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Teses / dissertações sobre o tema "Sedimentary"

Autor: Grafiati

Publicado: 4 de junho de 2021

Última modificação: 25 de julho de 2025

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1

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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2

Souza, Agda Eunice de [UNESP]. "Argilominerais: influência dos aditivos (cinza de bagaço de cana-de-acúcar e rocha sedimentar) no processo de sinterização." Universidade Estadual Paulista (UNESP), 2008. http://hdl.handle.net/11449/88494.

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Made available in DSpace on 2014-06-11T19:23:30Z (GMT). No. of bitstreams: 0 Previous issue date: 2008-06-20Bitstream added on 2014-06-13T18:09:40Z : No. of bitstreams: 1 souza_ae_me_bauru.pdf: 2026557 bytes, checksum: 7c154df4043c97f750918f33c97e250f (MD5)<br>Foi estudada a influência de cinza de bagaço de cana e rocha sedimentar, adicionadas a um material argiloso, durante o processo de sinterização. O material argiloso e os aditivos foram caracterizados utilizando Difratometria de Raio X, Espectrometria de flurescência de Raio X e Análise Térmica. As amostras de cinza e rocha foram moídas

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3

Souza, Agda Eunice de. "Argilominerais : influência dos aditivos (cinza de bagaço de cana-de-acúcar e rocha sedimentar) no processo de sinterização /." Bauru : [s.n.], 2008. http://hdl.handle.net/11449/88494.

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Resumo: Foi estudada a influência de cinza de bagaço de cana e rocha sedimentar, adicionadas a um material argiloso, durante o processo de sinterização. O material argiloso e os aditivos foram caracterizados utilizando Difratometria de Raio X, Espectrometria de flurescência de Raio X e Análise Térmica. As amostras de cinza e rocha foram moídas, peneiradas a 0,088 mm e 0,125 mm, respectivamente, e incorporadas nos teores de 0, 20, 40, 60 e 80% em massa ao material argiloso. Foram preparados corpos de prova, prensados uniaxialmente a 19 Mpa, para cada corpo de prova, em uma prensa manual. As peç

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4

Newman, Robert. "Mechanics of sedimentary basin extension." Thesis, University of Oxford, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.305480.

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5

Wilson, N. P. "Thermal studies in sedimentary basins." Thesis, University of Cambridge, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.383208.

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6

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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7

Turner, Jonathan David. "The subsidence of sedimentary basins." Thesis, University of Edinburgh, 1997. http://hdl.handle.net/1842/13150.

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Theoretical models for the evolution of extensional sedimentary basins make a number of simple, testable predictions for subsidence behaviour. These are that active extension (the syn-rift) will generally be accompanied by rapid subsidence on the downthrown side of normal faults. Once faulting has ceased (the post-rift) the entire basin is predicted to subside at an exponentially decreasing rate, driven by the cooling and thickening of the lithosphere. The aim of this thesis is to determine the significance of second-order departures from this predicted subsidence. Three periods of North Sea s

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8

Symons, William Owen. "Sedimentary processes in submarine canyons." Thesis, University of Southampton, 2017. https://eprints.soton.ac.uk/416834/.

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Submarine canyons are one of the most dramatic morphological features on continental margins and enable sediment transport from the shelf to the deep sea; however, the exact processes operating within submarine canyons are poorly understood. Much of our understanding of the dynamics of sediment-laden flows in submarine canyons results from making inferences from the deposits that they leave behind in the geological record. This thesis aimed to better understand what deposits can reveal about flow processes and ultimately to test the validity of this approach for reconstructing flow dynamics. T

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9

Bastow, Trevor. "Sedimentary Processes Involving Aromatic Hydrocarbons." Thesis, Curtin University, 1998. http://hdl.handle.net/20.500.11937/833.

