Дисертації з теми "Igneous intrusives"
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Pattison, Christopher Ian. "Igneous intrusions in the Bowen Basin." Thesis, Queensland University of Technology, 1990. https://eprints.qut.edu.au/35967/1/35967_Pattison_1990.pdf.
Повний текст джерелаNewman, Rowena Jane. "Igneous and hydrothermal minerals and textures in the offshore Canterbury Basin." Thesis, University of Canterbury. Geological Sciences, 2015. http://hdl.handle.net/10092/10856.
Повний текст джерелаBurns, Claire Elizabeth Graham. "Intrusive igneous control on groundwater in the Triassic sandstones of Northern Ireland." Thesis, Queen's University Belfast, 2014. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.669657.
Повний текст джерелаWigley, Rochelle Anne. "The geochemistry of the Karoo igneous volcanic and intrusive rocks of Botswana." Master's thesis, University of Cape Town, 1995. http://hdl.handle.net/11427/21335.
Повний текст джерелаThe Mesozoic basalts and dolerites of Botswana underlie an estimated area of 150 000km2 and form part of the Karoo Igneous Province of southern Africa. The distribution of Karoo basalts in Botswana is limited essentially to three main sub-basins, the Central Kalahari Subbasin, northern Botswana and the Tuli Syncline and a major dyke swarm, with a WNW strike, extends across Botswana from the Namibian to Zimbabwean borders. This dissertation is a reconnaissance study which concentrates on the recognition and definition of distinct geocheinical sub-groups within the Karoo volcanic and intrusive rocks of · Botswana. 128 new whole rock samples were analyzed for major and trace element concentrations, in addition to the 70 whole rock analyses from Botswana which were available in the UCT database.· Mineral analyses and rare earth element compositions for selected samples are also presented. The basalts and dolerites of Botswana are assigned to one of the three geochemical lineages, i.e. the low-K20, the high-K20 and the felsite lineages on the basis of Si02, MgO and K20 concentrations. A number of distinct geochemical sub-groups· are recognised within these lineages according to whole rock compositions, normative mineralogy, petrography and outcrop character. The low-K20 lineage is subdivided into two main sub-groups on the basis of the Ti02 and Zr concentrations, i.e. the LTZ- and HTZ-type basalt and dolerite sub-groups. The LTZtype basalt sub-group (with ~2% Ti02 and ~250ppm Zr) represents the bulk of the Botswana dataset where the LTZ basalts of Botswana are shown to be lateral equivalents to the Lesotho Formation basalts of the Central Karoo area, considerably expanding the known outcrop area of this basalt type. Two dolerites are the only samples of intrusive equivalents of this voluminous LTZ basalt type in Botswana.,
Al-Jawadi, A. F. "Minor igneous intrusions of the Lake District : geochronology, geochemistry and petrology." Thesis, University of Newcastle Upon Tyne, 1987. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.376308.
Повний текст джерелаBuick, Ian S. "The petrology and geochemistry of granitic rocks from the Entia domal structure, Harts Range, eastern Arunta Block, Central Australia /." Title page, contents and abstract only, 1985. http://web4.library.adelaide.edu.au/theses/09SM/09smb932.pdf.
Повний текст джерелаChristodoulou, C. "Petrology of the plutonic rocks of the Macquarie Island Complex /." Title page, contents and abstract only, 1990. http://web4.library.adelaide.edu.au/theses/09PH/09phc556.pdf.
Повний текст джерелаMiggins, Daniel Paul. "Temporal and geochemical insights related to volcanic and plutonic activity within Big Bend National Park, Texas." To access this resource online via ProQuest Dissertations and Theses @ UTEP, 2009. http://0-proquest.umi.com.lib.utep.edu/login?COPT=REJTPTU0YmImSU5UPTAmVkVSPTI=&clientId=2515.
Повний текст джерелаWilson, Kelly. "RARE EARTH ELEMENTS AT HICKS DOME, SOUTHERN ILLINOIS, THEIR MODE OF MINERALIZATION AND RELATIONSHIP WITH IGNEOUS INTRUSIONS." OpenSIUC, 2019. https://opensiuc.lib.siu.edu/theses/2581.
