Дисертації з теми "Granite generation"
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Richter, Fabiana. "Sedimentation, metamorphism and granite generation in a Back-Arc Region : the crustal processes recorded in the Ediacaran Nova Venécia Complex (Araçuaí Orogen, Southeast Brazil)." reponame:Repositório Institucional da UFOP, 2015. http://www.repositorio.ufop.br/handle/123456789/5427.
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O Complexo migmatítico-graniulítico-granítico Nova Venécia (CNV), localizado no núcleo do Orógeno Araçuaí (OA, 630-480 Ma), sudeste do Brasil, registra processos crustais anatéticos ocorridos no norte da Província Mantiqueira durante a amalgamação Brasiliana-Pan Africana de Gondwana Ocidental. O núcleo do OA compreende abundantes e volumosos granitoides tipo-S e –I (Supersuítes G1 a G5), que são espacialmente e temporalmente associados a eventos metamórficos de alto grau no NVC. Este estudo integra observações de campo, análises de química mineral, petrografia, geocronologia U-Pb LAICP- MS de zircões e monazitas e modelagem termodinâmica, a fim de definir a evolução dos migmatitos-granulitos do CNV, desde sua deposição até o metamorfismo de alto grau, e correlacionar a história metamórfica com os vários episódios de magmatismo granítico (G1-G5). Sete populações compõe a base de dados de zircões detríticos. A gama mais significativa de zircões detríticos concordantes zircão são representados pelas duas populações mais jovens, variando 650-610 Ma. Isso indica que a principal fonte do CNV é provavelmente o Arco Rio Doce, com contribuições menores de fontes contemporâneas ao Arco Rio Negro. Populações mais velhas sugerem proveniência dos primeiros registros do arco Rio Negro e de segmentos do OA relacionados a riftes de idades Criogeniana e Toniana. O período de sedimentação do CNV é limitado entre a idade máxima de sedimentação em ca. 606 Ma e a intrusão dos primeiros granitóides sin-colisionais (ca. 593 Ma), ou seja, durante ca. 13 Ma. Compilação dos dados disponíveis de U-Pb em zircão mostra que a maior parte dos granitoides G1 e G2 se cristalizaram contemporaneamente ao longo de um período de 15 Ma (595-570 Ma, com um pico a 575 Ma), interpretado como o período sin-colisional no OA. O período de pico metamórfico regional no OA é limitado em 575-560 Ma, o que pode ser uma consequência de magma underplating G1 + G2. Petrografia detalhada e análises de química mineral mostram diferentes assembléias de pico metamórfico (regional) que contêm quantidades variáveis de granada, ortopiroxênio e cordierita peritéticos e cordierite retrógrada. Sugerimos que essas diferenças são principalmente devidas a parâmetros de composição dos protólitos, e não devidas a diferentes evoluções de P-T entre as amostras. A química de rocha total neste estudo sugere que os protólitos do CNV eram grauvacas peraluminosas contendo diferentes quantidades de componentes de matriz (isto é, porções pelíticas) e que as rochas de alto-grau do CNV devem ter perdido melt para terem se tornado caracteristicamente restíticas. Isto é corroborado pelo nosso conjunto de dados de zircões detríticos, que mostram diferentes contribuições percentuais entre as 7 populações que compõem as amostras. Além disso, a modelagem termodinâmica indica que todas as amostras modeladas registram um caminho P-T semelhante, desde condições PT de metamorfismo regional de pico a 750-850 ° C e 5300-7500 bares (granulito, profundidades de ~ 25 km) a condições de estabilidade das assembléias preservadas a 640- 800 ° C e 4500-6000 bares (transição entre amfibolito superior a granulito, profundidades de ~ 18 km). Infere-se que o metamorfismo regional de alto grau (575-560 Ma) deve ter afetado ambos os metassedimentos e granitos pré-existentes, corroborado pelo fato de que ambos mostram feições anatéticas datadas em ca. 571 Ma. Os produtos da fusão parcial em todo o OA poderia ser, pelo menos, parte dos granitóides contemporâneos àqueles formados durante os períodos G2 (570-540 Ma) e G3 + G4 (540-525 Ma). O evento térmico póscolisional G5 (520-480 Ma), relacionado ao colapso tectônico do OA, é registrado em metagrauvacas (monazita U-Pb) e em granitos (monazita e zircão U-Pb) entre 507 e 495 Ma. Sugerimos que, a essa altura, as metagrauvacas já haviam sido submetidas a alguma descompressão e arrefecimento, com base em modelagem metamórfica, observações de campo e datação de um dique tardio não deformado que intrude rochas do CNV (518 Ma). Infere-se que o evento termal pós-colisional G5, registrado por abundantes intrusões de granitoides tipo-I em todo o OA, causou um segundo período de metamorfismo de alto-grau a ca. 500 Ma. A principal característica deste evento em rochas metassedimentares é, além das idades U-Pb em monazitas, um overprint parcial de Baixa Pressão-Alta Temperatura em assembléias regionais de pico, gerando cordierita texturalmente tardia e espinélio hercinítico. Em nossas amostras, este registro metamórfico limita-se a auréolas de contato. _____________________________________________________________________________________________________________