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Sedimentary organic matter contains many compounds that have no obvious biogenic precursors, so their formation and occurrence are of geochemical interest. The first part of this thesis (chapters 2-5) discusses the results obtained from studying hydrocarbon racemates. Some of the compounds identified are also suggested as intermediates in the formation of alkylnaphthalenes identified in chapters 6-7. The second part of this thesis (chapters 6-11) covers the identification of a range of alkylnaphthalenes and alkylphenanthrenes in sedimentary organic matter. Possible pathways for the formation o

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10

Bastow, Trevor. "Sedimentary Processes Involving Aromatic Hydrocarbons." Curtin University of Technology, School of Applied Chemistry, 1998. http://espace.library.curtin.edu.au:80/R/?func=dbin-jump-full&object_id=9379.

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Sedimentary organic matter contains many compounds that have no obvious biogenic precursors, so their formation and occurrence are of geochemical interest. The first part of this thesis (chapters 2-5) discusses the results obtained from studying hydrocarbon racemates. Some of the compounds identified are also suggested as intermediates in the formation of alkylnaphthalenes identified in chapters 6-7. The second part of this thesis (chapters 6-11) covers the identification of a range of alkylnaphthalenes and alkylphenanthrenes in sedimentary organic matter. Possible pathways for the formation o

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11

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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12

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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13

Bashir, Firdous Zahra. "Molecular characterization of sedimentary organic matter." Thesis, University of Newcastle Upon Tyne, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.246697.

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14

Harrison, Fiona Anne. "Seismic response to sedimentary facies variation." Thesis, University of Aberdeen, 1997. http://digitool.abdn.ac.uk/R?func=search-advanced-go&find_code1=WSN&request1=AAIU089772.

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This project investigates the seismic response to facies variation by modelling facies variation itself, using two different modelling techniques, and then by modelling the seismic response to this variation. This study looks at a new set of attributes, examines their potential both as standard seismic attributes (a qualitative approach), and uses geostatistical analysis to further develop the ability of these attributes to differentiate the seismic response to facies variation. Sedpak, a basin modelling package was used to try to create facies models as a basis for further geophysical modelli

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15

Mahamod, Yusuff. "Sedimentary processes in the Dwyryd Estuary." Thesis, Bangor University, 1989. https://research.bangor.ac.uk/portal/en/theses/sedimentary-processes-in-the-dwyryd-estuary(ca0aea23-480c-4032-ba10-12a9adee740c).html.

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This study aims to describe and quantify the important sedimentary processes which control the dispersal and accumulation of sediment in the Dwyryd Estuary, adjacent to Tremadog Bay in West Wales. It is shown that sedimentation in the estuary is dominantly control by fast tidal currents, and in the bay by weak tidal currents. Landward transport of coastal sediments by tidal currents is the residual sediment transport path. The spatial distribution of textural parameters of the estuarine sediments is related to the strength of tidal currents as well as the morphology and bathymetry of the study

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16

Lee, Jimin. "Earthquake site effect modeling in sedimentary basins using a 3-D indirect boundary element-fast multipole method." Diss., Online access via UMI:, 2007.

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17

Rahman, Mohammad Wahidur Uddin Ashraf. "Sedimentation and tectonic evolution of Cenozoic sequences from Bengal and Assam foreland basins, eastern Himalayas." Auburn, Ala, 2008. http://repo.lib.auburn.edu/EtdRoot/2008/SUMMER/Geology_and_Geography/Thesis/Rahman_Mohammad_54.pdf.

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18

Purvis, Martin. "The late Tertiary-Recent tectonic-sedimentary evolution of extensional sedimentary basins of the northern Menderes massif, West Turkey." Thesis, University of Edinburgh, 1999. http://hdl.handle.net/1842/12815.

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Tethyan suture zones commonly undergo a change from compression to extension shortly after suturing. The mechanics and timing of this change in tectonic regime are poorly understood, and the extensional sedimentary basins of west Turkey, and , in particular, the northern Menderes massif, provide an excellent natural laboratory for the study of the crustal response to these different processes. During this study, field observations of sedimentary, structural and lithological features of the Alasehir Graben, Gördes and Selendi Basins, and their surroundings were combined with new radiometric age

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19

Noll, Christian John. "A geological framework for temporal sedimentary dynamics." [College Station, Tex. : Texas A&M University, 2008. http://hdl.handle.net/1969.1/ETD-TAMU-2354.