Повний текст джерелаHulley, Vierah. "Reactions between country rock xenoliths and the magma of Uitkomst Complex, with implications for the origin of the sulphide mineralisation." Pretoria : [s.n.], 2005. http://upetd.up.ac.za/thesis/available/etd-05282008-101011.
Повний текст джерелаCooper, Jennifer Rebecca. "Igneous intrusions and thermal evolution in the Raton Basin, CO-NM contact metamorphism and coal-bed methane generation /." Diss., Columbia, Mo. : University of Missouri-Columbia, 2006. http://hdl.handle.net/10355/4606.
Повний текст джерелаThe entire dissertation/thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file (which also appears in the research.pdf); a non-technical general description, or public abstract, appears in the public.pdf file. Title from title screen of research.pdf file viewed on (February 6, 2007) Includes bibliographical references.
Moorehead, Anthony J. "IGNEOUS INTRUSIONS AT HICKS DOME, SOUTHERN ILLINOIS, AND THEIR RELATIONSHIP TO FLUORINE-BASE METAL-RARE EARTH ELEMENT MINERALIZATION." OpenSIUC, 2013. https://opensiuc.lib.siu.edu/theses/1240.
Повний текст джерелаCamp, Kristen F. "Mineralogy and Geochemistry of Anorogenic Granitic Miarolitic Pegmatites Associated with the White Mountain Intrusive Suite, New Hampshire." ScholarWorks@UNO, 2011. http://scholarworks.uno.edu/td/1363.
Повний текст джерелаLiu, Pingping, and 刘平平. "Petrogenesis of the Baima Fe-Ti-(V) oxide-bearing layered intrusion in the Emeishan large igneous province, SW China." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2014. http://hdl.handle.net/10722/207172.
Повний текст джерелаZoller, Kevin M. "Porphyritic Intrusions of the Helen Zone in the Cove Deposit, Lander County, Nevada." University of Akron / OhioLINK, 2014. http://rave.ohiolink.edu/etdc/view?acc_num=akron1398079611.
Повний текст джерелаBrown, Connie Lynn. "The construction of a plutonic complex in a continental arc setting the Skookum Butte stock, western Montana /." CONNECT TO THIS TITLE ONLINE, 2008. http://etd.lib.umt.edu/theses/available/etd-05302008-145300/.
Повний текст джерелаCavalheiro, Mara Lia Dias. "Levantamento gravimétrico na Jazida Carbonífera Morungava-Chico Lomã, RS." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2016. http://hdl.handle.net/10183/150209.
Повний текст джерелаThe present dissertation was developed according to standard 103 of the Graduate Program in Geosciences of the Federal University of Rio Grande do Sul, which provides for the submission of the dissertation in the form of article, predates by state of the art proposed theme. In the southeastern region of the Paraná Basin are located economically important coal deposits in the states of Parana, Santa Catarina and Rio Grande do Sul. These deposits are often much altered by volcanic intrusions. The objective of this study is to map the igneous intrusions affecting the thermal change of level of coal (rank) of the coal deposit Morungava-Chico Lomã in RS. The coal deposit Morungava-Chico Lomã was discovered in the last century and has never been mining. It is characterized by organic rocks of the Permian, coal and bituminous shale, in the southern portion of the Paraná Basin. The gravimetric acquisition was carried in área of the deposit Morungava and in the area of the deposit Chico-Lomã. For both areas the choice of acquisition locations was based on previously conducted drilling holes. With data from the holes drilling were prepared these thematic maps: depth of the first occurrence of coal; cumulative thickness of coal; depth of the first occurrence of diabase; cumulative thickness of diabase; cumulative thickness of diabase in Irati Formation and cumulative thickness of the diabase in Rio Bonito Formation. In the elaboration of article submitted the overriding of the isolines of cumulative thickness of coal and diabase in the filtered Bouguer anomaly maps was performed. These overrides presented correlations and assisted in the interpretation of gravity data. The predominant preferential orientation of the anomalies was NE-SW and a subsidiary orientation NW-SE direction, suggesting a structural control on the occurrence of dikes and/or sills, on gravimetric high. In Chico Lomã the occurrence of an extensive positive Bouguer anomaly forming a trend of NE-SW orientation was correlated with geological units of Rio Grande do Sul Coastal Plain: gravimetric characterized the high Barrier I and low gravimetric, Systems Lagunar I and II. The gravimetric method proved efficient for the characterization of the deposit through the correlation of positive gravity anomalies with occurrences of diabase.
