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Rozprawy doktorskie na temat „Rocks, Sedimentary”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 5 marca 2023

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1

Dodd, Matthew S. "Biosignatures in Precambrian sedimentary rocks." Thesis, University College London (University of London), 2018. http://discovery.ucl.ac.uk/10055383/.

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The overarching goal of this work was to trace the origins of organic matter as a possible biosignature for early life on Earth. This work documented the petrological, structural, isotopic, elemental and molecular properties of organic matter, in a suite of sediments ranging from the Eoarchean to the Phanerozoic. Particular attention was paid to iron formations which form a major part of the Precambrian sedimentological record. Optical and micro-Raman spectroscopy were used to document the petrological occurrences of organic matter and its associated diagenetic features. Focused ion beam and t

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2

Tavares, Sandra Aparecida Simionato 1969. "Fósseis do afloramento Santa Irene, cretácio superior da Bacia Bauru = inferências paleoecológicas." [s.n.], 2011. http://repositorio.unicamp.br/jspui/handle/REPOSIP/287322.

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Orientadores: Frésia Soledad Ricardi Torres Branco, Ismar de Souza Carvalho<br>Dissertação (mestrado) - Universidade Estadual de Campinas, Instituto de Geociências<br>Made available in DSpace on 2018-08-18T21:34:34Z (GMT). No. of bitstreams: 1 Tavares_SandraAparecidaSimionato_M.pdf: 8529535 bytes, checksum: 81caa7b6648edbc9a42d10c5ee967375 (MD5) Previous issue date: 2011<br>Resumo: O Afloramento Santa Irene tem sido considerado um dos mais significativos da Bacia Bauru, na Formação Adamantina, pela abundancia e boa conservação de fósseis associados ali encontrados, como dentes isolados de ar

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3

Malik, Qamar Mehboob. "Electrical and transport properties of sedimentary reservoir rocks." Thesis, Imperial College London, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.266398.

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4

Hattum, Marco Willem Alexander van. "Provenance of Cenozoic sedimentary rocks of northern Borneo." Thesis, Royal Holloway, University of London, 2005. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.423143.

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5

Lofts, Jeremy C. "Integrated geochemical-geophysical studies of sedimentary reservoir rocks." Thesis, University of Leicester, 1993. http://hdl.handle.net/2381/35058.

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6

Chernoff, Carlotta. "Origin and redistribution of metals in sedimentary rocks." Diss., The University of Arizona, 2002. http://hdl.handle.net/10150/289837.

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Integrated analysis of whole-rock and mineral geochemical data from black shale and metamorphosed black shale demonstrates the importance of sulfides as trace-element hosts and reveals the influence of depositional environment on whole-rock and mineral chemistries. Detailed analysis of Fe-sulfide contents provides evidence of considerable elemental redistribution during diagenesis and metamorphism, indicating that such sulfides plausibly serve as a source of metals and other elements to epigenetic fluids. Spatial and temporal analysis of the distribution of Phanerozoic black shale, phosphorite

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7

Putz-Perrier, Martin W. "Distribution and scaling of extensional strain in sedimentary rocks." Thesis, Imperial College London, 2008. http://hdl.handle.net/10044/1/1293.

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For this study, spatial and size distributions of normal faults and associated tensile fractures were directly measured in deformed sedimentary rocks in three extensional regions: Kimmeridge Bay and Kilve in the UK and the Maltese Islands. The collected data allow i) quantifcation of regional extension at different scales, ii) determination of the relative importance of large and small structures, iii) quan- tifcation of the spatial heterogeneity of brittle extension, iv) comparison of scaling laws for veins and faults belonging to the same extension event, and v) analysis of the evolution of

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8

Ruiz, Penã Franklin J. (Franklin José) 1962. "Elastic properties of sedimentary anisotropic rocks : (measurements and applications)." Thesis, Massachusetts Institute of Technology, 1998. http://hdl.handle.net/1721.1/58361.

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Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, February 1999.<br>Includes bibliographical references (leaves 75-78).<br>In multidisciplinary studies carried out in the Budare Oil Field of the Great Oficina Oil Field, there was difficulty matching well log synthetic seismograms with 2D and 3D seismic data. In addition, the seismically determined depths of reservoir horizons are greater than the well sonic log depths. To examine this discrepancy we conducted an experimental study of dynamic elastic parameters of the rocks in the oil fie

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9

Dalrymple, Mark. "Sedimentological evolution of the Statfjord Formation fluvial hydrocarbon reservoirs of the northern North Sea." Thesis, University of Aberdeen, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.302647.