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20

Velasco, Mansilla Domitila Violeta. "GIS-based hydrogeologica platform for sedimentary media." Doctoral thesis, Universitat Politècnica de Catalunya, 2013. http://hdl.handle.net/10803/135005.

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The detailed 3D hydrogeological modelling of sedimentary media that form important aquifers is very complex because of: (1) the natural intrinsic heterogeneity of the geological media, (2) the need for integrating reliable 3D geological models that represent this heterogeneity in the hydrogeological modelling process and (3) the scarcity of comprenhensive tools for the systematic management of spatial and temporal dependent data. The first aim of this thesis was the development of a software platform to facilitate the creation of 3D hydrogeological models in sedimentary media. It is composed

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21

Borge, Hans. "Fault controlled pressure modelling in sedimentary basins /." Doctoral thesis, Norwegian University of Science and Technology, Department of Mathematical Sciences, 2000. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-1763.

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<p>The starting point for this Dr. Ing. thesis was the requirement for models describing basin scale overpressure for use in basin modelling studies. It is necessary to identify, understand and describe both the generating mechanisms and the fluid flow in sedimentary basins in order to meet this requirement.</p><p>All of the models developed are based upon a study area consisting of fault bounded pressure compartments. A reservoir simulator has applied a lateral cross fault transmissibility model and by defining the overpressure history in some of the pressure compartments it has been possible

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22

Dempsey, Alexandra C. "Global Evaluation of Platform-Top Sedimentary Features." NSUWorks, 2013. http://nsuworks.nova.edu/occ_stuetd/170.

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Remote sensing has transformed coral reef science in the last decades. It is now possible to audit reef health and geomorphology at global scale and very high spatial resolution. This work utilizes the vast and no-cost archive of imagery housed within Google Earth (GE). GE was used to interrogate the morphometric properties (size, shape, complexity, etc) of the components that combine to yield a reef environment (reef structures, sediment sheets, and so forth). The data populated a morphometric database for reefs globally that are partitioned by their architecture. The database has been invest

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23

Cromack, Marianne. "A glacial sedimentary system in northwest Spitzbergen." Thesis, University of Cambridge, 1991. https://www.repository.cam.ac.uk/handle/1810/268051.

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The record of climate change in Signedalen and Krossfjorden, northwest Spitsbergen, since the Late Weichselian glacial maximum, has been constructed using an integrated analysis of lacustrine, terrestrial and marine sediments. Thirty-four piston cores were taken from two series of linked lakes in Signedalen, fed by three small cirque glaciers. Six further cores were taken from the fjord inlet, Signehamna, into which meltwater from the linked glacier-fed lakes and a further two glaciers drain. Signehamna drains into Lilliehookfjorden, which with Mollerfjorden, combines to form Krossfjorden, fro

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24

Morgan, Ruth. "Forensic geoscience : sedimentary materials in forensic enquiry." Thesis, University of Oxford, 2007. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.439810.

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25

Holden, Vanessa Judith Claire. "Sedimentary accretion of the north Sefton coast." Thesis, Lancaster University, 2008. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.493264.

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The response of salt marshes to sea level rise is dependent upon the availability of an adequate sediment supply and the subsequent rate of accretion of sediment on the salt marsh surface. On the north Sefton coast, the geomorphology and sedimentology of the area has resulted in the continued expansion of salt marsh within the outer reaches of the Ribble Estuary, enhanced by human activities over the last 200 years. The area has undergone significant human alteration in that time.

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Paulsen, Geir. "GPU Computing for Efficient Sedimentary Basin Simulations." Thesis, KTH, Numerisk analys, NA, 2014. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-148169.

