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Thèses sur le sujet « Petroleum Source Rocks »

Auteur : Grafiati

Publié le 4 juin 2021

Mis à jour le 9 février 2022

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1

Hill, Tyler J. "Potential source rocks in the western Kansas petroleum province." Thesis, Kansas State University, 2011. http://hdl.handle.net/2097/8776.

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Master of Science<br>Department of Geology<br>Matthew W. Totten<br>The source of the hydrocarbons in western Kansas has been an ongoing debate for many years. The highly organic-rich Anadarko basin, directly south of western Kansas, has been a very prolific producer for many years. This basin is the most widely accepted source of the oil in Kansas, as it is very deep and thermally mature. The main source rock in this area is the Woodford Shale, a very thick, very organic-rich unit which has been proven to produce many hydrocarbons. Several studies have been done on the oils that are presen

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2

Fan, Zhiqiang. "Primary migration of hydrocarbons through microfracture propagation in petroleum source rocks." Thesis, The University of Maine, 2013. http://pqdtopen.proquest.com/#viewpdf?dispub=3573311.

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<p>Petroleum is generated from finely grained source rocks rich in organic materials and accumulated and trapped in reservoir rocks with relatively higher permeability and porosity. Expulsion of petroleum through and out of source rocks is called primary migration. Primary migration, as a link between source rocks and carrier rocks, presents a vital challenge to the society of petroleum geosciences and exploration and attracts the research interests of many geologists and geochemists. Despite extensive research the effective mechanisms responsible for primary migration of hydrocarbons are stil

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3

McGinn, Allan. "Representative bulk and molecular information on petroleum source rocks from hydropyrolysis." Thesis, University of Strathclyde, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.248769.

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4

Wang, Huai Da. "A geochemical study of potential source rocks and crude oils in the Anadarko Basin, Oklahoma /." Full-text version available from OU Domain via ProQuest Digital Dissertations, 1993.

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5

Raji, Munira. "Unconventional offshore petroleum-extracting oil from active source rocks of the Kimmeridge Clay Formation of the North Sea." Thesis, Durham University, 2018. http://etheses.dur.ac.uk/12476/.

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The organic-rich Upper Jurassic Kimmeridge Clay Formation is the major source rock for conventional oil and gas in the North Sea with a maximum thickness of 1,100 m. TOC values range from 2 wt.%-10 wt.% and predominantly Type II (bacterially-degraded algal, and a mix of Type I (mainly algal) kerogens. The δ13Corg values for the investigated samples range from -29.73 ‰ to -26. 88 ‰, these values are characteristic of marine organic matter with terrestrial input. Sixteen billion barrels of commercial reserves have been discovered in conventional reservoirs in the UK Viking Graben area with 29 bi

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6

Jones, Bryn. "Relationships between organic maturity and inorganic geochemistry in Upper Jurassic petroleum source rocks from the Norwegian North Sea and the United Kingdom." Thesis, University of Newcastle Upon Tyne, 1991. http://hdl.handle.net/10443/679.

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The aim of this study was to. examine the relationship between organic maturity and trace element geochemistry of organic rich mudstones, to assess their behaviour as sources or sinks of metals during diagenesis, and their role in mineral deposit genesis. The suite studied consisted of 193 samples from the Draupne, Heather, and Kimmeridge Clay Formations from the Norwegian North Sea and onshore UK. All three formations had above average contents of C and S, and the Draupne and Heather Formations had a low carbonate content. The Draupne Formation was particularly enriched in a number of trace e

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7

Baldwin, Patrick W. "LITHOSTRATIGRAPHIC AND GEOCHEMICAL CHARACTERIZATION OF THE UPPER PENNSYLVANIAN ‘WOLFCAMP D’ SHALE, MIDLAND BASIN (USA): IMPLICATIONS FOR PALEOENVIRONMENTS AND UNCONVENTIONAL PETROLEUM RESERVIORS." UKnowledge, 2016. http://uknowledge.uky.edu/ees_etds/35.

