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Dissertations / Theses on the topic 'Facies (Geology)'

Author: Grafiati

Published: 4 June 2021

Last updated: 29 July 2024

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1

Gournay, Jonas Paul. "Phylloid algal bioherms and ooid grainstones : characterization of reservoir facies utilizing subsurface data from the Aneth Platform and outcrop data along the San Juan River, Paradox Basin, southeastern Utah /." Digital version accessible at:, 1999. http://wwwlib.umi.com/cr/utexas/main.

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2

Kattah, Senira da Silva. "Controls on deposition and resulting stratal architecture of coarse-grained alluvial and near-shore facies associations /." Digital version accessible at:, 1999. http://wwwlib.umi.com/cr/utexas/main.

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3

Elwerfalli, Hamed Omar. "Facies analysis of early Tertiary carbonates of northeast Libya." Thesis, University of Southampton, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.242780.

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4

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

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5

Pedley, Antony. "Eocene foreland basin carbonatae facies, the external Sierras, Spanish Pyrenees." Thesis, Royal Holloway, University of London, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.261690.

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This thesis explores the controls on carbonate platform formation in foreland basins through a study of the facies, and depositional architecture, of the Middle Eocene Guara Limestone Formation, from the External Sierras, Northern Spain. The Guara Limestone Formation formed in a ramp environment on the Iberian foreland margin of the South Pyrenean Foreland Basin. The facies are foraminifera and algal limestones, with minor shallow marine siliciclastics. A facies model has been erected indicating 19 facies, grouped into 6 facies associations. Using these facies and associations, the evolution o

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6

Martin, Keithan. "Integrating depositional facies and sequence stratigraphy in characterizing carbonate reservoirs: Mississippian limestone, western Kansas." Thesis, Kansas State University, 2015. http://hdl.handle.net/2097/20478.

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Master of Science<br>Geology<br>Matthew W. Totten<br>The Mississippian-aged St. Louis Limestone of Western Kansas is a carbonate resource play that has been producing oil, gas, and natural gas liquids (NGL) for over 50 years. The Mississippian Limestone is made up of heterogeneous limestones with interbedded layers of porous and non-porous units, abrupt facies changes, and diagenetic alterations. These factors combine to characterize the St. Louis Limestone's internal complexity, which complicates hydrocarbon exploration. This study focuses on improving the understanding of the geometry, distr

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7

Garnes, William Thomas. "Subsurface Facies Analysis of the Devonian Berea Sandstone in Southeastern Ohio." Bowling Green State University / OhioLINK, 2014. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1415920946.

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8

Higgs, R. "A facies analysis of the Bude Formation (Lower Westphalian), SW England." Thesis, University of Oxford, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.371512.

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9

Moukhsil, Abdelali. "Géochimie, pétrologie structurale et mode de mise en place du pluton de Father, zone volcanique nord, sous-province de l'Abitibi, Canada /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1996. http://theses.uqac.ca.

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10

Lichtblau, Andreas. "Stratigraphy and facies at the south margin of the Archean Noranda Caldera." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1989. http://theses.uqac.ca.

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11

Morin, Jean. "Facies analysis of Lower Permian cyclic carbonates, west-central Ellesmere Island, Canadian Arctic." Thesis, University of Ottawa (Canada), 1992. http://hdl.handle.net/10393/7553.

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At least 36 decametre-scale, largely symmetric high-frequency cycles spanning approximately 15 Ma make up the carbonate-dominated succession of Lower Permian sequence 3 of the Sverdrup Basin in Fosheim and Hamilton peninsulas. These cycles record a rift pulse caracterized by the uplift, passive subsidence, collapse and passive subsidence of the Fosheim-Hamilton subbasin and show that during the rifting phase of the Sverdrup Basin deposition of conformity-bounded sequences was tectonically rather than eustatically controlled. The active rifting-phase of the Sverdrup Basin comprises four unconfo

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12

AlShammary, Nawaf S. "Hetergenerous oil saturation in submarine channel and adjacent facies, monterey formation, point fermin, Palos Verdes, California." Thesis, California State University, Long Beach, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=1527300.

