Дисертації з теми "Petrologic analysis"
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Sheehan, Laura R. "Sedimentary and petrologic analysis of the Mississippian Price Formation at Sherwood Lake, West Virginia." Morgantown, W. Va. : [West Virginia University Libraries], 2002. http://etd.wvu.edu/templates/showETD.cfm?recnum=2544.
Повний текст джерелаTitle from document title page. Document formatted into pages; contains ix, 132 p. : ill. (some col.), maps (some col.). Includes abstract. Includes bibliographical references (p. 106-109).
Karel, Patrick Robert. "Seismic Analysis of the Tonga Subduction Zone and Implications on the Thermo-Petrologic Evolution of Deep Subduction." Miami University / OhioLINK, 2011. http://rave.ohiolink.edu/etdc/view?acc_num=miami1313773845.
Повний текст джерелаCunderla, Brent Joseph. "Stratigraphic and petrologic analysis of trends within the Spencer Formation sandstones : from Corvallis, Benton County, to Henry Hagg Lake, Yamhill and Washington counties, Oregon." PDXScholar, 1986. https://pdxscholar.library.pdx.edu/open_access_etds/3588.
Повний текст джерелаLindeberg, Tomas. "Indium Analysis and Small-scale Distribution in Sulphides from the Lindbom Prospect, Långban Area, Western Bergslagen Ore Province." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2013. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-196479.
Повний текст джерелаNejedlik, John. "Petrographic image analysis as a tool to quantify porosity and cement distribution." Title page, contents and abstract only, 2001. http://web4.library.adelaide.edu.au/theses/09SM/09smn417.pdf.
Повний текст джерелаDeBuhr, Christopher Leonard. "Metamorphic petrology and mass balance analysis in the Bugaboo contact aureole." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0019/NQ49488.pdf.
Повний текст джерелаHelbing, Heiko. "No suture in the Sardinian Variscides a structural, petrological and geochronological analysis /." Tübingen : Univ, 2003. http://www.bsz-bw.de/cgi-bin/xvms.cgi?SWB10733113.
Повний текст джерелаKoebli, Danielle. "A Geochemical and Petrological Analysis of the San Rafael Volcanic Field, Utah." Scholar Commons, 2017. https://scholarcommons.usf.edu/etd/7417.
Повний текст джерелаKhabir, Abdelrahim Mohamed. "Mesolithic and neolithic ceramics in the Central Sudan, 8th-3rd millennium B.C., with special reference to the physico-scientific approach." Thesis, University of Southampton, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.389855.
Повний текст джерелаClowes, Emma. "A microbiostratigraphical analysis of the Kolbano sequence (Jurassic to Pliocene), West Timor, and its radiolarian faunas." Thesis, University College London (University of London), 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.265805.
Повний текст джерелаZhao, Xianghong. "Automated image analysis for petrographic image assessments." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp03/MQ62444.pdf.
Повний текст джерелаCarvalho, Cássio Santos de. "Estudo do comportamento tecnológico e de alterabilidade das rochas ornamentais silicáticas verde Amazonas, preto Cajugram e bege Ipanema - (ES) /." Rio Claro : [s.n.], 2010. http://hdl.handle.net/11449/92894.
Повний текст джерелаBanca: Fabiano Cabañas Navarro
Banca: Tamar Milca Bortolozzo Galembeck
Resumo: As rochas ornamentais Verde Amazonas, Preto Cajugram e Bege Ipanema exploradas no estado do Espírito Santo, respectivamente um charnockito, um hiperstênio monzodiorito e um ortognaisse, foram submetidas a uma bateria de ensaios físico-mecânicos e de resistência ao ataque químico sob ação controlada dos compostos NH4Cl, NaClO, C6H8O7, HCl e KOH presentes na composição de produtos de uso doméstico e de determinadas soluções concentradas dos ácidas HCl, H2SO4 e HNO3 simulando atmosferas agressivas. A avaliação dos efeitos dos agentes químicos foram realizadas à luz das variações da propagação de ondas ultrassônicas, da resistência à flexão 4 pontos e do lustro da superfície polida das rochas testadas, bem como pela caracterização dos produtos de subeflorescências e eflorescências geradas pelas reações com os ácidos. Os resultados dos diferentes testes realizados foram confrontados com as propriedades petrográficas de cada rocha. Os resultados obtidos para os parâmetros físico-mecânicos e de alterabilidade química indicam, com algumas reservas, que as três rochas são detentoras de boas qualidades para utilização como rochas ornamentais e para revestimentos em obras civis. Os estudos revelaram que o comportamento tecnológico e de alterabilidade química dos materiais avaliados é controlado pela inter-relação dos aspectos composicionais, estruturais e texturais das rochas. O charnockito Verde Amazonas, rocha verde escura megaporfirítica gnaissificada com matriz de granulação média a grossa e com elevado grau de microfissuramento transgranulares, apresentou bom desempenho no tocante a resistência mecânica, mas foi o material que mostrou maior sensibilidade aos efeitos da maioria dos agentes químicos com desbotamento, clareamento, amarelamento e ofuscamento das superfícies polidas. O Preto Cajugram com estrutura isotrópica, textura equigranular... (Resumo completo, clicar acesso eletrônico abaixo)
Abstract: The Amazon Green, Cajugram Black and Ipanema Beige dimension stones explored in the state of Espirito Santo, respectively, a charnockite, a hypersthene monzodiorite and a orthogneiss, underwent a serie of physical-mechanical and resistance to chemical attack tests under controlled action of the chemicals NH4Cl, NaClO, C6H8O7, HCl and KOH, present in the composition of household products and certain concentrated solutions of the acids HCl, H2SO4 and HNO3, simulating aggressive atmospheres. The evaluation of the effects of the chemical agents was performed in the light of changes in the propagation of ultrasonic sound waves, the 4-point flexural strength and gloss of the polished surface of the tested rock samples, as well as the characterization of the products of efflorescences and subefflorescences, generated by reactions with the acids. The results of the different tests were compared with the petrographic properties of each rock. The obtained results for the physic-mechanical parameters and for the chemical alterability indicates, with some reservations, that the three rocks shows good quality for use as dimension stones and coatings in civil works. Studies show that the behavior of technology and chemical alterability of the tested materials is controlled by the interrelation of the compositional, structural and textural aspects of the rocks. The charnockite Verde Amazonas, dark green megaporphyritic gneissic rock, with medium to coarse grained matrix and a high degree of transgranular microcracking, showed good performance regarding mechanical strength, but was the most sensitive material to the effects of most chemical agents as fading, bleaching, yellowing and glare from the polished surfaces. The Preto Cajugram, with isotropic structure, medium equigranular texture, and low degree of microcracking, has the highest mechanical strengths. On the other hand, it displays the highest... (Complete abstract click electronic access below)
Mestre
Westby, Elizabeth G. "The Geology and Petrology of Enigmatic Rhyolites at Graveyard and Gordon Buttes, Mount Hood Quadrangle, Oregon." PDXScholar, 2014. https://pdxscholar.library.pdx.edu/open_access_etds/2063.
