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Dissertations / Theses on the topic 'Sedimentary environment'

Author: Grafiati

Published: 4 June 2021

Last updated: 26 July 2025

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1

Murdock, Christopher Paul. "A study of '2'1'0Pb in the atmosphere and estuarine sedimentary environment." Thesis, Lancaster University, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.310584.

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2

Forsythe, Joyce Christine. "A study of Foraminifera and their surrounding environment from intertidal sediments in Northern Ireland." Thesis, University of Ulster, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.339336.

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3

Assine, Mario Luis. "Sedimentação na bacia do Pantanal Mato-Grossense, Centro-Oeste do Brasil /." Rio Claro : [s.n.], 2003. http://hdl.handle.net/11449/108382.

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Resumo: O Pantanal é uma bacia sedimentar quaternária localizada na Bacia do Alto Rio Paraguai, na Região Centro-Oeste do Brasil. A sucessão estratigráfica mostra afinamento textural para o topo e preenchimento essencialmente siliciclástico. O trato de sistemas deposicionais é composto por uma planície fluvial meandrante como sistema distal de vários leques aluviais dominados por rios, dos quais o mais notável é o megaleque do rio Taquari. Na paisagem atual há muitas feições geomórficas herdadas de diferentes climas, que produziram registros de uma sucessão de eventos do Pleistoceno ao Holocen

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4

Campbell, Ian D. "Pollen-sedimentary environment relations and late holocene palynostratigraphy of the Ruby Range, Yukon Territory, Canada." Thesis, University of Ottawa (Canada), 1987. http://hdl.handle.net/10393/5188.

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5

Neto, Jose Antonio Baptista. "Sedimentological evidence for human impact on a nearshore sedimentary environment : Jurujuba Sound, Rio de Janeiro State, Brazil." Thesis, Queen's University Belfast, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.286855.

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6

Hernández-Guevara, Norma Angélica. "Distribution and mobility of juvenile polychaeta in a sedimentary tidal environment = Verbreitung und Mobilität juveniler Polychaeten in sandigen Watten /." Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung, 2005. http://www.loc.gov/catdir/toc/fy0605/2005477448.html.

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7

Nwaodua, Emmanuel Chukwukamadu. "Subsurface Facies Analysis of the Rose Run Sandstone Formation in south eastern Ohio." Bowling Green State University / OhioLINK, 2008. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1213202313.

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8

Asiashu, Mudau. "Sedimentological re-interpretation of the early cretaceous oil reservoir in the Northern Bredasdorp Basin, offshore South Africa." University of the Western Cape, 2015. http://hdl.handle.net/11394/5047.

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>Magister Scientiae - MSc<br>This study was aimed at determining the sedimentary environment, its evolution and facies areal distribution of the Upper Shallow Marine (USM, Late Valanginian). The study was conducted in wells E-S1, F-AH4 and E-W1 in the Bredasdorp basin between E-M and F-AH fields, located in a basinwards transect roughly transverse to the palaeocoast. The wells were studied by logging all the cores in detail between the chosen intervals, followed by facies analysis. Each core log was tied with its respective gamma ray and resistivity well logs. The logs were then correlated bas

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9

Abd, Elmola Ahmed. "Deformation conditions and 40Ar/39Ar dating of fault activity registered by phyllosilicates (clay minerals) in a sedimentary environment : examples of the south-verging thrust faults in the Pyrenees." Thesis, Bourgogne Franche-Comté, 2017. http://www.theses.fr/2017UBFCD033/document.

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La chaîne pyrénéenne présente des structures de déformation bien exposées et des roches sédimentaires syntectoniquesbien conservées qui en font un objet idéal pour étudier les failles. En effet, les textures, structures, compositions chimiques etisotopiques enregistrées par le coeur de la faille chevauchante peuvent renseigner sur les conditions et mécanismes de ladéformation et aussi contraindre dans le temps l’activité de la faille étudiée. Dans la présente thèse, trois chevauchements duversant sud Pyrénéen ont été étudiés pour mieux appréhender le comportement mécanique, chimique et isotopi

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10

Banjade, Bharat. "Subsurface Facies Aanalysis of the Cambrian Conasauga Formation and Kerbel Formation in East - Central Ohio." Bowling Green State University / OhioLINK, 2011. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1322525944.

