Relevant bibliographies by topics / Facies sedimentology / Dissertations / Theses
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Dissertations / Theses on the topic 'Facies sedimentology'

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Published: 4 June 2021
Last updated: 28 February 2023

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1

Artzani, Nasser. "Facies and diagenesis at the Triassic-Jurassic boundary in SW Britain." Thesis, University of Reading, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.363835.

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2

Faulkner, Thomas Joseph. "Carbonate facies on a Lower Carboniferous storm influenced ramp in SW Britain." Thesis, University of Bristol, 1989. http://hdl.handle.net/1983/a8be6732-2a17-4eff-9e2a-e703a1337c29.

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The Lower Carboniferous ('mid'-Courceyan to early Chadian) Black Rock Limestone ramp succession of SW Britain, accumulated along the southern margin of the Welsh-Brabant Massif during the early stage of development of the SW European foreland basin. Two depositional cycles are recognized which culminate in the subaerial exposure of those sequences in a more landward setting. The lower depositional cycle includes the Barry Harbour Limestone Formation, which contains a variety of storm-related sedimentary structures including hummocky cross-stratification. This is conformably overlain by the tid
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3

Carr, Ian Daniel. "Facies analysis and reservoir characterisation of Jurassic sandstones from Bjørnedal, central east Greenland." Thesis, University of Reading, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.269665.

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4

Moretti, Junior Paulo Augusto. "Analise de facies e modelo paleodeposicional da plataforma siliciclastica ordoviciana da Pre-Cordilheira Argentina." [s.n.], 2009. http://repositorio.unicamp.br/jspui/handle/REPOSIP/264814.

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Orientador: Giorgio Basilici<br>Dissertação (mestrado) - Universidade Estadual de Campinas, Faculdade de Engenharia Mecanica e Instituto de Geociencias<br>Made available in DSpace on 2018-08-14T04:13:31Z (GMT). No. of bitstreams: 1 MorettiJunior_PauloAugusto_M.pdf: 5701785 bytes, checksum: d478ca8c79173f62ad9807c930cc0332 (MD5) Previous issue date: 2009<br>Resumo: Esta dissertação consiste no estudo sedimentológico e paleodeposicional de quatro unidades litoestratigráficas da Pré-Cordilheira Argentina, depositadas durante o Ordoviciano: Formação Portezuelo del Tontal (FPT), Formação Sierra d
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5

Simoneau, Pierre. "Pétrographie, sédimentologie et analyse des facies de la formation de Daubrée, Chapais, Québec /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1986. http://theses.uqac.ca.

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Mémoire (M.Sc.A.)-- Université du Québec à Chicoutimi, 1986.<br>"Mémoire présenté en vue de l'obtention de la maîtrise en sciences appliquées en géologie" Page 157 manquante. CaQCU CaQCU Bibliogr.: ff. 99-110. Document électronique également accessible en format PDF. CaQCU
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6

Henrique, Andre. "Modelo de facies de um sistema profundo de rampa submarina (Formação Punta Negra), Devoniano, Pre-Cordilheira Argentina." [s.n.], 2009. http://repositorio.unicamp.br/jspui/handle/REPOSIP/264796.

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Orientador: Giorgio Basilici<br>Dissertação (mestrado) - Universidade Estadual de Campinas, Faculdade de Engenharia Mecanica e Instituto de Geociencias<br>Made available in DSpace on 2018-08-13T23:50:03Z (GMT). No. of bitstreams: 1 Henrique_Andre_M.pdf: 11951186 bytes, checksum: 6061e17e64f904f61a28dc56429cad0c (MD5) Previous issue date: 2009<br>Resumo: A Formação Punta Negra (Meso- Neodevoniano da Pré-Cordilheira Argentina) consiste em uma espessa sucessão de depósitos siliciclásticos de água profunda. Esta unidade aflora por cerca de 300 km em direção N-S nas províncias de San Juan, Mendoz
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7

Klute, Margaret Anne. "Sedimentology, sandstone petrofacies, and tectonic setting of the Late Mesozoic Bisbee Basin, southeastern Arizona." Diss., The University of Arizona, 1991. http://hdl.handle.net/10150/185723.

