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Dissertations / Theses on the topic 'Stratigraphic log'

Author: Grafiati

Published: 9 September 2021

Last updated: 29 July 2025

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1

Muslim, Mohanad Z. "A Sequence Stratigraphic Analysis of the Berea Sandstone in Athens County, Ohio." Ohio University / OhioLINK, 2014. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou1399291939.

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Harbi, Hussein M. "2-D MODELING OF SOUTHERN OHIO BASED ON MAGNETIC FIELD INTENSITY, GRAVITY FILED INTENSITY AND WELL LOG DATA." University of Akron / OhioLINK, 2005. http://rave.ohiolink.edu/etdc/view?acc_num=akron1125523809.

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3

O'Neal, Ryan J. "Seismic and well log attribute analysis of the Jurassic Entrada/Curtis interval within the North Hill Creek 3D seismic survey, Uinta Basin, Utah : case history /." Diss., CLICK HERE for online access, 2007. http://contentdm.lib.byu.edu/ETD/image/etd2017.pdf.

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4

Oehmig, Reinhard. "Petrographie und Log-Daten einer klastischen Rotliegend/Buntsandstein folge /." Heidelberg : [Ruprecht-Karls-Universität], 1988. http://catalogue.bnf.fr/ark:/12148/cb37429955c.

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5

Cousineau, Lyssa A. "Stratigraphy of Quaternary Dunes by Sand Mineralogy and Pedogenic Features, Los Osos, California." DigitalCommons@CalPoly, 2012. https://digitalcommons.calpoly.edu/theses/827.

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The goal of this study was to assess mineralogy and pedogenic features of sand dunes in a stratigraphic sequence. The purpose was to determine whether these features significantly differ to reflect age differences with depth within the sequence. This study was conducted in Montaña de Oro State Park, located on the central Californian coast eighteen kilometers northwest of San Luis Obispo in San Luis Obispo County. Samples were collected from the vertical exposure of one dune face by stratified random sampling at 1.0-m vertical intervals. Particle size distribution was determined through partic

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6

Ahmadi, Ziad M. "Sequence stratigraphy using wireline logs from Upper Jurassic of England." Thesis, Durham University, 1997. http://etheses.dur.ac.uk/1644/.

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7

Badescu, Adrian Constantin. "Reservoir characterization of the Miocene Starfak and Tiger Shoal fields, offshore Louisiana through integration of sequence stratigraphy, 3-D seismic, and well-log data." Access restricted to users with UT Austin EID, 2002. http://wwwlib.umi.com/cr/utexas/fullcit?p3108452.

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8

Hall, Lindsay Anne Forsyth. "Ordovician tectonic evolution of the southern Long Range Mountains, Newfoundland /." Internet access available to MUN users only, 1998. http://collections.mun.ca/u?/theses,39263.

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9

Hulsey, Josiah D. "Applying modern interpretation techniques to old hydrocarbon fields to find new reserves: A case study in the onshore Gulf of Mexico, U.S.A." ScholarWorks@UNO, 2016. http://scholarworks.uno.edu/td/2160.

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This study shows how the use of modern geological investigative techniques can reopen old, “drained” hydrocarbon fields. Specifically, it looks at the White Castle Field in South Louisiana. This field has pay sections ranging from late Oligocene to late Miocene. The late Oligocene package is underexplored and understudied and contains 3 primary reservoirs (Cib Haz (CH), MW, and MR). This study established the depositional history of these reservoirs. During most of the late Oligocene, the White Castle Salt Dome was located in a minibasin on the continental slope. The CH and MW deposited in thi

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10

Wrege, Beth Marie. "High-resolution stratigraphy at a coastal drillhole determined from a continuous core profile and a borehole geophysical log." Connect to this title online, 2007. http://etd.lib.clemson.edu/documents/1211384585/.

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11

Yarbrough, Christopher Neil. "Pliocene to recent stratigraphy of the Cuu Long and Nam Con Son Basins, offshore Vietnam." Thesis, Texas A&M University, 2006. http://hdl.handle.net/1969.1/3832.

