Дисертації з теми "Basin history"
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Smith, Stuart A. "The phanerozoic basin-fill history of the Roebuck Basin /." Title page, abstract and contents only, 1999. http://web4.library.adelaide.edu.au/theses/09PH/09phs6615.pdf.
Повний текст джерелаEnglish, Kara. "Burial history modelling and reservoir quality in exhumed basins : insights from the Illizi Basin, Algeria." Thesis, University of Manchester, 2017. https://www.research.manchester.ac.uk/portal/en/theses/burial-history-modelling-and-reservoir-quality-in-exhumed-basins-insights-from-the-illizi-basin-algeria(353e041a-1824-4233-bea5-5018e36485ea).html.
Повний текст джерелаWillis, M. G. "The tectonic history of the Lusitanian Basin of Portugal." Thesis, Open University, 1989. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.328835.
Повний текст джерелаSippel, Judith. "The paleostress history of the Central European basin system." Potsdam GFZ, Helmholtz-Zentrum, 2009. http://d-nb.info/996100245/34.
Повний текст джерелаClarke, Margaret L. "Reconstituting the fur trade community of the Assiniboine basin, 1793 to 1812." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp04/mq23256.pdf.
Повний текст джерелаAdriasola, Muñoz Yvonne. "The thermal history of the Western Lower Saxony Basin, Germany." Aachen Mainz, 2006. http://d-nb.info/99793090X/34.
Повний текст джерелаAdriasola, Muñoz Yvonne. "The thermal history of the Western Lower Saxony Basin, Germany /." Aachen : Mainz, 2007. http://d-nb.info/987484036/04.
Повний текст джерелаSatterfield, Dorothy Ann. "Sedimentary history of a senonian foreland basin, Languedoc, southern France." Thesis, University of Oxford, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.260757.
Повний текст джерелаCuevas, Leree Juan Antonio. "Analysis of subsidence and thermal history in the Sabinas Basin, northeasern Mexico." Thesis, The University of Arizona, 1985. http://hdl.handle.net/10150/558018.
Повний текст джерелаAllen, H. D. "Late Quaternary of the Kopais Basin, Greece : Sedimentary and environmental history." Thesis, University of Cambridge, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.383701.
Повний текст джерелаNewman, Lareen A. "Environmental history of the Willunga Basin, 1830's to 1990's /." Title page, contents and abstract only, 1994. http://web4.library.adelaide.edu.au/theses/09AR/09arn553.pdf.
Повний текст джерелаSippel, Judith [Verfasser]. "The paleostress history of the Central European basin system / Judith Sippel." Potsdam : GFZ, Helmholtz-Zentrum, 2009. http://d-nb.info/996100245/34.
Повний текст джерелаZin, Ismail Che Mat. "Tertiary tectonics and sedimentation history of the Sarawak Basin, east Malaysia." Thesis, Durham University, 1996. http://etheses.dur.ac.uk/5198/.
Повний текст джерелаLuyt, Julian Peter. "The tectono-sedimentary history of the coal-bearing Tshipise Karoo basin." Diss., University of Pretoria, 2017. http://hdl.handle.net/2263/63290.
Повний текст джерелаDissertation (MSc)--University of Pretoria, 2017.
Geology
MSc
Unrestricted
Lisk, Mark. "Fluid migration and hydrocarbon charge history of the vulcan sub-basin." Thesis, Curtin University, 2012. http://hdl.handle.net/20.500.11937/1932.
Повний текст джерелаHasan, Abed M. T. "The geomorphological history of the Gebel Al Akhdar valleys, North-eastern Libya." Thesis, University of Nottingham, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.243772.
Повний текст джерелаRamphaka, Lerato Priscilla. "Integrating 3D basin modelling concept to determine source rock maturation in the F-O Gas Field, Bredasdorp Basin (offshore South Africa)." Thesis, University of the Western Cape, 2015. http://hdl.handle.net/11394/5340.