Повний текст джерелаJones, Marilyn Gail 1963. "Clay mineralogy and petrology of the Lower Cretaceous fine-grained clastic rocks, southeastern Arizona." Thesis, The University of Arizona, 1989. http://hdl.handle.net/10150/558100.
Повний текст джерелаHulett, Sam Rw. "Detrital Zircon Analysis of Permian Victoria Group Sandstones, Transantarctic Mountains, Antarctica." The Ohio State University, 2012. http://rave.ohiolink.edu/etdc/view?acc_num=osu1355867143.
Повний текст джерелаCotton, Timothy Brett. "Petrological analysis of mineral scales formed during gas production from permian reservoirs in the Cooper Basin /." Title page, abstract and table of contents only, 2003. http://web4.library.adelaide.edu.au/theses/09SB/09sbc8511.pdf.
Повний текст джерелаGillam, Daniel J. "Structural and geomechanical analysis of naturally fractured hydrocarbon provinces of the Bowen and Amadeus Basins: onshore Australia /." Title page, table of contents and abstract only, 2004. http://web4.library.adelaide.edu.au/theses/09PH/09phg4758.pdf.
Повний текст джерелаDe, Gasperi Patricia Martins Silva. "Estimativa de propriedades petrofisicas atraves da reconstrução 3D do meio poroso a partir da analise de imagens." [s.n.], 1999. http://repositorio.unicamp.br/jspui/handle/REPOSIP/264010.
Повний текст джерелаDissertação (mestrado) - Universidade Estadual de Campinas, Faculdade de Engenharia Mecanica
Made available in DSpace on 2018-07-26T08:21:56Z (GMT). No. of bitstreams: 1 DeGasperi_PatriciaMartinsSilva_M.pdf: 13462853 bytes, checksum: cff9140cfbd41d9dc52865fb52425605 (MD5) Previous issue date: 1999
Resumo: Este trabalho tem como objetivos o estudo e a aplicação do processo de estimativa de propriedades petrofisicas a partir de informações obtidas em imagens petrográficas bidimensionais. O método assume a hipótese da homogeneidade estatística, e utiliza a simulação estocástica para a reconstrução do modelo tridimensional do meio poroso. A caracterização geométrica do meio simulado permite a elaboração de um modelo de rede para a simulação do fluxo e a estimativa da permeabilidade, fator de formação, pressão capilar por injeção de mercúrio e relação índice de resistividade versus saturação de água. Esta metodologia é aplicada a quatro sistemas porosos com diferentes níveis de heterogeneidade. Os resultados demonstram que estimativas confiáveis dependem da utilização de uma resolução apropriada de aquisição das imagens, que permita a identificação de poros e gargantas que efetivamente controlem as propriedades de fluxo do sistema. As curvas de pressão capilar simuladas sugerem a necessidade da composição de escalas. As propriedades elétricas são afetadas pela porosidade das amostras e sua confiabilidade é restrita a sistemas preferencialmente molháveis pela água
Abstract: The aim of this work is to investigate and apply a method for predicting petrophysical properties ftom bidimensional petrographic image data. Based on the assumption of statistical homogeneity, the method uses stochastic simulation to reconstruct the porous media tridimensional structure. The geometrical characterization of the simulated media allows the construction of a network model to simulate fluid flow and estimate permeability, formation factor, mercury capillary pressure curves and resistivity index as function of water saturation. This method is applied to four porous systems with different heterogeneity levels. The results demonstrate that good predictions depend on the appropriate image aquisition resolution, which identifies pores and throats that effectively control the flow properties of the system. The capillary pressure curves suggest the necessity of scale composition. The electrical properties are affected by samples porosity, with reliable estimates being restricted to water-wet systems
Mestrado
Mestre em Engenharia de Petróleo
Sales, Hillarie Jaye. "The Wildcat Creek Tuff, Eastern Oregon: Co-eruption of Crystal-poor Rhyolite and Fe-rich Andesite with Implication for Mafic Underpinnings to Voluminous A-type Rhyolites." PDXScholar, 2018. https://pdxscholar.library.pdx.edu/open_access_etds/4352.
Повний текст джерелаVaughan, Sarah J. "A fabric analysis of Late Cypriot Base Ring Ware : studies in ceramic technology, petrology, geochemistry and mineralogy." Thesis, University College London (University of London), 1987. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.281701.