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11

Accarie, Hugues. "Dynamique sedimentaire et structurale au passage plate-forme/bassin : les facies cretaces et tertiaires du massif de la maiella (abruzzes, italie)." Paris, ENMP, 1987. http://www.theses.fr/1987ENMP0056.

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L'etude des series cretacees a tertiaires du massif de la maiella est basee sur la cartographie detaillee du domaine de transition plateforme-bassin et sur le leve d'un certain nombre de coupes. Elle est completee par une etude de la fracturation et de la fraction fine. Ces donnees permettent de proposer un modele d'evolution du domaine depuis le cretace superieur jusqu'au miocene. Quatre grandes discontinuites sedimentaires sont reconnues. L'analyse sedimentologique des ensembles permet de preciser le cadre biostratigraphique, la nature et l'organisation des depots et de reconnaitre les princ

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12

Sin, Fung-siu Iris, and 冼鳳笑. "Offshore sedimentary environments in Mirs Bay, Hong Kong." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 1999. http://hub.hku.hk/bib/B31221610.

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13

Sin, Fung-siu Iris. "Offshore sedimentary environments in Mirs Bay, Hong Kong /." Hong Kong : University of Hong Kong, 1999. http://sunzi.lib.hku.hk/hkuto/record.jsp?B21021181.

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14

Brew, David Scott. "Sedimentary environments and Holocene evolution of the Suffolk estuaries." Thesis, University of East Anglia, 1990. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.235628.

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A stratigraphic investigation of the marshland adjacent to the five main estuaries in Suffolk and offshore of the Alde estuary has been made. The results are used to establish a Holocene evolution for the Suffolk coast and are compared with coastal sequences elsewhere in East Anglia. The stratigraphy of the Blyth estuary in north Suffolk comprises four lithostratigraphic units; a basal freshwater peat overlain by estuarine Lower Clay, Middle Peat and Upper Clay representing two phases of transgressive overlap sandwiching a phase of regressive overlap. Peat formation began about 6750 yrs BP and

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15

Abouessa, Ashour. "Sedimentological and ichnological characteristics of Dur At Tallah siliciclastic rock sequence, and their significance in the depositional environment interpretation of tidal-fluvial system (Upper Eocene, Sirt Basin, Libya)." Phd thesis, Université de Strasbourg, 2013. http://tel.archives-ouvertes.fr/tel-00985603.

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Dur At Talah sedimentary sequence, located at the southern side of the Sirt Basin in central Libya, is composed of 150 m thick of mainly siliciclastic rocks. The importance of this sequence is linked to the importance of the Sirt Basin as one of large hydrocarbon reservoirs in Libya. The sequence is also an excellent site for vertebrate fossils of Late Eocene, the age of the sequence. Previous studies, though very limited compared to the importance of this area, are focused on its paleontological content. Sedimentology received only scant attention before this project. This thesis is an outcro

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16

Woodward, Jamie C. "Late Quaternary sedimentary environments in the Voidomatis Basin, Northwest Greece." Thesis, University of Cambridge, 1990. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.358912.

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17

Vogel, Allan Hayes. "Some Relationships Between Sedimentary Trace Metal Concentrations and Freshwater Phytoplankton and Sedimentary Diatom Species Composition." PDXScholar, 1995. https://pdxscholar.library.pdx.edu/open_access_etds/1295.

