oil and gas, particularly the preparation of sediments for development and their operational drilling.
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Webb, Esmee. "Sand traps for the unwary - problems in the interpretation of sedimentological analyses." Queensland Archaeological Research 9 (December 1, 1992): 43. http://dx.doi.org/10.25120/qar.9.1992.110.

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The principles of sedimentology are briefly described. Four recently published archaeological reports containing sedimentological analyses are critically reviewed and it is suggested that they could all have been improved if the archaeologists who undertook them had discussed their investigations with a sedimentologist before beginning laboratory work. Finally, reference is made for comparative purposes to some sedimentological work recently undertaken in Western Australia and a plea is entered that archaeologists familiarise themselves with the full range of sedimentological techniques before undertaking their own analyses.
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Ares, María Guadalupe, Fabricio Bongiorno, Mauro Holzman, Celio Chagas, Marcelo Varni, and Ilda Entraigas. "Water erosion and connectivity analysis during a year with high precipitations in a watershed of Argentina." Hydrology Research 47, no. 6 (February 8, 2016): 1239–52. http://dx.doi.org/10.2166/nh.2016.179.

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Soil erosion is a global concern because of its consequences for the environment and the economy of countries. In the Argentine Pampas Region, soil erosion process is a priority issue, although there is little information about sediment concentration (SC) in agricultural catchments. The study aimed at assessing the factors that have a major influence on SC and discussing the dynamics of hydrological and sedimentological connectivity during 2012, a year with precipitation over the mean and significant erosive events. The study was conducted in a watershed of Buenos Aires province, Argentina. A linear regression model, that considered autocorrelation, was obtained. Maximum rainfall intensity in 30 minutes and peak flow were related to SC. An analysis of satellite images was carried out to discuss the hydrological connectivity, and a connectivity index was calculated to assess changes in sedimentological connectivity. The analyses suggested increments in hydrological and sedimentological connectivity, associated with the drainage area expansion and with water erosion rills. Hydrological connectivity is needed for sedimentological connectivity. However, increments in sedimentological connectivity may have been conditioned by the input of energy to detach and to transport particles. This may have been evidenced when flows exceeded a threshold runoff coefficient.
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Kanai, Yutaka. "Sedimentological studies using beryllium isotopes." Journal of the Sedimentological Society of Japan 73, no. 1 (2014): 19–26. http://dx.doi.org/10.4096/jssj.73.19.

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Benton, Michael J. "Ichnology: Sedimentological use of dinosaurs." Nature 321, no. 6072 (June 1986): 732. http://dx.doi.org/10.1038/321732a0.

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C., Burton, Rosenbaum M., and Stevens R. "Sedimentological considerations for predictive modelling." Bulletin of Engineering Geology and the Environment 61, no. 2 (May 1, 2002): 129–36. http://dx.doi.org/10.1007/s100640100128.

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SÜRÄINFN, ARI. "Sedimentological aspects in archaeological contexts." Boreas 16, no. 3 (January 16, 2008): 248. http://dx.doi.org/10.1111/j.1502-3885.1987.tb00093.x.

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Benn, Douglas I. "Glacial sedimentological research in Scotland." Scottish Geographical Magazine 112, no. 1 (March 1996): 57–61. http://dx.doi.org/10.1080/00369229618736980.

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Dissertations / Theses on the topic "Sedimentological"

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Russell, Andrew J. "The geomorphological and sedimentological effects of jokulhlaups." Thesis, University of Aberdeen, 1991. http://digitool.abdn.ac.uk/R?func=search-advanced-go&find_code1=WSN&request1=AAIU045907.