Повний текст джерелаCarvalho, Cássio Santos de [UNESP]. "Estudo do comportamento tecnológico e de alterabilidade das rochas ornamentais silicáticas verde Amazonas, preto Cajugram e bege Ipanema - (ES)." Universidade Estadual Paulista (UNESP), 2010. http://hdl.handle.net/11449/92894.
Повний текст джерелаCoordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)
As rochas ornamentais Verde Amazonas, Preto Cajugram e Bege Ipanema exploradas no estado do Espírito Santo, respectivamente um charnockito, um hiperstênio monzodiorito e um ortognaisse, foram submetidas a uma bateria de ensaios físico-mecânicos e de resistência ao ataque químico sob ação controlada dos compostos NH4Cl, NaClO, C6H8O7, HCl e KOH presentes na composição de produtos de uso doméstico e de determinadas soluções concentradas dos ácidas HCl, H2SO4 e HNO3 simulando atmosferas agressivas. A avaliação dos efeitos dos agentes químicos foram realizadas à luz das variações da propagação de ondas ultrassônicas, da resistência à flexão 4 pontos e do lustro da superfície polida das rochas testadas, bem como pela caracterização dos produtos de subeflorescências e eflorescências geradas pelas reações com os ácidos. Os resultados dos diferentes testes realizados foram confrontados com as propriedades petrográficas de cada rocha. Os resultados obtidos para os parâmetros físico-mecânicos e de alterabilidade química indicam, com algumas reservas, que as três rochas são detentoras de boas qualidades para utilização como rochas ornamentais e para revestimentos em obras civis. Os estudos revelaram que o comportamento tecnológico e de alterabilidade química dos materiais avaliados é controlado pela inter-relação dos aspectos composicionais, estruturais e texturais das rochas. O charnockito Verde Amazonas, rocha verde escura megaporfirítica gnaissificada com matriz de granulação média a grossa e com elevado grau de microfissuramento transgranulares, apresentou bom desempenho no tocante a resistência mecânica, mas foi o material que mostrou maior sensibilidade aos efeitos da maioria dos agentes químicos com desbotamento, clareamento, amarelamento e ofuscamento das superfícies polidas. O Preto Cajugram com estrutura isotrópica, textura equigranular...
The Amazon Green, Cajugram Black and Ipanema Beige dimension stones explored in the state of Espirito Santo, respectively, a charnockite, a hypersthene monzodiorite and a orthogneiss, underwent a serie of physical-mechanical and resistance to chemical attack tests under controlled action of the chemicals NH4Cl, NaClO, C6H8O7, HCl and KOH, present in the composition of household products and certain concentrated solutions of the acids HCl, H2SO4 and HNO3, simulating aggressive atmospheres. The evaluation of the effects of the chemical agents was performed in the light of changes in the propagation of ultrasonic sound waves, the 4-point flexural strength and gloss of the polished surface of the tested rock samples, as well as the characterization of the products of efflorescences and subefflorescences, generated by reactions with the acids. The results of the different tests were compared with the petrographic properties of each rock. The obtained results for the physic-mechanical parameters and for the chemical alterability indicates, with some reservations, that the three rocks shows good quality for use as dimension stones and coatings in civil works. Studies show that the behavior of technology and chemical alterability of the tested materials is controlled by the interrelation of the compositional, structural and textural aspects of the rocks. The charnockite Verde Amazonas, dark green megaporphyritic gneissic rock, with medium to coarse grained matrix and a high degree of transgranular microcracking, showed good performance regarding mechanical strength, but was the most sensitive material to the effects of most chemical agents as fading, bleaching, yellowing and glare from the polished surfaces. The Preto Cajugram, with isotropic structure, medium equigranular texture, and low degree of microcracking, has the highest mechanical strengths. On the other hand, it displays the highest... (Complete abstract click electronic access below)
McDaniel, Kyle. "Origin of Crystal Rock Cave, Ohio, USA and its record of Lake Erie variation through speleothem analyses." University of Akron / OhioLINK, 2018. http://rave.ohiolink.edu/etdc/view?acc_num=akron1530544408347209.
Повний текст джерелаAhsan, Abul. "Petrology and facies analysis of the upper sand, Hyland Bay Formation, the Petrol Gas Field, Bonaparte Gulf, Northern Australia /." Title page, contents and abstract only, 1996. http://web4.library.adelaide.edu.au/theses/09S.B/09s.ba2874.pdf.
Повний текст джерелаKaya, Egemen Tangut. "Estimation Of Expected Monetary Values Of Selected Turkish Oil Fields Using Two Different Risk Assessment Methods." Master's thesis, METU, 2004. http://etd.lib.metu.edu.tr/upload/1091495/index.pdf.
Повний текст джерелаmost likely&rdquo
results of variables that could be expected without sufficient consideration given to other possible outcomes and it is well known that initial estimates of all these variables have uncertainty. The data is usually obtained during drilling of the initial oil well and the sources are geophysical (seismic surveys) for formation depths and areal extent of the reservoir trap, well logs for formation tops and bottoms, formation porosity, water saturation and possible permeable strata, core analysis for porosity and saturation data and DST (Drill-Stem Test) for possible oil production rates and samples for PVT (Pressure Volume Temperature) analysis to obtain FVF (Formation Volume Factor) and others. The question is how certain are the values of these variables and what is the probability of these values to occur in the reservoir to evaluate the possible risks. One of the most highly appreciable applications of the risk assessment is the estimation of volumetric reserves of hydrocarbon reservoirs. Monte Carlo and moment technique consider entire ranges of the variables of Original Oil in Place (OOIP) formula rather than deterministic figures. In the present work, predictions were made about how statistical distribution and descriptive statistics of porosity, thickness, area, water saturation, recovery factor, and oil formation volume factor affect the simulated OOIP values. The current work presents the case of two different oil fields in Turkey. It was found that both techniques produce similar results for 95%. The difference between estimated values increases as the percentages decrease from 50% and 5% probability.