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The Late Mesozoic Bisbee basin of southeastern Arizona was an intracratonic back-arc rift basin. Extension was coupled with seafloor spreading in the Gulf of Mexico and back-arc extension behind a magmatic arc along the convergent Pacific continental margin. Tectonostratigraphic evolution of the basin occurred in three phases. Initial mid-Jurassic rifting of the basin, marked by eruption of the Canelo Hills Volcanics, may have been complicated by sinistral strike-slip motion along the Mojave-Sonora megashear. During continued rifting, from latest Jurassic to Early Cretaceous time, the Glance C
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8

Buck, S. G. "Facies and sedimentary structures of the Folkestone beds (Lower Greensand, Early Cretaceous) and equivalent strata in Southern England." Thesis, University of Reading, 1987. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.381923.

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9

Leith, Thomas Leslie. "The role of coals and carbonaceous shale facies in the petroleum reservoir system : a case study from the Gullfaks Field, Norwegian North Sea." Thesis, Heriot-Watt University, 2000. http://hdl.handle.net/10399/545.

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10

Stouten, Craig A. "Subsurface Facies Analysis of the Clinton Sandstone, Located in Perry, Fairfield, and Vinton Counties." Bowling Green State University / OhioLINK, 2014. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1416147053.

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11

Copus, Jonathan Michael Jacks. "Sedimentology and facies architecture of the early Silurian slope-apron turbidite systems of the Welsh Basin." Thesis, University of Cambridge, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.624497.

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12

Hill, Robert E. (Robert Einar). "Stratigraphy and sedimentology of the Middle Proterozoic Waterton and Altyn Formations, Belt-Purcell Supergroup, southwest Alberta." Thesis, McGill University, 1985. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=63330.

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13

Gowland, Stuart. "Facies analysis of three members of the Scarborough Formation (Middle Jurassic : Lower Bajocian) in the Cleveland Basin, northeast England : Blea Wyke, Byland Limestone and Crinoid grit members." Thesis, University of Hull, 1987. http://hydra.hull.ac.uk/resources/hull:3919.

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The Scarborough Formation is the youngest marine horizon of formation status within the dominantly deltaic Aalenian - Bajocian Ravenscar Group, Cleveland Basin, northeast England. Sedimentary facies analysis has been performed on the three conformable lithostratigraphic units which make up the bulk of the Scarborough Formation outcrop: Blea Wyke, Byland Limestone and Crinoid Grit Members. This form of analysis was performed in an effort to determine the depositional environments of the members. The information derived from the study enables one to trace the palaeogeographic evolution of the Cl
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14

Ranson, Andrew M. "Transitional Facies and Sequence Stratigraphic Complexity of Shallow-Marine Star Point Formation to Coastal-Plain Blackhawk Formation Along Depositional-Strike, Wasatch Plateau, Utah." ScholarWorks@UNO, 2012. http://scholarworks.uno.edu/td/1476.

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Facies and stratigraphic architecture right at the transition from marine to non-marine environments is poorly documented. In the Cretaceous outcrops of Utah, Star Point and Blackhawk Formations are well studied. The nature of spatio-temporal transition of these two Formations, in the deposition-strike orientation, remains undocumented. This study characterizes facies and stratigraphic complexity at the transition of the two Formations that crop out in depositional-strike orientation in the Wasatch Plateau. Data from outcrop including photomosiacs and measured sections demonstrate this complex
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15

Chaney, Alistair John. "Sedimentology, facies architecture and hydrocarbon potential of the Merrimelia Formation (glacial Permo-Carboniferous), Southern Cooper Basin, South Australia." Thesis, University of Aberdeen, 1990. http://digitool.abdn.ac.uk/R?func=search-advanced-go&find_code1=WSN&request1=AAIU125529.

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Sedimentological analysis of cored sections within the Merrimelia Formation (basal Gidgealpa Group, Cooper Basin, South Australia) reveals a complex glacigenic environment, including glaciolacustrine, deltaic, shorezone, fluvial, aeolian and other associated terrestrial facies (over 20 different facies have been identified). These facies are observed within terminoglacial and proglacial environments and interfinger laterally and vertically constantly throughout the Merrimelia Formation, exhibiting rapid environment change related to the position of ice sheet. Detailed sedimentological and petr
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16

Taylor, Andrew W. "Sedimentology, Facies Architecture, and Reservoir Characterization of Lacustrine Rocks, Eocene Green River and Colton Formations, Uinta Basin, Utah." DigitalCommons@USU, 2002. https://digitalcommons.usu.edu/etd/6780.