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The aim of this study was to test a predictive model of the geomorphological and sedimentological effects of floods resulting from the sudden drainage of ice-dammed lakes (jokulhlaups). A process-based, conceptual model for channel and sedimentary characteristics was tested within a jokulhlaup routeway near Sondre Stromfjord, west Greenland. River channel change resulting from a jokulhlaup monitored in 1987 was studied in three channel types along the flood routeway: deltaic, high gradient bedrock-controlled, and low gradient confined valley sandur. Flood powers, sediment supply and channel resistance to erosion were found to vary considerably between the channel types. Consequently, amounts of channel change and the character of the sedimentary record showed extreme variation. In addition, parts of the jokulhlaup channel which experienced backwater effects may have experienced two sediment transport peaks. Variations between the character of deposits found within each of the three channel types reflect local differences in sediment supply, stream power and channel resistance to erosion. Deposition in the delta and the sandur records sedimentation related to a number of jokulhlaups, whilst the spillway and the bedrock-confined channel provide a record of the action of the last jokulhlaup as low stage deposits, as well as that of the earliest flood events as high stage deposits. This study has shown that it is possible to predict the morphology of channel macroforms. The internal structure of these macroforms is strongly dependent upon both the amount and character of sediment supplied to the channel during a jokulhlaup. The more detailed the knowledge of the controlling variables for any one channel, the more detailed the resulting predictions are. At present, the model concerns only the products of turbulent, Newtonian, water floods. It may, however, be possible to predict thresholds marking the transition to non-Newtonian flows where sediment supply conditions and hydrograph characteristics are known. The model may also be used in reverse to reconstruct the magnitude and frequency of former jokulhlaups where sufficient geomorphological and sedimentary evidence is available.
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Dutson, Andrew S. "A Multifaceted Sedimentological Analysis on Hobble Creek." BYU ScholarsArchive, 2011. https://scholarsarchive.byu.edu/etd/2625.

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Due to the endangerment of the June sucker (Chasmistes liorus), the lower two miles of Hobble Creek, Utah has been the focus of several restoration efforts. The portion of the creek between Interstate 15 and Utah Lake has been moved into a more "natural" channel and efforts are now being made to expand restoration to the east side of the freeway. This thesis reports on three different parts of a sedimentological analysis performed on Hobble Creek. The first part is a data set that contains information about the particle size distribution on the bed of Hobble Creek between 400 W and Interstate 15 in Springville, Utah. Particle size distributions were obtained for eleven sub-reaches within the study section. Particle size parameters such as D50 were observed to decrease from an average of 72 mm to 24 mm downstream from the 1650 W crossing and Packard Dam. Streambed armoring was observed along most of the reach. This data set can be used as input for PHABSIM software to determine the location and availability of existing spawning material for June sucker during a range of flows. The second part of this thesis compares predictions from four bed-load transport models to bed-load transport data measured on Hobble Creek. In general, the Meyer-Peter, Muller and Bathurst models overpredicted sediment transport by several orders of magnitude while the Rosgen and Wilcock methods (both calibrated models) were fairly accurate. Design channel dimensions resulting from the bed-load transport predictions diverged as a function of discharge. Once validated, the models developed in this section can be used by design engineers to better understand sediment transport on Hobble Creek. The models may also be applied to other Utah Lake tributaries. The third section of the thesis introduces a detailed survey data set that covers the Hobble Creek floodplain on the shifted section between Interstate 15 and Utah Lake with an approximate 10 foot resolution grid. Water surface elevations at two flows, along with invert, fence, saddles, and other points, are labeled in the survey. A comparison with a survey completed last year did not reveal any significant lateral changes caused by the 2010 spring runoff. Due to the potential importance of the side ponds to June sucker survival, this data set can be used to monitor sedimentation in the side ponds. It may also be used in a GSSHA model to determine the magnitude of flow that is required before each side pond will be connected to the main channel.
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Nelson, Anna Elizabeth. "A sedimentological investigation of glacigenic deposits in Iceland." Thesis, University of Cambridge, 2006. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.613671.

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Hutchison, Matthew P. "The sedimentological & petrophysical characterisation of dryland mudstones." Thesis, University of Aberdeen, 2014. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=210857.