Wilson, Penelope Irene Rose. "Direct linking of host rock deformation structures to the emplacement, morphology and accommodation of high-level igneous intrusions : the Henry Mountains, Utah." Thesis, Kingston University, 2015. http://eprints.kingston.ac.uk/34543/.
Повний текст джерелаGallagher, Brookie Jean. "A Comparative Study of the Badger Pass Igneous Intrusion and the Foreland Volcanic Rocks of the McDowell Springs Area, Beaverhead County, Montana: Implications for the Local Late Cretaceous Sequence of Events." Digital Archive @ GSU, 2008. http://digitalarchive.gsu.edu/geosciences_theses/11.
Повний текст джерелаHansen, Jógvan. "Petrogenetic evolution, geometries and intrusive styles of the early Cenozoic saucer-shaped sills of the Faroe Islands." Thesis, Durham University, 2011. http://etheses.dur.ac.uk/3631/.
Повний текст джерелаSuarez, Tatiana Arenas. "Resfriamento de corpos intrusivos no interior da crosta continental: o efeito da liberação do calor latente." Universidade de São Paulo, 2017. http://www.teses.usp.br/teses/disponiveis/14/14132/tde-02072018-164306/.
Повний текст джерелаThe purpose of this work is to study the thermal evolution of intrusive bodies formed by successive sills injection in different levels of the crust, taking into account the phase change and latent heat release in a finite temperatures interval. Our numerical models involve heat transfer only by conduction. Thermal evolution of the system is found with the energy balance equation of enthalpy that includes phase and composition change of magmas. The thermal evolution of the basaltic igneus body intruded into the lower crust is evaluated using finite difference scheme. At this level of the crust we develop two different ways of igneus body construction: over- accretion and under-accretion. Over-accretion is the more efficient way for keeping high temperatures in the time. In the upper crust, the thermal evolution of a tonalite igneus body formed by successive sils injection is computed with finite elements method in a geometry with rotational symmetry about z axis. Thermal and geological development of this igneus bodys strongly depends on magma emplacement rate and magma and crust thermal proprerties. These features defines if the igneus body develops in a magmatic chamber, a melt reservior or a high crystalline body. In the second part of this work we examine heat transfere from magamatic chambers of different geometries into the country rock, solving the entalphy equation with latent heat release effects with finite element method. The magmatic chambers geometries constructed are oblate spheroid, prolate spheroid and spherical. The viscosity of the rock is also obteined from temperature field.
Schucker, Dennis Eugene. "Mesozoic igneous intrusions in New England and Quèbec : implications from lead (Pb) isotopes on petrogenesis and mantle sources (Ascutney Mountain, VT; Mont Saint Hilaire, Quèbec; Pliny Complex, NH) /." The Ohio State University, 1992. http://rave.ohiolink.edu/etdc/view?acc_num=osu1487779120909591.
Повний текст джерелаOliveira, Eduardo Barreto. "Geração não convencional de hidocarbonetos na região carbonífera de Santa Catarina." Universidade do Estado do Rio de Janeiro, 2009. http://www.bdtd.uerj.br/tde_busca/arquivo.php?codArquivo=1105.