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Outcrop and petrographic studies of the Eocene Green River and Colton formations in the Uinta basin, Utah, document the facies architecture and heterogeneity characteristic of lacustrine reservoirs. A southwest-northeast transect of Eocene strata in the Uinta basin records three main marginal lacustrine depositional environments: fluvial, deltaic, and wave-dominated. Heterogeneity exists between and within individual depositional systems. Reservoir rocks of Outcrops One and Two (the flu vial facies of the Colton Formation and the deltaic facies of the Green River Formation, respectively) consi
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17

Devereaux, Alexander R. "A quantified facies scale depositional model for current controlled siliciclastic deep marine depositional systems." Thesis, Queensland University of Technology, 2022. https://eprints.qut.edu.au/235129/1/Alexander_Devereaux_Thesis.pdf.

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Detailed analysis was carried out on sediment samples collected from the Gulf of Cádiz during Integrated Ocean Drilling Program 339. Grain size analysis is a vital sedimentological tool used to unravel the hydrodynamic conditions, modes of transport, and depositional environment. Statistical parameters, bivariate analysis, and log-probability curves were used to quantify the physical sedimentological characteristics and compare them to previously established conceptual models.
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18

Powell, Kristopher Michael. "Facies Analysis, Sedimentary Petrology, and Reservoir Characterization of the Lower Triassic Sinbad Limestone Member of the Moenkopi Formation, Central Utah: A Synthesis of Surface and Subsurface Data." BYU ScholarsArchive, 2017. https://scholarsarchive.byu.edu/etd/6672.

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Lower Triassic strata in the Wellington Flat and Tully cores reflect a lateral transition from shallow water strata (Wellington Flats core) to strata that indicate deposition on a relatively more distal, storm-dominated ramp (Tully core). The Sinbad Member, along with the upper part of the underlying Black Dragon Member and the lower part of the overlying Torrey Member (Moenkopi Formation), are composed of ten carbonate, siliciclastic and mixed carbonate/siliciclastic facies deposited on a west-facing ramp/shelf that reached maximum flooding during Smithian time. Individual beds and facies dis
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19

Wulff, Keiran. "Upper Jurassic of the Barrow sub-basin: sedimentology, sequence stratigraphy and implications for reservoir development." Thesis, Curtin University, 1991. http://hdl.handle.net/20.500.11937/1177.

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A chronostratigraphic subdivision of the Upper Jurassic synrift sediments in the eastern Barrow Sub-basin was developed from the integration of core logging, petrography, well log sequence analyses and seismic stratigraphy. From this basis, the Callovian to base Cretaceous sediments may be subdivided into five depositional sequences. The development of the sequence boundaries, in most part, is closely related to periods of major changes in basin configuration associated with the sequential breakup of eastern Gondwanaland. Initiation of the Upper Jurassic rift complex occurred during late Callo
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20

Mekhnache, Rachid. "Étude sédimentologique des dépôts graveleux du corridor Métabetchouan - Larouche /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 2005. http://theses.uqac.ca.

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21

Souza, Pricilla. "Evolution and stratigraphic architecture of tidal point bars with and without fluvial input: influence of variable flow regimes on sediment and facies distribution, and lateral accretion." ScholarWorks@UNO, 2019. https://scholarworks.uno.edu/td/2705.

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Tide-influenced point bars represent a significant proportion of shallow-marine deposits, commonly developed along meandering channels in most backbarrier and estuarine systems. However, sedimentological studies to characterize this type of deposit are still emerging. They often present very heterogeneous internal architectures which development is controlled by the complex flow patterns operating in tidal environments. The study of the sedimentological and morphological characteristics of these features provides better understanding of the hydrodynamic processes that shape coastal systems and
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22

Wulff, Keiran. "Upper Jurassic of the Barrow sub-basin: sedimentology, sequence stratigraphy and implications for reservoir development." Curtin University of Technology, National Drug Research Institute, 1991. http://espace.library.curtin.edu.au:80/R/?func=dbin-jump-full&object_id=17024.

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A chronostratigraphic subdivision of the Upper Jurassic synrift sediments in the eastern Barrow Sub-basin was developed from the integration of core logging, petrography, well log sequence analyses and seismic stratigraphy. From this basis, the Callovian to base Cretaceous sediments may be subdivided into five depositional sequences. The development of the sequence boundaries, in most part, is closely related to periods of major changes in basin configuration associated with the sequential breakup of eastern Gondwanaland. Initiation of the Upper Jurassic rift complex occurred during late Callo
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23

Cauxeiro, Cirilo. "Architecture stratigraphique du prisme néogène de la Kwanza, Angola, et relations avec les mouvements verticaux." Thesis, Montpellier 2, 2013. http://www.theses.fr/2013MON20120.