ABSTRACT: The Nova Venécia migmatite-granulite-granite Complex (NVC) in the core of the Araçuaí Orogen (AO, 630-480 Ma), southeast Brazil, records anatectic crustal processes occurring in the northern Mantiqueira Province during the Brasiliano-Pan African amalgamation of West Gondwana. The AO core comprises abundant S- and I-type granitoids (G1 to G5 Supersuites) that are spatially and temporally associated with high-grade metamorphic events in the NVC. This study integrates field-based observations, textural and mineral chemistry analyses, zircon and monazite U-Pb LA-ICP-MS geochronology and thermodynamic modeling in order to constrain the evolution of the NVC migmatites-granulites from deposition to high-grade metamorphism, and to correlate the metamorphic history with the several episodes of granite magmatism (G1-G5). Seven populations compose the NVC zircon detrital dataset. The most significant range of concordant detrital zircon ages are obtained from the two youngest populations, ranging from 650 to 610 Ma. This indicates the main NVC source is probably the Rio Doce Arc, with minor contributions from sources contemporaneous to the Rio Negro Arc. Older populations suggest provenance from the early Rio Negro arc and from Cryogenian and Tonian rift-related segments of the AO. The period of NVC protolith sedimentation is bracketed between its maximum sedimentation age at ca. 606 Ma and the intrusion of early syn-collisional granitoids (ca. 593 Ma), i.e. ca. 13 My. Compilation of the available U-Pb data shows that the bulk of the G1 and G2 rocks crystalized contemporaneously over a period of 15 Ma (595-570 Ma, with a peak at 575 Ma), interpreted to represent the AO syn-collisional period. The period of peak regional metamorphism in the AO is constrained at 575-560 Ma, which may be a consequence of G1 + G2 magma underplating. Detailed petrography and extensive mineral chemistry analyses show different (regional) peak metamorphic assemblages containing variable amounts of peritectic garnet, orthopyroxene and cordierite, and retrograde cordierite. We suggest these differences are mainly due to protoliths compositional parameters, and not due to different P-T evolution among samples. Our whole-chemistry suggests that NVC protoliths were peraluminous greywackes probably containing different amounts of matrix components (i.e. pelitic portions) and that NVC high-grade metagreywackes must have lost melt to become restitic in character. This is corroborated by our detrital zircon dataset showing different percentage contributions from 7 populations among samples. Moreover, thermodynamic modeling indicates that all modeled samples record a similar P-T path, recording P-T conditions of peak regional metamorphism of 750-850 °C and 5300-7500 bars (granulite, depths of ~25 km) and stability of preserved assemblages of 640-800 °C and 4500-6000 bars (transition between upper amphibolite to granulite, depths of ~18 km). The high-grade regional metamorphism (575-560 Ma) is inferred to have affected both metasediments and pre-existing granites, as suggested by partial melting in both of sampled rock-types at ca. 571 Ma. The products of partial melting throughtout the AO could be at least part of the granitoids contemporaneous to G2 (570- 540 Ma) and G3 + G4 (540-525 Ma) periods. The post-collisional G5 thermal event (520-480 Ma), related to tectonic collapse of OA, is recorded in metagraywackes (monazite U-Pb) and granites (monazite and zircon U-Pb) between 523 and 495 Ma. We infer that, by this time, the metagreywackes had already undergone some decompression and cooling, based on metamorphic modeling, field observations and dating an undeformed late dyke (518 Ma). The post-collisional G5 thermal event, recorded by abundant granitic intrusions of I-type granitoids throughout the AO, is inferred to have caused a second high-grade metamorphic event at ca. 500 Ma. In addition to monazite U-Pb ages, the main record of this event in metasedimentary rocks is a partial LP-HT overprinting in regional peak assemblages, with generation of texturally late cordierite and hercynitic spinel. In our samples, this metamorphic record is limited to contact aureoles.