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The Cuu Long and Nam Con Basins, offshore Vietnam, contain sediment dispersal systems, from up-dip fluvial environments to down-dip deep-water slope and basinal environments that operated along the southern continental margin of Vietnam during Pliocene to Recent time. The available data enabled sediment thickness patterns, sequence-stratigraphic relationships, and channel types (fluvial to deep-water channels) within the lower Pliocene to Recent stratigraphic succession in the Cuu Long and Nam Con Son basins of offshore Vietnam to be analyzed. At least nine sequences and their accompanying s

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12

Miner, Michael David. "Long and Short-Term Morphologic Evolution and Stratigraphic Architecture of a Transgressive Tidal Inlet, Little Pass Timbalier, Louisiana." ScholarWorks@UNO, 2007. http://scholarworks.uno.edu/td/557.

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The majority of changes to barrier island shorelines can be attributed to tidal inlet processes, and therefore an understanding of these processes is important to effectively manage barrier systems. High rates of relative sea-level rise within the Mississippi River delta plain have resulted in rapid landwardmigration of barrier island and tidal inlet systems. Moreover, ongoing conversion of back barrier and interior wetlands to open water increases tidal exchange. Enlarging tidal prisms, together with the landward migration of the barrier systems, results in a dynamic environment within w

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13

Olivier, Marie. "Environnements mixtes fluviatiles et éoliens : facteurs de contrôle et de préservation des dépôts éoliens en domaines endoréique et côtier : exemples du Permien du Sud de la Mer du Nord et du Sud-Est de l’Utah (USA)." Electronic Thesis or Diss., Rennes 1, 2017. http://www.theses.fr/2017REN1S173.

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Le Permien, dernière période du Paléozoïque, est marquée par la fin de l'assemblage de la Pangée induisant une continentalisation de vastes étendues sans équivalent dans les temps géologiques. Cette évolution géodynamique s'accompagne d'une aridification liée à la déglaciation du Permien Inférieur favorisant la sédimentation d'importants dépôts éoliens. La bonne préservation de ces dépôts dans l'enregistrement sédimentaire fait du Permien une période privilégiée pour l'étude des sédiments continentaux éoliens et fluviatiles que ce soit en contexte endoréique ou exoréique. Ce travail s'intéress

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14

Martillo, Bustamante Carlos. "Enregistrements stratigraphiques des cycles glacio-eustatiques et de la déformation durant le Pléistocène le long de la marge centrale d’Équateur : exploitation des données de la campagne ATACAMES." Thesis, Nice, 2016. http://www.theses.fr/2016NICE4020/document.

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L’objectif de cette étude est de contraindre les déformations au cours du Pléistocène d'une marge active à partir de l’analyse sismo-stratigraphique des sédiments conservés sur la plate-forme et la pente supérieure, le long de la marge centrale d’Equateur. A partir les données de sismique haute résolution et de carottage collectées pendant l'expédition Atacames (2012), plusieurs bassins ont été identifiés. La répartition latérale et de la succession des séquences T-R dans ces bassins montrent une distribution complexe des sédiments dans le temps et l'espace. Ce travail montre que, le long des

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15

Custerson, Brian David. "The micro-stratigraphy of weathering effects upon long-exposed Palaeolithic chert artifacts from central Arabia." Thesis, University of Leicester, 1992. http://hdl.handle.net/2381/34927.

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Examination by lOX optical- and Scanning Electron- microscopy of 91 chert tools found on surface sites in central Arabia disclosed a suite of weathering characteristics such as subsurface fabric changes (Weathering Fronts), loss of Silica (Corrosion Pitting), deposition on- and penetration of- fabric by externally sourced materials (Manganese) (Fe- Rock Varnish), and the effects of various edaphic, aeolian and biotic elements, which appeared to have an order to their occurrence. The tools were typo 1ogically classified as Mousterian and Rub' al Khali "Neolithic", and are common to the area. Th

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16

Aichholzer, Coralie. "Le log complet de la stratigrahie de la zone rhénane ainsi que les modilités stratigraphiques, sédimentaires et structurales de la transition socle-couverture : application à la géothermie profonde." Thesis, Strasbourg, 2019. http://www.theses.fr/2019STRAH008/document.