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Sjunneskog, Charlotte. "Diatom and Sedimentological Investigations on West Antarctic Shelf Sediment." Doctoral thesis, Uppsala : Acta Universitatis Upsaliensis : Univ.-bibl. [distributör], 2002. http://publications.uu.se/theses/91-554-5256-6/.

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Orlowski, R. J. "A sedimentological profile of the Pahau Terrane type locality." Thesis, University of Canterbury. Geology, 2001. http://hdl.handle.net/10092/7121.

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The Pahau Terrane as part of the Torlesse Superterrane extends for over 30% of the New Zealand landmass. Although an unofficial type locality around the Pahau River has been proposed, it has never been adequately described or defined. One of the main goals of this research was to describe in detail the deposits of the Pahau River area in order to define the type locality. In total ~900m of section was logged describing four lithofacies; mudstone, interbedded mudstone - sandstone, sandstone, and conglomerate. Two formation names and a group name are proposed and intended for widespread use. The Mt Saul Formation is proposed for coarse-grained conglomeratic lithofacies whereas the Ship Spur Formation is proposed for the combined fine-grained sedimentary lithofacies. The Pahau River Group encompasses these formations. Stratigraphic logs clearly show coarsening and thickening upward, progradational sequences, at the tops of which either highly carbonaceous beds or rootlets can be observed. The bedding in the conglomerate lithofacies are dominated by bedload transport structures including large scale cross stratification, imbrication and clast support. Micro and macrofossil collection suggest a nearshore marine sequence yet rootlets suggest subaerial indicating a range from fully marine to terrestrial depositional environments, making them the only known terrestrial deposits in the Pahau Terrane. This suggests a fan-delta depositional setting. Very few bi-directional structures were observed, suggesting that these deposits were not influenced by wave reworking and tidal currents to any great degree but are fluvially dominated. Thin section analysis of fine to medium sandstones suggests a transitional to mixed arc provenance. Measurable indicators suggest a palaeoflow direction towards the east to northeast. These results are similar to previous studies indicating the suitability of the Pahau River area as a type locality for the Pahau Terrane.
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Newell, Andrew John. "Sedimentological controls on vertebrate taphonomy in Triassic fluvial environments." Thesis, Queen's University Belfast, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.317467.

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Smith, R. D. A. "A sedimentological analysis of the late LLandovery Welsh Basin." Thesis, University of Cambridge, 1988. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.234921.

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An integrated, multidisciplinary basin analysis has been carried out for an approximately isochronous stratal interval of the Silurian fill of the Welsh Basin. The selected interval is the Upper Llandovery griestoniensis Chronozone which represents a time interval of probably less than one million years. Two mapped areas with contrasting structural styles illustrate the heterogeneous response of the basin-fill to basin inversion and shortening. One major Welsh structure, the Central Wales Synclinorium, is shown to be related to a long-lived structural discontinuity which significantly influenced early Silurian sedimentation patterns. During extension/transtension in the basin this structure, as the edge of a tilted fault block, formed a palaeohigh. Turbidite systems were confined to either side and were ponded in relatively small-scale sub-basins defined by the tilted fault block geometry. In basinal facies of griestoniensis Zone age four major lithofacies associations are recognized: the channel-lobe transition, sandstone lobe, lobe fringe, and lateral basin-slope facies associations. They represent deposits of the outer area of a moderately large (minimum length of 100 km), elongate turbidite system and its bounding slope. Large scale erosional structures, filled with conglomerates and pebbly sandstones, occur in the more proximal areas of exposure. They are either channels or huge scours excavated by large volume turbidity currents undergoing hydraulic jumps. Lateral facies variations in sandstone lobes reflect down-system and cross-system variations in competence and capacity of flows. Palaeocurrent patterns and inferred onlap relationships reflect confinement by structurally-controlled slopes. Since the system developed during a time of widespread transgression sandstone lobes probably record pulses of rapid tectonic uplift at source. Unconformities, corresponding to times of active growth of depositional sandstone lobes in the basin, were generated on the southern basin margin. Lateral gradients in palaeo-oxygenation of bottom waters and fluctuations in oxicity through time are reconstructed using trace fossil evidence and diagenetic mineral assemblages. Relic downward-migrating oxidation fronts are recorded for the first time from ancient turbidites. A diverse trace fossil assemblage associated with the turbidite system is described and interpreted. Detailed logging through the basinal sequence reveals that times of dysaerobic bottom water conditions, during which turbidites and hemipelagites were reworked by soft-bodied infauna, alternated with periods of bottom water anoxia, during which laminated hemipelagites containing a pelagic fauna of graptolites were preserved. Such alternations may be very rapid, suggesting close proximity of the anoxic-oxic interface to the sediment surface, or may have far longer periodicities, reflecting periods of stable pycnocline development above anoxic bottom waters. Phosphate cements are shown to have initiated very close to the sediment surface beneath oxygen-deficient bottom waters in the basin.
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Santos, Julio Cesar Neves dos. "Hydrological and sedimentological processes in a tropical semiarid climate." Universidade Federal do CearÃ, 2015. http://www.teses.ufc.br/tde_busca/arquivo.php?codArquivo=15010.