Neumann, Narelle L. "Isotopic and geochemical characteristics of the British Empire granite as indicators of magma provenance and processes of melt generation in the Mount Painter Inlier, South Australia /." Title page, contents and abstract only, 1996. http://web4.library.adelaide.edu.au/theses/09S.B/09s.bn492.pdf.
Повний текст джерелаJackson, Matthew David. "The generation, segregation and mobilisation of granitic melt in the continental crust." Thesis, University of Liverpool, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.364199.
Повний текст джерелаIwasaki, Kenta. "Effects of bedrock groundwater dynamics on hydro-biogeochemical processes in granitic headwater catchments." Kyoto University, 2018. http://hdl.handle.net/2433/232152.
Повний текст джерелаHatami, Maryam [Verfasser], and Thomas [Akademischer Betreuer] Skutella. "Combination of Prox1/NeuroD1 Transcription Factor Overexpression Boosts Generation of Dentate Gyrus Granule Neurons from Pluripotent Stem Cells / Maryam Hatami ; Betreuer: Thomas Skutella." Heidelberg : Universitätsbibliothek Heidelberg, 2018. http://d-nb.info/1177386011/34.
Повний текст джерелаPaolillo, Michael [Verfasser], and Robert [Akademischer Betreuer] Feil. "Identification of a cGMP/Ca2+ crosstalk in cerebellar granule neurons and development of a new method for cell-specific NO generation / Michael Paolillo ; Betreuer: Robert Feil." Tübingen : Universitätsbibliothek Tübingen, 2019. http://d-nb.info/1182985521/34.
Повний текст джерелаGarcía, García Sandra. "Generation, stability and migration of montmorillonite colloids in aqueous systems." Doctoral thesis, KTH, Kemiteknik, 2010. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-11847.
Повний текст джерелаDeptuch, Grzegorz. "New Generation of Monolithic Active Pixel Sensors for Charged Particle Detection." Université Louis Pasteur (Strasbourg) (1971-2008), 2002. http://www.theses.fr/2002STR13115.
Повний текст джерелаSilva, Vera Terezinha Carvalho da. "Jovens rurais que permanecem no campo : a sucessão na agricultura familiar em dois municípios gaúchos." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2015. http://hdl.handle.net/10183/132855.