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Ce travail pionnier porte sur l'étude de l'architecture stratigraphique du Bassin de la Cuanza à partir d'une approche conjuguée multi-échelle croisant la géomorphologie, l'interprétation sismique et la sédimentologie de faciès de l'intervalle Oligocène à Actuel. L'objectif est de préciser l'âge, le partitionnement de faciès, les milieux de dépôts de la zone littorale dans le but de dater et de caractériser les mouvements verticaux en relation avec le fluage du sel (tectonique gravitaire) et le soulèvement général de la marge en lien avec la déformation de la lithosphère. L'analyse détaillée d
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24

Bloxson, Julie M. Bloxson. "MINERALOGICAL AND FACIES VARIATIONS WITHIN THE UTICA SHALE, OHIO USING VISIBLE DERIVATIVE SPECTROSCOPY, PRINCIPAL COMPONENT ANALYSIS, AND MULTIVARIATE CLUSTERING." Case Western Reserve University School of Graduate Studies / OhioLINK, 2017. http://rave.ohiolink.edu/etdc/view?acc_num=case1498664669872459.

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25

Duchesne, Mathieu. "Sédimentologie de dépôts quaternaires graveleux dans le bassin versant de la Rivière Chicoutimi à Laterrière, Québec /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 2001. http://theses.uqac.ca.

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26

Warusavitharana, Chamandika J. "Sedimentology and stratigraphy of microbialite facies in the roubidoux and Jefferson City formations of central and southwest Missouri and central Kansas." Thesis, Wichita State University, 2012. http://hdl.handle.net/10057/5981.

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Outcrop studies of sedimentary and stratigraphic features of microbial buildups are important in developing conceptual models for exploration of potential microbialite reservoirs. This study examines the occurrence and distribution of Lower Ordovician microbial fabrics in central Missouri and Kansas. The units studied include the Roubidoux and Jefferson City-Cotter Formations of the Arbuckle Group. To determine the depositional environments suitable for microbialite development, micro, meso, and macro-scale features were examined and their stratigraphic relationships established to the surroun
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27

Le, Gouche Chloé. "Sédimentation de la matière organique dans les bassins profonds : cas du Bassin Arctique à l'Eocène." Thesis, Rennes 1, 2017. http://www.theses.fr/2017REN1S025/document.

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La matière organique continentale déposée dans les bassins profonds est peu décrite et représente un intérêt certain pour l'industrie pétrolière. Comprendre les processus sédimentaires qui permettent le dépôt et la préservation de cette matière organique d'origine terrestre dans les bassins profonds est alors fondamental. Durant le Paléogène, période de transition climatique greenhouse à icehouse, le Delta de Mackenzie, situé dans le Bassin Arctique, reçoit de la matière organique continentale du continent et en préserve une partie. Quel est le contexte stratigraphique et climatique qui a rend
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Trueman, Jonathon David. "Stratigraphy and sedimentology of the Burdekin Delta, Queensland and comparisons with Permian coastal facies in the Denison Trough, SW Bowen Basin, Australia /." St. Lucia, Qld, 2002. http://www.library.uq.edu.au/pdfserve.php?image=thesisabs/absthe17342.pdf.

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29

Bergen, Anika. "Vertical and Lateral Facies Architecture of Levees and Their Genetically-Related Channels, Isaac Formation, Neoproterozoic Windermere Supergroup, Cariboo Mountains, B.C." Thesis, Université d'Ottawa / University of Ottawa, 2017. http://hdl.handle.net/10393/36434.

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At the Castle Creek study area, levee deposits are well-exposed over an area of ~2.6 km wide and ~90 m thick. This provides an opportunity to describe their lateral and vertical lithological changes, and accordingly details about their reservoir geometry and stratal continuity. Here, levee deposits are divided vertically into packages, each consisting of a sand-rich lower part overlain sharply by a mud-rich upper part. Each lower part displays a consistent thickening then thinning trend laterally away from its genetically related channel. The characteristics of these packages suggest that they
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Ferry, Mark Peter. "An evaluation of the sedimentology and the influence of grain size and facies on permeability for the White Rose A-17 cored interval, White Rose Oilfield, offshore eastern Newfoundland /." Internet access available to MUN users only, 2005. http://collections.mun.ca/u?/theses,16593.

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31

Luca, Pedro Henrique Vieira de 1983. "Processos de transporte e deposição de material clástico em sistemas depocisionais costeiro e de plataforma marinha dominados por ondas (formações Lagarto e Palmares, Brasil e Formação Punta Negra, Argentina)." [s.n.], 2013. http://repositorio.unicamp.br/jspui/handle/REPOSIP/287329.