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Conselho Nacional de Desenvolvimento CientÃfico e TecnolÃgico
The understanding of processes such as the generation of surface runoff, sediment yield and their relations with the rainfall regime is the basis for the planning and effective management of soil and water resources in a watershed. In this context, the present study aims to identify the main processes that influence the generation of surface runoff and sediment yield in small watersheds, and determine parameters for empirical sedimentological models, as well as the Sediment Delivery Ratio (SDR) for the tropical, semi-arid region of Brazil. The study area is the Iguatu Experimental Basin (IEB), which comprises a watershed of 16.74 km2, three small nested watersheds (from 1 to 3 ha) and three erosion plots of 20 m2. One of the watersheds had been under regenerating Caatinga for 35 years, another subjected to a management, which involved thinning the Caatinga, and the last faced deforestation followed by burning and the cultivation of grass. The period of study was six years (2009 to 2014). Collections to quantify surface runoff and sediment yield were taken for each erosive rainfall event in an accumulated period of 24 hours. Surface runoff in the watersheds was quantified using Parshall flumes, and sediment yield was measured with towers and trenches to collect suspended sediment and bedload. On the watershed scale, runoff was measured by means of a spillway, and sediment yield by a turbidimeter. Cluster analysis was used to determine rainfall regimes and groups of similar rainfall-runoff events. With data from the erosion plots and watersheds, the C factors and coefficients of the Modified Universal Soil Loss Equation (MUSLE) were calibrated and validated. From data measured in the basin, sediment delivery ratios were determined. The occurrence of dry spells and the formation of cracks in the soil were important factors in controlling the generation of runoff and consequently sediment yield. The dry spells made it possible for the soil to dry out, with the formation of cracks, which acted as pathways for preferential flow, generating higher initial abstraction during the start of the rainy season. Changes in ground cover had little influence on accumulated flow, demonstrating that the soil characteristics and conditions as moisture and the presence of cracks, best explain the generation of runoff on expansive soils. The greatest runoff losses in all the watersheds under study were for Rainfall Regime II, characterized by higher depth, intensity and occurrence of the rainfall. For the ground covers under study, values for the C factors and the fit of the coefficients "a" and "b" of MUSLE, proved to be appropriate and recommended according to the statistical indices employed. Values for sediment delivery ratio for individual rainfall events ranged from 0.08 to 1.67%, with an average of 0.68%. In the basin, extreme events may cause high disaggregation of soil particles, but without sufficient transporting energy for dragging the sediment, generating low SDR.
O entendimento de processos como geraÃÃo do escoamento superficial, produÃÃo de sedimentos e suas relaÃÃes com o regime pluviomÃtrico à a base para o planejamento e a gestÃo eficaz dos recursos solo e Ãgua em uma bacia hidrogrÃfica. Nesse contexto, o presente estudo tem como objetivos identificar os principais processos que influenciam a geraÃÃo do escoamento superficial e a produÃÃo de sedimento em pequenas bacias hidrogrÃficas, e calibrar parÃmetros de modelos sedimentolÃgicos empÃricos, bem como a razÃo de aporte de sedimentos (SDR) para a regiÃo semiÃrida tropical do Brasil. A Ãrea de estudo à a Bacia Experimental de Iguatu (BEI), composta de uma bacia de 16,74 km2, trÃs pequenas microbacias aninhadas (de 1 a 3 ha) e trÃs parcelas de erosÃo de 20 m2. Uma das microbacias foi mantida com Caatinga em regeneraÃÃo hà 35 anos, outra submetida ao manejo de raleamento da Caatinga e na Ãltima foi realizado o desmatamento seguido de queimada e cultivo de capim. O perÃodo de estudo foi de seis anos (2009 a 2014). As coletas para quantificaÃÃo do escoamento superficial e da produÃÃo de sedimentos foram realizadas a cada evento de chuva erosiva, no acumulado de 24 horas. O escoamento superficial nas microbacias foi quantificado atravÃs de calhas Parshall e as produÃÃes de sedimentos foram mensuradas atravÃs de torres e fossos coletores de sedimentos em suspensÃo e arraste. Na bacia de 16,74 km2, o escoamento superficial foi mensurado por meio de um vertedor e a produÃÃo de sedimentos atravÃs de um turbidÃmetro. AnÃlises de agrupamento foram utilizadas para determinaÃÃo de regimes de chuvas e grupos de eventos similares de chuva-deflÃvio. Com dados das parcelas de erosÃo e das microbacias foram calibrados e validados os fatores C e os coeficientes da EquaÃÃo Universal de Perdas de Solo Modificada (MUSLE). A partir dos dados medidos na bacia foram determinadas as razÃes de aporte de sedimentos. A ocorrÃncia de veranicos e a formaÃÃo de fendas no solo foram determinantes no controle da geraÃÃo de escoamento e consequentemente da produÃÃo de sedimentos. A ocorrÃncia de veranicos possibilitou o secamento do solo com a formaÃÃo de fendas, que agem como caminhos preferenciais para o fluxo de Ãgua, gerando elevadas abstraÃÃes inicias durante o inÃcio da estaÃÃo chuvosa. As mudanÃas da cobertura vegetal apresentaram pouca influÃncia sobre o escoamento acumulado, indicando que as caracterÃsticas e condiÃÃes do solo, como umidade e presenÃa de fendas, explicam melhor a geraÃÃo de escoamento em solos expansivos. Maiores perdas por escoamento em todas as microbacias estudadas foram para chuvas do Regime II caracterizado por maiores alturas pluviomÃtricas, intensidades e ocorrÃncias. Quanto aos valores dos fatores C e dos coeficientes de ajuste âaâ e âbâ da MUSLE, para as coberturas estudadas, mostraram-se apropriados e recomendados de acordo com os Ãndices estatÃsticos empregados. Os valores da razÃo de aporte de sedimentos para eventos pluviomÃtricos individuais variaram de 0,08 a 1,67%, com mÃdia de 0,68%. Na bacia, eventos extremos podem causar elevada desagregaÃÃo de partÃculas de solo, mas podem nÃo dispor de energia de transporte suficiente para arrastÃ-las, gerando baixo SDR.
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Al-Washmi, Hamad Abdullah. "St Andrews Bay : a sedimentological, geophysical and morphological investigation." Thesis, University of St Andrews, 1996. http://hdl.handle.net/10023/15558.