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Sediments from 21 Oregon lakes were analyzed for seven metals (Fe, Mn, Zn, Cu, Co, Ni, V) in three forms (exchangeable, organic+sulfides, and oxyhydroxides+ oxides+ carbonates) using a sequential fractionation procedure. The summer epilimnetic filterable concentration of an eighth (Mo) was also determined. Sedimentary diatom remains and summer phytoplankton populations of the lakes were correlated with the 22 metal parameters and with conservative water chemistry parameters, estimators of lake productivity, and watershed geology. Both the sedimentary metals and the two populations of primary p

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18

Roberts, David H. "The development of criteria to distinguish glaciotectonic and glaciomarine sedimentary environments." Thesis, University of Southampton, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.307150.

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19

Watson, Diane F. "Environmental distribution and sedimentary fate of hopanoid biological marker compounds." Thesis, University of Newcastle Upon Tyne, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.246657.

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20

Crook, Nigel Paul. "The application of quantitative environmental magnetic measurements to sedimentary systems." Thesis, Manchester Metropolitan University, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.248812.

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21

Cowan, Greig. "The sedimentary environments and diagenesis of Namurian reservoir sandstones, Trumfleet Field, Yorkshire." Thesis, Imperial College London, 1988. http://hdl.handle.net/10044/1/47009.

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22

Allen, H. D. "Late Quaternary of the Kopais Basin, Greece : Sedimentary and environmental history." Thesis, University of Cambridge, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.383701.

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23

King, D. H. "Modification of sedimentary communities of nitrate-reducing bacteria by environmental perturbations." Thesis, University of Essex, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.373211.

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24

Fryer, Rosemarie. "Quantification of the Bed-Scale Architecture of Submarine Depositional Environments and Application to Lobe Deposits of the Point Loma Formation, California." Thesis, Colorado School of Mines, 2018. http://pqdtopen.proquest.com/#viewpdf?dispub=10844938.

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<p> Submarine-fan deposits form the largest sediment accumulations on Earth and host significant reservoirs for hydrocarbons. While many studies of ancient fan deposits qualitatively describe lateral architectural variability (e.g., axis-to-fringe, proximal-to-distal), these relationships are rarely quantified. In order to enable comparison of key relationships that control the lateral architecture of submarine depositional environments, I digitized published bed-scale outcrop correlation panels from five different environments (channel, levee, lobe, channel-lobe-transition-zone, basin plain).

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25

Borgomano, Jean. "La plate-forme et le talus carbonates du cretace superieur du gargano et des murges (italie meridionale) : stratigraphie, sedimentologie, diagenese, fonctionnement tectono-sedimentaire." Aix-Marseille 1, 1987. http://www.theses.fr/1987AIX11063.

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Ce travail concerne les formations du cretace superieur du massif du gargano et des murges (italie meridionale). L'etude stratigraphique, basee sur la faune de foraminiferes et de rudistes, permet de mettre en evidence plusieurs discontinuites dans la serie et une tendance a l'emersion marquee egalement par la formation de bauxite. Les depots sont caracteristiques de milieux de plateforme carbonatee et de talus. Les breches et depots bioclastiques du talus correspondent a des mises en place par ecoulements ou glissements gravitaires controles par des phenomenes tectoniques en relation avec la

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26

Bronikowski, Jason Lee. "Sedimentary environments and processes in a shallow, Gulf Coast Estuary-Lavaca Bay, Texas." Texas A&M University, 2004. http://hdl.handle.net/1969.1/1098.

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Sedimentation rates in sediment cores from Lavaca Bay have been high within the last 1-2 decays within the central portion of the bay, with small fluctuations from river input. Lavaca Bay is a broad, flat, and shallow (<3 m) microtidal estuary within the upper Matagorda Bay system. Marine derived sediment enters the system from Matagorda Bay, while two major rivers (Lavaca & Navidad) supply the majority of terrestrially derived sediment. With continuous sediment supply the bay showed no bathymetric change until the introduction of the shipping channel. Processes that potentially lead to se

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27

MacGregor, Robert A. "The geochemistry of selenium in sedimentary environments : examples from the UK and Jordan." Thesis, University of Reading, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.363858.