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Depuis la mise en place en 2010, d’une nouvelle tarification française sur le tarif de l’énergie géothermique, l’Alsace est la région de France la plus dynamique quant à la réalisation de forages géothermiques profonds à haute température (>150°C). Ainsi, l’approche géologique, qui a été primordiale pour les forages de Rittershoffen, le sera encore davantage pour les projets à venir compte tenu de la méconnaissance géologique de certaines zones profondes du bassin rhénan. Cette étude propose d’appréhender la compréhension de l’architecture stratigraphique et séquentielle des formations de l

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17

Soyer, Christian. "Inversions structurales le long de la direction atlasique en Tunisie centrale le Jebel Boudinar /." Phd thesis, Grenoble 2 : ANRT, 1987. http://catalogue.bnf.fr/ark:/12148/cb37610054h.

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18

Navarro, Ugueto Lilian Leomer. "Stratigraphic Architecture, Depositional Processes and Reservoir Implications of the Basin Floor to Slope Transition, Neoproterozoic Windermere Turbidite System, Canada." Thesis, Université d'Ottawa / University of Ottawa, 2016. http://hdl.handle.net/10393/35023.

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Deep-water strata of the Neoproterozoic Kaza Group and Isaac Formation (Cariboo Group) in the southern Canadian Cordillera (B.C.) were deposited in a passive-margin basin during the break-up of supercontinent Rodinia. At the Castle Creek and Mount Quanstrom study areas, a remarkably continuous stratigraphic interval throughout these units preserves a record of basin-floor overlain by strata deposited in the lowermost part of the slope. Although similar stratal intervals have been described from ancient and modern deep-marine settings, they still remain poorly understood. Three main stratal un

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19

Arriagada, César. "Rotations tectoniques et déformation de l'avant arc des Andes centrales au cours du Cénozoïque = Rotaciones tectónicas y deformación del antearco en los Andes centrales durante el cenozoico /." Rennes : Géosciences Rennes, Université de Rennes 1, 2004. http://catalogue.bnf.fr/ark:/12148/cb392302035.

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Th. doct.--Sci. de la terre--Rennes 1, 2003. Th. doct.--Ciencias, mention Geologia--Universidad de Chile, 2003.<br>Mention parallèle de titre ou de responsabilité : Rotaciones tectónicas y deformación del antearco en los Andes centrales durante el cenozoico. Textes en français et en anglais. Bibliogr. p. 301-308. Notes bibliogr. Résumé en français, en anglais et en espagnol.

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20

Deschamps, François. "Évolution post-rift et enregistrement des mouvements verticaux le long des marges passives : effets des processus intrinsèques aux marges passives." Rennes 1, 2010. https://hal-insu.archives-ouvertes.fr/tel-01137274.

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Les marges passives sont des structures lithosphériques intra-plaques, assurant la transition entre une croûte continentale non amincie et une croûte océanique. Du fait de leur position en bordure des continents, les marges passives sont soumises à des flux sédimentaires externes au système, produits par l'érosion de reliefs continentaux en amont de la marge, et elles sont affectées par une déformation complexe et de faible intensité qui intègre la déformation produite par les processus intrinsèques au système (ex : isostasie flexurale, subsidence thermique) mais aussi les déformations intra-p

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21

Adekola, Solomon Adeniyi. "Integrated approach to solving reservoir problems and evaluations using sequence stratigraphy, geological structures and diagenesis in Orange Basin, South Africa." Thesis, University of the Western Cape, 2010. http://etd.uwc.ac.za/index.php?module=etd&action=viewtitle&id=gen8Srv25Nme4_6861_1298537140.

