989 resultados para Tectônica. Arquitetura Moderna. Paraíba
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Pós-graduação em Geociências e Meio Ambiente - IGCE
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Several publications have contributed to improve the stratigraphy of the Paraíba Basin in northeastern Brazil. However, the characterization and distribution of sedimentary units in onshore areas of this basin are still incomplete, despite their significance for reconstructing the tectono-sedimentary evolution of the South American passive margin. This work provides new information to differentiate among lithologically similar strata, otherwise entirely unrelated in time. This approach included morphological, sedimentological and stratigraphic descriptions based on surface and sub-surface data integrated with remote sensing, optically stimulated luminescence dating, U+Th/He dating of weathered goethite, and heavy mineral analysis. Based on this study, it was possible to show that Cretaceous units are constrained to the eastern part of the onshore Paraíba Basin. Except for a few outcrops of carbonatic rocks nearby the modern coastline, deposits of this age are not exposed to the surface in the study area. Instead, the sedimentary cover throughout the basin is constituted by mineralogically and chronologically distinctive deposits, inserted in the Barreiras Formation and mostly in the Post-Barreiras Sediments, of early/middle Miocene and Late Pleistocene-Holocene ages, respectively. The data presented in this work support tectonic deformation as a factor of great relevance to the distribution of the sedimentary units of the Paraíba Basin.
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Entre os mamíferos marinhos, a baleia é um dos animais que mais desperta atenção, especialmente no atinente ao seu sistema urinário. Este sistema segue o padrão entre os mamíferos quanto a sua constituição, entretanto, difere na morfologia renal, em número de lobos, que por sua vez, forma renículos completos, aglutinados às centenas. Esta estrutura é sustentada por tecido conjuntivo fibroso, mas altamente capaz de manter o equilíbrio hidroeletrolítico. Foram dissecados 6 pares de rins de baleia Minke (Balaenoptera acutorostrata), colhidos em 1982, Cabedelo, Estado da Paraíba, Brasil, na última pesca autorizada. Estes rins estavam conservados em formol 10% e apresentaram uma camada histológica de colágeno muito grande circundando a parede medular. O duto coletor urinário forma cálices papilares, desembocando num único centro coletor que desemboca no ureter. Verificou-se que o rim da baleia Minke apresenta característica lobulada possuindo em média 700 renículos, cada renículo possui características anatômicas e funcionais de um rim unipiramidal, com uma camada interna (medula), e uma camada externa (córtex), e irrigação independente, com formação das artérias arqueadas individualmente, como observadas em mamíferos terrestres unipiramidais. Entretanto, o conjunto destes renículos constitui ao final um rim multilobular e polipiramidal, contrariando a morfologia da maioria dos mamíferos terrestres. Não foi possível distinguir ao nível de microscopia de luz as estruturas do córtex renicular da baleia Minke. Na microscopia eletrônica de varredura foi possível visualizar uma camada cortical que fica localizada entre duas cápsulas fibrosas. Esta junção por sua vez é feita por tecido conjuntivo o qual juntamente com uma camada de colágeno e fibras elásticas, separa o córtex da medula , foram visualizados os glomérulos renais, completamente tomados pelos vasos glomerulares e dispostos em várias camadas. Percebe-se que a cavidade glomerular é praticamente um espaço virtual para onde o filtrado glomerular é drenado, não apresentando o formato globular. A vascularização intensifica-se ao chegar à região medular. A diferença entre rins de mamíferos terrestres e marinhos está na disposição dos componentes morfológicos, favorecendo a fisiologia do órgão.