Повний текст джерелаNa região de Lauro Müller, sul de Santa Catarina, a presença de óleo nos arenitos das formações Rio Bonito e Palermo foi observada em diversos poços e nas galerias de uma das minas da Carbonífera Catarinense. Amostras desse óleo foram submetidas às análises de isótopos estáveis de carbono e cromatografia gasosa espectrometria de massas visando, a princípio, identificar a sua origem. O óleo apresentou feições moleculares típicas de ambiente anóxico hipersalino, sendo correlacionado ao Membro Assistência da Formação Irati. Parâmetros moleculares revelaram que o mesmo foi gerado durante o pico de geração de hidrocarbonetos e encontra-se leve a moderadamente biodegradado. A comparação entre o óleo catarinense e os arenitos asfálticos de Anhembi (SP) revelou diferenças moleculares relacionadas à fácies orgânica, grau de evolução térmica e biodegradação. A geração do óleo no sul catarinense está intimamente relacionada ao efeito térmico das intrusões ígneas cretácicas sobre os intervalos geradores da Formação Irati, haja vista que a unidade encontra-se termicamente imatura na maior parte da bacia. O óleo teria migrado lateralmente da Formação Irati para os arenitos reservatório da Formação Rio Bonito através de falhas com rejeitos verticais superiores a 150 m, as quais foram identificadas em mapas e seções geológicas. Também foram realizadas análises de pirólise, isótopos de carbono e de biomarcadores em amostras da Formação Irati no poço CAT 204, realizado pela Carbonífera Catarinense, a fim de avaliar o efeito térmico de duas soleiras de diabásio intrudidas no Membro Assistência. Foi observado um aumento dos valores de δ13C em direção ao contato com as intrusivas e a completa senilização da unidade. O halo termal abaixo da soleira inferior se estendeu, pelo menos, até a base da Formação Irati, situada a uma distância de 1,4 vezes a espessura do corpo intrusivo. Amostras da parte inferior da Formação Palermo, coletadas no poço CAT 204, e das três principais camadas de carvão do sul catarinense, coletadas nas minas da Carbonífera Catarinense, também se encontram termicamente maturas, sugerindo a proximidade de outros corpos intrusivos. Dessa forma, conclui-se que deve ter havido um aquecimento generalizado dos sedimentos no sul de Santa Catarina causado pela grande incidência de soleiras na região.
In the region of Lauro Müller, south of Santa Catarina, the presence of oil in sandstones of Rio Bonito and Palermo formations were observed in several wells and in the galleries of a coal mine. Samples of oil were subjected to stable carbon isotopes and gas chromatography mass spectrometry analysis to identify its origin. The oil had typical features of a hypersaline anoxic environment, achieving a positive correlation with Assistência Member of Irati Formation. Molecular parameters revealed that it was generated during the peak of hydrocarbon generation and is light to moderately biodegraded. The comparison between oil encountered in Lauro Müller and the tar sands of Anhembi (SP) revealed molecular differences related to organic facies, level of biodegradation and thermal maturity. The generation of oil in southern Santa Catarina is closely related to the thermal effect of igneous intrusions in the source rocks of Irati formation, given that the unit is thermally immature in most of the basin. The oil would have migrated laterally from Irati Formation to the reservoir sandstones of Rio Bonito Formation through faults with vertical slips over 150 m, identified on maps and geological sections. Pyrolysis, stable carbons isotopes and biomarkers analysis was also performed in a local section of Irati Formation to evaluate the heating effect of two dolerite sills intruded into Assistência Member. It was observed an increase in δ13C toward the intrusive contacts and that Assistência Member was completely overmature. The thermal halo below the lower sill reached, at least, the bottom of the Irati Formation, located at a distance of 1.4 times the thickness of the intrusive body. Samples from the lower portion of Palermo Formation, collected in the well CAT 204, and the three main coal layers from southern Santa Catarina, collected in Carbonífera Catarinenses mines, are also thermally mature, suggesting the proximity of other intrusive bodies. Thus, it is concluded that there was a general heating of the sediments of southern Santa Catarina caused by the high incidence of igneous intrusions in the region.
Howarth, Geoffrey Hamilton. "Petrogenesis and metallogenesis of the Panzhihua Fe-Ti oxide ore-bearing mafic layered intrusion, SW China." Thesis, Rhodes University, 2013. http://hdl.handle.net/10962/d1001810.
Повний текст джерелаCorrêa, Luís Maurício Salgado Alves. "Avaliação do efeito térmico das soleiras de diabásio nas rochas geradoras da formação Irati (Bacia do Paraná, Brasil) através de técnicas de modelagem numérica." Universidade do Estado do Rio de Janeiro, 2006. http://www.bdtd.uerj.br/tde_busca/arquivo.php?codArquivo=322.