MacSween, Ann. "The Neolithic and late Iron Age Pottery from Pool, Sanday, Orkney : an archaeological and technological consideration of coarse pottery manufacture at the Neolithic and late Iron Age site of Pool, Orkney incorporating X-Ray Fluorescence, Inductively Coupled Plasma Spectrometric and Petrological Analyses." Thesis, University of Bradford, 1990. http://hdl.handle.net/10454/3375.
Повний текст джерелаBarone, Jessica Lynn. "Petrological and geochemical analysis of coal mine spoil to determine the source of magnesium-rich groundwater, Star Fire Mine, Eastern Kentucky." Virtual Press, 2000. http://liblink.bsu.edu/uhtbin/catkey/1189406.
Повний текст джерелаDepartment of Geology
Murgatroyd, Jennifer Leigh. "Ancient mortar production in Ostia, Italy : builders and their choices." Thesis, University of Oxford, 2016. https://ora.ox.ac.uk/objects/uuid:358de9ea-d89b-4053-84c7-0fdc29340bb2.
Повний текст джерелаOsborn, Caleb R. "Microfacies Analysis, Sedimentary Petrology, and Reservoir Characterization of the Sinbad Limestone Based Upon Surface Exposures in the San Rafael Swell, Utah." BYU ScholarsArchive, 2007. https://scholarsarchive.byu.edu/etd/1414.
Повний текст джерелаNavarro, Fabiano Cabañas. "Influência da petrografia sobre a anisotropia à tensão de compressão e dilatação térmica de rochas ornamentais /." Rio Claro : [s.n.], 2006. http://hdl.handle.net/11449/103006.
Повний текст джерелаBanca: Antenor Braga Paraguassú
Banca: José Eduardo Rodrigues
Banca: Maria Heloisa Barros de Oliveira Frascá
Banca: Peter Christian Hackspacher
Resumo: Considerando um conjunto de 21 tipos de rochas utilizadas como revestimento e subdivididas em quatro conjuntos por afinidade da composição mineral (rochas carbonáticas, quartzosas, feldspáticas e quartzo-feldspáticas) foram realizados ensaios tecnológicos para a determinação do coeficiente de dilatação térmica linear e da resistência à compressão uniaxial, bem como a anisotropia dessas propriedades. Os dados tecnológicos obtidos foram correlacionados com informações petrográficas qualitativas e quantitativas referentes à composição mineral, variações texturais e estruturais determinadas em seções ortogonais entre si a partir de um sistema de referência (xyz) baseado na foliação e lineação macroscopicamente visíveis. A análise integrada dos dados utilizando estatística convencional e multivariada procurou apontar as variáveis petrográficas mais relevantes para as duas propriedades tecnológicas enfocadas e suas respectivas anisotropias. A dilatação térmica e sua anisotropia são influenciadas principalmente pela composição mineral e pela orientação preferencial dos minerais embora as microfissuras desempenhem papel importante em alguns casos. A tensão de compressão mostra sua variabilidade e anisotropia influenciadas pela granulação média, tipos de contatos minerais predominantes e padrões de microfissuras mais ou menos definidos por influência da foliação presente. Constatou-se que no conjunto analisado a presença da foliação não implica necessariamente em anisotropia das duas propriedades estudadas.
Abstract: The anisotropy of thermal expansion coefficient and compressive tensile strength were determined for 21 commercially used stones gathered in four set according the main mineral composition named carbonatic, quartz-rich, feldspar-rich and quartz-feldspar-rich rocks. Using a coordinate reference system (xyz) based on the macroscopic visible foliation and lineation the samples were submitted to normalized laboratorial analyses for determination of the both technological properties and the petrographical features such as mineral composition, texture and fabric. Additionally was carried out measurements of weathered area and microcrack quantification by image analysis and texture quantification by U-stage methods. In order to understand the relationship between the anisotropy measured and petrographical data it was applied traditional and multivariate statistical analysis. The results pointed to the great significance of mineral composition and the crystallographic preferred orientation for thermal expansion and respective anisotropy, especially to monomineralic and/or foliated rocks, in spite of some cases microcracks play this role. The compressive strength is mainly controlled by a complex interaction between grain size distribution, grain boundary and microcrack patterns related or not to foliation.
Doutor
Gillings, Mark. "Ceramic production in a Roman frontier zone: A comparative Neutron Activation and Petro-Textural analysis of Roman coarse pottery from selected sites on and around the Antonine wall, Scotland." Thesis, University of Bradford, 1991. http://hdl.handle.net/10454/3374.
Повний текст джерелаSERC
Butland, Caroline. "Coal seam gas associations in the Huntly, Ohai and Greymouth regions, New Zealand." Thesis, University of Canterbury. Geological Sciences, 2006. http://hdl.handle.net/10092/1304.
Повний текст джерелаCassle, 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.
Повний текст джерелаDodson, Scott A. "Petrographic and Geochronologic Provenance Analysis of Upper Pennsylvanian Fluvial Sandstones of the Conemaugh and Monongahela Groups, Athens County, Ohio." Ohio : Ohio University, 2008. http://www.ohiolink.edu/etd/view.cgi?ohiou1218658592.