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The sedimentological evolution of the Statfjord Formation of the Viking Graben at the Triassic - Jurassic transition is detailed by integration of studies of mineral assemblages, isotope age data, sedimentological core analysis, palaeosol / mineralogical wireline analysis and regional correlation of subsurface wireline information, combined with theories on basin evolution in continental settings. The aim of this study is to enhance the description of, and correlation within, hydrocarbon reservoirs developed within intra-continental alluvial sediments which have been deposited in areas above t

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10

Andrea, Martijn. "The anisotropic elastic properties of clay-rich rocks." Thesis, Imperial College London, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.243413.

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11

Kars, Myriam. "Calibration and Application of the MagEval geothermometer in sedimentary rocks." Thesis, Pau, 2012. http://www.theses.fr/2012PAUU3003/document.

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Pour évaluer la température d’enfouissement subie par les roches sédimentaires, une large gamme de géothermomètres est disponible, basés sur les constituants organiques ou minéralogiques de ces roches. Comme pour toutes les techniques expérimentales, elles présentent des avantages et des inconvénients. Dans cette thèse, nous utilisons une approche magnétique pour estimer la température d’enfouissement. Dans une première partie, nous avons étudié l’assemblage magnétique de puits sélectionnés à travers le monde pour mieux caractériser le géothermomètre magnétique MagEval. Deux calibrations ont p

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12

Harper, Emily. "Investigating Sedimentary Rocks to Understand Past Wet Climate of Mars." ScholarWorks@UNO, 2015. http://scholarworks.uno.edu/honors_theses/70.

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The “deltaic” geomorphology in the Eberswalde Crater is often considered a “smoking gun” for the warm-and-wet ancient climate of Mars. The Crater displays sedimentary features, which many argue, can only be found in a river-delta system (Bhattacharya et al., 2005). However, with the advent of high-resolution images, the Eberswalde Crater delta’s geomorphology has been revealed to be more complicated than could be seen previously. These high-resolution data suggest that the development of the Eberswalde delta is likely more episodic (Schieber 2007). While better resolution data has placed doub

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13

Key, Wendy R. O. "Fault formation in porous sedimentary rocks at high strain rates /." abstract and full text PDF (UNR users only), 2009. http://0-gateway.proquest.com.innopac.library.unr.edu/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:1464442.

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Thesis (M.S.)--University of Nevada, Reno, 2009.<br>"May 2009." Includes bibliographical references (leaves 31-37). Library also has microfilm. Ann Arbor, Mich. : ProQuest Information and Learning Company, [2009]. 1 microfilm reel ; 35 mm. Online version available on the World Wide Web.

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14

Noad, Jonathan James. "The sedimentary evolution of the tertiary of eastern Sabah, Northern Borneo." Thesis, Birkbeck (University of London), 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.369289.

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15

Robert, Rodolphe. "Analytical characterization of porous geomaterials reference assessment in some sedimentary rocks /." [S.l.] : [s.n.], 2004. http://deposit.ddb.de/cgi-bin/dokserv?idn=976457164.

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16

Sisavath, Sourith. "Fundamental pore-scale modelling of single-phase flow through sedimentary rocks." Thesis, Imperial College London, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.394470.

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17

Zwing, Alexander. "Causes and Mechanisms of Remagnetisation in Palaeozoic Sedimentary Rocks - a Multidisciplinary Approach." Diss., lmu, 2003. http://nbn-resolving.de/urn:nbn:de:bvb:19-15780.

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18

Panahi, Alireza. "Geochemistry of Precambrian paleosols and Huronian sedimentary rocks, Ontario and Québec, Canada." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0021/NQ58156.pdf.

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19

Best, Angus Ian. "The prediction of the reservoir properties of sedimentary rocks from seismic measurements." Thesis, University of Reading, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.331984.

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Recent technological advances have led to dramatic improvements in seismic resolution which now enable seismic attenuation to be measured on a routine basis. The usefulness of seismic attenuation as an interpretation parameter is restricted at present by our incomplete knowledge of the relationships between attenuation and important reservoir parameters such as porosity, permeability and the nature of the pore fluid. In order to redress this imbalance, P-wave and S-wave velocities and attenuations were measured in the laboratory at a frequency of about 0.8 MHz and at an effective pressure of 6

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20

Finlay, Alexander James. "RE–OS and PGE geochemistry of organic-rich sedimentary rocks and petroleum." Thesis, Durham University, 2010. http://etheses.dur.ac.uk/399/.