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No presente trabalho apresentamos o resultado das pesquisas geológicas efetuadas na província alcalina do Itatiaia. Decorridos 25 anos após o trabalho de LAMEGO (23) houve considerável avanço no conhecimento dos maciços alcalinos; a melhoria nas condições de acesso ao corpo intrusivo possibilitou-nos a coleta de novas informações sobre aquela região. Dada a grande extensão da área, o relevo acentuado e a floresta densa, o nosso trabalho constou da elaboração de um mapa geológico na escala 1:50.000 e coleta de dados estruturais e morfológicos de natureza geral, sem a possibilidade de nos aprofundarmos nos detalhes. Do ponto de vista da geologia regional, foram tiradas algumas conclusões interessantes: a) As rochas alcalinas não ocorrem além das imediações da cidade de Passa Quatro, contrariamente ao que se imaginava. b) Não foi confirmada a existência de rochas alcalinas na serra da Bocaina, mencionadas por DERBY (11). c) As rochas alcalinas, dadas por LAMEGO (23) como um corpo único, na realidade formam 2 corpos distintos: maciço de Passa Quatro e maciço do Itatiaia, conforme indicação de ABSABER e BERNARDES (1). d) A área de 1450 km2 assinalada por LAMEGO (23) para as intrusivas, ficou reduzida a menos da quarta parte, ou seja, 330 km2. Na fase preliminar dos trabalhos de campo, fizemos algumas observações macroscópicas das rochas mais representativas da província alcalina: gnaisses do embasamento, rochas intrusivas dos corpos alcalinos (Itatiaia, Passa Quatro e Morro Redondo) e sedimentos clássicos senozóicos da Bacia de Resende do Rio Paraíba. O maciço do Itatiaia foi o objeto principal das nossa pesquisas, e a ele dedicamos a maior parte da intrusão, foram anotados importantes elementos morfológicos e climáticos, bem como aquele ligados aos fenômenos do processo intrusivo: diques, xenólitos, etc. Dentre os tipos litológicos) mapeados, a brecha magmática de conduto mereceu d observações mais pormenorizadas. São 10 km2 de rochas alcalinas de granulação fina, apresentando concentrações locais de fragmentos de rochas alcalinas trituradas. Parece-nos que está ligada à fase final da consolidação do maciço e ao provável abatimento do topo da intrusão. As grandes estruturas do relevo, principalmente na zona do planalto, refletem a influência de falhamentos e de intenso diaclasamento. Cristas, estruturas arqueadas e vales tectônicos condicionam as formas do relevo e o comportamento da drenagem. No estudo da tectônica regional do sudeste brasileiro, procuramos discutir as ideias de CLOOS e ARGAND, que postulam um determinismo estrutural do escudo pré-cambriano sobre as feições mais modernas. Os levantamentos epirogenéticos são dados como causadores de derrames basálticos e da evolução do magma alcalino. Mesmo os falhamentos cretáceo-terciários, que deram origem ao vale do Paraíba e afetarm as rochas alcalinas, talvez estejam solidários com as linhas de fraqueza do pré-cambriano. A intrusão magmática do Itatiaia, considerada como jura-cretácea, certamente ganhou o seu espaço através do deslocamento do seu teto através de falhas verticais do escudo cristalino. No seu resfriamento diferenciou-se uma fração rica em sílica, dando origem ao quartzo-sienito que hoje ocupa a parte central do corpo do maciço. A área rebaixada do planalto e a grande estrutura anelar foram por nós interpretadas como consequência de uma fase de colapso, ligada talvez à intrusão da brecha magmática; porém, não foi assinalada a ocorrência dos diques anelares que habitualmente se associam aos fenômenos de abatimento. Falhamentos pós-intrusivos ressaltaram morfologicamente as rochas alcalinas, afetando a área do planalto e o flanco sul da intrusão, propiciando a formação de espesso depósito de tálus dentro do Vale do Paraíba. O problema das formas do relevo do planalto, para muitos, tomadas como evidências de fenômenos glaciais de altitude durante o Pleistoceno, foi por nós discutido nos seus pontos essenciais. Os fatores climáticos foram considerados de importância secundária, pois os elementos tectônicos são os responsáveis pelos aspectos principais da morfologia.