Повний текст джерелаGillings, Mark. "Ceramic production in a Roman frontier zone : a comparative Neutron Activation and Petro-Textural analysis of Roman coarse pottery from selected sites on and around the Antonine wall, Scotland." Thesis, University of Bradford, 2009. http://hdl.handle.net/10454/3374.
Повний текст джерелаLigouis, Bertrand. "La grande couche de bourran du bassin stephanien de decazeville (aveyron) : petrologie et environnements de depot du charbon, genese d'une veine puissante." Orléans, 1988. http://www.theses.fr/1988ORLE2027.
Повний текст джерелаPowell, Kristopher Michael. "Facies Analysis, Sedimentary Petrology, and Reservoir Characterization of the Lower Triassic Sinbad Limestone Member of the Moenkopi Formation, Central Utah: A Synthesis of Surface and Subsurface Data." BYU ScholarsArchive, 2017. https://scholarsarchive.byu.edu/etd/6672.
Повний текст джерелаErturk, Mehmet Cihan. "Production Performance Analysis Of Coal Bed Methane, Shale Gas, Andtight Gas Reservoirs With Different Well Trajectories And Completiontechniques." Master's thesis, METU, 2013. http://etd.lib.metu.edu.tr/upload/12615510/index.pdf.
Повний текст джерелаNavarro, Fabiano Cabañas [UNESP]. "Influência da petrografia sobre a anisotropia à tensão de compressão e dilatação térmica de rochas ornamentais." Universidade Estadual Paulista (UNESP), 2006. http://hdl.handle.net/11449/103006.
Повний текст джерелаConselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)
Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
Considerando um conjunto de 21 tipos de rochas utilizadas como revestimento e subdivididas em quatro conjuntos por afinidade da composição mineral (rochas carbonáticas, quartzosas, feldspáticas e quartzo-feldspáticas) foram realizados ensaios tecnológicos para a determinação do coeficiente de dilatação térmica linear e da resistência à compressão uniaxial, bem como a anisotropia dessas propriedades. Os dados tecnológicos obtidos foram correlacionados com informações petrográficas qualitativas e quantitativas referentes à composição mineral, variações texturais e estruturais determinadas em seções ortogonais entre si a partir de um sistema de referência (xyz) baseado na foliação e lineação macroscopicamente visíveis. A análise integrada dos dados utilizando estatística convencional e multivariada procurou apontar as variáveis petrográficas mais relevantes para as duas propriedades tecnológicas enfocadas e suas respectivas anisotropias. A dilatação térmica e sua anisotropia são influenciadas principalmente pela composição mineral e pela orientação preferencial dos minerais embora as microfissuras desempenhem papel importante em alguns casos. A tensão de compressão mostra sua variabilidade e anisotropia influenciadas pela granulação média, tipos de contatos minerais predominantes e padrões de microfissuras mais ou menos definidos por influência da foliação presente. Constatou-se que no conjunto analisado a presença da foliação não implica necessariamente em anisotropia das duas propriedades estudadas.
The anisotropy of thermal expansion coefficient and compressive tensile strength were determined for 21 commercially used stones gathered in four set according the main mineral composition named carbonatic, quartz-rich, feldspar-rich and quartz-feldspar-rich rocks. Using a coordinate reference system (xyz) based on the macroscopic visible foliation and lineation the samples were submitted to normalized laboratorial analyses for determination of the both technological properties and the petrographical features such as mineral composition, texture and fabric. Additionally was carried out measurements of weathered area and microcrack quantification by image analysis and texture quantification by U-stage methods. In order to understand the relationship between the anisotropy measured and petrographical data it was applied traditional and multivariate statistical analysis. The results pointed to the great significance of mineral composition and the crystallographic preferred orientation for thermal expansion and respective anisotropy, especially to monomineralic and/or foliated rocks, in spite of some cases microcracks play this role. The compressive strength is mainly controlled by a complex interaction between grain size distribution, grain boundary and microcrack patterns related or not to foliation.
Faßmer, Kathrin [Verfasser]. "Petrological analyses and Lu-Hf geochronology of subducted continental and oceanic crust from different locations in the upper and lower plate of the Caledonian Orogen / Kathrin Faßmer." Bonn : Universitäts- und Landesbibliothek Bonn, 2020. http://d-nb.info/1207923613/34.
Повний текст джерелаSILVA, Andrezza Sousa. "Fatores controladores dos aspectos texturais em rochas siliciclásticas deformadas por bandas cataclásticas." Universidade Federal de Campina Grande, 2018. http://dspace.sti.ufcg.edu.br:8080/jspui/handle/riufcg/1596.