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The research in this thesis is presented in paper format with each of four chapters representing one complete study. Chapter two presents Re–Os and geochemical fingerprint data for UK Atlantic margin oils. organic and δ13C geochemical data demonstrate that the oil is sourced from Upper Jurassic marine shales and the Re–Os data yields an age of 68 ± 13 Ma. Comparison of this date with published basin histories and Ar-Ar geochronology demonstrate that Re–Os ages correspond with the timing of oil generation. Furthermore the similarities between oil and source rock 187Os/188Os at the time of oil g

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21

Henderson, Alexandra Louise. "The geology of the Indus Basin sedimentary rocks, Ladakh Himalaya, NW India." Thesis, Lancaster University, 2010. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.547983.

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22

Nunn, Jacob. "Investigations of Partial Gas Saturation on Diffusion in Low-permeability Sedimentary Rocks." Thesis, Université d'Ottawa / University of Ottawa, 2018. http://hdl.handle.net/10393/38396.

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The effect of partially saturated conditions on aqueous diffusion was investigated on the Upper Ordovician Queenston Formation shale from the Michigan Basin of southwest Ontario, Canada. Effective diffusion coefficients (De) were determined for iodide tracer on duplicate cm-scale samples from a core segment. Partially saturated conditions were created with a new gas-ingrowth method that takes advantage of the variability of N2 solubility with pressure. The method is designed to create partially saturated pores, quantify the level of partial gas/brine saturation within the tracer-accessible por

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23

Halsall, Carol Elaine. "The relationship between intrusive magmatism, volcanism, and massive sulphide mineralisation at Rio Tinto, Spain." Thesis, Imperial College London, 1989. http://hdl.handle.net/10044/1/8894.

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24

Shakeel, Ahmed. "The effect of oriented fractures on elastic wave velocities, attenuation and fluid permeabilities of sandstones." Thesis, Imperial College London, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.318186.

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25

North, C. P. "Structure and sedimentology of the Mercia Mudstone Group (Upper Triassic), Severn Estuary region, SW Britain." Thesis, University of Bristol, 1988. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.233789.

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26

McCune, Julian Glenn. "Cenozoic sedimentary evolution of the Helmville Basin, west-central Montana." CONNECT TO THIS TITLE ONLINE, 2008. http://etd.lib.umt.edu/theses/available/etd-05282008-101831/.

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27

Vieira, Lucas Valadares. "Arquitetura de fáceis e estratigrafia de sequências em alta resolução do sistema eólico fluvial e marinho raso da Formação Piauí, carbonífero da Bacia do Parnaíba, Brasil." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2018. http://hdl.handle.net/10183/182022.

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A Formação Piauí registra a deposição de um sistema eólico, fluvial e marinho raso acumulado em uma bacia de sinéclise intracratônica. A caracterização das associações de fácies e do arcabouço estratigráfico foi feito através de uma descrição detalhada das fácies sedimentares e levantamento de perfis de afloramentos. As fácies foram classificadas de acordo com a textura dos grãos (tamanho e seleção) e estruturas sedimentares observadas. Medidas de paleocorrentes foram feitas nas estratificações e laminações cruzadas. Os perfis foram medidos na escala 1:50 em locais com boa exposição vertical.

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Minehan, Kathleen. "Paleotectonic setting of Takla Group volcano-sedimentary rocks Quesnellia, North Central British Columbia." Thesis, McGill University, 1989. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=59412.

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Upper Triassic Takla Group rocks occur in Quesnellia and Stikinia, two allochthonous terranes of the Canadian Cordillera. The terranes are separated by the major, north-northwest trending, dextral transcurrent Findlay fault. The stratigraphy of the study area, east of the fault in Quesnellia, is comprised of interlayered volcaniclastic, volcanic, and sedimentary rocks. The strata have been intruded by abundant dykes, a felsic pluton, and satellite intrusions of an Alaskan-type ultramafite. Volcaniclastic rocks range from basic to felsic compositions and were deposited by several pyroclastic fl

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Hill, Kristina M. "Diagenetic and compositional controls of wettability in siliceous sedimentary rocks, Monterey Formation, California." Thesis, California State University, Long Beach, 2015. http://pqdtopen.proquest.com/#viewpdf?dispub=1587286.