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An integrated stratigraphic analysis of a ~350 ft drill core from Upton County (Texas) has revealed pervasive variability of several key siliciclastic and carbonate lithofacies in vertical section, where organic-rich siliceous mudrock beds alternate with aluminum-rich mudrocks and calcareous gravity flow deposits. Sediment chemistry, especially major and trace elements derived from x-ray fluorescence, captures this variability with high sensitivity. The high frequency chemostratigraphic variability appears to be cyclic, and it is interpreted to represent the first example of deep-water Late Pe

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8

Salgado, Souto Sergio Adrian, and Souto Sergio Adrian Salgado. "A Re-Os Geochronology and Multi Stable Isotope (C, N, S, Sr, Pb) Systematics of Source Rocks and Crude Oils from the Sonda de Campeche Petroleum System, Mexico." Diss., The University of Arizona, 2018. http://hdl.handle.net/10150/626760.

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In this work, I present a multi-isotopic study (carbon, nitrogen, sulfur, strontium and lead) and Re-Os geochronology in rocks and crude oils of the Sonda de Campeche Petroleum System (SCPS). Since crude oils are complicated chemical systems easily disturbed, the Re-Os isotopic system could be affected if secondary processes perturb crude oils. Therefore, the multi stable isotopic study allows the identification of the presence and grade of these secondary processes in crude oils. The δ13C values of crude oils from the SCPS distinguish between: 1) crude oils with the fingerprint of source roc

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9

Sachse, Victoria Frederike [Verfasser]. "Petroleum source rocks of western and central Africa : the examples of the marine Tarfaya Basin, Morocco and the continental Congo Basin, Democratic Republic of Congo / Victoria Frederike Sachse." Aachen : Hochschulbibliothek der Rheinisch-Westfälischen Technischen Hochschule Aachen, 2011. http://d-nb.info/1018190163/34.

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10

Mohammed, R. Luma Jassim [Verfasser], Lorenz [Akademischer Betreuer] Schwark, and Wolfgang [Gutachter] Kuhnt. "Petroleum system analysis of the Lower Jurassic-Upper Cretaceous source rocks and Miocene reservoirs in the NE of Iraq / Luma Jassim Mohammed R ; Gutachter: Wolfgang Kuhnt ; Betreuer: Lorenz Schwark." Kiel : Universitätsbibliothek Kiel, 2016. http://d-nb.info/1236286944/34.

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11

Mendelson, J. D. (James D. ). "Petroleum source rock logging." Thesis, Massachusetts Institute of Technology, 1985. http://hdl.handle.net/1721.1/15126.

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12

Balbinot, Mariana. "Caracterização geoquímica de rochas geradoras do intervalo Cretáceo-Terciário da Bacia de Santos, Brasil." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2012. http://hdl.handle.net/10183/63146.

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A Bacia de Santos é uma das principais bacias brasileiras para exploração e produção de hidrocarbonetos, e vem recebendo grandes investimentos em pesquisa nos últimos anos. O estudo das rochas geradoras serve como importante ferramenta para o estudo de modelos de geração, explusão e migração de hidrocarbonetos e na identificação de sistemas petrolíferos. O principal objetivo deste trabalho é a identificação de intervalos e áreas com maior potential para a geração de hidrocarbonetos dentro do pacote sedimentar estudado (Cretáceo-Terciário). As amostras de calha de 6 poços exploratórios, obtidas

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13

Abdulla, Fawzeiah Hussien Ali. "Source rock evaluation and maturity studies of Lower and Middle Cretaceous formations in Kuwait." Thesis, Imperial College London, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.312472.

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14

J, Staples Christine. "Source rock potential and petroleum geochemistry of the Eringa Trough area, Pedirka Basin /." Adelaide, 1995. http://web4.library.adelaide.edu.au/theses/09SB/09sbs794.pdf.