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This study investigates the religious group named 'shoe wearing carmelites' (or Calced Carmelites) from Brazil´s Order of Carmo, from 1580 until 1800, in the Capitaincy of Bahia de Todos os Santos (Recôncavo, city of Salvador and Sergipe) and in the Capitaincy of Pernambuco (Alagoas, Pernambuco and Itamaracá). The study does not include the religious group known as the 'Reformed' Carmelites from Goiana, Recife and Paraíba convents. The Order of Carmo is a religious order from the Roman Catholic Church, founded in the 12th century. By the 16th century they were split into 'Calced' and 'Discalced'. In 1580 the Calced ones came from Portugal to Brazil, built convents in urban areas and were able to acquire slaves, farms and other assets. As any other religious order, the Carmelites had their modus operandi. This work emphasizes the way they operated or acted in the city, either individually or in association with other Carmelite religious foundations elsewhere (networking). Their action affected, although indirectly, the building of some specific aspects of the architecture, the city and the territory in colonial Brazil. The main objective of this study is to demonstrate the impact of the Calced Carmelites from Bahia and Pernambuco upon the territory of colonial Brazil, which is analyzed according to three scales: 1) the region or interurban; 2) the city or intraurban; 3) the building or the architecture. The research employs the comparative method of analysis, especially for the architectural scale. The work demonstrates that although not acting as architects or urbanists, the Carmelites contributed to the formation of the colonial territory of Brazil, behaving as a well-articulated and hierarchized religious network, from an economic and social perspective. Moreover, they influenced the emergence and growth of several colonial urban nuclei, from Bahia to Pernambuco, mainly in the surroundings of their religious buildings. Finally, it is very clear this religious order’s contribution to colonial architecture, as it can be seen by the architectural characteristics of the convents and churches which have been analyzed, many of which still stand in a good state of conservation nowadays.
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Recent endogenous processes provide dynamic movements in the lithosphere and generate the varied forms of relief, even in areas of passive continental margins, such as the research area of this work located in northeastern Brazil. The reactivation of Precambrian basement structures, after the breakup between South America and Africa in the Cretaceous played an important role in the evolution of basins, which provided generated forms of relief. These morphodynamic characteristics can be easily observed in marginal basins that exhibit strong evidence fault reactivations. The purpose of this study is to investigate the influence of morphotectonic processes in the landscape structuring of Paraíba Basin. Therefore, we used aeromagnetic, high–resolution images of the Shuttle Radar Topographic Mission–SRTM, structural geological data, deep well data and geological field data. Based on the results of the data was observed that some preexisting structures in the crystalline basement coincide with magnetic and topographic lineaments interpreted as fault reactivation of the Post–Miocene units in the Paraíba Basin. Faults that offset lithostratigraphic units provided evidence that tectonic activity associated with the deposition and erosion in the Paraíba Basin occurred from Cretaceous to the Quaternary. The neotectonic activity that occurred in Paraíba Basin was able to influence the deposition of sedimentary units and landforms. It indicates that the deposition of post–Cretaceous units was influenced by reactivation of Precambrian basement structures in this part of the Brazilian continental margin.
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The towns presently named Pombal and Sousa, located in the hinterland of the State of Paraíba, Brazil, still keep vestiges of the colonization process they went through along the 18th and 19th centuries, when they both emerged as settlement nuclei in the extreme West of the then captaincy of Paraíba and attained the status of freguesia and vila in a later period. This research aims to comprehend the process of urban formation and development of the colonial urban nuclei of Pombal and Sousa as they became povoados (hamlets), freguesias (parishes) and vilas (small urban communities with a local government), according to territorial expansion policies implemented by the Portuguese government from 1697 to 1800. The choice of the two urban settlements for this survey lies in the fact that they were part of the great conquest and colonization program undertaken by the Portuguese Crown. Another aspect that was considered was the fact that those towns are the oldest urban nuclei of Paraíba s hinterland. They came into being as early as in the times of the colony, thus producing a favorable environment to the study of the changes that occurred in the captaincy s hinterland scenery resulting from the process of formation and development of the colonial urban space. Three fundamental categories of analysis were defined since they have a direct bearing upon the urban configuration of the two colonization nuclei: povoado, freguesia and vila. The three of them are related to civil and ecclesiastic jurisdictions. Field, documentation and bibliography surveys were undertaken in order to develop the study. They allowed for the finding of vestiges of the old, colonial urban structures and for the development of theoretical analysis based on present-day studies of issues relating to the colonial urban history. The study purposes were, therefore, to try to understand how the old urban nuclei of Pombal and Sousa fit in the territorial expansion policies undertaken by the Portuguese government; to relate the process of urban formation and development of such nuclei with the categories of analysis povoação-freguesia-vila by discussing the relations and influences they exert over one another and their territory, as well as to unveil, as much as possible, the configuration the urban spaces that were shaped along the 18th century