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<p> Modified imbibition tests were performed on 69 subsurface samples from Monterey Formation reservoirs in the San Joaquin Valley to measure wettability variation as a result of composition and silica phase change. Contact angle tests were also performed on 6 chert samples from outcrop and 3 nearly pure mineral samples. Understanding wettability is important because it is a key factor in reservoir fluid distribution and movement, and its significance rises as porosity and permeability decrease and fluid interactions with reservoir grain surface area increase. Although the low permeability sil

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Chen, Guohui. "Provenance-related studies of Triassic-Miocene Tethyan sedimentary and igneous rocks from Cyprus." Thesis, University of Edinburgh, 2018. http://hdl.handle.net/1842/33185.

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Cyprus comprises three tectono-stratigraphic terranes: first, the Troodos Massif made up of Late Cretaceous oceanic lithosphere and its sedimentary cover in the centre of the island; secondly, the Mamonia Complex (and Moni Melange) a passive margin lithological assemblage in the west (and south) and thirdly, the Kyrenia Range, an active margin lithological assemblage in the north. This study focuses on the sedimentary cover of the Troodos Ophiolite in W Cyprus, the Triassic-Cretaceous sedimentary rocks of the Mamonia Complex and Late Cretaceous-Miocene igneous and sedimentary rocks in the Kyre

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31

Bouchard, Laurianne. "Rb-Sr Age Estimates of Pore Fluids in Sedimentary Rocks, DGR Site, Kincardine, Ontario." Thesis, Université d'Ottawa / University of Ottawa, 2015. http://hdl.handle.net/10393/32271.

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This study is part of a project aiming for the long-term burying of nuclear wastes in Kincardine, Ontario. Bedrock formations as well as their associated waters were analyzed in drill cores from the Michigan sedimentary basin, southwest Ontario. This research utilizes geochemistry combined to strontium and rubidium isotope ratios in order to determine the origin of porewaters from Ordovician shales and limestones. It is demonstrated that these waters are the result of a mixing line between the Silurian (Guelph) and Cambrian groundwaters. This last end-member was also mixed with Precambrian bri

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32

Wang, Wei, and 王伟. "Sedimentology, geochronology and geochemistry of the proterozoic sedimentary rocks in the Yangtze Block, South China." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2013. http://hdl.handle.net/10722/196033.

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The South China Craton comprises the Yangtze Block in the northwest and Cathaysia Block in the southeast. Located in the southeastern Yangtze Block, the Jiangnan Orogen formed through the amalgamation between the Yangtze and Cathaysia Blocks. The Yangtze Block has sporadically exposed Archean rocks in the north, Paleoproterozoic to Mesoproterozoic volcano-sedimentary sequences in the southwest and widespread Neoproterozoic sedimentary sequences accompanied by syn-sedimentary igneous rocks on the western and southeastern margins. The late Paleoproterozoic to early Mesoproterozoic Dongchuan, Da

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33

Zhang, Xiping. "Geochemical exploration for polymetallic ores in volcano-sedimentary Rocks : studies in China and Finland /." Oulu : Oulun Yliopisto, 2000. http://herkules.oulu.fi/isbn9514257871.

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Legault, Marc Ian. "Petrology and geochemistry of Timiskaming Group sedimentary rocks, Kirkland Lake area, Abitibi greenstone belt." Thesis, University of Ottawa (Canada), 1993. http://hdl.handle.net/10393/6510.

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The Timiskaming Group is a late Archaean syn-tectonic lithological unit which lies unconformably on greenstone-belt volcanic rocks and consists of an alluvial-fluvial assemblage intercalated with alkalic volcanic rocks and a turbidite assemblage. The fine-grained sedimentary rocks of the alluvial-fluvial assemblage and turbidite north unit have similar mineralogical and chemical compositions such as high SiO$\sb2$, U, Th and total rare-earth elements (REE). The turbidite south unit has high Fe$\sb2$O$\sb{3(\rm tot)}$, MgO, TiO$\sb2$, Cr and Ni. Petrographic and geochemical examinations of clas

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35

Gunawan, Indra. "Mesozoic and Cenozoic siliciclastic sedimentary rocks of the Bird's head of new Guinea, Indonesia." Thesis, University of London, 2013. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.603458.