Повний текст джерелаThe burial history, thermal maturity and petroleum generation history of the F-O Gas Field, Bredasdorp Basin have been studied using 3D basin and petroleum systems modelling approach. The investigated sedimentary basin for this study evolved around mid-late Jurassic to early Cretaceous times when Southern Africa rifted from South America. The F-O field is located 40 km SE of the F-A platform which supplies gas and condensate to the PetroSA ‘Gas to Liquid’ plant located in Mossel Bay. As data integration is an integral part of the applied modelling concept, 2D seismic profile and well data (i.e. logs and reports from four drilled wells) were integrated into a 3D structural model of the basin. Four source rock intervals (three from the Early Cretaceous stages namely; Hauterivian, Barremian, Aptian and one from the Late Cretaceous Turonian stage) were incorporated into the 3D model for evaluating source rock maturation and petroleum generation potential of the F-O Gas Field. Additionally, measured present-day temperature, vitrinite reflectance, source potential data, basin burial and thermal history and timing of source rock maturation, petroleum generation and expulsion were forwardly simulated using a 3D basin modelling technique. At present-day, Turonian source rock is mainly in early oil (0.55-0.7% VRo) window, while the Aptian and Barremian source rocks are in the main oil (0.7-1.0% VRo) window, and the Hauterivian source rock is mainly in the main oil (0.7-1.0% VRo) to late oil (1.0-1.3% VRo) window. In the entire four source rock intervals the northern domain of the modelled area show low transformation, indicated by low maturity values that are attributable to less overburden thickness. Petroleum generation begins in later part of Early Cretaceous, corresponding to high heat flow and rapid subsidence/ sedimentation rates. The Barremian and Aptian source rocks are the main petroleum generators, and both shows very high expulsion efficiencies. The modelling results however indicate that the younger Aptian source rock could be regarded as the best source rock out of the four modelled source rocks in the F-O field due to its quantity (i.e. highest TOC of 3%), quality (Type II with HI values of 400) and highest remaining potential. At present-day, ~1209 Mtons of hydrocarbons were cumulatively generated and peak generation occurred at ~43 Ma with over 581 Mtons generated. Finally, the results of this study can directly be applied for play to prospect risk analysis of the F-O gas field.
Smyth, Helen. "Eocene to Miocene basin history and volcanic activity in East Java, Indonesia." Thesis, Royal Holloway, University of London, 2005. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.417139.
Повний текст джерелаMachado, Vladimir Alberto Gouveia. "Sand provenance, diagenesis and hydrocarbon charge history of the Kwanza Basin, Angola." Thesis, University of Aberdeen, 2007. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=225701.
Повний текст джерелаGillies, Douglas. "Diagenetic history of the Waulsortian carbonate buildups, (Dinantian), Craven Basin, NW England." Thesis, University of Edinburgh, 1987. http://hdl.handle.net/1842/13904.
Повний текст джерелаGemperle, Christine K. "Kokanee Fry Recruitment and Early Life History in the Lake Tahoe Basin." DigitalCommons@USU, 1998. https://digitalcommons.usu.edu/etd/6686.
Повний текст джерелаBrewster, Melvin G. 1960. "Numu views of Numu cultures and history : cultural stewardship issues and a Punown view of Gosiute and Shoshone archaeology in the northeast Great Basin." Thesis, University of Oregon, 2003. http://hdl.handle.net/1794/9452.
Повний текст джерелаThe culture history of the northeastern Great Basin, as currently written by the archaeological profession, is silent as to the view of Gosiute and Shoshone natives about their own ancestors. The goal of this dissertation is the infusion of Punown (interrelated Numic speaking peoples) epistemology into mainstream anthropological interpretation, as provided through North American Desert West prehistory. The hypothesized Numic expansion into the Northeast Great Basin, according to which the Punown natives now resident throughout the region are very recent immigrants, is problematic on several grounds. In the dissertation I show that late population movement into this region by Numic ancestors has not been demonstrated. After a hundred years of research no consensus yet exists as to the origins of the Northern Uto-Aztecan speaking Numic peoples (Punown). In spite of that, and in spite of the fact that it takes no account of the natives' own view of their origins, the Numic Expansion Hypothesis is being used in a way by some archaeologists and cultural resource managers that denies to the Punown their cultural heritage. The archaeological record of the region, extending back into deep time, is rich in the similarities it shows with the native Punown cultures of the contact-historic period. The epistemology and spiritual beliefs of the Punown also assert their cultural continuity with the ancient traditions documented in that archaeological recoret;It is not acceptable that a scientific hypothesis impedes native people's role in the care and stewardship of sites and places throughout the region that their own spiritual traditions tell them they are responsible for. The mainstream anthropological concept of science and the epistemology of the Punown are opposed diametrically. Punown view the world and its people as interconnected through the Sacred Earth Matrix, while anthropologists see the human world as bifurcated from nature. Punown understand archaeology and relatedness spiritually, while archaeologists see dead objects in an "objectified" way. Conformity to the existing paradigm, with its persistent building and rebuilding of earlier untenable Euroamerican views of Numic origins, makes the Punown outsiders to the region in which they live. This goes on even though many scholars, reviewing the case for a Numic Expansion, find it seriously lacking. Infusion of Punown epistemology into current archaeological practice offers a basis for pooling Punown and mainstream anthropological approaches to the prehistory of the Desert West. A mutually enhancing research partnership based on beneficial objectives is advocated; this will go far to repair a strained relationship that now exists between Punown and archaeological researchers, and result in a fuller and richer history for all to contemplate.