Повний текст джерелаThe Family agriculture is going through a tense and instable moment due the migration of youth to large urban centers, threatening the continuity of family production units in Rio Grande do Sul. Such migration, rather than an urban general demographic movement of contemporary industrial societies, is a problem that causes not only a demographic emptying of the countryside, but also a decommissioning and abandonment of social facilities remaining in rural areas, such as churches, schools, health centers, community halls, among others. In this scenario, there are currently around 25% of farms in Rio Grande do Sul that won’t have a successor. In order to contribute with the knowledge of the issues regarding the succession in family farming, this Master’s Dissertation investigates what factors influenced the young people that decided by the succession and remained on the family production unit, against the majority who chooses to exit the rural area. The chosen methodological approach was a qualitative research; conducting eleven narrative interviews with rural youth in two counties in Rio Grande do Sul. The young people interviewed were selected according to the following criteria, aged 15 to 29 years; interested in continuing the rural setting; existence of family succession planning; young women presence in at least two families; and that the young people surveyed reflected the characteristics of three forms of succession previously developed. Also was incorporated the perception of two parents that were present during the young people interview. The analysis of empirical data determined the absence of an explicit succession planning in family production units. Among the main factors that awaken the desire of young men to remain in family production units found: the proximity of UPFs with urban centers, which guarantees access to public services and leisure facilities, allowing them to develop activities in one of the two universes and reside in another; some financial autonomy made possible by the fact that all family production units surveyed can alternating the monthly income with the annual income, which contributes to the sustainability of the family group; as well as emotional issues such as the desire to be close to family and community. With regard to young women, we realized that gender relations are still strongly marked by inequality of participation in the activities and decisions in the family productive unit, but this factor seems to be a naturalized matter by family groups.
Rola, Marcelo Coleto. "Previsão da geração de energia elétrica no médio prazo para o Estado do Rio Grande do Sul empregando redes neurais artificiais." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2017. http://hdl.handle.net/10183/157828.
Повний текст джерелаThe demand and, consequently, the generation of electric power are very important issues for social and economic development of countries. Models to forecast these parameters in long and medium terms are used to anticipate possible sceneries and propose strategies for the energy planning of countries. In this context, the present study aims to forecast the generation of electric energy in Rio Grande do Sul State (RS) in a medium-term horizon (one year) using, Artificial Neural Networks (ANNs) of the feedforward type with algorithm of supervised learning backpropagation. For the development of this work, a script was elaborated in order to execute the necessary simulations, which were carried out through Matlab® software. The selected variables of influence as inputs of forecasting model refer to economy (State and National), to the electric energy balance and to the meteorology State, during the period from January, 2009 to March, 2016. In order to train the neural network, this data set was added to the entrance matrix, with monthly frequency, from January, 2009 to March, 2015 and for prediction, data were inserted from April, 2015 to March, 2016. Finally, after RNA complete simulation, the observed result of the electric power generation of the State was compared with the one obtained through the prediction model, indicating a mean absolute percent error (MAPE) of 5.86% and a mean absolute deviation (MAD) of 134.15 average MW. The obtained results in this work are promising, besides; they are similar to those found in literature, in this way demonstrating the reliability and efficacy of the using method.
França, Maria Cristina Caminha de Castilhos. "Memórias familiares em festa : estudo antropológico dos processos de reconstrução das redes de parentesco e trajetórias familiares." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2009. http://hdl.handle.net/10183/15913.
Повний текст джерелаAnthropological study on family memories that are reorganized with Family Parties, seen as contemporary family rituals, being called Party or Gathering of a given family. The ethnographical research was done with families "in and from" different cities in Rio Grande do Sul between 2004 and 2009. A Family Party is understood as a happening that has become frequent in contemporary Brazilian society. The event presents the ambiguous aspect of the individual's search for their ancestors amidst a modern world, in which the valorization of individualization seems to make people less connected to local and fixed forms of solidarity. Seen as a rite - which aims to revive or engender new forms of identity, with new behaviors, with the family rearrangements required by contemporary situations - the Family Parties can be seen as a learning instrument, implying the continuity of the generations, of the age groups or social groups in which they are produced.
Néry, Carlos Henrique Cardona. "A geração de resíduos sólidos no festival gastronômico de Carlos Barbosa : o Festiqueijo." reponame:Repositório Institucional da UCS, 2008. https://repositorio.ucs.br/handle/11338/448.
