Litofácies e relações estratigráficas da formação Aquidauana no nordeste da Bacia do Paraná - São Sebastião do Paraíso (MG)

The Aquidauana Formation is characterized by sandstones of variable granulation, mudstones and diamectites abundant in clay, typical colors like brick red (vermelho tijolo) of glacial, fluvial and lacustrine origin. It’s chronostratigraphic equivalent to the Itarará group from the Neo Carboniferous age, that under the exploratory view, such units represent important intervals in the basin, occurring together with them minerals as well as energy resources as petroleum, underground water and coal – what requires a great paleogeography and stratigraphy knowledge for its exploration. By gathering information from the columnar sections of the area, it was possible to characterize the sedimentary facies, the stacking pattern as well as the association. It was also made an attempt of stratigraphic correlation, which showed great difficulties since glacial environments present a great lateral discontinuity of the facies besides the complex relationship process of formation. As a result, it was obtained 8 sedimentary facies, the lateral and vertical relations and genesis process. It is proposed that the sedimentary environment in the study area is the fluvio glacial, characterized by alluvial systems formed by defrosted water which transport the sediments that are deposited in plains in front of the glacier (distal outwash). Petrographic thin section analysis showed that the transportation process was ineffective. The grains present punctual to lobular contacts, characterizing good porosity and permeability to the rock, varying these qualities according to more or less existence of matrix. The presence of Iron Oxide deposited between the recrystallization border and feldspathic mineral indicates that this rock has possibly presented a primary rubefaction, intensified by alkaline fluid percolation

Caracterização litogeoquímica dos basaltos do município de Monções -SP

The paper deals with the petrographic and geochemical investigation of basalt flows present in a gravel quarry in the town of Monções in northwestern São Paulo State, members of the Serra Geral Formation of the Paraná Basin. Were collected 11 samples from different horizons within a topographic vertical profile with an average of 18 meters in height. The samples were subjected to macroscopic and microscopic petrographic and chemical major, minor and trace. The results indicated that it is tholeiitic basalts with dense fine grained average. Petrographic analyzes show that basalts studied are basically constituted by plagioclase (between 33 and 49%), labradorite and clinopyroxenes (between 29 and 46%) represented by the subordinate pigeonite and augite, having as accessories opaque (between 3 and 15% ), olivine (<2%), apatite and zircon as dashes. The secondary minerals correspond to cloropheite, chlorite, serpentine, epidote, albite and iron oxides and hydroxy as well as bowlingit of clay, nontronite, and celadonite. The basalts are kind of high-titanium (Hti)> 1.8% TiO2, and apparently belong to the Pitanga magma-type. The geochemical analyzes proved unsatisfactory for the determination of a probable lithogeochemistry differentiation within the vertical stroke for generating multiple data correlation or no immediately discernible trends

Estudo da influência do lineamento Tibagi e Sinclinal de Torres na estruturação da porção norte da bacia de Pelotas

The area of this work is located along the Northern portion of the Pelotas´s basin. The onshore region extends from the Southern portion São Paulo State to the North of Rio Grande do Sul State, with a total area of 440 530 km ². The objective of the research is to characterize the main geological structures of the outcropping basement in the Paraná Basin and its correlation with the offshore portion of the Pelotas Basin. The characterization was performed through the integration of surface (SRTM images and outcrops) and subsurface data (seismic data and well logs), the method includes the use of remote sensing techniques and seismic interpretation. The main structures to be analyzed are the Tibagi Lineament and the “Torres Syncline in order to verify its influence on the geological evolution and deformation of the basin. As result, it was identified the continuity of the both structures inside the offshore basin (Pelotas Basin); but only the Tibagi Lineament represents an important structural feature in the offshore basin. In this sense, the Tibagi lineament shows a NW-SE direction along the both basins (Pelotas and Paraná) and it is defined by drainages and relief on the continental portion. It was classified as a graben structure limited by normal faults and it also was verified a trend of faults inside the lineament that cuts all the sedimentary package of Itararé Group from Paraná Basin. The Torres syncline is a structure that connects the arches of Ponta Grossa and Rio Grande, showing NW-SE orientation and a low angle dip in the NW direction. Its projection into the Pelotas Basin was not recognized by the methods applied in this work, because a preliminary analyze indicates that its projection corresponds to a structural high inside the Pelotas Basin

