28 resultados para Guapiara Lineament
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Structures transverse/sub-transverse to the shoreline have been identified and characterized on the precambrian basement outcrop on the continent adjacent to the northern Santos Basin. These structures were analyzed from images of digital elevation model SRTM 90m by extracting NW-SE lineaments that intersect the NE-SW foliation. The lineaments were selected, classified into 48 segments that extend toward offshore, and correlated with basin structures. In the basin 25 2D seismic sections, 12 well logs and data from potential methods were interpreted, identifying the key stratigraphic levels and the major structures. Structural maps of each horizon were generated. Six transfer faults (FTs) were recognized and named FT-1 to FT-6, whose extensions correspond to continental lineaments named FC1 to FC6. The FTs are related to the basin deformation and evolution. In seismic sections, these faults have lateral slip in flower structures, displacement inversions from normal at the top to reverse at the base, abrupt changes in thickness or even disappearance of the seismic reflectors. The structural map of the Basement and Top of the Rift shows control of some depocenters by faults and displacements in some areas. The maps of potential methods indicate that there are pronounced anomaly shifts in some areas, associated with FTs. Some seismic sections indicate reactivation of FTs when they intersect horizons from the basement until the most recent layers. The 3D integration of data facilitated the observation of the FT extensions in the continent discontinuity.
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The Nabileque fluvial fan is a Quaternary depositional system located along the southwestern border of the Pantanal, covering an area of approximately 9,100 km 2. It is a peculiar alluvial system because it is not associated with inflow from adjacent plateaus. The Nabileque megafan is formed by the Paraguay River at the exit of the Pantanal wetland, coalescing with the Pilcomayo megafan of the Chaco basin. A geomorphological zonation analysis was performed making use of remote sensing data with field verification. Most of the area is a vast alluvial plain made of Pleistocene deposits, whose surface is marked by the presence of an intricate network of distributary paleochannels. Areas blanketed by Pleistocene deposits are dissected by erosional streams and subject to frequent flooding events. The Paraguay River flows in a meander belt constrained by NE fractures associated with the Transbrasiliano Lineament, but deflects towards the SSE after the Negro River confluence composing the system's peripheral drainage. An abandoned meander belt is preserved within a remarkable N-S incised-valley that is interpreted as the ancient Paraguay River course. Processes of avulsion and river capture are suggested to explain the observed changes of the river course. The Nabileque River is an underfit stream within the incised-valley, cutting paleomeanders and point bars of the previous Paraguay River course.
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The present work aimed at characterizing geological features that identify areas with high ruptibility (fracturing) in the Osvat/Osplan pipeline in São Sebastião, São Paulo. The analysis of ruptile geological structures (lines of strikes and structural lineaments) through the use of orbital remote sensing was used as systematic mapping. The analysis of these features enables the inference of factors, such as permeability, infiltration and degree of shear in the region, factors which influence the processes of erosion and landslides in the area. On the map of structural lineaments, points of lineaments intersection from different directions were analyzed, followed by the counting of the frequency of these items per unit area, allowing the statistical modeling of spatial distribution, generating the map of density of structural lineament intersections, which allows determining areas with the highest percolation of fluid in the rock structure. However, on the map of lines of strikes, a space analysis was conducted to identify the two directions with higher frequency of lines of strikes in order to establish the maximums 1 and 2 and to identify the areas of abrupt changes of direction of these strike lines. In such areas where abrupt changes of directions of maximum lines of strikes occur, consequently there will be intense percolation of fluids, responsible for higher alterability of the rock/soil complex, facilitating the installation of erosion processes and landslides, increasing the area instability and consequently the vulnerability of the pipeline.