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The Bird's Head area of New Guinea is underlain by Australian continental crust and has a relatively complete Palaeozoic to Recent stratigraphic record . There are a number of siliciclastic dominated formations which include the Mesozoic Tipuma Formation and the Cenozoic Sirga, Klasafet, Klasaman. and Steenkool Formations. The aim of this study was to investigate their provenance, date them better, and interpret their significance for the history of New Guinea. New fieldwork was carried out, complemented by analysis of light and heavy minerals, X-ray diffraction of clay minerals, U-Pb zircon g

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36

Abdullah, Wan Hasiah. "A regional organic geochemical evaluation of sedimentary rocks of Spitsbergen and their hydrocarbon potential." Thesis, University of Newcastle Upon Tyne, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.386050.

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Mustard, Peter Steele Carleton University Dissertation Geology. "Upper proterozoic-lower cambrian sedimentary rocks of the Mount Harper group, Ogilvie mountains, Yukon." Ottawa, 1990.

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Souza, André Alves de. "Estudo de propriedades petrofísicas de rochas sedimentares por Ressonância Magnética Nuclear." Universidade de São Paulo, 2012. http://www.teses.usp.br/teses/disponiveis/88/88131/tde-26072012-161426/.

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A Ressonância Magnética Nuclear (RMN) é uma das técnicas mais versáteis de investigação científica experimental, com destaque para o estudo da dinâmica, estrutura e conformação de materiais. Em particular, sua utilização na ciência do petróleo é uma de suas primeiras aplicações rotineiras. Metodologias desenvolvidas especificamente para atender esta comunidade científica mostraram-se desde cedo muito úteis, sendo o estudo da interação rocha/fluido uma de suas vertentes mais bem sucedidas. Desde então, importantes propriedades petrofísicas de reservatórios de óleo e gás têm sido determinadas e

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Baskerville, Stuart Linsey. "The Carboniferous (Courceyan-Chadian) sedimentary facies mosaic of the Keel-Ardagh area of County Longford, Eire." Thesis, University of South Wales, 1998. https://pure.southwales.ac.uk/en/studentthesis/the-carboniferous-courceyanchadian-sedimentary-facies-mosaic-of-the-keel-ardagh-area-of-county-longford-eire(494fa07a-0492-496c-b3f3-913a96732ef9).html.

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The stratigraphic relationships and sedimentary environments of the Silurian, Devonian and Lower Carboniferous lithologies in the Keel area are deduced and described. This was accomplished by the analysis of over 10.000M. of diamond drilled core from the area. The oldest rocks are Silurian shales with turbidites. Deposition was in forearc basins in an active subduction zone on the north margin of lapetus. The area was one of net erosion in the Lower Devonian following the continental collision which closed lapetus. The Upper Devonian of the area is represented by the Microconglomerate lying un

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Keene, David G. "An analysis of fracture systems, lithologic character and kinematic history of Paleozoic rock formations in a portion of southeastern Indiana." Virtual Press, 1989. http://liblink.bsu.edu/uhtbin/catkey/722793.

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This is an analysis of fractures occurring within the Paloezoic sedimentary rocks in a portion of southeastern Indiana. Fifteen hundred seventy-two fractures were used in analysis of distribution, orientation, pervasiveness, persistence, and intensity. The data collected is representative of eight counties and seventeen different collection sites.All fracture data were given an associated numerical value identifying each variable used for analysis and recorded into computer data files. A computer program was used for statistical analysis and construction of equal area nets which graphically di

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41

Peterson, John Aaron. "Geochemical Provenance of Clastic Sedimentary Rocks in the Western Cordillera: Utah, Colorado, Wyoming, and Oregon." DigitalCommons@USU, 2009. https://digitalcommons.usu.edu/etd/439.

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Sedimentary rocks are an important source of information about previous orogenic conditions and the composition of which may describe the evolution of provenance and tectonic setting. Many factors influence sediment composition, namely, source rock composition, chemical weathering, climate, transport burial, and diagenesis. As the sediment composition changes through time, the geochemical characteristics of the sediment can be used to understand its geologic history. The geochemical characteristics of clastic sedimentary rocks are useful in determining the depositional setting and its associ

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Beasley, Justin M. "Geochemistry and fluid evolution of a carboniferous-hosted sphalerite breccia deposit, Isle of Man." Diss., Columbia, Mo. : University of Missouri-Columbia, 2008. http://hdl.handle.net/10355/6524.