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<p>Sandstone and shale samples were selected within the systems tracts for laboratory analyses. The sidewall and core samples were subjected to petrographic thin section analysis, mineralogical analyses which include x-ray diffraction (XRD), scanning electron microscopy (SEM), energy dispersive spectroscopy (EDS), and stable carbon and oxygen isotopes geochemistry to determine the diagenetic alteration at deposition and post deposition in the basin. The shale samples were subjected to Rock-Eval pyrolysis and accelerated solvent extraction (ASE) prior to gas chromatographic (GC) and gas chromat

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22

Strzerzynski, Pierre. "Évolution tectono-métamorphique et modélisation 3D le long du projet ferroviaire Lyon-Turin : Maurienne, Alpes." Lyon 1, 2006. http://www.theses.fr/2006LYO10129.

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Le projet ferroviaire Lyon-Turin offre l’opportunité de disposer de nombreuses données du sous-sol dans le secteur de Modane-Aussois (Briançonnais, France) qui, combinées aux structures géologiques de surface permettent de progresser dans la connaissance des processus de subduction continentale, d’exhumation et de collision dans les Alpes. Plusieurs étapes dans l’exhumation sont mises en évidence : - Un empilement des unités de couverture à la faveur de chevauchements vers le NW (D1-D2) permet l’exhumation entre 37 et 35 Ma depuis des conditions de HP BT (1. 02 GPa - 350°C) jusqu’à 0. 75 GPa –

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23

Smith, Quinn Eric. "Volcanic stratigraphy, alteration zoning, and vein paragenesis of the Sascha-Pelligrini low-sulphidation epithermal system, Santa Cruz, Argentina." Thesis, Queensland University of Technology, 2009. https://eprints.qut.edu.au/39142/1/Quinn_Smith_Thesis.pdf.

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The Sascha-Pelligrini low-sulphidation epithermal system is located on the western edge of the Deseado Massif, Santa Cruz Province, Argentina. Outcrop sampling has returned values of up to 160g/t gold and 796g/t silver, with Mirasol Resources and Coeur D.Alene Mines currently exploring the property. Detailed mapping of the volcanic stratigraphy has defined three units that comprise the middle Jurassic Chon Aike Formation and two units that comprise the upper Jurassic La Matilde Formation. The Chon Aike Formation consists of rhyodacite ignimbrites and tuffs, with the La Matilde Formation includ

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24

Rosaz, Thierry Marie. "Le passage des Cordillères Nord-Américaines aux Sierras Madres mexicaines le long du « Texas lineament » : stratigraphie et tectonique du SW du Nouveau-Mexique et du Nord de Chihuahua (USA et Mexique)." Nice, 1990. http://www.theses.fr/1990NICE4446.

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Le passage des Cordillères Nord-Américaines aux Sierras Madres mexicaines est assuré par la bande crustale du « Texas lineament » qui, du crétacé au tertiaire, accommode les contraintes tectoniques au cours des phases suivantes : 1) crétacé inferieur rifting intra-continental ; 2) crétacé supérieur compression liée aux phases orégoniennes puis sub-hercynienne responsables de l'écrasement des bassins du crétacé inferieur ; 3) paléocène-éocenetectonique polyphasée (orogenèse laramienne) matérialisée par des systèmes d'abord chevauchants puis transpressifs ; 4) néogène : distention généralisée (b

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25

Briand, Bernard. "Caractérisation des métamagmatites en domaine profond et reconnaissance des sites géotectoniques : exemple du complexe leptyno-amphibolique de la vallée du Lot (Massif Central français)." Lyon 1, 1986. http://www.theses.fr/1986LYO19039.

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Le "groupe leptyno-amphibolique" de la vallee du lot est une association magmatique bimodale affectee par une evolution metamorphique de haut degre. Il est constitue des metagabbros metadolerites, pyrigarnites, eclogites et leptynites, encaisses dans un ensemble de gneiss d'origine sedimentaire et volcano-sedimentaire. La composition lithologique et les caracteres de ses constituants excluent, pour ce complexe, toute analogie avec les associations ophiolitiques; ils sont en acord avec un cadre de mise en place ensialique, dans un environnement de type marginal

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26

Anderson, Alvin D. "Geology of the Phil Pico Mountain Quadrangle, Daggett County, Utah, and Sweetwater County, Wyoming." Diss., CLICK HERE for online access, 2008. http://contentdm.lib.byu.edu/ETD/image/etd2384.pdf.