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This paper presents PDEs that describes sedimentation by a system of diffusion and transportation equations. These PDEs are implemented with a semi-implicit scheme and solved on a Graphics Processing Unit (GPU). The equations are solved with the iterative solvers (conjugate gradient and biconjugate gradient stabilized method) provided by the software ViennaCL. The timings from these operations are compared with a CPU implementation. Before using the iterative solvers, a sparse matrix and a right hand side vector is set. The sparse matrix and the right hand side vector are efficiently updated o

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27

Lee, Simon Edward. "Sedimentary processes recorded by continental slope morphology." Thesis, University of Bristol, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.398697.

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28

Alzaylaie, Marwan. "Stiffness and strength of Dubai sedimentary rock." Phd thesis, Institut und Versuchsanstalt für Geotechnik der Technischen Universität Darmstadt, 2018. https://tuprints.ulb.tu-darmstadt.de/8153/1/Alzaylaie%282017%29_DissNr102.pdf.

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Safety, optimisation and the sustainability are the most important aspects for the design of any foundation system. An optimised and safe design of foundation systems for high-rise structures in difficult soil and groundwater conditions is based on a reduction of construction material used, construction time spent, energy consumed and the adequate consideration of the soil-structure interaction. This is also important for the high-rise structures like skyscrapers and bridge piers in Dubai, UAE. Due to the large loads most of these structures are founded in the Dubai sedimentary rock. Up to now

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DI, CAPUA ANDREA. "Volcanism vs tectonics in the sedimentary record." Doctoral thesis, Università degli Studi di Milano-Bicocca, 2015. http://hdl.handle.net/10281/75294.

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Il significato del materiale vulcaniclastico in bacini ricchi in sequence torbiditiche sembra essere assodato ed ambiguo nello stesso tempo. Il problema si pone quando il sistema area sorgente-bacino depositionale non risulta perfettamente preservato e/o differenti cicli magmatici sono registrati nel record stratigrafico, e risulta pragmaticamente difficile interpretare il segnale vulcaniclastico. Il problema principale riguarda discriminare la produzione di sedimento sin-magmatica da quella post-magmatica, tettonicamente controllata, nei depositi distali. In questo lavoro abbiamo preso in con

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Sieger, Danielle. "Re-examination of changes in fluvial stacking pattern across the p-t boundary in the central transantarctic mountains, Antarctica." Thesis, The University of Wisconsin - Milwaukee, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=1548394.

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<p> A change in fluvial style and a change in the stacking pattern of fluvial channel sandstone bodies occur across the Buckley&square;Fremouw formational contact in the central Transantarctic Mountains in Antarctica. Strata in the Buckley Formation are characterized by thick floodplain deposits in the Middle to Upper Permian Buckley Formation; whereas, stacked interconnected sandstone bodies occur in the Triassic Fremouw Formation (Barrett et al., 1986; Isbell & Macdonald, 1991a, 1991b; Collinson et al., 1994; Isbell et al., 1997; 2005). Such changes in fluvial stacking patterns have be

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31

Morse, Trevor John. "Biostratigraphical constraints (calcareous nannofossils) on the Late Cretaceous to Late Miocene evolution of S.W. Cyprus." Thesis, Durham University, 1996. http://etheses.dur.ac.uk/1565/.

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Coolidge, Kyle Marvin. "Phosphorus Cycling in Maine Lakes: A Sedimentary Analysis." Fogler Library, University of Maine, 2004. http://www.library.umaine.edu/theses/pdf/CoolidgeKM2004.pdf.

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McCarthy, Laura Anne. "South Australian sedimentary opals : evidence for syngenetic deposition /." Title page, contents and abstract only, 2001. http://web4.library.adelaide.edu.au/theses/09SB/09sbm1234.pdf.

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Ferrero, Charlie David. "Stochastic modelling of thermal histories in sedimentary basins." Thesis, Imperial College London, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.408156.

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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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Husain, Mohd Lokman bin. "Salt marsh sedimentary response to sea level rise." Thesis, University of Hull, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.384865.

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Edwards, G. R. H. "Inverse modelling of extensional sedimentary basins and margins." Thesis, University of Cambridge, 2006. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.598779.