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This thesis examines past and present day processes responsible for the morphological development of St Andrews Bay in eastern Scotland. Quaternary glacial events have contributed large volumes of sediment from the Scottish Mainland to the North Sea Basin over the last 3 million years. Since the most recent glacial event, the Late Devensian, which terminated some 14,000 years ago in Scotland, the sediments of the coastal areas have been redistributed by wave and tidal activity. Thus the bathymetry and platform of St Andrews Bay has evolved since that time, although some elements of the morphology appear to predate the last glaciation. The grain size distributions of the bed sediments of the bay show a narrow range of mean sizes between fine and very fine sand. These are indicative of a low energy tidal environment although Quartile Deviation - Median Diameter plots suggest the importance of wave activity in determining their distribution. Current measurements in the bay confirm that the hydrodynamic environment is of low energy with average current speeds rarely exceeding 15 cm s −1 one metre above the bed. Progressive vector plots show closed ellipses during calm weather but meteorological forcing and wave activity generate residual currents predominantly in the direction of wave propagation or down wind. Application of a transfer function to the current data predicts low rates of bedload transport, the residual of which generally accords with the recent pattern of sedimentation at the head of the bay. The rocky platforms of the southern margins of the bay cannot easily be sub-divided into features at different elevations. No firm evidence is presented for a pre-Late Devensian origin of the platform but it is argued that such a chronology explains the morphology of the platform. Offshore sedimentary sequences, up to 30 metres in thickness, are reported from geophysical surveys which have been laid down since the last glaciation. The units identified reflect changing environments of deposition associated with climatic and sea level changes over the last 14,000 years.
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Books on the topic "Sedimentological"