Committee in Charge: Dr. C. Melvin Aikens, Chair; Dr. Jon Erlandson; Dr. Lawrence Sugiyama; Dr. Scott DeLancey
Tozer, Brook. "Crustal structure, gravity anomalies and subsidence history of the Parnaíba cratonic basin, Northeast Brazil." Thesis, University of Oxford, 2017. https://ora.ox.ac.uk/objects/uuid:90ce8bb0-e55d-4b3c-87e1-aab60084ef42.
Повний текст джерелаSwindell, Bryan Cameron. "Tree-ring reconstructed streamflow and drought history for the Bighorn River Basin, Wyoming." Thesis, Montana State University, 2011. http://etd.lib.montana.edu/etd/2011/swindell/SwindellB1211.pdf.
Повний текст джерелаDwane, Zandile. "Burial history and source rocks characteristics of the montney formation, Alberta basin, Canada." University of the Western Cape, 2016. http://hdl.handle.net/11394/5732.
Повний текст джерелаMore than 300 samples from the Montney Formations in the Alberta basin, offshore, Canada have been analysed with locations in various parts of the Alberta basin. These samples were mainly analyzed from two wells (well M28 & M22) to assess the organic quality, quantity as well as thermal maturation by Tmax versus PI (Production Index) from Rock-Eval Pyrolysis and Vitrinite Reflectance data. Two well locations (301 & 306) have been chosen for calibrating burial history and thermal maturation models in the Alberta basin because of their measured bottom hole temperature data which was assumed to be taken from the nearby well. These well locations also have measured Vitrinite Reflectance data which was taken directly from coal-bearing Mannville Group. The Triassic Montney Formation silty shale and shale, was deposited within an anoxic depositional environments and shows a wide variability of organic oil and gas prone Type II, II-III and III source rocks. M22 samples display excellent organic matter quantity (TOC up to 5.80%), and Type II and Type III kerogens, which are favourable for hydrocarbon generation. The high TOC values generally indicate that the condition during the deposition of sediments was favourable for organic matter production and preservation. The genetic potential (GP) and hydrogen Index (HI) is above the minimum values required for a potential source rock, suggesting that the sediments have gas and oil generating potential. However, in M22, only few samples met the requirements for the organic matter quantity, quality, and thermal maturity in order to be called source rocks. This could be because the samples from M28 were collected from outcrops which are easily affected by weathering. This significantly changed the TOC values and affected thermal maturation and Rock-eval Pyrolysis parameters.
Butler, Sarah Marie. "Forest Disturbance History and Stand Dynamics of the Coweeta Basin, Western North Carolina." Fogler Library, University of Maine, 2006. http://www.library.umaine.edu/theses/pdf/ButlerSM2006.pdf.
Повний текст джерелаTabibian, Mahmoud. "Natural gas stability and thermal history of the Arbuckle Reservoir, Western Arkoma Basin /." Access abstract and link to full text, 1993. http://0-wwwlib.umi.com.library.utulsa.edu/dissertations/fullcit/9318178.
Повний текст джерелаJoy, Aidan Michael. "An analysis of the post-rift subsidence history of the North Sea Basin." Thesis, Imperial College London, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.261244.
Повний текст джерелаSpathopoulos, Phoebus. "The geological structure and history of the Gambia Basin and Senegal Continental Margin." Thesis, University College London (University of London), 1990. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.284802.