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28

Nunn, Brook L. "Moving beyond amino acids : examinations of the protein component in sedimentary marine environments /." Thesis, Connect to this title online; UW restricted, 2004. http://hdl.handle.net/1773/11054.

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29

Almasinia, Banafsheh [Verfasser], and Franz [Gutachter] Fürsich. "Microfacies, biostratigraphy and sedimentary environments of the Eocene sedimentary successions in the Zagros and Sanandaj-Sirjan Zone (Iran) / Banafsheh Almasinia ; Gutachter: Franz Fürsich." Erlangen : Friedrich-Alexander-Universität Erlangen-Nürnberg (FAU), 2017. http://d-nb.info/1138115770/34.

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30

Coates-Marnane, Jack. "Sedimentary Archives of Environmental Change and Human Impact in a Shallow Embayment." Thesis, Griffith University, 2017. http://hdl.handle.net/10072/365843.

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This research uses a series of deep (1.5 - 5m) sediment cores collected from sub-tidal sediment of a shallow bay to explore connectivity within the catchment to coast continuum. Specifically, this thesis investigates; 1) the variation in sediment yield of a coastal catchment subject to widespread land-use changes, 2) Historical trends in metal pollution in a shallow bay and the relative impact of a high magnitude flood. 3) Relative changes in coastal primary production and algal community shifts following land use changes in the adjacent catchment, and 4) Long-term climatic features of the eas

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31

Leng, Melanie Jane. "Late Ordovician-early Silurian palaeo-environmental analysis in the Tywyn-Corris area of mid-Wales." Thesis, Aberystwyth University, 1990. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.388533.

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32

Soltanian, Mohamad Reza. "RELATING REACTIVE TRANSPORT TO HIERARCHICAL AND MULTISCALE SEDIMENTARY ARCHITECTURE." Wright State University / OhioLINK, 2015. http://rave.ohiolink.edu/etdc/view?acc_num=wright1428521270.

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33

Bohlin, Hanna. "The influence by point sources on carbon, nitrogen and metals in two sedimentary environments." Doctoral thesis, Stockholm : Dept. of geology and geochemistry, Stockholm university, 2005. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-753.

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34

Holloway, Lucy Katherine. "Sedimentary environments in the western Forth valley during the late Devensian and early Holocene." Thesis, Coventry University, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.271257.

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35

García, Comendador Julián. "Sediment fingerprinting and hydro-sedimentary monitoring as tools for catchment management in Mediterranean environments." Doctoral thesis, Universitat de les Illes Balears, 2021. http://hdl.handle.net/10803/672333.

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[eng] Soil erosion is a natural process that encompasses weathering, transport and deposition of soil particles. These processes are essential in terrestrial geochemical cycles. However, the on- and off-site erosion effects are considered to be one of the most important causes of terrestrial and aquatic ecosystems degradation. The characteristics of the Mediterranean region are marked by complex relationships between natural, human, biotic and abiotic variables. In addition, an irregular rainfall distribution, strong seasonality and the physiographic landscape characteristics promote divergent

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36

BONJOUR, JEAN-LUC. "Sedimentation paleozoique initiale dans le domaine centre-armoricain (massif armoricain)." Rennes 1, 1988. http://www.theses.fr/1988REN10132.

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Etude des premiers depots paleozoiques reposant en discordance sur le substratum brioverien en centre armorique. Il s'agit des series rouges initiales (formation du cap de la chevre et formation de pont-rean) organises en prismes sedimentaires et se developpant en domaine continental ou a l'interface avec le domaine marin. L'evolution de la sedimentation se fait dans un cadre tectonique distensif, les niveaux volcanoclastiques interstratifies temoignant de l'instabilite de l'aire de depot. Les donnees petrographiques et geochimiques montrent que le materiel detritique provient du remaniement d

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37

Kervella, Youen. "IMPACT DES INSTALLATIONS OSTREICOLES SUR L'HYDRODYNAMIQUE ET LA DYNAMIQUE SEDIMENTAIRE." Phd thesis, Université de Caen, 2010. http://tel.archives-ouvertes.fr/tel-00706590.