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J, Beven K., Carling Paul, British Geomorphological Research Group, and British Hydrological Society, eds. Floods: Hydrological, sedimentological, and geomorphological implications. Chichester [England]: J. Wiley, 1989.

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Fayazi, Farajollah. Sedimentological studies in the Qom area, Central Iran. Norwich: University of East Anglia, 1991.

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Čáp, Pavel. Microfacies analysis of Silurian and Devonian type sections (Barrandian, Czech Republic). Prague: Czech Geological Survey, 2003.

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International, Sedimentological Congress (13th 1990 Nottingham England). Sediments 1990: 13th International Sedimentological Congress, Nottingham, England, 26th-31st August 1990. Keyworth: British Geological Survey, 1990.

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International Sedimentological Congress (13th 1990 Nottingham, England). Sediments 1990: 13th International Sedimentological Congress, Nottingham, England, 26th-31st August 1990. Keyworth: British Geological Survey, 1990.

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D'Anglejan, Bruno. Potential sedimentological impacts of hydro-electric developments in James Bay and Hudson Bay. Montréal: North Wind Information Services, 1994.

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D'Anglejan, Bruno. Potential sedimentological impacts of hydro-electric developments in James Bay and Hudson Bay. Montréal: North Wind Information Services, 1994.

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International Sedimentological Congress (12th 1986 Canberra, A.C.T.). Sediments down-under: 12th International Sedimentological Congress, Canberra, Australia, 24-30 August 1986 : abstracts. Canberra: The Congress, 1986.

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Ping, Sha Li. Sedimentological studies of the ebb-tidal deltas along the west Frisian Islands, the Netherlands. [Utrecht: Instituut voor Aardwetenschappen der Rijksuniversiteit te Utrecht, 1990.

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Combellick, R. A. Sedimentological and radiocarbon-age data for tidal marshes along eastern and upper Cook Inlet, Alaska. Fairbanks, Alaska: State of Alaska, Dept. of Natural Resources, Division of Geological and Geophysical Surveys, 1994.

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Book chapters on the topic "Sedimentological"

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Catt, J. A., and S. J. Staines. "Sedimentological investigations." In Late Quaternary Environmental Change in North-west Europe: Excavations at Holywell Coombe, South-east England, 69–105. Dordrecht: Springer Netherlands, 1998. http://dx.doi.org/10.1007/978-94-011-4908-2_4.