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In this dissertation, a fully depth-dependent 2D kinematic model of the lithosphere is developed. This forward model forms the basis of an inversion scheme capable of recovering the temporal and spatial strain rate history of a basin from present-day observed stratigraphic and subsidence data. The inversion scheme does not assume any <i>a priori </i>form for the strain rate distribution and unlike previous inversion schemes does not assume that the strain rate is invariant with depth (White and Bellingham, 2002). The depth-dependent inversion is applied to two sedimentary basins. Data from th

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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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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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Hutchison, John. "Structural studies of sulphur-rich sedimentary organic matter." Thesis, University of Bristol, 1990. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.303759.

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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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Parke, Jeffrey Robert. "Active tectonic and sedimentary processes in Western Turkey." Thesis, University of Cambridge, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.621363.

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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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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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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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Ertel, John Richard. "The lignin geochemistry of sedimentary and aquatic humic substances /." Thesis, Connect to this title online; UW restricted, 1985. http://hdl.handle.net/1773/11002.

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47

Tunnicliffe, Jon Francis. "Holocene sedimentary history of Chilliwack Valley, Northern Cascade Mountains." Thesis, University of British Columbia, 2008. http://hdl.handle.net/2429/526.

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I seek to reconstruct the balance between sediment storage and yield across multiple drainage basin scales in a large (1 230 km2) watershed in the Northern Cascade range, British Columbia and Washington. Chilliwack Valley and surrounding area has been the site of numerous studies that have detailed much of its Quaternary sedimentary history. In the present study this information is supplemented by reconstruction of the morphodynamic trajectory of the river valley though the Holocene Epoch, and development of a sediment transfer model that describes the relaxation from the Fraser glaciation. Th

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48

Rooney, Alan. "Re-Os geochronology and geochemistry of Proterozoic sedimentary successions." Thesis, Durham University, 2011. http://etheses.dur.ac.uk/621/.

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The Re-Os organic-rich sedimentary rocks (ORS) geochronometer has the potential to provide precise depositional ages and vital information on the Os isotope composition of palaeo-seawater. This thesis presents new geochronology data from Proterozoic sedimentary successions and insights into Re-Os systematics of organic-rich sedimentary rocks and petroleum products such as bitumen and oil. New Re-Os ORS geochronology from two drill cores indicate that the Proterozoic Atar Group of the Taoudeni basin, Mauritania is ~200 Ma older than previous estimates (1107 ± 12 Ma, 1109 ± 22 Ma and 1105 ± 37 M

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49

Holt, Peter Jonathan. "Subsidence mechanisms of sedimentary basins developed over accretionary crust." Thesis, Durham University, 2012. http://etheses.dur.ac.uk/3584/.

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This thesis uses forward modelling to investigate the formation of intercratonic basins upon accretionary crust. It began from the hypothesis that accretionary crust forms with a near normal thickness crust, but a thin lithosphere inherited from the terranes that compose it. After the accretion process has ceased the lithosphere stabilises and begins to cool, causing it to grow thicker and this in turn drives subsidence of the accretionary crust. A 1-D finite difference computer code was developed to model conductive heat flow through a column of cooling lithosphere and asthenosphere. To test

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50

Yang, Xin-She. "Mathematical modelling of compaction and diagenesis in sedimentary basins." Thesis, University of Oxford, 1997. http://ora.ox.ac.uk/objects/uuid:0bdc6c43-4534-4f08-97e2-8a33d6b13e61.

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Sedimentary basins form when water-borne sediments in shallow seas are deposited over periods of millions of years. Sediments compact under their own weight, causing the expulsion of pore water. If this expulsion is sufficiently slow, overpressuring can result, a phenomenon which is of concern in oil drilling operations. The competition between pore water expulsion and burial is complicated by a variety of factors, which include diagenesis (clay dewatering), and different modes (elastic or viscous) of rheological deformation via compaction and pressure solution, which may also include hysteres

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