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27

Gámez, Torrent Desiré. "Sequence Stratigraphy as a tool for water resources management in alluvial coastal aquifers: application to the Llobregat delta (Barcelona, Spain)." Doctoral thesis, Universitat Politècnica de Catalunya, 2007. http://hdl.handle.net/10803/6255.

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Most coastal aquifers undergo seawater intrusion. Mitigating this risk depends on a sound knowledge of flow mechanisms, well located and constructed wells, an effective management, suitable policies and the desire to conserve the aquifer. To this end, a comprehensive geological model is essential. The single most important question that the geological model should address is the degree and nature of the connection of the aquifer to the sea. Differences in the connection explain why apparently similar coastal aquifers display very different salinitzation behavior. Some aquifers salinize with mo

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28

Mele, Antoni Rosell i. "Long-chain alkenone and alkyl alkenoate, and total pigment abundancies as climatic proxy-indicators in the the northeastern Atlantic : analytical methods, calibration and stratigraphy." Thesis, University of Bristol, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.386102.

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29

Stobart, Ryan Patrick. "The Kaskaskia-Absaroka Boundary in the Subsurface of Athens County, Ohio." Ohio University / OhioLINK, 2019. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou1574437212920114.

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30

Duboy, Maryse. "Histoire sociale comparée de Fumel, Penne, Villeneuve et Aiguillon en Agenais au XVIIIe siècle." Thesis, Bordeaux 3, 2018. http://www.theses.fr/2018BOR30046/document.

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Dans la perspective d’une contribution à l’histoire de l’Aquitaine, l’étude s’attache à définir un cadre spatial suffisamment représentatif – à savoir la vallée du Lot de Fumel à la confluence avec la Garonne. Le fait d’adjoindre à notre recherche, la zone de la confluence, place automatiquement notre étude dans la dépendance de l’axe garonnais, et du débouché en aval que constitue la ville portuaire de Bordeaux, dont on sait l’extraordinaire dynamisme au XVIIIe siècle. Quelles sont les stratégies de nos quatre communautés face au pôle d’attraction bordelais qui impulse, à la descente comme à

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31

Harsolumakso, Agus Handoyo. "Étude lithostratigraphique et structurale le long du transect Wini-Kolbano, à Timor-ouest (Indonésie)." Nice, 1993. http://www.theses.fr/1993NICE4665.

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Située au contact entre la plaque australienne et l'arc de Banda, l'ile de Timor, est classiquement considérée comme une chaine issue d'un modèle géodynamique de subduction/collision. Cette ile constituait la bordure septentrionale de la marge passive australienne avant d'être incorporée au fore-arc de Banda. Pour comprendre ce mécanisme tectonique nous avons réalisé un transect tectonique qui recoupe toutes les structures du nord au sud. Les recherches ont porté essentiellement sur l'établissement d'une échelle lithostratigraphique et sur l'étude de la déformation des séries rencontrées le lo

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32

Barriere, Vivien. "Les portes de l'enceinte antique d'Autun et leurs modèles (Gaule, Italie, provinces occidentales de l'Empire romain)." Thesis, Dijon, 2012. http://www.theses.fr/2012DIJOL042/document.

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Augustodunum, civitas Aeduorum, fondée à l’époque augustéenne, fut dotée de quatre portes urbaines : la porte d’Arroux et la porte Saint-André qui sont les mieux conservées, la porte Saint-Andoche dont il ne reste qu’une tour de flanquement et la porte de Rome, depuis longtemps disparue. L’étude stratigraphique du bâti des portes et la réflexion sur le fonctionnement du chantier de construction des portes urbaines d’Autun constituent le cœur de ce travail. Par ailleurs, antiquaires, voyageurs et artistes ont laissé depuis le XVIème siècle de nombreux témoignages de leur visite des portes romai

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33

Vallini, Daniela Alessandra. "The formation of authigenic xenotime in Proterozoic sedimentary basins : petrography, age and geochemistry." University of Western Australia. Geology and Geophysics Discipline Group, 2006. http://theses.library.uwa.edu.au/adt-WU2006.0070.