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Abdullatif, Osman, Mohammad Makkawi, and Mohamed Yassin. "Field Sedimentological Study." In Geological and Geostatistical Aquifer Characterization of Wajid Sandstone, Saudi Arabia, 17–41. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-12191-3_2.

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Orfeo, Oscar, José Stevaux, and Daniel Parsons. "Geomorphological and sedimentological characteristics." In The Paraná River Basin, 42–60. Abingdon, Oxon ; New York, NY : Routledge, 2020. | Series: Earthscan series on major river basins of the world: Routledge, 2020. http://dx.doi.org/10.4324/9780429317729-3.

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Neto, Carlos, Miguel Geraldes, and Diana Almeida. "The Tróia Peninsula—An Aeolian Sedimentological Legacy." In World Geomorphological Landscapes, 99–108. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-319-03641-0_7.

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Bosence, D. W. J. "Stratigraphic and sedimentological models of rift basins." In Sedimentation and Tectonics in Rift Basins Red Sea:- Gulf of Aden, 9–25. Dordrecht: Springer Netherlands, 1998. http://dx.doi.org/10.1007/978-94-011-4930-3_2.

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Kiefert, L., G. H. McTainsh, and W. G. Nickling. "Sedimentological Characteristics of Saharan and Australian Dusts." In Environmental Science and Technology Library, 183–90. Dordrecht: Springer Netherlands, 1996. http://dx.doi.org/10.1007/978-94-017-3354-0_17.

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Bjørlykke, Knut Olav. "Chemical and Mineralogical Factors Which Influence Sedimentological Processes." In Sedimentology and Petroleum Geology, 112–25. Berlin, Heidelberg: Springer Berlin Heidelberg, 1989. http://dx.doi.org/10.1007/978-3-642-72592-0_6.

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Friedman, Gerald M. "Gulf of Elat (Aqaba) Geological and Sedimentological Framework." In Hypersaline Ecosystems, 39–71. Berlin, Heidelberg: Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-642-70290-7_6.

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Torres, Nalini, and Danny W. Harrelson. "The Great Red River Raft and its Sedimentological Implications." In Reconstructing Human-Landscape Interactions - Volume 1, 35–55. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-23759-1_4.

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Mann, Ulrich. "Sedimentological and Petrophysical Aspects of Primary Petroleum Migration Pathways." In Sediments and Environmental Geochemistry, 152–78. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-75097-7_9.

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Conference papers on the topic "Sedimentological"

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Mezghani, Mokhles, and Mohammed Masrahy. "Digital Sedimentological Core Description Through Machine Learning." In Abu Dhabi International Petroleum Exhibition & Conference. Society of Petroleum Engineers, 2020. http://dx.doi.org/10.2118/203341-ms.

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Mingjun*, Su, Liu Huaqing, and Yuan Shuqin. "Isochronous seismic lithosomic body and sedimentological analysis." In SEG Technical Program Expanded Abstracts 2014. Society of Exploration Geophysicists, 2014. http://dx.doi.org/10.1190/segam2014-0103.1.

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Charara, M., and N. Rabadi. "Lithological and Sedimentological Evaluation Using Computerized Interpretation Programs." In Middle East Oil Show. Society of Petroleum Engineers, 1987. http://dx.doi.org/10.2118/15731-ms.

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Narro Perez, Rodrigo, Carolyn H. Eyles, and Rebecca E. Lee. "SEDIMENTOLOGICAL ANALYSIS OF A LATERAL MORAINE, GÍGJÖKULL, ICELAND." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-358574.

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Gendel, D. L., and A. V. Maksimenko. "Sedimentological Features of Jurassic Deposits of Novoportovskoe Field." In Tyumen 2013 - New Geotechnology for the Old Oil Provinces. Netherlands: EAGE Publications BV, 2013. http://dx.doi.org/10.3997/2214-4609.20142670.