Tecnologias, conceitos e propostas de materiais de construção sustentável do Centro de Vivências da UNESP, Rio Claro/SP

Due to the great impact caused by construction, the university has a major role in the development of alternative projects and studies aimed at sustainable development. This project presents the advantages and importance of building in a sustainable manner from the beginning to end of the Center of Experiences at UNESP, Rio Claro / SP. It will be presented alternative building materials that have high environmental performance and that bring the least negative impacts as possible. Providing a Center of Experiences through a sustainable building is in need of the university to renovate the new trends of society in which the construction is in harmony with the environment in which it is inserted. This sustainable building will serve as a model for students and residents of Rio Claro, since the building itself will serve as a way of learning to the audience goer, as well as for the other campuses of UNESP. Thus, this project will serve as a guide for decision makers facing the huge amount of building materials available in the market

Caracterização estrutural da porção central da Bacia de Santos e seu embasamento continental adjacente, através de interpretação de imagens de satélites e geofísicas

The Santos Basin is located in the Brazilian continental margin and includes the coast of Santa Catarina, Paraná, São Paulo and Rio de Janeiro states. Its northern limit is the Campos Basin through the High of Cabo Frio and the southern one with the Pelotas Basin through the Platform of Florianópolis, totaling an area of approximately 350,000 square kilometers in a water depth of 3,000 m. The Paranapanema Lineament has WNW / ESE direction, and extends from the area filled by the Paraná Basin, on the border between the states of Sao Paulo and Parana, lasting up to near the ocean floor along with the fracture zone of Rio de Janeiro. The Capricorn Lineament is a feature inherited from the separation between the continents of Africa and South America, and is the main structural feature NW / SE of the Santos Basin center-south region. These two structures together with other ones with continental origin may be associated with structural features in the sediments from the Santos Basin. This work aims to characterize the structures operating in the central portion of the Santos Basin based on subsurface data in the offshore area (2D seismic) together with data from the surface of the continental basement in a way to correlate the Santos Basin structures with the continental regional traits. This data interpolation showed that the structural features of the continent operates on the submerged zone, the seismic sections show these structural trends for the Paranapanema Lineament / Fracture Zone of Rio de Janeiro, Capricorn Lineament and two fault zones that exhibit structures typical of a transfer zone

Levantamento estrutural da porção norte do Greenstone Belt do rio Itapicuru e dos Alvos Encantado e C1W, Bahia

The study area is located in the geological context of the northern portion of the Rio Itapicuru Greenstone Belt (GBRI), located northeast of the São Francisco Craton, Bahia State. The GBRI is known for its great economic potential for gold mineralization, looking south at Fazenda Brasileiro Mine and North Mine Maria Preta, is situated in the study área. The structural pattern of the northern portion of the Greenstone, theme of this work, is of great importance to understand the mineralization present. To characterize the structural model three geologic sections (scale 1:25000) were made with NW-SE and EW directions and detailing two mineralized targets, Encantado, located northwest of the area, near the city of Nordestina, and C1W, located near Itapicuru River, west of the Maria Preta mine. Thus, field work and petrographic analysis were conducted, that allow to indicate the existence of two structural domains characterized by the existence of a main foliation, low angle dipping main foliation and another with high dip angle, both with NW, moreover, folds occur in the area Dn-1 and post-Dn folds. Dn-1 folds are observed less frequently but they occur mainly forming an oblique foliation and the Sn is present in porphyroblasts observed in petrographic analysis, whereas in relation to the folds post Dn, there are more than one type of folding in area, which differ by the orientation of their axis, a post Dn NS and EW Dn another post. Moreover, two areas of metamorphic green schist (biotite zone) and medium amphibolite, which are directly related to the structural domains found

Levantamento e censo de aves e mamíferos cinegéticos no Parque Estadual Turístico do Alto Ribeira (PETAR), SP