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15

Kagya, Meshack L. N. "The source rock and petroleum geochemistry of the Early Jurassic Poolowanna Formation, Eromanga Basin /." Title page, contents and abstract only, 1997. http://web4.library.adelaide.edu.au/theses/09PH/09phk118.pdf.

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16

Long, David E. "Source rock geochemistry of the southern Tyee Basin, southwest Oregon." PDXScholar, 1994. https://pdxscholar.library.pdx.edu/open_access_etds/4040.

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This study examined source rock geochemistry of the southern Tyee Basin. Total organic carbon, rock-eval pyrolysis, vitrinite reflectance, thermal alteration index and visual assessments were performed on splits from cutting samples from five wells and on outcrop samples from four measured sections. Organic matter was found to be dispersed, averaging about 0.5 weight percent. The organic matter is primarily terrestrial in origin, or type I l l , with low potential for gas production and no oil potential. Three coal samples are clearly the richest sources of organic matter examined in this stud

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17

Laggoun-Defarge, Fatima. "Etude de la diagenese organique des series paleozoiques du bassin de sbaa (algerie) : approche geochimique et petrologique." Orléans, 1987. http://www.theses.fr/1987ORLE2031.

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L'etude porte sur la genese des reserves d'huile trouvees dans le bassin de sbaa, sahara algerien, notamment dans la formation du tournaisien des "gres de sbaa". Les echantillons sont analyses du point de vue petrologique par microspectrofluorimetrie et du point de vue geochimique par pyrolyse et chromatographie en phase gazeuse. La roche mere des hydrocarbures est le silurien; leur generation, suivie de peu par la migration date probablement de la fin du primaire. L'orogenie hercynienne est responsable de la mise en place des pieges structuraux. D'autre part, un concentre d'algues tasmanacees

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18

McColloch, Austin. "Distribution and source rock potential of the Chattanooga shale in Kansas." Thesis, Kansas State University, 2015. http://hdl.handle.net/2097/20595.

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Master of Science<br>Geology<br>Matthew W. Totten<br>Organic-rich shales were deposited over a large part of what is now North America during the Late Devonian. North America in the late Devonian was located in the tropics (Woodrow et al., 1973), possibly in low southerly latitudes (Heckel and Witzke, 1979; Witzke and Heckel, 1988; Streel et al., 1990). This environment creates an organic-rich environment that resulted in thick, black shales. The Devonian-Mississippian Chattanooga (Woodford) shale is known to be an important petroleum source rock in many intracratonic basins of the Midcontinen

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19

Amansure, Giovanni Ricardo. "Source rock characterization of the organic rich intervals of the Taranaki Basin, Offshore New Zealand." University of the Western Cape, 2015. http://hdl.handle.net/11394/5057.

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>Magister Scientiae - MSc<br>The Taranaki Basin is a large (ca. 330,000 km²) sedimentary basin found along the west coast of the northern island of New Zealand. The basin lies partly onshore but mostly offshore below the broad continental shelf to the west of central North Island. The Taranaki Basin is the first sedimentary basin to be explored in New Zealand and is currently New Zealand’s only hydrocarbon producing basin, with approximately 418 million barrels (MMbbl) of oil and 6190 billion cubic feet (bcf) of gas produced by the end of 2011. Most of New Zealand’s known oil and gas accumulat

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20

McClave, Graham A. "Stratigraphy and source rock analyses of the Heath Formation in Fergus, Garfield, Golden Valley, Musselshell, Petroleum, and Rosebud counties, central Montana." Colorado School of Mines, 2013.

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21

Mueller, Eric. "Temporal and spatial source rock variations and the consequence on crude oil composition in the Tertiary petroleum system of the Uinta Basin, Utah, U.S.A. /." Full-text version available from OU Domain via ProQuest Digital Dissertations, 1998.