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Kedzierski, P., J. L. Mallet, and G. Caumon. "Combining Stratigraphic and Sedimentological Information for Realistic Facies Simulations." In EAGE Conference on Petroleum Geostatistics. European Association of Geoscientists & Engineers, 2007. http://dx.doi.org/10.3997/2214-4609.201403080.

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Schulze, Nina Sabine Margarete, Jonathan Woodruff, Kinuyo Kanamaru, and Hannah Baranes. "SEDIMENTOLOGICAL SIGNATURES OF REGIONAL SEISMICITY IN WESTERN SHIKOKU, JAPAN." In 51st Annual Northeastern GSA Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016ne-272895.

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Pojar, Iulian, Bogdan Ispas, Laura Dutu, Andrei Briceag, and Florin Dutu. "SEDIMENTOLOGICAL INVESTIGATIONS ON ST. GEORGE DISTRIBUTARY, DANUBE DELTA, ROMANIA." In 21st SGEM International Multidisciplinary Scientific GeoConference Proceedings 2021. STEF92 Technology, 2021. http://dx.doi.org/10.5593/sgem2021/1.1/s01.017.

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J. Buter, S., D. Mikes, and H. Dronkert. "3D Sedimentological Modelling of Pennsylvanian Fluvio-Deltaic Reservoirs, Kentucky, USA." In 57th EAEG Meeting. Netherlands: EAGE Publications BV, 1995. http://dx.doi.org/10.3997/2214-4609.201409656.

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Haskell, Norman L., Susan E. Nissen, John A. Lopez, and Mike S. Bahorich. "3‐D seismic coherency and the imaging of sedimentological features." In SEG Technical Program Expanded Abstracts 1995. Society of Exploration Geophysicists, 1995. http://dx.doi.org/10.1190/1.1887265.

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Reports on the topic "Sedimentological"

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Binney, W. P. A Sedimentological Investigation of Maclean Channel Transported Sulphide Ores. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/122399.

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Higgs, R. Sedimentological aspects of the Skonun Formation, Queen Charlotte Islands, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127413.

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Wilson, R. C. L. A Reconnaissance Sedimentological Study of the Middle Jurassic Shaunavon Formation, southwestern Saskatchewan. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/130159.

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Devaney, J. R. Sedimentological Highlights of the Lower Triassic Bjorne Formation, Ellesmere Island, Arctic Archipelago. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132544.

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Davis, J. M. A conceptual sedimentological-geostatistical model of aquifer heterogeneity based on outcrop studies. Office of Scientific and Technical Information (OSTI), January 1994. http://dx.doi.org/10.2172/656642.

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Kalkreuth, W., D. A. Leckie, and M. Labonté. Gates Formation [Lower Cretaceous] coals in western Canada: a sedimentological and petrographical study. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/126739.

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Cranston, R. E., and P. D. Standing. Geochemical and Sedimentological Results From Sediment Cores Collected in the Okhotsk / Japan Seas. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/133478.

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Combellick, R. A., and R. D. Reger. Sedimentological and radiocarbon-age data for tidal marshes along eastern and upper Cook Inlet, Alaska. Alaska Division of Geological & Geophysical Surveys, 1993. http://dx.doi.org/10.14509/1622.

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Combellick, R. A., and R. D. Reger. Sedimentological and radiocarbon-age data for tidal marshes along eastern and upper Cook Inlet, Alaska. Alaska Division of Geological & Geophysical Surveys, 1994. http://dx.doi.org/10.14509/2492.

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Rice, R. J., D. G. F. Long, W. K. Fyson, and S. M. Roscoe. Sedimentological Evaluation of Three Archean Metaquartzite - and Conglomerate - Bearing Sequences in the Slave Province, N.W.T. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131268.

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