Nas florestas Neotropicais, os mamíferos podem desempenhar papéis importantes como predadores e/ou dispersores de sementes, polinizadores, frugívoros, folívoros ou até mesmo predadores de topo e, por isso, são importantes para a manutenção e regeneração das comunidades biológicas. Os objetivos deste trabalho foram: (i) realizar um levantamento da diversidade de espécies de aves e mamíferos cinegéticos no PETAR, (ii) estimar a abundância relativa, densidade, biomassa e tamanho populacional das aves e mamíferos mais avistados, (iii) comparar a diversidade e abundância das espécies estudadas em dois núcleos com diferentes pressões antrópicas. A área de estudo esta localizada na Serra da Paranapiacaba, que é a segunda maior área protegida do estado de São Paulo, possuindo mais de 125 000 ha, onde quatro Unidades de Conservação estão conectadas (Parque Estadual Turístico do Alto Ribeira, Parque Estadual de Intervales, Parque Estadual de Carlos Botelho e Estação Ecológica Xituê). Ligadas a Serra do Mar, estas UC´s formam um grande corredor de biodiversidade que compreende o maior contínuo florestal de Mata Atlântica. O presente estudo segue o mesmo protocolo de amostragem do projeto BIOTA Fapesp (01/14463-05). As espécies alvo da amostragem foram aves de grande porte (Cracídeos, Tinamídeos e Fasianídeos) e mamíferos acima de 1kg, com exceção do esquilo (Guerlinguetus ingrami) que é uma espécie indicadoras de áreas defaunadas. Para o levantamento qualitativo (riqueza) foram utilizadas identificação de pegadas, carcaças, rastros e observações ad libitum. Já o levantamento quantitativo (abundância, densidade, biomassa e tamanho populacional) foi obtido pelo método de transecções lineares, em que para cada indivíduo observado foram obtidas a distância perpendicular animal-trilha, horário do avistamento, número de indivíduos e sua localização... (Resumo completo, clicar acesso eletrônico abaixo)

Estudo da distribuição e das densidades larvais do bivalve invasor Limnoperna fortunei (Dunker, 1857) nos principais corpos d’água da bacia do rio da Prata

O mexilhão-dourado (Limnoperna fortunei) é um bivalve de água doce pertencente à família Mytilidae. Originário de rios e arroios da China e do sudeste asiático, foi introduzido acidentalmente na América do Sul em 1991, no estuário do rio da Prata, provavelmente através de água de lastro. Como encontrou condições propícias para o seu desenvolvimento, se expandiu através dos rios Uruguai, Paraná e Paraguai, sendo atualmente o principal responsável pelo macrofouling em ecossistemas de água doce do continente. O presente estudo compreende uma área de grande extensão na bacia do Rio da Prata, onde foram amostrados pontos estratégicos nos rios Paraná (e seus principais afluentes), Uruguai e Paraguai. A partir de coletas de organismos do plâncton, realizadas por arrasto vertical, foram quantificadas as densidades de larvas de L. fortunei em cada local de amostragem. Assim, obteve-se um panorama atual da ocorrência do mexilhão, registrando-se, inclusive, alguns limites de sua distribuição. As densidades mostraram-se, no geral, elevadas, provavelmente em decorrência do período de amostragem (verão 2010), onde a atividade reprodutiva da espécie é maior devido às altas temperaturas. Porém, grandes variações ao longo da bacia foram registradas, o que pode estar relacionado ao grau de antropização, disponibilidade de substratos, velocidade da corrente, tempo de introdução, entre outras variáveis

A espacialização do atendimento médico no Alto Vale do Ribeira (Ribeira/SP e Adrianópolis/PR) sob a ótica da geografia da saúde

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A conformidade do projeto da usina hidrelétrica de Tijuco Alto em relação às áreas prioritárias para a conservação da diversidade biológica

A biodiversidade pode ser considerada como uma base da existência por proporcionar recursos e regular os processos naturais responsáveis pela manutenção da vida. Nas últimas décadas, a biodiversidade vem sendo perdida rapidamente, apresentando taxas de decréscimo nunca antes vistas, o que reduz a capacidade de aporte de recursos naturais para as gerações futuras. Em relação às estratégias de conservação da biodiversidade, os orgãos ambientais brasileiros têm empreendido diversos esforços na sistematização de dados e informações sobre biomas, ecossistemas e espécies ameaçadas com a finalidade do estabelecimento de indicadores e diretrizes para a conservação da diversidade biológica direcionados à tomada de decisões por parte de gestores públicos e privados, como aquelas que são deflagradas no âmbito dos processos de licenciamento ambiental. Dentre os instrumentos de gestão ambiental, o licencimaneto ambiental é aquele responsável pela autorização da implantação de empreendimentos potencialmente causadores de significativo impacto ambiental, como é o caso de usinas hidrelétricas. Para isso, o licenciamento ambiental deve estar baseado em estudos ambientais realizados a partir dos procedimentos metodológicos de avaliação de impacto ambiental, os quais devem preconizar os aspectos que caracterizam a vulnerabilidade ambiental da localidade geográfica onde está planejado o empreendimento. Neste sentido, o presente trabalho objetivou analisar de que forma os dados, informações, indicadores e diretrizes sobre a diversidade biológica brasileira, produzidos e estabelecidos pelo governo federal estão sendo utilizados no processo de licenciamento ambiental da usina hidrelétrica de Tijuco Alto do rio Ribeira de Iguape.