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Pós-graduação em Geologia Regional - IGCE
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Pós-graduação em Geologia Regional - IGCE
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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
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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
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Tem havido uma preocupação global com o desaparecimento de polinizadores dos campos de cultivo, podendo causar uma queda na produção de alimentos, e consequentemente, afetar a segurança alimentar em decorrência de déficits de polinização. Dessa forma, ações visando à conservação de espécies polinizadoras e de seus habitats vem assumindo uma importância cada vez maior. A região do município de Guapiara destaca-se no Estado de São Paulo como a principal produtora de tomate. O tomateiro possui flores hermafroditas e autofecundadas, porém uma melhor produtividade pode ser alcançada com a polinização por abelhas. A região apresenta uma diversidade de habitats agrícolas próximos a ambientes naturais preservados (Parque Estadual Intervales e Parque Estadual Turístico do Alto Ribeira), o que favorece o estabelecimento de uma fauna de polinizadores diversificada, mas fortemente impactada pela aplicação intensiva de produtos químicos nos cultivos. A proposição de um plano de manejo objetivando a conservação de espécies de abelhas junto às áreas cultivadas se justifica plenamente para a região, considerando a fauna rica em espécies de abelhas com potencial de polinização para cultivos agrícolas. Planos de divulgação sobre a importância da conservação das espécies ou habitats alvo são parte integrante dos planos de manejo. Entre as ações de divulgação, a elaboração de material impresso é importante pela capacidade de alcance de diferentes setores envolvidos com as espécies e habitats a serem manejados e conservados. Este trabalho é parte integrante de um amplo estudo sobre a importância das abelhas em cultivos de tomate na região de Guapiara. Informações foram coletadas ao longo de dois anos, no qual foi elaborado um diagnóstico do estado de conservação da área, uma descrição da fauna de abelhas associada às flores de tomateiros e uma avaliação do potencial de manejo. O objetivo geral...
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The area chosen for this study is the island of Trinidade, which is located 1167 km off the Brazilian coast, in parallel Victory at 20 ° 30'S and 29 º 19'W, being the most easterly point of our continent. The isolation of oceanic island of Trinidade leaves no noticeable that she is part of a large submarine volcanic chain oriented east-west lineament known as Vitória- Trindade. Along with the island of Martin Vaz, who is Federal Territory is administered by the Navy of Brazil. Both correspond to Source alkaline volcanic islands. The area of the island of Trinidad has approximately 10 km2. Geologically consisting ankaratritic spills, spills tannbuschiticos, volcanic tuff spills analcite-ankaratrite, phonolite spills, spills nefelinite, pyroclastics, spills grazinite, tinguaitos, olivine-analcitito, calcarenite dunes and wind according to Almeida (1961). The island has its base on the ocean floor, at 5,800 m depth. It is the only place still recognizes preserved volcanic necks and plugs, as well as remnants of a volcano in Brazil. Magmatism occurred here a sodium alkali-silica subsaturated where his wrist was last 50,000 years according to Almeida (1961). It is a place with restricted access due to their distance from the coast, his contribution and hard to be an exclusive area of the Navy. On the island with peaks occur up to 620 meters high, and its rugged mountainous terrain and difficult access to very specific points, as the peak of Desire, peak Fazendinha, Monument and other points on the island. Because of its location far from the coast, its small infrastructure, difficulty of landing and restricted access by sea, the island of Trinidad offers no possibility of tourism, being a military outpost, and scientific basis of great importance, which conduct research in area of marine biology, oceanography, geology and others
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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)
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Pós-graduação em Ciências Biológicas (Zoologia) - IBRC
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Pós-graduação em Geologia Regional - IGCE
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Cerca de 90% das plantas com flores e 35% das culturas agrícolas são dependentes de animais para polinização, e as abelhas são os principais agentes polinizadores de uma ampla variedade de espécies de plantas de ambientes naturais e agrícolas. Assim, as abelhas não só são imprescindíveis para a manutenção e conservação de comunidades de plantas em sistemas naturais, como também na atuação direta e significativa na produtividade agrícola. Atualmente, as populações de abelhas estão em declínio no mundo todo, em decorrência, principalmente, do crescente desmatamento e consequente perda de habitas adequados, além de outras ações antrópicas que modificam os seus nichos. Tendo em vista que muitos estudos, realizados principalmente em regiões temperadas, têm demonstrado que a paisagem do entorno dos cultivos agrícolas influencia a diversidade e abundância de polinizadores, avaliações sobre o efeito do contexto da paisagem na fauna de abelhas se tornam fundamentais. Este estudo teve como objetivo geral identificar os fatores que influenciam a riqueza e a abundância/diversidade de abelhas nativas em áreas agrícolas inseridas em um gradiente de quantidade de habitat e níveis de heterogeneidade da paisagem. O estudo foi conduzido no município de Guapiara, SP, região predominantemente agrícola, com fragmentos florestais de Mata Atlântica no entorno das propriedades rurais. Para amostrar a distribuição e a diversidade das abelhas foram usadas armadilhas do tipo pan trap (nas cores amarelo, azul e branco). Em cada ponto amostral foram instaladas cinco estações (cada estação composta por um pan traps de cada cor) de 1,5m de altura, cuja distribuição espacial dentro das propriedades de estudo tem formato de X e distantes uma das outras 5m. As amostragens foram de 30h/coleta em cada ponto amostral (n=17, cada um com raio de 1000m), realizadas em uma única época do ano (primavera/verão, quente e chuvoso)...