Повний текст джерелаMade available in DSpace on 2018-08-29T23:45:59Z (GMT). No. of bitstreams: 1 ANDREZZA SOUSA SILVA – DISSERTAÇÃO (PPGEPM) 2018.pdf: 5233631 bytes, checksum: 12ad47a8373c6479a15d2cbfeba06e8d (MD5) Previous issue date: 2018-03-19
A Bacia Rio do Peixe (BRP) apresenta diversas estruturas rúpteis, dentre elas as bandas de deformação, que podem controlar as propriedades petrofísicas e aspectos texturais das rochas. Portanto, o objetivo deste trabalho é identificar os efeitos causados pelos diferentes tipos de bandas de deformação cataclásticas, em função da cinemática, sobre os aspectos texturais, distribuição de tamanho de grãos e poros, bem como porosidade em arenitos conglomeráticos. As propriedades dos grãos e dos poros foram extraídas através da análise de imagens em seções delgadas no Avizo Fire 8.1. No total foram analisadas 23 amostras, 19 com bandas de deformação (CB) com orientação definida (NW, NE, NS e EW), 2 amostras deformadas, porém sem bandas (SB) e 2 amostras da rocha hospedeira (ND). As rochas deformadas (CB e SB), apresentam redução no tamanho de grãos e pequeno acréscimo nos valores dos aspectos texturais em comparação a rocha não deformada (ND). Em relação à porosidade foi encontrada redução de 66% nas amostras CB e acréscimo de 13% nas SB. Ambos agrupamentos possuem maior conexão de grãos, permitindo o surgimento da macroporosidade, que não havia sido detectada nas amostras ND. Dentre as amostras com banda de deformação e cinemática definida, a rochas associadas ao sistema transcorrente dextral, de direção NW, possuem maior redução de diâmetro de grão, e menor redução de porosidade, cerca de 29%. As amostras com bandas de deformação NE e NS, formadas por cinemática transtensiva, são as amostras nas quais houve a menor quebra dos grãos, entretanto caracterizam-se pela presença de porosidade por fraturamento de grãos, gerando altos picos de macroporosidade. As amostras oriundas do sistema distensivo de direção EW possuem segunda maior redução de grãos, maior redução de porosidade e ausência de macroporosidade. Os aspectos texturais (circularidade, convexidade e razão de aspecto) das amostras com banda (NW, NE, NS e EW) é dependente da intensidade de cisalhamento provocado por diferentes sistemas deformacionais, quanto mais intenso mais cominuído será o grão, e consequentemente mais convexo, circular e menos alongado. Logo, é possível observar que a cinemática e a presença de bandas de deformação exercem controle sobre os aspectos texturais e petrofísicos dos arenitos conglomeráticos da Formação Antenor Navarro. E esse controle é definido pela compactação da rocha, rearranjo dos grãos, intensidade da catáclase, presença de fraturamento de grãos e cinemática atuante.
The Rio do Peixe Basin (RPB) presents several rump structures, among them the deformation bands, which can control the petrophysical properties and textured aspects of the rocks. Therefore, the objective of this work is to identify the effects caused by the different types of cataclastic deformation bands, as a function of kinematics, on the textural aspects, grain and pore size distribution, as well as porosity in conglomeratic sandstones. The grain and pore properties were extracted by thin section image analysis in Avizo Fire 8.1. In total, 23 specimens were analyzed, 19 with deformation bands (CB) with defined orientation (NW, NE, NS and EW), 2 deformed samples, but without bands (SB) and 2 samples of host rock (ND). The deformed rocks (CB and SB), present a reduction in grain size and small increase in the values of the textured aspects in comparison to the non-deformed rock (ND). In relation to the porosity, a reduction of 66% was found in the CB samples and a 13% increase in the SB. Both clusters have a larger grain connection, allowing the appearance of macroporosity, which had not been detected in the ND samples. Among the samples with deformation band and defined kinematics, the rocks associated to the dextral transcurrent system, NW direction, have a larger reduction of grain diameter, and a smaller reduction of porosity, about 29%. The samples with NE and NS deformation bands, formed by transtensive kinematics, are the samples with the lowest grain breakage. However, they are characterized by the presence of porosity by grain fracturing, generating high peaks of macroporosity. The samples from the EW steering distance system have the second largest grain reduction, greater reduction of porosity and absence of macroporosity. The textural aspects (roundness, convexity and aspect ratio) of the banded samples (NW, NE, NS and EW) are dependent on the shear strength caused by different deformation systems, the more intense the grain is, the more convex, circular and less elongated. Therefore, it is possible to observe that kinematics and the presence of deformation bands exert control over the texture and petrophysical aspects of the conglomeratic sandstones of the Antenor Navarro Formation. And this control is defined by the rock compaction, rearrangement of the grains, the intensity of the catachase, presence of grain fracture and active kinematics.
Cruz, Matthew. "Field Mapping Investigation and Geochemical Analysis of Volcanic Units within the Dinner Creek Tuff Eruptive Center, Malheur County, Eastern Oregon." PDXScholar, 2017. https://pdxscholar.library.pdx.edu/open_access_etds/3837.
Повний текст джерелаPickett, Clarence. "A sedimentary facies analysis of the >2.8 Ga Beniah and Bell Lake formations, Slave Province, Northwest Territories." Thèse, Chicoutimi : Université du Québec à Chicoutimi, 2002. http://theses.uqac.ca.
Повний текст джерелаIsom, Shelby Lee. "Compositional and Physical Gradients in the Magmas of the Devine Canyon Tuff, Eastern Oregon| Constraints for Evolution Models of Voluminous High-silica Rhyolites." Thesis, Portland State University, 2017. http://pqdtopen.proquest.com/#viewpdf?dispub=10606618.
Повний текст джерелаLarge-volume silicic ignimbrites erupt from reservoirs that vary in composition, temperature, volatile content and crystallinity. The 9.7 Ma Devine Canyon Tuff (DCT) of eastern Oregon is a large-volume (>250 km3), compositionally zoned and variably welded ignimbrite. The ignimbrite exhibits heterogeneous trace element compositions, variable volatile content and crystallinity. These observations were utilized in the investigation into the generation, accumulation and evolution of the magmas composing the DCT. Building off previous research, pumices were selected from the range of trace element compositions and analyzed with respect to crystallinity, mineral abundances and assemblages. The DCT displays a gradational trace element enrichment and decrease in crystallinity from least evolved, dacite, at ∼22% crystals to most evolved high-silica rhyolite at 3% crystals. Two distinct mineral populations of feldspar and clinopyroxene were identified in previous work, one belonging to the rhyolitic magma and the other to the dacitic magma. Volatile content derived from melt inclusion Fourier Transform Infrared (FTIR) spectrometer analysis revealed an increase in water content from 1.2 to 3.7 wt.% in the most evolved rhyolite. The DCT exhibits low and variable δ18 O signatures, 4.52‰ to 5.76‰, based on δ 18O values measured on quartz and sanidine. Low δ18O signatures of all DCT rhyolites suggest the incorporation of hydrothermally altered crust into the melt. Furthermore, quartz phenocrysts from all high-silica rhyolite groups display dark oscillatory zoned cores and Ti-rich bright rims.