Monitoramento espacial e análise das características climáticas na influência sobre a cultura de soja no estado do Paraná

In the past years, soya has increased itself as the mean agro export culture in Brazil, encouraging the expansion of its agricultural frontier throughout the country. Brazil is the second biggest soya producer around the world, with a 59,8 million ton production in 2008, according to the Instituto Brasileiro de Geografia e Estatística (IBGE), only behind United States. Around the country, the four leading producer states are Mato Grosso, Paraná, Rio Grande do Sul e Goiás. Therefore, geotechnologies may be used to monitor use and soil occupation in various analyzes periods. In this review, the tools are important to illustrate the soya production areas and also the weather behavior around its production evolution in the territory through the years. Its utilization can contribute to the evolution and optimization around real time monitoring of the Agricola cultures, without being necessary to be in the area with a low financial cost. Generally, this information is strongly important for decision makers in both government and private sector, as soon as the achievement information regards the quantification of area, yield and development of agricultural crops are essential to the economic behavior of culture during the season and even beyond. By obtaining data regarding climate crops 2008/09 and 2009/10, held the climatic water balance calculation based on the dynamics of water storage in soil temperature and precipitation data, interpolation of the data through the interpolator (IDW) that generated thematic precipitation maps. Overall, the use of geotechnology to monitor agricultural areas, can strongly contribute to this monitoring, generating raw material for further analysis at low cost

Interferência do bullying no esporte de alto rendimento

Examine the phenomenon of bullying behavior that makes people teased, laughter, sarcasm, irony, among other types of attacks. This is not only physically, but with moral violence, emotional or psychological. When there is an effective intervention against bullying, all individuals in the group start to suffer with this situation, which can lead to psychological disorders, hampering the progress of relations as well as team sports, over a period of training and competition. This article analyzed a sample of athletes in order to find behaviors that characterize the extent of bullying and can see the consequences of it, as early drop out. Through the results it was concluded that the actions that characterize bullying are present in very high performance football and may even lead to drop out the sport. We also evaluate the environments frequented by teams can become enhancers of this phenomenon, they are times when athletes have a living space and one that may become amenable to the events, plus the fact that many athletes have already thought about leaving the sport because to bullying

The stream fish fauna from the rio Machado basin, Rondônia State, Brazil

The rio Machado (also known as Ji-Paraná) is a tributary of the rio Madeira in the Amazon basin. Currently, the rio Madeira contains the greatest fish species richness of the world, with approximately 1,000 species. The present study presents the fish inventory from streams of the rio Machado basin. In total, 75 stream reaches, 80 meter-length, randomly selected, were sampled in 2011 (August to October) and 2012 (June to July). Overall, 22,875 fish in eight orders, 32 families, 89 genera, and 140 species were collected. Richness estimators indicate that almost 90% of the expected richness was registered. The great majority of specimens (52.2%) was represented by small sized piabas such as Serrapinnus aff. notomelas, Moenkhausia collettii, Serrapinnus microdon, and Hemigrammus melanochrous. Of the total richness, 25 species were restricted to 9°00’ S and 10°00’ S; among them, 14 were exclusive to the lower portion of the basin, which exhibits the larger proportion of native vegetation covering.

Interferência das construções sucessivas de Pequenas Centrais Hidroelétricas (PCH), sobre a ictiofauna do rio Sapucaí-Mirim-SP, Brasil

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Desenvolvimento territorial, políticas públicas e inovação social no Alto Jequitinhonha - MG

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)