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Les structures ostréicoles constituent des obstacles artificiels pouvant perturber l'écoulement des courants de marée et la propagation des vagues, et ainsi modifier le transport sédimentaire. Il en résulte des envasements locaux parfois très prononcés et menaçants pour l'activité ostréicole. L'impact des structures sur les forçages hydrodynamiques, vagues et courants, est donc évalué à différentes échelles spatiales par le biais de mesures in-situ, de modélisation expérimentale et de modélisation numérique. Ces différentes approches ont permis de montrer qu'en champ proche, les courants sont

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38

Paradis, Vilar Sarah. "Physical and Biogeochemical Impacts of Deep Bottom Trawling in Sedimentary Environments of the Western Mediterranean." Doctoral thesis, Universitat Autònoma de Barcelona, 2020. http://hdl.handle.net/10803/670718.

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La pesca d’arrossegament és considerada una de les activitats antròpiques més nocives pel medi marí, degut a la seva extensió global, i l’elevada freqüència i intensitat. Com que aquest art està en contacte continu amb el fons marí, pot modificar la morfologia del fons i resuspendre grans volums de sediment, que poden ser advectats, erosionant els caladors i alterant les propietats del sediment. Amb la expansió global de la pesca d’arrossegament a caladors més profunds des dels anys 1950, s’estima que els impactes ocasionats per aquesta activitat poden ser intensificats, però encara hi ha una

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39

Raine, Pamela. "Sedimentary processes and depositional environments in Caldera Lakes : Scafell (U.K.) and La Primavera (Mexico) Calderas." Thesis, University of Liverpool, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.251484.

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40

Lovelock, Clifford Earnest. "The sedimentary environments and biofacies of the Silurian inlier at Lesmahagow Midland Valley of Scotland." Thesis, University of Edinburgh, 1998. http://hdl.handle.net/1842/12476.

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The primary aim of this research is to answer some of the questions about the role of Lesmahagow in the Caledonian orogeny. Other important considerations include how it correlates with the other inliers of the southern Midland Valley and why such an unusual fauna should be preserved here. The basin model to emerge from this study shows that the sediments of Lesmahagow accumulated in a narrow, trans-tensional basin within a largely extinct volcanic arc. The basin subsided quickly and was filled by organic rich muds. Arenaceous sediment was supplied by two turbidite sources; a fine to course gr

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41

Burt, Caroline Elaine. "Sedimentary environments and basin evolution of the Upper Dalradian : Tayvallich subgroup and Southern Highland Group." Thesis, Kingston University, 2002. http://eprints.kingston.ac.uk/20695/.

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The Dalradian Supergroup is divided into four groups, the uppermost of which is the Southern Highland Group (SHG). To date there are few sedimentological data that pertain to the SHG. In this thesis new field, petrographic and geochemical data are provided for the SHG and a model for its evolution outlined. The Killin and Aberfoyle areas together provide one of the most complete sections through the SHG. New sedimentological data from these sections are used here as a basis on which to build a correlative stratigraphy for the entire SHG basin which extents from Banff in NE Scotland southwestwa

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42

Gassiat, Claire. "Simulating regional groundwater flow in layered, faulted sedimentary basins: implications for groundwater age and shale gas." Thesis, McGill University, 2013. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=119745.

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Groundwater plays an important role in a wide range of geologic processes. Sedimentary basins are heterogeneous, layered and faulted which strongly impacts regional groundwater flow. An important concern is how anthropogenic alterations such as groundwater or shale gas development affect these complex systems. Heterogeneities are likely to impact groundwater age and affect geologic processes that depend on groundwater or solute fluxes. They may also enhance long term contamination of shallow aquifers from the fracturing of the target shale unit, as contaminants may migrate from the shale to sh

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43

Johnson, Geoffrey. "Environmental History of Estuarine Dissolved Oxygen Inferred from Trace-Metal Geochemistry and Organic Matter." Thesis, University of Oregon, 2017. http://hdl.handle.net/1794/22296.