These data provide insight into how these magmas were generated and subsequently stored in the crust. Commonalities of petrographic and compositional features among rhyolites, especially the zoning characteristics of quartz phenocrysts, exclude the possibility of storage and evolution in multiple reservoirs. Envisioning a scenario where all magmas are stored within a single reservoir prior to eruption and assuming rhyolites A and D are the product of partial melting. The mixing of A and D rhyolites produced rhyolite B, and subsequent mixing of intermediate rhyolite B and end-member rhyolite D generated rhyolite C. However, some trace element inconsistencies, between mixing model and observed intermediate rhyolites suggest a secondary process. Post mixing, rhyolites B and C require some modification by fractional crystallization to account for LREE and other inconsistencies between mixed models and observed rhyolites. Finally, the origin of the dacite is likely through mixing of group D rhyolite and an intrusive fractionated basalt, which could have led to the eruption of the Devine Canyon Tuff.
Grand'homme, Alexis. "Etude de la monazite comme chronomètre et traceur géochimique des minéralisations hydrothermales : Approche expérimentale et analyses de monazites de veines alpines." Thesis, Université Grenoble Alpes (ComUE), 2016. http://www.theses.fr/2016GREAU004/document.
Повний текст джерелаMonazite is commonly found in most of geological environments. Monazite can be rich in uranium and thorium, does not incorporate lead, and its isotopic (U-Th-Pb) system is very robust to diffusion in most of crustal conditions, which makes it a very attractive chronometer. In addition, it represents the main source of thorium and a major source of rare earth elements (REE), in the crust. During fluid-monazite interaction, monazite can recrystallize by a coupled dissolution-precipitation process, with a chemical/isotopic composition different from the initial monazite. These recrystallizations involve a redistribution of the elements contained in monazite (REE, Th, U, Pb) and understanding of the mobility of these strategic elements is crucial for their economic (lanthanides resources and actinides) and environmental (storage of radioactive waste) aspects.The aim of this thesis is to investigate the behaviour of monazite during fluid-monazite interactions and its potential as chronometer and geochemical tracer of fluid mineralization, via a multi-disciplinary approach including mineralogy, experimental petrology, geochronology and tectonic. The work presented here is organized in two parts: one on Alpine hydrothermal monazite dating and the other on the results of hydrothermal alteration experiments in laboratory.About forty monazite and ten xenotime crystals were collected in Alpine clefts (hydrothermal veins formed during exhumation) of the external (Argentera, Belledonne, Mont-Blanc) and the internal (Briançonnais Zone) domains. The LA-ICP-MS in-situ U-Th-Pb dating allowed to better constrain the age and duration of hydrothermal circulation during the late deformation stages related to the exhumation of the western Alps. The fluid inclusion analysis of monazite crystals coupled with zircon fission-track dating have brought new constrains on the geothermal gradient induced by fluid circulations in the hydrothermal veins. Systematic analysis of experimental products (monazite and fluid) of 18 experiments confirmed the mobility of elements such as uranium or heavy REE during hydrothermal reactions. The nanoscale study of monazite recrystallized domains showed a new replacement mechanism characterized by the propagation of the reaction front through nano-pores and nano-fractures. This mechanism leads to anisotropic replacement and a mixture of nano-domains of primary and recrystallized monazite. These observations have major implications for the storage of radioactive waste or in geochronology to explain the disturbances of monazite ages that have reacted with fluid in hydrothermal or metamorphic environments
Fragomeni, Paulo Roberto Pizarro. "Levantamento e estudo das ocorrências de grafita do Distrito Grafitífero Aracoiába-Baturité, CE." Universidade do Estado do Rio de Janeiro, 2011. http://www.bdtd.uerj.br/tde_busca/arquivo.php?codArquivo=8824.
Повний текст джерелаThe Aracoiába-Baturité Graphite-bearing District has graphitic gneiss deposits (disseminated ore) and vein (solid ore) with different genetic origins and their own physical characteristics and geological environments. The graphite gneiss ore is of sedimentary, syngenetic origin, with 1.5% to 8% C content, which is distributed along two long parallel belts, hosted in the Baturité Sub-unit, which consists of a major regional metallotect. The association of metamorphic graphite disseminated in metasediments of the Acarápe Sequence consists of a geoindicator of an old Neo-Proterozoic sedimentary basin and also can be considered a geosuture zone, the result of the subsequent closing of a primitive ocean. The rocks of this subunit correspond in the paleogeography of the Acarápe Sequence to the facies of the bottom of a slope and of an abyssal plain. The vein ore (deposited fluid) is epigenetic and, with C contents of between 20% and 70%, forms tabular bodies and pockets, controlled on a local scale by relief structures (faults, fractures, contact zones, fold axes, etc.), which allowed seepage of pneumatolithic solutions relating to the plutonic body of Pedra Aguda. The variations in the values of the ratios between stable carbon isotopes (δ13C) in the graphite of the disseminated ore are -26.72 to -23.52 and of the solid ore -27.03 to -20.83, showing a sign of biological activities (biosignatures), and it can be said that the graphite of the above samples is derived from organic matter. The main prospecting guides for graphite were presented and the following geophysical methods tested: Electro-resistivity (ER); Ground Penetrating Radar (GPR); Magnetometry; Very Low Frequency (VLF); and Spectral Induced Polarization (SIP) / Electro-resistivity (ER). It was found that the combination of the Spectral Induced Polarization (SIP) and Electro-resistivity (ER) methods proved the most efficient. In relation to determining the carbon content using thermogravimetry (TG), which is the most commonly used method for this element, it was found that the bands of burning attributed to the carbon in the ore in the Aracoiába-Baturité District (340 to 570C and from 570oC to 1050C) were different from the bands of the ore in Minas Gerais (350C to 650C and 650C to 1050C). This finding suggests the need to determine beforehand the temperature ranges for each region studied.