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[Truncated abstract] The realization in 1999 that the authigenic phosphate, xenotime, could be used in geochronological studies to place age constraints on burial events that affected sedimentary basins has opened numerous opportunities for establishing timeframes for sedimentary basin analysis. Since then, the mineral has been used to place new and novel age constraints on diagenesis, metamorphism, and hydrothermal alteration and mineralization events. Whilst these studies were successful, they identified many complexities in xenotime growth and were restricted to specific areas or single bas

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34

Klopfenstein, Trey. "High-frequency Sequences within the Lower Mississippian Allensville Member, Logan Formation, South-central Ohio." Ohio University / OhioLINK, 2018. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou1525864536290455.

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Oliveira, Siana Soares de. "Caracterização de reservatórios não convencionais Shale Gas na Formação Barreirinha Bacia do Amazonas." Universidade do Estado do Rio de Janeiro, 2015. http://www.bdtd.uerj.br/tde_busca/arquivo.php?codArquivo=8731.

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Os folhelhos pretos devonianos da Formação Barreirinha caracterizamse pela alta radioatividade na porção basal, grande extensão areal, espessura e profundidade de soterramento variável que vão de exposição na superfície até mais de 3000 m. Eles são as principais rochas geradoras do sistema petrolífero convencional da Bacia do Amazonas, e recentemente foram consideradas como promissores plays de gás não convencional. Folhelhos são geralmente caracterizados por uma matriz fechada, que faz com que sejam relativamente impermeáveis em relação ao fluxo de gás, a menos que ocorram fraturas, e depende

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Laneville, Michael Warren. "Subsurface Depositional Systems Analysis of the Cambrian Eau Claire Formation in Western Ohio." Bowling Green State University / OhioLINK, 2018. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu154220482332536.

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37

Fadipe, Oluwaseun Adejuwon. "Reservoir quality, structural architecture, fluid evolution and their controls on reservoir performance in block 9, F-O gas field, Bredasdorp Basin, offshore South Africa." Thesis, University of the Western Cape, 2012. http://hdl.handle.net/11394/4005.

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Philosophiae Doctor - PhD<br>The use of integrated approach to evaluate the quality of reservoir rocks is increasingly becoming vital in petroleum geoscience. This approach was employed to unravel the reason for the erratic reservoir quality of sandstones of the F-O gas field with the aim of predicting reservoir quality, evaluate the samples for presence, distribution and character of hydrocarbon inclusions so as to gain a better understanding of the fluid history. Information on the chemical conditions of diagenetic processes is commonly preserved in aqueous and oil fluid inclusion occu

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38

Haupert, Isabelle. "Etude des hauts et bas topographiques dans les marges profondes de type « upper plate » : exemple des unités du Briançonnais et du Prépiémontais dans les Alpes et comparaison avec des analogues modernes." Thesis, Strasbourg, 2015. http://www.theses.fr/2015STRAH016/document.

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Cette étude se concentre sur la caractérisation des blocs-H préservés dans les marges de type « upper plate ». L’approche terre-mer a permis de diviser l’architecture crustale d’une « upper plate » en trois terrasses et deux zones d’escarpement, possédant leurs propres architectures crustales et stratigraphiques. Les limites de terrasses sont liées à des changements dans les modes d’extensions et définissent des points majeurs. Dans les Alpes il apparait que les principales structures Alpines correspondent à la réactivation des zones d’escarpements ou des failles de détachement. La collision f

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Furlong, Pierce James. "Aspects of ancient Near Eastern chronology (c. 1600-700 BC)." Melbourne, 2007. http://repository.unimelb.edu.au/10187/2096.

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The chronology of the Late Bronze and Early Iron Age Near East is currently a topic of intense scholarly debate. The conventional/orthodox chronology for this period has been assembled over the past one-two centuries using information from King-lists, royal annals and administrative documents, primarily those from the Great Kingdoms of Egypt, Assyria and Babylonia. This major enterprise has resulted in what can best be described as an extremely complex but little understood jigsaw puzzle composed of a multiplicity of loosely connected data. I argue in my thesis that this conventional chronolog

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40

Ortiz, Trujillo John Rafael. "SDAR: a package for plotting and analyzing stratigraphy data in R." Master's thesis, 2015. http://hdl.handle.net/10362/14554.