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22

Wall, Meagan. "An oil-source rock correlation examining the potential of the Chattanooga shale as a source rock for oil within the Spivey-Grabs-Basil Field, Kingman and Harper Counties, Kansas." Thesis, Kansas State University, 2015. http://hdl.handle.net/2097/19013.

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Master of Science<br>Department of Geology<br>Matthew Totten<br>Oil production in Kansas has a long history with plays being found on all sides of the state. The source of Kansas’s hydrocarbons has been traditionally thought to be outside the state due to low thermal maturity and the shallow burial of potential source rocks within Kansas. This research addresses the question regarding the source of the oil in Kansas, at least within a small geographic area of roughly 146mi[superscript]2. The Spivey-Grabs-Basil Field has been one of the more successful fields within the state of Kansas since th

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23

Vellutini, David. "Organic maturation and source rock potential of Mesozoic and Tertiary strata, Queen Charlotte Islands, British Columbia." Thesis, University of British Columbia, 1988. http://hdl.handle.net/2429/28526.

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The level of organic maturation, thermal history, and source rock potential of Mesozoic and Tertiary strata in the Queen Charlotte Islands have been investigated with vitrinite reflectance measurements (%Ro rand)> numerical modelling (modified Arrhenius and Lopatin models), and Rock-Eval pyrolysis (source rock potential). The level of organic maturation increases from north to south and is primarily controlled by high heat flow associated with plutonism on Moresby Island. Upper Triassic-Lower Jurassic strata are overmature on Moresby Island with vitrinite reflectance values ranging from 2.40 t

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24

Bou, Daher Samer Verfasser], Ralf [Akademischer Betreuer] [Littke, and Rudy [Akademischer Betreuer] Swennen. "Source rock characterization and petroleum generation modelling of the Levant Basin, onshore-offshore Lebanon : an integrated approach / Samer Bou Daher ; Ralf Littke, Rudy Swennen." Aachen : Universitätsbibliothek der RWTH Aachen, 2016. http://d-nb.info/1130151352/34.

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25

Al-Arouri, Khaled R. "Petroleum geochemistry, source rock evaluation and modelling of hydrocarbon generation in the southern Taroom Trough, with particular reference to the Triassic Snake Creek Mudstone /." Title page, abstract and contents only, 1996. http://web4.library.adelaide.edu.au/theses/09PH/09pha321.pdf.

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26

Bou, Daher Samer [Verfasser], Ralf [Akademischer Betreuer] Littke, and Rudy [Akademischer Betreuer] Swennen. "Source rock characterization and petroleum generation modelling of the Levant Basin, onshore-offshore Lebanon : an integrated approach / Samer Bou Daher ; Ralf Littke, Rudy Swennen." Aachen : Universitätsbibliothek der RWTH Aachen, 2016. http://d-nb.info/1130151352/34.

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27

Böcker, Johannes Verfasser], Ralf [Akademischer Betreuer] [Littke, and Detlev [Akademischer Betreuer] Leythaeuser. "Petroleum system and thermal history of the Upper Rhine Graben : implications from organic geochemical analyses, oil-source rock correlations and numerical modelling / Johannes Böcker ; Ralf Littke, Detlev Leythaeuser." Aachen : Universitätsbibliothek der RWTH Aachen, 2015. http://d-nb.info/1130151387/34.

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28

Schmid, Jean-Claude. "Marqueurs biologiques soufres dans les petroles." Université Louis Pasteur (Strasbourg) (1971-2008), 1986. http://www.theses.fr/1986STR13146.

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Identification et geochimie des marqueurs biologiques soufres dans deux petroles particulierement riches en soufre: petroles de marvejols, bassin d'alis france et de rozel point, utch, etats-unis. La diversite des composes organo-soufres et leur teneur dans les petroles indiquent que la formation de ces molecules se fait tres probablement par un processus non-biologique. L'incorporation de soufre dans la matiere organique sedimentaire se ferait principalement a un stade precoce de la maturation sur des molecules fonctionnalisees, notamment des alcenes

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29

Atmani, Léa. "Study of organic matter decomposition under geological conditions from replica exchange molecular dynamics simulations." Thesis, Aix-Marseille, 2017. http://www.theses.fr/2017AIXM0104/document.