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Orientador: Giorgio Basilici<br>Tese (doutorado) - Universidade Estadual de Campinas, Instituto de Geociências<br>Made available in DSpace on 2018-08-24T01:34:47Z (GMT). No. of bitstreams: 1 Luca_PedroHenriqueVieirade_D.pdf: 18777385 bytes, checksum: c055caccb8a267d7dde58a2477d6acb9 (MD5) Previous issue date: 2013<br>Resumo: As formações Lagarto e Palmares (Cambriano-Ordoviciano, Domínio Estância) e a Formação Punta Negra (Devoniano, Precordilheira Argentina) representam unidades sedimentares antigas desenvolvidas em ambientes marinhos costeiros e plataformais dominados pela ação de ondas de
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Cook, Preston Scott. "Sedimentology and Stratigraphy of the Middle Jurassic Preuss Sandstonein Northern Utah and Eastern Idaho." BYU ScholarsArchive, 2016. https://scholarsarchive.byu.edu/etd/6206.

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The purpose of this study is to analyze the sedimentology and stratigraphy of the Middle Jurassic Preuss Sandstone and re-evaluate past sedimentological interpretations. The Preuss is located in northern Utah, western Wyoming and eastern Idaho and is stratigraphically equivalent to the Entrada Sandstone, which is Callovian in age (Dossett et al., 2014). This study is the first attempt at 1) a sequence stratigraphic framework, 2) a petroleum system analysis and 3) an extraterrestrial analog study for the Preuss. This study frames the Preuss within three broad facies groups: marine, coastal and
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Briais, Justine. "Le Cénozoïque du bassin de Paris : un enregistrement sédimentaire haute résolution des déformations lithosphériques en régime de faible subsidence." Thesis, Rennes 1, 2015. http://www.theses.fr/2015REN1S002/document.

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Le bassin de Paris est considéré comme un exemple typique de bassin intracratonique (sag) affecté par une subsidence thermique long terme. Le Cénozoïque correspond à une période de faible subsidence (épaisseurs inférieures à 350m) et marque la fin du fonctionnement de ce bassin. C'est en outre une période de forte déformation de la plaque européenne, dans un contexte de convergence Afrique-Eurasie et d'ouverture de l'Atlantique Nord caractérisée par des inversions de grabens dans le Nord et l'Est de l'Europe. Si de nombreux hiatus ont été identifiés, les déformations cénozoïques du bassin de P
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Megner-Allogo, Alain-Cedrique. "Sedimentology and stratigraphy of deep-water reservoirs in the 9A to 14A Sequences of the central Bredasdorp Basin, offshore South Africa." Thesis, Stellenbosch : Stellenbosch University, 2006. http://hdl.handle.net/10019.1/17400.

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Thesis (MSc)--University of Stellenbosch, 2006.<br>ENGLISH ABSTRACT: The Barremian to Albian siliciclastic deep-water deposits of the central Bredasdorp Basin were investigated primarily in terms of their stratigraphic evolution, depositional characteristics and facies distribution. Cores from the deep-water deposits reveal that the facies successions are composed of massive, ripple cross- to parallel-laminated sandstones, conglomerate, massive claystone, alternating laminated to interbedded sandstone/siltstone and claystone, laminated and clay-rich siltstone. These facies are grouped i
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Santos, Mauricio Guerreiro Martinho dos. "Evolução dos sistemas fluviais através do tempo geológico: fácies sedimentares, arquitetura deposicional e estruturas de deformação sinsedimentar em exemplos do Torridonian, Bacia do Camaquã e Old Red Sandstone." Universidade de São Paulo, 2014. http://www.teses.usp.br/teses/disponiveis/44/44141/tde-10102014-085051/.

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Uma série de pesquisas realizadas em depósitos de sistemas fluviais, desenvolvidos anterior e concomitantemente à colonização dos continentes por vegetação, são aqui apresentadas com o intuito de investigar as principais características deposicionais destes sistemas, particularmente suas assembléias de fácies e elementos arquitetônicos preservados. Esta pesquisa busca, desta maneira, propor modelos deposicionais para sucessões fluviais pré-vegetação e contribuir para o avanço do conhecimento sobre as mudanças seculares em padrões de sedimentação, principalmente em relação à evolução dos rios a
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Klopfenstein, Trey. "High-frequency Sequences within the Lower Mississippian Allensville Member, Logan Formation, South-central Ohio." Ohio University / OhioLINK, 2018. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou1525864536290455.