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Environmental history recorded in sediments can reconstruct estuarine water quality metrics, such as dissolved oxygen, through the use of geochemical and biological proxies. I collected sediment cores from two locations in the Coos Bay Estuary, at South Slough and Haynes Inlet, spanning from ~1680 AD to the present. To address the historical record of water column oxygen in the estuary I measured a suite of geochemical proxies including organic matter, magnetic susceptibility, and redox-sensitive metals to calibrate against a detailed 15-year record of dissolved oxygen. High visual correlation

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44

Crossing, Adam. "Sedimentary environments and carbonates of the Appila Tillite in the Pt. Augusta-Hawker area, South Australia /." Title page, contents and abstract only, 1991. http://web4.library.adelaide.edu.au/theses/09SB/09sbc951.pdf.

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Thesis (B. Sc.(Hons))--University of Adelaide, 1992.<br>One chart in pocket. National Grid reference: Orroroo 1:250 000 SI 54-1 -- Parachilna 1:250 000 SH/54-13 -- Port Augusta 1:250 000 SI 53-4. Includes bibliographical references (leaves [5-8]).

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45

Lee, Mui-fa Alison, and 李梅花. "Sedimentary facies of fluvial-marine transition environments in Hong Kong: Ting Kok and Pak Nai Deltas." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 1999. http://hub.hku.hk/bib/B31221270.

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46

Lee, Mui-fa Alison. "Sedimentary facies of fluvial-marine transition environments in Hong Kong : Ting Kok and Pak Nai Deltas /." Hong Kong : University of Hong Kong, 1999. http://sunzi.lib.hku.hk/hkuto/record.jsp?B21021211.

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47

Jennings, Jonathan Simon. "Fracture kinematics, cementation and burial history of a structurally polyphase sedimentary basin, Tunisia." Thesis, Kingston University, 2001. http://eprints.kingston.ac.uk/20680/.

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Basin analysis of over 1000km of 2-D seismic profiles and thirteen exploration wells from the North and South Kairouan Permits in the foreland region of the Tunisian Atlas has led to the identification of a number of late Mesozoic to recent basin systems. The generation of these basin systems resulted in the development of fractures and emplacement of diagenetic fluids and hydrocarbons in the early Campanian to early Maastrichtian (83.5-70Ma) chalks of the Abiod Formation. Recognition of the basin-forming events has been based on the identification of regional unconformities, subsurface thickn

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48

Sauer, Robert Eugene Jr. "Development and use of saltmarsh mesocosms in studies of sedimentary mercury transformation." Thesis, Georgia Institute of Technology, 2002. http://hdl.handle.net/1853/19608.

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49

Werner, Axel. "Reconstruction of environmental change during the Holocene based on the multiproxy study of sedimentary archives." Thesis, Edith Cowan University, Research Online, Perth, Western Australia, 2022. https://ro.ecu.edu.au/theses/2544.

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Monitoring-based management is expensive and short scaled. The long-term history recorded in natural archives, which encompass pre-anthropogenic periods, allows deciphering of shifting baselines to define reliable management targets. The research presented in this thesis reconstructs millenary environmental change using novel natural archives and proxies. The results validate glomalin as a new and cost-effective proxy to reconstruct land-use change in colluvial soils, and show the benefits associated with coastal management actions since 1970s to reduce metal/nutrient pollution in a coastal se

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50

SUGITANI, KENICHIRO, and KOICHI MIMURA. "Redox change in sedimentary environments of Triassic bedded cherts, central Japan: possible reflection of sea-level change." Cambridge University Press, 1998. http://hdl.handle.net/2237/10289.

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