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Pétrole et gaz proviennent de la décomposition de la matière organique dans la croûte terrestre. En s’enfouissant, les résidus organiques se décomposent en un solide poreux et carboné, appelé kérogène et en un fluide composé d’hydrocarbures et de petites molécules telles que de l’eau. Le processus de formation du kérogène n’est pas totalement élucidé et une modélisation aiderait à une meilleure compréhension à la fois de sa structure et de sa composition et serait utile à l’industrie pétrolière.Dans le présent travail, nous adoptons une approche thermodynamique ayant pour but, à l’aide de simu

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30

Pethe, Swardhuni. "Subsurface analysis of Sundaland basins : source rocks, structural trends and the distribution of oil fields." 2013. http://liblink.bsu.edu/uhtbin/catkey/1741652.

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According to the Ade observation (Ade, W., pers. Comm.) “95% of all commercial oil fields in the Sumatra region occur within 17 km of seismically mappable structural grabens in the producing basins”. The Ade observation proposes a link between the subsidence of the source rocks (the Talang Akar Formation) in the grabens and the maturity of the organic material. To test the validity of the Ade observation, subsurface mapping of the region was carried out using geophysical logs. Using the well log information, the basement and the formation tops have been mapped with a special emphasis on Talang

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31

Volk, Herbert [Verfasser]. "Source rocks, bitumens and petroleum inclusions from the prague basin (Barrandian, Czech Republic) : constraints for petroleum generation and migration from petrology, organic geochemistry and basin modelling / vorgelegt von Herbert Volk." 2000. http://d-nb.info/961896094/34.

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32

Tischler, Keith Louris. "Paradox Basin source rock, southeastern Utah : organic geochemical characterization of Gothic and Chimney Rock units, Ismay and Desert Creek zones, within a sequence stratigraphic framework." 1995. http://hdl.handle.net/2152/18461.

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The Chimney Rock and Gothic units of the Pennsylvanian Paradox Formation have long been considered source rocks for the rich hydrocarbon fields of southeastern Utah. Fundamental questions about these units include: source and nature of the organic material, source rock character, and position of the source rocks in the existing sequence stratigraphic framework. The Chimney Rock and Gothic, historically referred to as shales, are composed of calcareous mudstone, dolomudstone, and calcareous sandstone. High total organic carbon (TOC) values are more closely linked to sequence stratigraphic posit

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33

Quick, Russell Emerson Edward. "Petroleum geochemistry of a source rock-reservoir contact /." 1991. http://collections.mun.ca/u?/theses,126100.

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34

Morelos, Garcia Javier Alejandro. "Geochemical evaluation of southern Tampico-Misantla Basin, Mexico : oil-oil and oil source rock correlations /." 1996. http://proquest.umi.com/pqdweb?did=742492401&sid=1&Fmt=2&clientId=10361&RQT=309&VName=PQD.

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35

Adams, Rupert Spencer. "An examination of the role of sediment surface area in controlling the preservation of organic matter in a paralic environment and its influence on petroleum source rock formation and contaminant adsorption, Howe Sound, British Columbia." Thesis, 2003. http://hdl.handle.net/2429/14057.

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Howe Sound, a glacial fjord situated between Vancouver and Squamish, British Columbia, is subject to a semi-restricted, estuarine type flow regime that results in easily quantifiable sources for the organic matter present in the sediments. Therefore, it was chosen as an ideal location to examine the effects of sediment surface area on the preservation of organic matter and industrial pollutants in the paralic environment. A variety of surface sediment and core samples were retrieved and analyzed for organic content and surface area, as well as other sediment biomarkers and organic pollutant co

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