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An event (gastronomical festival) has the characteristics of a touristic enterprise consuming water, energy and goods, which generate solid residues, gas emissions and residuary water. Thus the identification of the different forms of environmental impacts resulting from that kind of festival is important so that the environmental variable can be best evaluated when planning such events. The present study aims at the evaluation of solid residues generated in a gastronomical festival which has been part of the touristic calendar for over 19 years (FESTIQUEIJO 2007, a gastronomical festival held in the town of Carlos Barbosa, in the Rio Grande do Sul state). The research initial problem came from the question: how does the generation of solid residues occur in a gastronomical festival? To find the answer to that question, the solid residues generated during the festival were characterized, all the sectors generating them during were observed directly, the conditions for handling those residues in the festival environment were identified and visitors were interviewed (825 individuals). The study on the diagnosis of solid residues generation allowed for the determination of the gravimetric composition of the residues in the event, and consequently establish management actions for the next festivals. The largest fractions of components which were present in the composition of solid residues were: glass (81.79%), paper and cardboard (5.49%) putrefiable organic matter (4.60%) and plastic (4.05%). The studies also point to the ethical and legal responsibility of the participants, once they have to find themselves responsible for the generation and the handling of solid residues coming from their stands. The development of this study allows for filling in the existing gaps in tourism, specially regarding the environmental issue while planning for gastronomical events.
Jonqueres, Jean-marie. "Génération de routage contraint en courant pour les applications analogiques forts courants." Thesis, Aix-Marseille, 2012. http://www.theses.fr/2012AIXM4768/document.
Повний текст джерелаIn deep submicron VLSI circuits, excessive current density in interconnects is a major concern for analog high current application. If current over maximum density is not effectively mitigated, this can lead to phenomena like electromigration, voltage drop and electrical overload. It is a hot topic of interest in modern circuits due to the decrease of metal track sizes while high currents are necessary in automotive or mobile applications. This thesis had as goal to develop solutions for the consideration of the constraints in the current phase of routing analog blocks strong currents. After a presentation of the phenomena and the state of the art, an algorithmic approach to current driven net generation is introduced. A method to characterize the current is defined. Then an exhaustive routing algorithm is presented and used to search criteria for a good topology. Next, two algorithms are studied and compared, first a greedy algorithm, used as a reference, and a "Divide & Conquer" original algorithm. It shows results improved on average by about 10% for area and almost 27% for CPU time compared with existing solution. The next section focuses on current crowding correction, with a method based on a set of mathematical models. Finally, a conception flow based on the developed solutions is introduced and validated
Koteas, George Christopher. "Analysis of the gouldsboro pluton and the fehr granite: Understanding the scales of magmatic processes and partial melt generation from the deep to shallow crust." 2010. https://scholarworks.umass.edu/dissertations/AAI3427548.
Повний текст джерелаNeumann, N. L. "Isotopic and geochemical characteristics of the British Empire Granite as indicators of magma provenance and processes of melt generation in the Mount Painter Inlier, South Australia." Thesis, 1996. http://hdl.handle.net/2440/114328.
Повний текст джерелаThe production of granitic magmas at shallow to midcrustal depths by anatexis of crustal material requires a significant thermal perturbation of the normal crustal geothermal regime. Thermal perturbations leading to anatexis may be initiated by crustal thickening associated with deformation, intrusion and/or upwelling of heat sources from lower crust or mantle regions or by anomalous concentrations of heat-producing elements, U, Th and K. This thesis explores the origin of shallow to mid-crustal peraluminous granites within the Mount Painter Inlier, together with their relationship to older granite suites, as indicators of magmatic processes during crustal deformation of the Delamerian Orogeny. The geochemical and isotopic characteristics of granites and gneisses of the Mount Painter Inlier indicate two distinct periods of granitic evolution involving different source regions and magmatic processes. Proterozoic granites and gneisses reflect magmatic sources and processes similar to those involved in the evolution of other Australian anorogenic Proterozoic terrains, although extreme concentrations of U, Th and K suggest an important role for element concentration within accessory minerals during granite genesis. Field relationships, together with geochemical and isotopic characteristics of the Palaeozoic(?) British Empire Granite indicate evolution from a complex mixture of surrounding metasediments and granites in a number of possible scenarios. The additional thermal energy required to produce the British Empire Granite from partial melting of this package at depths of approximately 12 to 15 km is consistent with perturbed thermal regimes resulting from anomalous internal heat production due to the extreme concentration of U, Th and K within the Proterozoic units.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1996
Martin, N. H. "A coupled thermo-mechanical model for deformation in high temperature-low pressure metamorphic terrains: implications for the Palmer region, southern Adelaide Fold Belt." Thesis, 1990. http://hdl.handle.net/2440/119373.