Повний текст джерелаNa avaliação da maturidade de horizontes geradores e da história térmica de uma bacia com registro de atividade magmática é preciso considerar o efeito térmico imposto pela intrusão de corpos ígneos, como diques e soleiras. Dessa maneira, foi realizada a análise numérica transiente, pelo método de diferenças finitas, do fluxo térmico por condução provocado pela intrusão das soleiras básicas cretáceas nos horizontes geradores do Membro Assistência, Formação Irati, Bacia do Paraná. Esta análise, por sua vez, viabilizou a modelagem do parâmetro de reflectância da vitrinita nos estratos de folhelhos adjacentes às soleiras. Para tanto, foram utilizados os dados de seção de três poços, os quais registram espessuras de soleiras de até 4 m, e um poço com uma soleira de 27 m de espessura. Os poços localizam-se na porção sudeste da bacia. Na simulação numérica, foi considerado o processo de solidificação do magma ou de cristalização das suas fases minerais. A modelagem de reflectância da vitrinita baseou-se em um modelo pré-concebido da história térmica da Formação Irati, sendo os resultados desta simulação de maturidade do querogênio obtidos através do uso do programa EASY%Ro. Considerando-se os erros embutidos no modelo numérico e na discretização da história térmica dos estratos estudados, foram obtidos valores modelados de reflectância da vitrinita similares aos valores medidos nos poços pelo método tradicional. Somente no caso da seção com a soleira de 27 m de espessura houve uma grande diferença entre estes valores. Contudo, o alto coeficiente de correlação (0,95) entre estes possibilita a correção do efeito da espessura da soleira em análises futuras. Assim, a análise numérica simulou o halo térmico da soleira, caracterizado, segundo os dados de modelagem de refletância da vitrinita, por uma faixa acima e abaixo da soleira com espessura equivalente à espessura da soleira encaixada nos estratos geradores da Formação Irati. Essa metodologia de avaliação propicia um estudo preditivo das condições de maturidade de horizontes geradores em bacias ou áreas com magmatismo intrusivo, nas quais as análises do parâmetro de reflectância da vitrinita sejam ausentes ou escassas.
To evaluate the thermal maturity and thermal history of source rocks in basins with magmatic activity it is important to consider the thermal effects imposed by igneous intrusions, such as sills and dykes. This work uses the finite difference method for such evaluation, with the transient numerical analysis of heat conduction from Cretaceous diabase sills intruded into the source rocks of the Assistência Member, Irati Formation, Paraná Basin. This analysis has permitted modeling vitrinite reflectance of the shale strata adjacent to the sills. The data of four wells are used from the southeastern portion of the basin, with diabase thicknesses, respectively, of 1m, 2 m, 4 m and 27 m. The numerical simulation includes the process of magma solidification or mineral phase crystallization. The vitrinite reflectance modeling followed a pre-established thermal history of the Irati Formation, using the EASY%Ro program to simulate kerogen maturity levels. Considering the errors built into the numerical model and the thermal history discretisation of studied strata, the acquired values of modeled vitrinite reflectance closely resembled well data analyzed by the traditional method. Major discrepancies were observed in the case of the well containing a sill 27 m thick, but even in this case the high correlation coefficient (0,95) between the measured and calculated values is expected to permit correction of the sill thickness effect in future studies. The numerical analysis correctly simulated the thermal halo induced by sill emplacement, enabling vitrinite reflectance modeling to characterize it as a zone extending both above and below the sill with thicknesses similar to that of the sills. This evaluation methodology contributes to a predictive study of the maturity conditions of source rocks within basins or areas with intrusive magmatism where analysis of the vitrinite reflectance parameter are sporadic or absent.
Bouabsa, Lakhdar. "Intrusions granitiques à albite et topaze : Minéralisations stanno-wolframifères et altérations hydrothermales associées, l'exemple du hoggar central, Algérie." Nancy 1, 1987. http://www.theses.fr/1987NAN10329.
Повний текст джерелаLaporte, Didier. "Un exemple d'intrusion syntectonique : l'intrusion d'Ile-Rousse, Corse du nord-ouest : étude pétrographique, minéralogique et géochimique, analyse structurale." Saint-Etienne, 1987. http://www.theses.fr/1987STET4001.
Повний текст джерелаBarra-Pantoja, Luis Fernando. "A Re-Os Study of Sulfides from the Bagdad Porphyry Cu-Mo Deposit, Northern Arizona, USA." Thesis, The University of Arizona, 2001. http://hdl.handle.net/10150/249252.