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Thesis (M.S.)--University of Missouri-Columbia, 2008.<br>The entire dissertation/thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file (which also appears in the research.pdf); a non-technical general description, or public abstract, appears in the public.pdf file. Title from title screen of research.pdf file (viewed July 14, 2009). Includes bibliographical references.

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43

Grobbelaar, Mareli. "A comparison between diamictites at the Witteberg-Dwyka contact in southern South Africa." Thesis, Stellenbosch : Stellenbosch University, 2015. http://hdl.handle.net/10019.1/97091.

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Thesis (MSc)--Stellenbosch University, 2015.<br>ENGLISH ABSTRACT: Diamictites are sedimentary deposits that originate from a number of different environments, the most common being associated with a glacial environment. Although this association is not, in all cases correct, it is still being used due to the lack of knowledge to confidently identify, classify and interpret a depositional environment for diamictite deposits. During the late Carboniferous to early Permian, two diamictite deposits formed during the development of the Cape Basin and Main Karoo Basin in the southern margins of Sou

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Bath, Octavia. "Provenance of Siliclastic Sedimentary Rocks in the Eastern Portion of the North Caribou Greenstone Belt." Thesis, Université d'Ottawa / University of Ottawa, 2017. http://hdl.handle.net/10393/36115.

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The Zeemal Heaton Lake metasedimentary assemblage comprises ~50% of the eastern limb of the North Caribou greenstone belt, which hosts the Musselwhite gold deposit (~ 5.4 Moz Au). The metasedimentary assemblage is divided into two based on their distribution: the Central-belt and North-rim of the belt. The Zeemal Heaton Lake metasedimentary rocks have been interpreted to represent a turbidite succession, consisting of pelite, arkose, wacke and conglomerate. Detrital U-Pb zircon age populations from this study indicate variable sources in the Central-belt metasediments with a maximum age of dep

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Papp, Matthias Laszlo. "A study of Neoproterozoic-Cambrian sedimentary rocks of the Nagur basin in Marwar, Rajasthan, India." Thesis, University College London (University of London), 2013. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.590576.

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Abdi, Hadj. "Mechanical and Hydromechanical Behavior of Host Sedimentary Rocks for Deep Geological Repository for Nuclear Wastes." Thèse, Université d'Ottawa / University of Ottawa, 2014. http://hdl.handle.net/10393/30924.

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Sedimentary rocks are characterized with very low permeability (in the order of 10-22 m2), low diffusivity, a possible self-healing of fractures, and a good capacity to retard radionuclide transport. In recent years, sedimentary rocks are investigated by many research groups for their suitability for the disposal of radioactive waste. Development of deep geologic repositories (DGRs) for the storage of radioactive waste within these formations causes progressive modification to the state of stress, to the groundwater regime, and to the chemistry of the rock mass. Thermal effects due to the ongo

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Hall, Dwight Lyman 1953. "Stratigraphy and sedimentary petrology of the Mesozoic rocks of the Waterman Mountains, Pima County, Arizona." Thesis, The University of Arizona, 1985. http://hdl.handle.net/10150/558034.

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Falck, Hendrik Carleton University Dissertation Geology. "Volcanic and sedimentary rocks of the Yellowknife Bay Formation, Giant Section, Yellowknife Greenstone Belt, NWT." Ottawa, 1990.

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Cullen, R. D. "Structural geology and metamorphism of archean volcanic and sedimentary rocks at Fenton Lake, Slave Province, N.W.T." Thesis, University of Ottawa (Canada), 1989. http://hdl.handle.net/10393/5794.

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Haughton, David Lindsay. "The development and distribution of sedimentary rocks in the Rangal Coal Measures, South Blackwater, Central Queensland." Thesis, Queensland University of Technology, 1986. https://eprints.qut.edu.au/35984/1/35984_Haughton_1986.pdf.

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An investigation of the elastic interseam sedimentary rocks has elucidated the depositional and contemporaneous tectonic history of the Upper Permian Rangal Coal Measures at the C.S.R. South Blackwater Mine, Central Queensland, The studied section is stratigraphically bound by the Orion and Aries coal seams. The approximately 84 square km study area is located on the eastern flank of the Comet Ridge, within the Bowen Basin. The geological data used in this study consists of Qorehole information, approximately derived 2800 from bores, a geological and detailed database, containi

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