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37

Backert, Nicolas. "Interaction tectonique-sédimentation dans le rift de Corinthe, Grèce. Architecture stratigraphique et sédimentologie du Gilbert-delta de Kerinitis." Phd thesis, Institut National Polytechnique de Lorraine - INPL, 2009. http://tel.archives-ouvertes.fr/tel-00457060.

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La stratigraphie synrift du bloc de faille est divisée en trois groupes stratigraphiques, représentant une épaisseur de 1624 m. Le Groupe inférieur est composé de sédiments fluvio-lacustres, le Groupe moyen comporte les Gilbert-deltas géants et leurs faciès fins associés, le Groupe supérieur est formé de Gilbert-deltas récents à actuels ainsi que de formations superficielles. La discordance basale de l'Unité du prérift présente une paléotopographie. La phase d'extension précoce (Groupe inférieur) est caractérisée par une très faible subsidence assurée par l'activité précoce de la faille de Pir
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Olivier, Marie. "Environnements mixtes fluviatiles et éoliens : facteurs de contrôle et de préservation des dépôts éoliens en domaines endoréique et côtier : exemples du Permien du Sud de la Mer du Nord et du Sud-Est de l’Utah (USA)." Electronic Thesis or Diss., Rennes 1, 2017. http://www.theses.fr/2017REN1S173.

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Le Permien, dernière période du Paléozoïque, est marquée par la fin de l'assemblage de la Pangée induisant une continentalisation de vastes étendues sans équivalent dans les temps géologiques. Cette évolution géodynamique s'accompagne d'une aridification liée à la déglaciation du Permien Inférieur favorisant la sédimentation d'importants dépôts éoliens. La bonne préservation de ces dépôts dans l'enregistrement sédimentaire fait du Permien une période privilégiée pour l'étude des sédiments continentaux éoliens et fluviatiles que ce soit en contexte endoréique ou exoréique. Ce travail s'intéress
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Lanzarini, Wilson Luiz. "Modelos e simulações de facies e sequências sedimentares fluviais e eólicas de reservatórios petrolíferos." Universidade de São Paulo, 1995. http://www.teses.usp.br/teses/disponiveis/44/44136/tde-27112015-110757/.

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Nas bacias sedimentares brasileiras produtoras de hidrocarbonetos (petróleo e gás natural), três unidades estratigráficas de origem fluvial e/ou eólica se destacam como reservatórios: a Formação Sergi, do Jurássico, fase pré-rifte da Bacia do Recôncavo; a Formação Açu, do Cretáceo Superior, fase drift da Bacia Potiguar; e a Formação Monte Alegre, base da seqüência clástico-evaporítica de idade carbonífero-permiana da Bacia do Solimões. A Formação Sergi, principal objetivo deste estudo, apresenta fácies de sistema fluvial de canais entrelaçados, associados às fácies eólicas de dunas e interduna
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Zacharias, Angélica Álida. "Preenchimento de vales incisos por associações de fácies estuarinas, formação Rio Bonito, nordeste do Paraná /." Rio Claro : [s.n.], 2004. http://hdl.handle.net/11449/92857.

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Orientador: Mario Luis Assine<br>Banca: Rosemarie Rohn Davies<br>Banca: Almério Barros França<br>Resumo: A Formação Rio Bonito é a unidade inferior do Grupo Guatá, Eopermiana da Bacia do Paraná. Compreende, da base para o topo, os membros Triunfo, Paraguaçu e Siderópolis. No Estado do Paraná, a espessura da Formação Rio Bonito diminui para norte, principalmente em conseqüência do adelgaçamento e acunhamento do Membro Triunfo, que desaparece no sul do Estado de São Paulo. Para investigar estas variações de espessura e de fácies na Formação Rio Bonito, foi escolhida uma área no nordeste do Estad
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41

Landro, Federica. "Studio sedimentologico e micropaleontologico di una carota prelevata nel Delta del Po (Olocene della Pianura Padana)." Bachelor's thesis, Alma Mater Studiorum - Università di Bologna, 2016. http://amslaurea.unibo.it/10823/.

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L'integrazione di dati micropaleontologici a dati sedimentologici ha permesso la ricostruzione paleoambientale di una porzione di carota prelevata nel Delta del Po. Sono state riconosciute 5 associazioni di facies riconducibili ad altrettanti ambienti deposizionali: retrobarriera, barriera trasgressiva, piattaforma, transizione fra piattaforma e prodelta e prodelta. Lo studio delle associazioni a foraminiferi bentonici ha consentito la caratterizzazione micropaleontologica delle facies riconosciute. E' stato cosi possibile definire la superficie di massima ingressione marina (MFS) al tetto d
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MENEZES, FILHO Nelson Ramos de. "Geologia da sinclinal de Ituaçu, escala 1:100.000." reponame:Repositório Institucional da CPRM, 1998. http://rigeo.cprm.gov.br/jspui/handle/doc/14687.