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In the social-historical moment we live in, it is each time more evident the necessity of the people to learn to deal with the environment in conscientious way, taking care of themselves properly through it. In this direction, considering the school as a place where children, young and adolescents spend great part of their time, this work had as objective to examine the perception of school environment for students, professors and employees of two schools in João Pessoa city - Centro Estadual Experimental de Ensino-Aprendizagem Sesquicentenário and Escola Estadual de Ensino Fundamental e Médio Presidente Emílio Garrastazu Médici (Experimental State Center of Learning-teaching Sesquicentenário and Basic and High State School Education Emilio Garrastazu Médici President). From the presupposed that the environments in which and with which people live reflect their daily practices, the field work searched to identify the social-environmental practices that characterize the relation of these users with the school and, from this understanding, to infer some of their concerns regarding the environment as a whole. To analyze the use of the available physical space in the two institutions it was opted the use of the After-Occupation Evaluation, one of the approaches that feed the process of building production or built set, rescuing aspects related to its use, operation and maintenance. Besides analyzing diverse school environments (such as classroom circulations/accesses, library, pedagogical and sportive spaces) in relation to the environmental comfort and the perceptions of the main users of the schools (pupils, professors and employees), the dissertation tried to inquire the care (ambient education) of these users with the school space. In general, it was verified that the two schools have evaluations and perceptions really different for four reasons: (i) management of the schools; (ii) the users perception; (III) localization of schools and (IV) feeling of place, territoriality and appropriation
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This work regards to the structural conception as a formal element of design in wood architecture. On this approach, the group of projects studied is formed by some realized works of two important Brazilian architects: Severiano Porto and Marcos Acayaba. The time interval comprises the period from 1971 to 1997, which correspond respectively to the years of the creation of first and the last of the analyzed constructions. The research perspective concerns to the relationship between the parts, the whole and the building techniques adopted in each project. Moreover, the analysis focuses on the structure as the link among the different projectual ideas. Thus, the research method firstly includes a survey of specific bibliographies and documents which refer to the structural conception in wood architecture. Secondly,the buildings are analyzed according to the methods of architectural composition discussed through this work.
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This essay studies about contemporary architecture in João Pessoa, capital city of Paraiba State, which analyzes the utilization of steel and aluminum materials from 1990 to 2002, period when significant increase of this utilization is seen. As references, the architectural analysis and Engel structures definitions were used to analyze 40 built buildings, universe researched, to bring together subsidies to comprehend the contemporary production, especially which use the metal as structural and esthetic-formal element
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Académico - Licenciaturas
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Académico - Licenciaturas
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Académico - Licenciaturas
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Académico - Licenciaturas
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The towns presently named Pombal and Sousa, located in the hinterland of the State of Paraíba, Brazil, still keep vestiges of the colonization process they went through along the 18th and 19th centuries, when they both emerged as settlement nuclei in the extreme West of the then captaincy of Paraíba and attained the status of freguesia and vila in a later period. This research aims to comprehend the process of urban formation and development of the colonial urban nuclei of Pombal and Sousa as they became povoados (hamlets), freguesias (parishes) and vilas (small urban communities with a local government), according to territorial expansion policies implemented by the Portuguese government from 1697 to 1800. The choice of the two urban settlements for this survey lies in the fact that they were part of the great conquest and colonization program undertaken by the Portuguese Crown. Another aspect that was considered was the fact that those towns are the oldest urban nuclei of Paraíba s hinterland. They came into being as early as in the times of the colony, thus producing a favorable environment to the study of the changes that occurred in the captaincy s hinterland scenery resulting from the process of formation and development of the colonial urban space. Three fundamental categories of analysis were defined since they have a direct bearing upon the urban configuration of the two colonization nuclei: povoado, freguesia and vila. The three of them are related to civil and ecclesiastic jurisdictions. Field, documentation and bibliography surveys were undertaken in order to develop the study. They allowed for the finding of vestiges of the old, colonial urban structures and for the development of theoretical analysis based on present-day studies of issues relating to the colonial urban history. The study purposes were, therefore, to try to understand how the old urban nuclei of Pombal and Sousa fit in the territorial expansion policies undertaken by the Portuguese government; to relate the process of urban formation and development of such nuclei with the categories of analysis povoação-freguesia-vila by discussing the relations and influences they exert over one another and their territory, as well as to unveil, as much as possible, the configuration the urban spaces that were shaped along the 18th century