Повний текст джерелаCostarella, René. "Le complexe annulaire alcalin de Combeynot ( Massifs cristallins externes, Alpes françaises), témoin d'un magmatisme en régime distensif. Pétrogéochimie et signification géodynamique." Phd thesis, Grenoble 1, 1987. http://tel.archives-ouvertes.fr/tel-00539879.
Повний текст джерелаFumerton, Stewart Lloyd. "The felsic intrusives In E.R.P.M., Boksburg." Thesis, 2015. http://hdl.handle.net/10539/17282.
Повний текст джерелаScogings, Andrew John. "Alkaline intrusives from the Tugela terrane, Natal metamorphic province." Thesis, 1991. http://hdl.handle.net/10413/11162.
Повний текст джерелаThesis (Ph.D.)-University of Durban-Westville, 1991.
Kimpton, B. J. "The geological relationship between Kanmantoo Cu-Au deposit mineralisation, hydrothermal metasomatism and igneous intrusives." Thesis, 2018. http://hdl.handle.net/2440/130628.
Повний текст джерелаThe Kanmantoo Cu-Au deposit has been in episodic operation since 1846, one decade after the capital city of Adelaide was established some 40 kilometres to the NW. Regionally and within the host stratigraphy there exists archetypal evidence of the Cambrian Delamerian Orogeny through a complex structural, metamorphic and intrusive history. Consequently, numerous theories exist within the literature regarding a syngenetic or epigenetic style of mineralisation and the debated contribution, if any, of magmatic hydrothermal fluids. This study has documented numerous felsic intrusive vein sets within the Kanmantoo Cu-Au deposit which have been utilised to constrain the role of igneous activity on mineralisation within a wider Delamerian context. Monazite U–Pb ages of felsic veins show that intrusion first occurred at syn-peak metamorphic, syn-orogenic conditions (495.11 ± 2.79 Ma), continuing periodically until post-peak metamorphic, extensional conditions (483.43 ± 2.52 Ma). Intrusions are coeval with mineralisation and are temporally and geochemically analogous to magmatic activity in the adjacent Monarto and Murray Bridge provinces. Analysis of trace elements in monazites identifies the Kanmantoo Cu-Au deposit as a syn- to post-peak metamorphic hydrothermal anomaly which, combined with the presence of felsic veins, indicates that mineralisation resulted partly from fluids generated by a pluton at depth. These findings broadly confirm the prospectivity of Delamerian-affected terranes throughout large parts of South Eastern Australia where pervasive intrusive geology exists.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2018
Maes, Stephanie M. "Magnetic fabric constraints on the emplacement of igneous intrusions." 2006. http://www.library.wisc.edu/databases/connect/dissertations.html.
Повний текст джерелаBrandt, R. T. "The Geology Of Certain Igneous Intrusive Rocks In The Far East Rand, Transvaal, South Africa." Thesis, 2015. http://hdl.handle.net/10539/16428.
Повний текст джерелаMorrison, Robert Sinclair. "Igneous intrusive rocks of the peake and denison ranges within the Adelaide geosyncline / Robert Sinclair Morrison." 1989. http://hdl.handle.net/2440/18901.
Повний текст джерелаTitle page, contents and abstract only. The complete thesis in print form is available from the University Library.
Thesis
Thesis (Ph.D.)--University of Adelaide, Dept. of Geology and Geophysics, 1989
Rahilly, Kristen Elizabeth. "The Forsterite-Anorthite-Albite system at 5 kb pressure." 2010. http://hdl.handle.net/10090/15194.
Повний текст джерелаChristodoulou, C. (Constaninos). "Petrology of the plutonic rocks of the Macquarie Island Complex / C. Christodoulou." 1990. http://hdl.handle.net/2440/19657.
Повний текст джерелаIncludes bibliography (25 leaves)
ca 400 leaves in various foliations : ill. (some col.), maps ; 31 cm.
Title page, contents and abstract only. The complete thesis in print form is available from the University Library.
Thesis (Ph.D.)--University of Adelaide, Dept. of Geology and Geophysics, 1992
Chan, Christine F. "Constructing a sheeted magmatic complex within the lower arc crust : insights from the Tenpeak pluton, North Cascades, Washington." Thesis, 2012. http://hdl.handle.net/1957/36070.
Повний текст джерелаGraduation Date: 2013