Повний текст джерелаJennings, Jonathan Simon. "Fracture kinematics, cementation and burial history of a structurally polyphase sedimentary basin, Tunisia." Thesis, Kingston University, 2001. http://eprints.kingston.ac.uk/20680/.
Повний текст джерелаBritton, Layne. "Depositional history of a low sulfur coal in a typically high sulfur basin /." Available to subscribers only, 2009. http://proquest.umi.com/pqdweb?did=1796356181&sid=2&Fmt=2&clientId=1509&RQT=309&VName=PQD.
Повний текст джерелаWilson, Doyle Coley. "Post-middle Miocene Geologic History of the Tualatin Basin, Oregon with Hydrogeologic Implications." PDXScholar, 1997. https://pdxscholar.library.pdx.edu/open_access_etds/4711.
Повний текст джерелаMogren, Eric Thomas. "Governance in the United States Columbia River Basin: An Historical Analysis." PDXScholar, 2011. https://pdxscholar.library.pdx.edu/open_access_etds/48.
Повний текст джерелаPugh, Jeremy Mark. "The late Quaternary environmental history of the Lake Heron basin, Mid Canterbury, New Zealand." Thesis, University of Canterbury. Geological Sciences, 2008. http://hdl.handle.net/10092/1766.
Повний текст джерелаBatterson, Martin Jonathan. "Quaternary history, palaeo-geography and sedimentology of the Humber River basin and adjacent areas." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape11/PQDD_0006/NQ42472.pdf.
Повний текст джерелаRiches, Peter Frank. "The palaeoenvironmental and neotectonic history of the Early Pleistocene Crag basin in East Anglia." Thesis, Royal Holloway, University of London, 2012. http://repository.royalholloway.ac.uk/items/eb59ceaa-948a-01c8-30e1-4c06a764447a/8/.
Повний текст джерелаKiconco, Lyoidah. "The Semliki Basin, Uganda : its sedimentation history and stratigraphy in relation to petroleum accumulation." Master's thesis, University of Cape Town, 2005. http://hdl.handle.net/11427/8656.
Повний текст джерелаThe Semliki Basin is covered by sediments that represent the Middle Miocene to Recent, which are described from outcrop and well data, underlain by possible Jurassic or Permo-Triassic to Early Tertiary sediments, which rest unconformably on Basement, described from seismic data. Thin-section analysis of selected samples, collected from the field, has shown that sandstones from the Semliki Basin are predominantly composed of quartz, potassium feldspars and plagioclase feldspars with subordinate clay minerals. Accessory minerals, such as micas (biotite and muscovite), heavy minerals, garnet and epidote, are present in minor amounts. This mineralogy indicates that the sediments have a granitic and gneissose origin, related to continental-block provenances. The X-ray diffraction scans of bulk samples reveal that the mudrocks/claystones are dominated by clay minerals with subordinate quartz, feldspars and calcite. The clay minerals include illite, illite-smectite, kaolinite, montmorillonite, illite-monnnorillonite, and mica with mixed layer illite-smectite and illite layers dominating. The clay minerals in the sediments were interpreted to be as a result of weathering of feldspars and volcaniclastic sediments. Authigenic minerals such as anatase and jarosite and secondary precipitates such as calcite and gypsum have also been interpreted as oxidation products of sulphides in the sediments. The study has allowed a better understanding of the stratigraphic relationship of the different rock units that are exposed on outcrop, those encountered in the wells, plus a section interpreted from seismic data. In general, the depositional environment of the sediments in the Semliki Basin is fluvial-lacustrine/deltaic showing significant variations in gamma-ray character, which reflect the water-level changes and river interactions through the depositional period and the influence of rifting tectonics on sediment deposition through time and space. The sediments in the Semliki Basin represent a petroleum play for hydrocarbon accumulations, in which the necessary elements of a valid petroleum system were identified. These include excellent or good potential for reservoirs and top seals as well as circumstantial evidence of regionally mature source rocks, possible seals, traps and hydrocarbon-migration pathways.
Downey, Nathan John Avouac Jean-Philippe Stock J. M. Gurnis Michael Clayton Robert W. "Tectonic history of the Osbourn spreading center and dynamic subsidence of the Congo basin /." Diss., Pasadena, Calif. : California Institute of Technology, 2009. http://resolver.caltech.edu/CaltechETD:etd-08282008-093820.