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Stratigraphic Columns (SC) are the most useful and common ways to represent the eld descriptions (e.g., grain size, thickness of rock packages, and fossil and lithological components) of rock sequences and well logs. In these representations the width of SC vary according to the grain size (i.e., the wider the strata, the coarser the rocks (Miall 1990; Tucker 2011)), and the thickness of each layer is represented at the vertical axis of the diagram. Typically these representations are drawn 'manually' using vector graphic editors (e.g., Adobe Illustrator®, CorelDRAW®, Inskape). Nowaday

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Igbokwe, Onyedikachi Anthony. "Stratigraphic interpretation of Well-Log data of the Athabasca Oil Sands of Alberta Canada through Pattern recognition and Artificial Intelligence." Master's thesis, 2011. http://hdl.handle.net/10362/8281.

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Dissertation submitted in partial fulfillment of the requirements for the Degree of Master of Science in Geospatial Technologies.<br>Automatic Stratigraphic Interpretation of Oil Sand wells from well logs datasets typically involve recognizing the patterns of the well logs. This is done through classification of the well log response into relatively homogenous subgroups based on eletrofacies and lithofacies. The electrofacies based classification involves identifying clusters in the well log response that reflect ‘similar’ minerals and lithofacies within the logged interval. The identifica

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"The reconstruction of late quaternary depositional environments in the vicinity of Yuen Long." Chinese University of Hong Kong, 1996. http://library.cuhk.edu.hk/record=b5888963.

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by Cheung May Shuen.<br>Thesis (M.Phil.)--Chinese University of Hong Kong, 1996.<br>Includes bibliographical references (leaves 157-165).<br>ABSTRACT --- p.i<br>ACKNOWLEDGEMENTS --- p.ii<br>LIST OF FIGURES --- p.vi-ix<br>LIST OF PLATES --- p.x<br>LIST OF TABLES --- p.xi<br>Chapter CHAPTER I - --- INTRODUCTION<br>Chapter 1.1 --- Background of Quaternary Studies in Hong Kong --- p.1<br>Chapter 1.2 --- The Necessity of Regional and Local Practice --- p.3<br>Chapter 1.3 --- The Need for Regional Synthesis --- p.6<br>Chapter 1.4 --- Linking Onshore Studies with Offshore Ones --- p.8<br>Cha

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Hummon, Cheryl. "Subsurface Quaternary and Pliocene structures of the northern Los Angeles Basin, California." Thesis, 1994. http://hdl.handle.net/1957/35964.

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The northern Los Angeles basin is influenced by two structural styles: the west-trending compressional Transverse Ranges to the north, and the strike-slip Peninsular Ranges to the south. The interaction of these two structural styles has resulted in a complex fold/fault belt at the northern margin of the Los Angeles basin, which deforms a variable sequence of late Miocene through Quaternary marine strata. Subsurface mapping of Quaternary marine gravels by electric-log correlation documents the latest phase of deformation in the northern Los Angeles basin. The Quaternary marine gravels are fold

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Langsford, N. "Long structural zones in the Archaean Yilgarn Craton, Western Australia." Thesis, 1994. https://eprints.utas.edu.au/20343/7/whole_LangsfordNick1995.pdf.

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Eight structural zones from 250km to 800km long, traverse the granite-greenstone terrane of the Eastern Goldfields and Murchison districts of the Yilgam Craton. The structural zones, herein called LSZ, (long structural zones) have been traced using 1 :500,000 geological compilations and AGSO (Australian Geological Survey Organisation) aeromagnetic and gravity data. LSZ are complex linear deformation zones, resulting in the reactivation of structures formed prior to a craton wide shortening episode. Some of the pre-existing structures are interpreted as low angle extensional features, po

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Tian, Yao. "An Investigation of Regional Variations of Barnett Shale Reservoir Properties, and Resulting Variability of Hydrocarbon Composition and Well Performance." Thesis, 2010. http://hdl.handle.net/1969.1/ETD-TAMU-2010-05-7829.