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<p> Extreme heterogeneity in oil saturation between closely adjacent sandstone beds reflects different timing and degree of diagenesis. Understanding the distribution and origin of such heterogeneity is critical to effectively exploiting intercalated sandstone deposits within fine-grained unconventional reservoirs and in unraveling subtleties of stratigraphic traps. Sea cliff exposures at Point Fermin, California, expose a submarine channel facies within the largely hemipelagic facies. Separated by only meters, Point Fermin Sandstone is oil-saturated, whereas Altamira Shale sandstone is not. S

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13

Martin, Charlotte Ann Lesley. "The origin of massive sandstone facies in an ancient braided river deposits." Thesis, Durham University, 1995. http://etheses.dur.ac.uk/5326/.

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Lateral profiling techniques have been utilised to define the three-dimensional fluvial architecture of the Fell Sandstone Group (Arundian-Holkerian) of the Northumberland Basin, UK; the Lee-type sandstones (Morrowan-Atokan) of the central Appalachian Basin, USA; the Mansfield and Brazil Formations (Morrowan-Atokan) of the Illinois Basin, USA; and the Anisian Hawkesbury Sandstone of the Sydney Basin, Australia. These strata are characterised by sandstones of braided fluvial origin. Individual fluvial channels are dominated by downstream accreting mesoforms and macroforms, interpreted to repres

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14

Albert, Villanueva Eduard. "Facies y secuencias deposicionales mixtas carbonático-siliciclásticas del mioceno inferior de la cuenca de Falcón (Noroeste de Venezuela) como modelo exploratorio en el Caribe." Doctoral thesis, Universitat de Barcelona, 2016. http://hdl.handle.net/10803/396341.

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Las sucesiones sedimentarias mixtas carbonático-siliciclásticas del Mioceno Inferior que afloran en los márgenes norte y sur de la Cuenca de Falcón (noroeste de Venezuela) se analizaron mediante un enfoque multidisciplinario y multiescala. El análisis de cuenca presentado en esta tesis proporciona nuevos resultados e interpretaciones que se han sintetizado en un mapa geológico, un mapa paleogeográfico, paneles de correlación secuencial y cronoestratigráfica, y en modelos deposicionales y arquitectónicos de los sistemas mixtos carbonatico-siliciclásticos investigados. La evolución de la acomoda

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15

Henderson, Penny J. "Provenance and depositional facies of surficial sediments in Hudson Bay, a glaciated epeiric sea." Thesis, University of Ottawa (Canada), 1990. http://hdl.handle.net/10393/5998.

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A model for Wisconsinan glaciation and deglaciation of Hudson Bay is proposed based on depositional facies of the surficial sediments. These facies, defined on the basis of texture, composition, and acoustic character, indicate that sediment distribution is controlled primarily by Late Wisconsin glaciation. Post-glacial sedimentation is restricted to the shallow marine environment (100m deep) and involves reworking of glacially-derived sediments by rivers and/or marine currents. Deposition due to sea-ice rafting is minor. Within the glacigenic sediments, dispersal trends of distinctive litholo

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16

Llewellyn, Huw Richard. "Facies modelling of a low angle shield volcano and associated extrusive volcanics within the North Atlantic Igneous Province." Thesis, University of Aberdeen, 2015. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=230048.

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17

Lanners, Rebecca K. "Chemostratigraphy of hemipelagic facies of the montery formation and equivalent semimentary rocks, Los Angeles basin, California." Thesis, California State University, Long Beach, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=1527388.

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<p> The submarine-fan-dominated, proximal Los Angeles basin contains interstratified hemipelagic strata coeval with the widespread Miocene Monterey Formation that accumulated in other California margin basins. Although more detritalrich and containing greater abundance of plagioclase and muscovite than more distal, outboard basins, a four-part compositional zonation is recognized in the fine-grained facies, similar to the stratigraphic succession of the Santa Barbara coastal area. In ascending stratigraphic order, these include a basal interbedded calcareous-siliceous zone, a phosphatic zone,

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18

Azambuja, Filho Nilo Chagas de. "The Oligo-Miocene turbidites and associated facies of the Campos Basin, offshore Brazil." Thesis, Imperial College London, 1990. http://hdl.handle.net/10044/1/8408.