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Submitted by Teresa Cristina Rosenhayme (teresa.rosenhayme@cprm.gov.br) on 2014-12-03T12:47:29Z No. of bitstreams: 1 Nelson Ramos de Menezes Filho (M).pdf: 92351850 bytes, checksum: 5d3d87e8986992fc31ffa889be749a51 (MD5)<br>Approved for entry into archive by Roberta Silva (roberta.silva@cprm.gov.br) on 2014-12-03T13:24:49Z (GMT) No. of bitstreams: 1 Nelson Ramos de Menezes Filho (M).pdf: 92351850 bytes, checksum: 5d3d87e8986992fc31ffa889be749a51 (MD5)<br>Approved for entry into archive by Roberta Silva (roberta.silva@cprm.gov.br) on 2014-12-03T13:25:15Z (GMT) No. of bitstreams: 1 Nelson Ra
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Canuto, Jose Roberto. "Facies e ambientes de sedimentação da formação Rio do Sul (Permiano), Bacia do Paraná, na região de Rio do Sul, Estado de Santa Catarina." Universidade de São Paulo, 1994. http://www.teses.usp.br/teses/disponiveis/44/44136/tde-17072013-144504/.

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A \"depressão\" de Rio do Sul é uma ampla área de deposição relativamente espessa de sedimentos clásticos, predominantemente finos (acima de 400 m) da Formação Rio do Sul, unidade superior do Subgrupo Itararé (Carbonífero superior), mostrada em mapas de isópacas e litofacies, na parte centro-leste de Santa Catarina, Bacia do Paraná, Brasil. A subsidência da área iniciou-se durante o Permiano inferior (Intervalo H; DAEMON & QUADROS, 1970) controlada por sistemas de falhamentos sudeste-noroeste e nordeste-sudoeste, resultando em uma depressão de mais de 200 km de comprimento por mais de 100 km d
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44

Zacharias, Angélica Álida [UNESP]. "Preenchimento de vales incisos por associações de fácies estuarinas, formação Rio Bonito, nordeste do Paraná." Universidade Estadual Paulista (UNESP), 2004. http://hdl.handle.net/11449/92857.

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Made available in DSpace on 2014-06-11T19:26:13Z (GMT). No. of bitstreams: 0 Previous issue date: 2004-07-19Bitstream added on 2014-06-13T18:54:20Z : No. of bitstreams: 1 zacharias_aa__me_rcla.pdf: 13755139 bytes, checksum: 4926147f9c0352f4aa2b425673d963b5 (MD5)<br>Agência Nacional do Petróleo, Gás Natural e Biocombustíveis (ANP)<br>A Formação Rio Bonito é a unidade inferior do Grupo Guatá, Eopermiana da Bacia do Paraná. Compreende, da base para o topo, os membros Triunfo, Paraguaçu e Siderópolis. No Estado do Paraná, a espessura da Formação Rio Bonito diminui para norte, principalmente em c
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Castro, Darcilea Ferreira. "Sedimentologia, estratigrafia, palinologia, diatomáceas e geoquímica de depósitos quaternários na margem leste da Ilha de Marajó, Pará, Brasil." Universidade de São Paulo, 2010. http://www.teses.usp.br/teses/disponiveis/44/44141/tde-23012011-182838/.

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O registro de depósitos quaternários tem aumentado em áreas costeiras da região Amazônica. No entanto, estudos detalhados são ainda necessários visando interpretar seus ambientes de deposição, bem como reconstituir sua evolução ao longo do Quaternário. Em particular, faltam informações sobre a reconstituição das variações do nível relativo do mar ao longo da margem equatorial brasileira de modo a possibilitar a inclusão dessa área em discussões de interesse regional e global enfocando clima, tectônica e eustasia. O presente trabalho representa um esforço de integração de vários tipos de dados,
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46

Lopez, Benjamin. "Architecture et distribution des systemes carbonatés se développant autour des sources hydrothermales : cas d’étude du basin de Denizli (Turquie), de la region de Rapolano (Italie) et de Mammoth Hot Springs (Wyoming, USA)." Thesis, Aix-Marseille, 2015. http://www.theses.fr/2015AIXM4326.