Повний текст джерелаBlinnikov, Mikhail S. "Late-Pleistocene history of the Columbia Basin grassland based on phytolith records in loess /." view abstract or download file of text, 1999. http://wwwlib.umi.com/cr/uoregon/fullcit?p9948017.
Повний текст джерелаTypescript. Includes vita and abstract. Includes bibliographical references (leaves 202-211). Also available for download from the Internet; free to University of Oregon users. Address: http://wwwlib.umi.com/cr/uoregon/fullcit?p9948017.
Batterson, Martin J. "Quaternary history, palaeo-geography and sedimentology of the Humber River basin and adjacent areas /." Internet access available to MUN users only, 1998. http://collections.mun.ca/u?/theses,57121.
Повний текст джерелаMurphy, Michael J. "Geophysical investigation of the tectonic and volcanic history of the Nauru Basin, Western Pacific /." Electronic version, 2004. http://dl.uncw.edu/etd/2004/murphym/michaelmurphy.html.
Повний текст джерелаSteinmann, Michael. "The Cuenca basin of southern Ecuador : tectono-sedimentary history and the Tertiary Andean evolution /." Zurich : Swiss federal institute of technology, 1997. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=12297.
Повний текст джерелаJames, Jonathan Scott. "Exploration, monetization, disillusion: a history of upstream oil development in the onshore Algoa basin." Thesis, Rhodes University, 2016. http://hdl.handle.net/10962/3870.
Повний текст джерелаWhite, Helena Elizabeth. "Establishing the chronostratigraphy and Miocene-Pliocene palaeoenvironmental history of the Fazzan Basin, Libyan Sahara." Thesis, University of Leicester, 2017. http://hdl.handle.net/2381/39907.
Повний текст джерелаAsmussen, Pascal. "Insights from the Devonian Adavale Basin on the tectonic history of the Thomson Orogen." Thesis, Queensland University of Technology, 2020. https://eprints.qut.edu.au/200906/1/Pascal_Asmussen_Thesis.pdf.
Повний текст джерелаElliott, Emily Maureen. "Organic nitrogen isotope stratigraphy, palynology, and sediment history of freshwater wetlands in the Chesapeake Bay basin comparison with land use history /." Available to US Hopkins community, 2003. http://wwwlib.umi.com/dissertations/dlnow/3080655.
Повний текст джерелаCollins, Michael L. "Norfolk and North Sea Southern Basin natural gas 1966-1995 : a study in political economy." Thesis, University of East Anglia, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.389372.
Повний текст джерелаZiegler, Karen. "Diagenetic and geochemical history of the Rotliegend of the southern North Sea (UK sector) : a comparative study." Thesis, University of Reading, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.321269.
Повний текст джерелаVolkmann, Abigail J. "River Basin Management and Restoration in Germany and the United States: Two Case Studies." Scholarship @ Claremont, 2013. http://scholarship.claremont.edu/scripps_theses/165.
Повний текст джерелаMazel, Aron D. "People making history : the last ten thousand years of hunter-gatherer communities in the Thukela Basin." Doctoral thesis, University of Cape Town, 1988. http://hdl.handle.net/11427/21814.
Повний текст джерелаThe primary aim of this thesis is to document and explain the 10 000 BP AD 1800 history of the Thukela Basin hunter-gatherers. The primary information for this study comes from my excavation, between 1981 and 1984, of eight rock shelters in the upper Thukela catchment. My aims and theoretical orientation have altered substantially since the project's ,inception. They have changed from being concerned primarily with ecological phenomena to the reconstruction of a regional social history. As part of this redefinition I have developed a critique of South African Later Stone Age (LSA) studies from the early 1960s, arguing that the predominant, ecological, approaches of this period are inadequate in dealing with past human societies. My reasons for adopting a socially orientated historical approach concern the social relevance of archaeology, and the need to generate the best possible insights into past societies. I submit that historical materialism offers a very valuable framework for social historical analysis. The theoretical propositions germane to this study are presented. I then concentrate specifically on Thukela Basirr hunter-gatherer history. The periods dating to before and after 2000 BP are dealt with separately because of the arrival of farmers in the Thukela Basin around AD 500.