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19

Rose, Lila Eve. "Recent Sedimentation Patterns and Facies Distribution on the Waipaoa River Shelf, N.Z." W&M ScholarWorks, 2008. https://scholarworks.wm.edu/etd/1539617878.

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20

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

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21

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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22

Marroquín, Herrera Iván Dimitri. "Reservoir characterization through the application of seismic attributes : multiattribute and unsupervised seismic facies analyses." Thesis, McGill University, 2007. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=95679.

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Seismic attributes are a descriptive and quantifiable characteristic of seismic data, and so they represent subsets of the total information contained in the original seismic data. Consequently, seismic attrjbutes can be important qualitative and quantitative predictors of physical reservoir properties. Seismic attribute analysis began with the search for bright spots in the late 1960s and early 1970s. Subsequent work in the last decades has established seismic attribute analysis as a valuable tool in reservoir characterization studies. I present in this thesis two seismic attribute analyses f

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23

Ascaria, Ngakan Alit. "Carbonate facies development and sedimentary evolution of the Miocene Tacipi formation, South Sulawesi, Indonesia." Thesis, Birkbeck (University of London), 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.274389.

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24

Cripps, David W. "A facies analysis of the upper great oolite group in central and eastern England." Thesis, Aston University, 1986. http://publications.aston.ac.uk/14357/.

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25

Tyler, Jeremy Edward. "Clastic marine facies in the Ludlow of the Central Welsh Region." Thesis, University of Cambridge, 1988. https://www.repository.cam.ac.uk/handle/1810/283658.

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A wide range of clastic marine facies have been studied in the Ludlow sequences of the Central Welsh Region. By considering these sequences in a regional context it has been possible to review previous lithostratigraphic and biostratigraphic correlations used in the Central Welsh Region. This review has led to the production of a comprehensive stratigraphic framework for the Central Welsh Region, and has revealed the need for a significant revision of the biostratigraphic correlations presently in use. Analysis of facies patterns in Gorstian (Lower Ludlow) sequences has led to the recognition

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26

Dalton, Edward. "Sedimentary facies and diagenesis of the Lower Devonian Temiscouata and Fortin Formations, Northern Appalachians, Quebec and New Brunswick." Thesis, McGill University, 1987. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=63856.

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27

Van, der Linden Thérèse E. (Thérèse Elizabeth). "Depositional facies, cyclicity and sequence stratigraphy of the oligo-myocene Torquay Basin, Southeastern Australia." Thesis, The University of Sydney, 1997. https://hdl.handle.net/2123/27648.

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The Torquay Group outcrops between Bells Headland and Bird Rock, southwest of Torquay on the coast of Victoria. It formed part of the basis of the Haq et al. (1988) sealevel Curve, and has been portrayed as a classical example of sequence stratigraphic development generated by global eustatic oscillations. This study tests that assertion, based on a detailed investigation of the sedimentology and stratigraphy within the Torquay section, using mainly three cores from the larger Torquay Drilling Program, supplemented by cliff face stratigraphic sections from the present and previous stud

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28

Xu, Jingqi. "Facies and sequence stratigraphic analyses of the Upper Ordovician shales in northeast Indiana and northwest Ohio." Thesis, Indiana University, 2016. http://pqdtopen.proquest.com/#viewpdf?dispub=10142334.

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<p> The Upper Ordovician Maquoketa Group equivalent strata in Indiana and Ohio were part of a westward-thinning shale-dominant succession. Large amounts of fine-grained siliciclastics were shed from the eastern highlands during the Taconic Orogeny. </p><p> The detailed lithofacies analysis of the Upper Ordovician shales has yielded recognition of a series of genetically related sequences in a seemingly homogenous succession. The lower succession is pyritic laminated/banded organic-rich mudstone that accumulated after the onset of a major flooding event. Cryptobioturbation, bottom current rip

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29

Cassle, Christopher F. "Petrographic Analyses of Late Pennsylvanian Limestones within the Northern Appalachian Basin, USA." Ohio University / OhioLINK, 2005. http://www.ohiolink.edu/etd/view.cgi?ohiou1121435271.

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30

Wang, Dong 1963. "Continental-slope sedimentation adjacent to an ice-margin, Labrador sea : depositional facies and glacial cycles." Thesis, McGill University, 1992. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=56949.