Повний текст джерелаPeak metamorphic growth in high temperature - low pressure terrains is commonly associated with crustal thickening strains reflected in syn-tectonic fabrics. Conductive heat transfer through the lithosphere for geologically plausible thermal and mechanical configurations is unable to produce such temperatures and thus an advective thermal perturbation is required, and is commonly in the form of granitic melts. Thermal weakening of the lithosphere as a consequence of this advective heat allows the potential for crustal thickening strain increments. In this thesis a coupled thermo-mechanical model is presented which allows quantification of this thermal weakening effect. Two granite generation models are investigated; firstly, lower crustal melting due to conductive heating of the lithosphere during orogenesis and secondly, segregation or roof rock melting from mafic sills located at the base of the crust. Results from the model indicate that, for granites produced by melting of the lower crust, crustal thickening strains increments are only in the order of 5 -10 %. However, for granites produced by segregation from a mafic sill crustal strain increments of up to 30% may occur during emplacement. Thus, in order to produce peak metamorphic temperatures associated with significant crustal strain a system analogous to the second model is required. Structural and metamorphic studies of the Palmer region in the southern Adelaide Fold Belt reveal the associated development of partial melting and peak metamorphism with the intrusion of the orthogneissic Rathjen Gneiss during the regional D1 folding event. Thermal weakening triggered by the Rathjen Gneiss has produced a local D2 folding event. Areas at some distance from the Rathjen Gneiss exhibit peak metamorphic growth during D2 consistant with the delayed peak temperatures from the cooling body.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1990
Ackermann, Ines. "Granice języka. Różne samookreślenia „Polaka“ na Białorusi i Litwie." Doctoral thesis, 2014.
Знайти повний текст джерелаThe theses analyses the idiolects of different aged persons who live in the Polish-Belarusian-Lithuanian borderland and who spontaneously characterise themselves as Poles. Basing on their self-description, the aim is to show the numerous individual identifications behind the statement “I am a Pole”. This social-cultural belonging correlate in different ways with the second statement: “I speak Polish”. The 22 interviewees are members of six families and they all live in an area that belonged to Poland in the interwar period. Based on those interviews the interviewees' idiolects, their usage of language and their cultural identification among different generations, but also among regions are presented. From every family the author recorded at least three members presenting different generations. All interviewees declared at the first meeting that they are Poles and they were all able to communicate fluently in Polish. The interviews were all provided by the author according to a semi-standardized guide and evaluated qualitatively with the program MAXQDA11. For the analysis of the interviews the core questions were: To what extend the idiolect of the interviewees differs from standard Polish? What has – according to the interviewees – strong influence on the preservation of the Polish language in Belarus or Lithuania? How do the interviewees judge the vitality of Polish in their region? What is their individual language attitude? How do they describe the imagined picture of Poland as a country and the contacts the interviewees have with the reverence nation?
Bhattacharya, Shrema. "Generation of granitic magmas in the lower crust: a natural example from Mt Daniel, Fiordland, New-Zealand." Thesis, 2010. https://researchonline.jcu.edu.au/19040/1/JCU_19040-bhattacharya-thesis-2010.pdf.
Повний текст джерелаLevine, Jamie Sloan Fentiman 1979. "In situ melt generation in anatectic migmatites and the role of strain in preferentially inducing melting." Thesis, 2011. http://hdl.handle.net/2152/ETD-UT-2011-08-3955.
Повний текст джерелаtext