Yang, Xin-She. "Mathematical modelling of compaction and diagenesis in sedimentary basins." Thesis, University of Oxford, 1997. http://ora.ox.ac.uk/objects/uuid:0bdc6c43-4534-4f08-97e2-8a33d6b13e61.
Повний текст джерелаStandley, Carl Eldon. "Banda Forearc Metamorphic Rocks Accreted to the Australian Continental Margin: Detailed Analysis of the Lolotoi Complex of East Timor." BYU ScholarsArchive, 2007. https://scholarsarchive.byu.edu/etd/1304.
Повний текст джерелаBouenitela, Vicky Tendresse Télange. "Le domaine paléoprotérozoïque (éburnéen) de la chaîne du Mayombe (Congo-Brazzaville) : origine et évolution tectono-métamorphique." Thesis, Rennes 1, 2019. http://www.theses.fr/2019REN1B008/document.
Повний текст джерелаThe Mayombe belt is the congolese part of the Araçuaï-West Congo belt system which extend from eastern margin of Brazil to western margin of central Africa. It runs parallel to the Atlantic coastline with NW-SE trend. Considering geochronological data, it is subdivided into two lithostratigraphic domains : (i) the Paleoproterozoic domain and (ii) the Neoproterozoic domain. The Paleoproterozoic domain of the Mayombe range corresponds to the inner part of the belt and is characterized by the coexistence of para and orthoderived rocks deformed and metamorphosed to varying degrees. These rocks are distributed among the three main lithological Groups : (i) the Loémé Group, (ii) the Loukoula Group and (iii) the Bikossi Group. Structural analysis of Loémé and Loukoula Groups shows folded and fractured stuctures. In the Loémé Group, folds trend NE-SW, NNE-SSW and N-S while in the Loukoula Group, the main shortening trends NE-SW. The Bikossi Group is characterized by folds oriented in the directions identified in the preceding Groups. The geochemical study carried out on samples from the Paleoproterozoic domain of the Mayombe belt shows that the latter is heterogeneous, by involving rocks of various origin and lithology. The petrological characterization of Loémé and Loukoula Groups shows that they are affected by at least two distinct metamorphic events that overlap. The first event is characterized by garnet-biotite-oligoclase parageneses in metapelites and by the development of brown hornblende in metabasites, thus allowing the evolution context to be situated in the amphibolite facies. The second event is recorded differently in Loémé Group and Loukoula Group. It consits respectively in garnet-biotite-oligoclase assemblages in the Loemé Group and in chlorite-albite-epidote paragenesis in the Loukoula Group. Samples from Bikossi Group present only traces of a single metamorphic event marked by garnet-biotite-muscovite and garnet-chloritoid-chlorite parageneses whose temperature is estimated at 510-568°C for 8 kbar of pressure. U-Pb dating of zircons allows to : (i) define the Archean-Paleoproterozoic (3300-1500Ma) sources of metasedimentary rocks (ii) confirm Paleoproterozoic (2070-2040 Ma) age of Eburnean magmatism and Neoproterozoic (925 Ma) Mfoubou and Mont Kanda type magmatism and (iii) to highlight the perturbations of zircons U-Pb isotopic system at 642 ± 36 Ma and 539 ± 18 Ma. The 40Ar-39Ar analyzes on biotite, muscovite and amphibole from samples of the western domain of Mayombe betl provided since the age range of Pan-African tectono-thermal event at 615-496 Ma
Boulanger, Marine. "Le devenir des liquides au sein de la croûte océanique des dorsales à expansion lente : nouveaux apports de l'étude d'Atlantis Bank (dorsale Sud-Ouest Indienne)." Electronic Thesis or Diss., Université de Lorraine, 2020. http://www.theses.fr/2020LORR0030.
Повний текст джерелаMagmatic processes that govern crustal accretion at mid-ocean ridges still need to be better constrained. Among the processes potentially involved in the evolution of the lower crust magma reservoirs, reactions associated with reactive porous flow through crystal mushes tend to be considered as one of the predominant processes together with simple crystallization of magmas. The share of these processes during magma differentiation is dependent on the modes of melt migration and is thus correlated to the geometry of the reservoirs considered. By combining high-resolution structural, petrographic and geochemical studies of in situ sections drilled in an oceanic core complex of the Southwest Indian Ridge, I was able to bring new constraints on the formation and evolution of magmatic reservoirs involved in crustal accretion. All or part of the igneous reservoir model developed herein can be applied to other sections of lower oceanic crust. This model, together with additional constraints obtained by the coupled experimental petrology study of crystallization processes, paves the way for new quantifications of the involvement of melt-rock reactions in the differentiation of gabbroic lithologies, and more generally in the evolution of melts within the oceanic crust. Those developments are consistent with the constant evolution in recent decades of the understanding of crustal magmatic systems, which shifted from melt-filled magma chambers to igneous reservoir models mostly composed of crystal mushes
Coetzee, Grace. "Petrology and geochemistry of the Tjakastad (Barberton) ICDP cores." Thesis, 2014. http://hdl.handle.net/10539/14936.
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