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Analyses of 13 sediment cores and 2800 km of 3.5 kHz seismic profiles reveal that the majority of the sediments on the Labrador continental slope was deposited by hemipelagic settling and ice-rafting (53%), debris flows (7%) and turbidity currents (34%) during the Wisconsinan Glaciation. Only minor amounts (6%) are attributed to contour current activity and related processes. Eight sedimentary facies were differentiated which include (1) hemipelagic (H); (2) hemipelagic (HI) with ice-rafted detritus (IRD); (3) debris-flow deposits (subfacies D1, D2, D3), spill-over turbidite (T), headspill tur

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31

Machel, Hans-G. (Hans-Gerhard). "Facies and diagenesis of the Upper Devonian Nisku formation in the subsurface of central Alberta." Thesis, McGill University, 1985. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=71974.

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The Nisku Formation in the Alberta subsurface consists of bank facies, reefal facies, and basinal/slope facies along the Outer Shelf. The bank facies was not previously recognized, and is here designated the Dismal Creek Member. Most buildups are coral-bearing mudmounds.<br>The Nisku Formation was affected by more than twenty diagenetic processes, most notably by dolomitization and anhydritization. The buildups were partially lithified in shallow phreatic environments, and some were subaerially exposed. Dolomitization took place at depths of about 300 to 1000 m by fluids that were derived main

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32

Collier, Richard E. Ll. "Sedimentary facies evolution in Continental fault-bounded basins formed by crustal extension : the Corinth Basin, Greece." Thesis, University of Leeds, 1988. http://etheses.whiterose.ac.uk/2616/.

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Characteristic half-graben and graben geometries are generated by extensional tectonics. The sedimentary infill to such basins reflects their structural evolution. The actively extending basins of central Greece have provided an opportunity to study the mechanisms that control sediment distribution and the resultant facies patterns and geometries produced in such environments. The modern and precedent Neogene to Quaternary sediments studied, and their controlling processes, provide predictive templates for the analysis of controls acting upon ancient extensional basin fills. On a basinwide sca

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33

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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34

Kelly, Ranald. "The distribution of fluids in amphibolite and granulite facies rocks from central Madagascar and southern West Greenland." Thesis, Royal Holloway, University of London, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.313701.

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35

Harwood, C. "A facies analysis of shale-nodular limestone cycles from the Upper Ordovician of the Oslo region, Norway." Thesis, University of Liverpool, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.356265.

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36

Sanborn-Barrie, Mary. "Geology, geothermobarometry and geochronology of the high-P granulite-facies Kramanituar Complex, Western Churchill Province." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape8/PQDD_0016/NQ48336.pdf.

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37

Sanborn-Barrie, Mary Carleton University Dissertation Earth Sciences. "Geology, geothermobarometry and geochronology of the high-P granulite-facies Kramanituar Complex, Western Churchill Province." Ottawa, 1999.

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38

Khodabakhsh, Saeed. "Pleistocene Laurentide Ice Sheet drainage into the Labrador Sea : sedimentary facies, depositional mechanisms, stratigraphy and significance of Heinrich events." Thesis, McGill University, 1996. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=42067.

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On the basis of sedimentary structures and textures, six depositional facies have been identified in Labrador Slope, Rise and Basin cores. They include: (1) turbid-surface plume sediments (facies P; plumites) comprising 4% of the total length of the slope cores; (2) hemipelagic sediments (facies HI and H) with and without ice-rafted debris (IRD) (48% and 20% on the slope/rise and basin centre, respectively); (3) nepheloid-layer deposits (facies N; 9% on the slope); (4) contourites (facies C; 4% on the slope); (5) turbidite facies (30% on the slope and $>$40% on the levees of the Northwest Atla

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Davis, Laurence H. M. "Allostratigraphic interpretation of a modern coarse clastic barrier complex : depositional facies, processes and relative sea level relationships /." Internet access available to MUN users only, 2003. http://collections.mun.ca/u?/theses,60897.

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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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Elfigih, Omar Bouzid. "Regional diagenesis and its relation to facies change in the Upper Silurian, Lower Acacus formation, Hamada (Ghadames) Basin, northwestern Libya /." Internet access available to MUN users only, 2000. http://collections.mun.ca/u?/theses,50430.