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Les carbonates de sources hydrothermales (ou Geothermal Spring Carbonate, GSC) sont des systèmes carbonatés qui se développent autour de sources dont les eaux ont circulé en profondeur et sont remontées le long de failles perméables. Leur développement est contrôlé en tout premier lieu par la nature des eaux souterraines auxquelles ils sont liés. La formation de ces carbonates dépend d’interactions complexes entre les processus hydrologiques, tectoniques et structuraux se produisant avant l’émergence. Par la suite, la sédimentation est régie par de nombreux processus résultant des variations h
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GEILLER, MAGALI. "Sedimentologie de facies, mineralogie et stratigraphie genetique des reservoirs silico-clastiques du lias inferieur de cere-la-ronde (d'apres les donnees de forages gdf de sologne - sw du bassin de paris)." Université Louis Pasteur (Strasbourg) (1971-2008), 1997. http://www.theses.fr/1997STR13238.

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Les niveaux reservoirs silicoclastiques du sud-ouest du bassin de paris sont exploites par gaz de france pour le stockage du gaz naturel en nappe aquifere. L'ojectif est de definir la geometrie des reservoirs, et les differents facteurs controlant leur mise en place dans le bassin de sologne, au rhetien et a l'hettangien. La demarche pluridisciplinaire adoptee allie des analyses palynologiques, sedimentologiques, mineralogiques et sequentielles. Elle est appliquee aux depots de chenaux, ainsi qu'aux depots d'interchenaux plus rarement consideres dans le cadre de l'etude de reservoirs. L'ensemb
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48

Chanvry, Emmanuelle. "Caractérisation et facteurs de contrôle des distributions minéralogiques du Bassin Piggyback de Graus-Tremp-Ainsa (Espagne), à l’Eocène Inférieur." Thesis, Lyon, 2016. http://www.theses.fr/2016LYSEM034/document.

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Cette thèse propose une méthodologie pour caractériser et intégrer les distributions minéralogiques des dépôts de l’Eocène Inférieur du Bassin de Graus-Tremp-Ainsa dans un cadre séquentiel reconstruit à haute résolution. Le couplage des approches stratigraphiques et géochimiques/minéralogiques permet d’évaluer la part des forçages tectoniques, climatiques, eustatiques et diagénétiques sur l’enregistrement sédimentaire et minéralogique du bassin. La caractérisation de la minéralogie repose sur un calcul automatisé utilisant la géochimie multi-élémentaire et calibré ponctuellement par les outils
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49

Bibonne, Romain. "Sédimentologie et stratigraphie des séries clastiques du Trias inférieur à moyen du bassin de Ghadamès et de la Jeffara (Tunisie et Libye)." Thesis, Strasbourg, 2014. http://www.theses.fr/2014STRAH020.

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L’ouverture de l’Océan Néotéthys au nord du bassin de Ghadamès et de la Jeffara s’accompagne d’une phase d’extension. Ceci engendre une phase de subsidence qui se traduit par le dépôt des premières séries syn-rift d’âges Permien moyen à supérieur (formation El Watiah) et Trias inférieur à moyen (formations Bir el Jaja, Ouled Chebbi et Ras Hamia/Kirchaou). Cette étude propose la compréhension de l’architecture stratigraphique et séquentielle des formations triasiques détritiques, et de la partie supérieure clastique de la formation El Watiah. 221 puits et 18 coupes sédimentologiques de terrain
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Grieswald, Heike. "Ablagerungsfazies der Grobklastika der oberen Halle-Formation." Master's thesis, Technische Universitaet Bergakademie Freiberg Universitaetsbibliothek "Georgius Agricola", 2016. http://nbn-resolving.de/urn:nbn:de:bsz:105-qucosa-204756.

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Die Sedimente des Halleschen Permokarbonkomplexes gaben schon immer Raum für Spekulationen. Aufgrund ihrer Dominanz an rhyolithischen Geröllen wurden sie über einen langen Zeitraum einheitlich als Postporphyrschutt ausgehalten. Vielfältig wechselnde Faziesbedingungen machten es jedoch notwendig, die Sedimente aufzugliedern. Neuere Erkenntnisse in der Erforschung des Halleschen Permokarbonkomplexes erfordern eine Überprüfung v. a. der nach KUNERT (1995) aufgestellten allgemeinen stratigraphischen Gliederung der Unterrotliegendsedimente in Halle,- Hornburg,- Sennewitz- und Brachwitz-Formation an
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