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In 2007, the Barnett Shale in the Fort Worth basin of Texas produced 1.1 trillion cubic feet (Tcf) gas and ranked second in U.S gas production. Despite its importance, controls on Barnett Shale gas well performance are poorly understood. Regional and vertical variations of reservoir properties and their effects on well performances have not been assessed. Therefore, we conducted a study of Barnett Shale stratigraphy, petrophysics, and production, and we integrated these results to clarify the controls on well performance. Barnett Shale ranges from 50 to 1,100 ft thick; we divided the forma

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Herzog, David W. "Subsurface structural evolution along the northern Whittier fault zone of the eastern Los Angeles basin, Southern California." Thesis, 1998. http://hdl.handle.net/1957/33340.

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The Whittier fault forms the central part of a fault system extending from the East Montebello fault at Whittier Narrows to the Elsinore fault, which is traced as far as the Mexican border. The Whittier fault forms a restraining bend in this fault system, resulting in uplift of the Puente Hills. The northwestern part of the Whittier fault in the Whittier oil field in the eastern Los Angeles basin strikes approximately N65��W and dips 70-75�� northeast. The fault is near the range front of the Puente Hills northwest of Turnbull Canyon, and within the Puente Hills to the southeast. The central r

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Krentz, Sarah. "Potentially tsunamigenic event layer in late Holocene Great South Bay, Long Island, New York constraints on origins, processes, and effects /." Diss., 2009. http://etd.library.vanderbilt.edu/available/etd-07232009-175830/.

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Isdiken, Batur. "Integrated geological and petrophysical investigation on carbonate rocks of the middle early to late early Canyon high frequency sequence in the Northern Platform area of the SACROC Unit." 2013. http://hdl.handle.net/2152/23212.

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The SACROC unit is an isolated carbonate platform style of reservoir that typifies a peak icehouse system. Icehouse carbonate platforms are one of the least well understood and documented carbonate reservoir styles due to the reservoir heterogeneities they embody. The current study is an attempt to recognize carbonate rock types defined based on rock fabrics by integrating log and core based petrophysical analysis in high-frequency cycle (HFC) scale sequence stratigraphic framework and to improve our ability to understand static and dynamic petrophysical properties of these reservoir rock type

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Ramazanova, Rahila. "Sequence stratigraphic interpretation methods for low-accommodation, alluvial depositional sequences: applications to reservoir characterization of Cut Bank field, Montana." 2006. http://hdl.handle.net/1969.1/ETD-TAMU-1127.

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In South Central Cut Bank Sand Unit (SCCBSU) of Cut Bank field, primary production and waterflood projects have resulted in recovery of only 29 % of the original oil in place from heterogeneous, fluvial sandstone deposits. Using highresolution sequence stratigraphy and geostatistical analysis, I developed a geologic model that may improve the ultimate recovery of oil from this field. In this study, I assessed sequence stratigraphic concepts for continental settings and extended the techniques to analyze low-accommodation alluvial systems of the Cut Bank and Sunburst members of the lower Kooten

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Karaman, Ozge. "Shoreline architecture and sequence stratigraphy of Campanian Iles clastic wedge, Piceance Basin, CO : influence of Laramide movements in Western Interior Seaway." Thesis, 2012. http://hdl.handle.net/2152/ETD-UT-2012-08-5956.

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The Campanian Iles Formation of the Mesaverde Group in northwestern Colorado contains a stacked series of some 11 shoreline sequences that form clastic wedges extending east and southeastwards from the Sevier orogenic belt to the Western Interior Seaway. Iles Formation shorelines and their alluvial and coastal plain equivalents (Neslen Formation, Trail and Rusty members of the Ericson Formation) are well exposed from Utah and from southern Wyoming into northwestern Colorado. The Iles Clastic Wedge was examined in the subsurface Piceance Basin and at outcrops in Meeker and south of Rangely, NW

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