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42

Cox, Richard Alexander. "Eclogite facies metamorphism of mafic and ultramafic rocks in the Tshenukutish terrane, Manicouagan Imbricate Zone, eastern Grenville Province." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp02/NQ54832.pdf.

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Petrie, Meredith Blair. "Evolution of eclogite facies metamorphism in the St. Cyr klippe, Yukon-Tanana terrane, Yukon, Canada." Thesis, The University of Iowa, 2016. http://pqdtopen.proquest.com/#viewpdf?dispub=3628428.

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<p> The St. Cyr klippe hosts well preserved to variably retrogressed eclogites found as sub-meter to hundreds of meter scale lenses within quartzofeldspathic schists in the Yukon-Tanana terrane, Canadian Cordillera. The St. Cyr area consists of structurally imbricated, polydeformed, and polymetamorphosed units of continental arc and oceanic crust. The eclogite-bearing quartzofeldspathic schists form a 30 by 6 kilometer thick, northwest-striking, coherent package. The schists consist of metasediments and felsic intrusives that are intercalated on the tens of meter scale. The presence of phe

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Smith, Roger M. H. "Fluvial facies, vertebrate taphonomy and palaeosols of the Teekloof formation (Permian) near Beaufort West, Cape Province, South Africa." Doctoral thesis, University of Cape Town, 1989. http://hdl.handle.net/11427/23646.

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The main Karoo Basin of South Africa contains a relatively continuous sequence of continental deposits that accumulated over a 100 million year period from Permo-Carboniferous (280 Ma) to early Jurassic (180 Ma). In the southwestern region of the basin the Karoo succession is approximately 4 000 m thick, the upper half of which consists of vertebrate fossil-bearing fluvial rocks of the Beaufort Group. This study deals with Lower Beaufort (Adelaide Subgroup) strata belonging to the Teekloof Formation which are exposed in the cast-west trending erosional escarpment between the towns of Beaufort

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Piché, Mathieu. "La formation de Hauy à l'ouest de Chapais ; volcanisme sub-aérien en milieu fluviatile /." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 1985. http://theses.uqac.ca.

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Mémoire (M.Sc.A.Geologie)--Université du Québec à Chicoutimi, 1985.<br>Une carte pliée, en pochette. "Mémoire présenté en vue de l'obtention de la maîtrise en sciences appliquées en géologie" CaQCU CaQCU Document électronique également accessible en format PDF. CaQCU

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Paiva, Francisco. "Fluvial facies architecture and provenance history of the Abrahamskraal-Teekloof formation transition (lower Beaufort group) in the main Karoo Basin." Master's thesis, University of Cape Town, 2016. http://hdl.handle.net/11427/20615.

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The Middle Permian lower Beaufort Group in the southern main Karoo Basin comprises of the fluvio-lacustrine Abrahamskraal and the overlying Teekloof and correlative Middleton Formations. These units are mainly made up of mudrocks with subordinate fine-grained sandstone-rich intervals. The objective of this mainly qualitative facies analysis study is the evaluation of the vertical and lateral abundances of the facies associations in order to decouple the preserved tectonic and climatic signals in the formations. The results on the stratigraphic trends should aid paleo-environmental, paleontolog

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Maseko, Phindile Pearl. "Petrophysical evaluation and characterization of sandstone reservoirs of the western Bredasdorp Basin, South Africa for well D-D1 and E-AP1." Thesis, University of the Western Cape, 2016. http://hdl.handle.net/11394/5181.

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>Magister Scientiae - MSc<br>The Bredasdorp Basin was formed consequent to extensional episodes during the initial stages of rifting in the Jurassic age. The basin acted as a local depocentre and was primarily infilled with late Jurassic and early Cretaceous shallow-marine and continental sediments. Two wells namely; D-D1 and E-AP1 were studied in order to evaluate the petrophysics and characterize sandstone reservoirs of the western Bredasdorp basin. This could be achieved by generating and comparing results from core analysis and wireline in order to determine if the two wells are comprised

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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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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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Xu, Jian-hong. "Sedimentary facies, diagenesis and petrophysical properties of the Triassic Reservoir sandstones of the Morecambe Gas Field, East Irish Sea, UK." Thesis, University of Reading, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.363404.

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