Geologia e Litogeoquímica das Rochas Graníticas do Maciço Capão Bonito e O Contexto Geológico da Sequência Vulcano-sedimentar Açungui

O Maciço Granítico Capão Bonito encontra-se associado à evolução da granitogênese neoproterozóica da Província Mantiqueira Central e localiza-se no sudeste do estado de São Paulo, intrusivo em rochas epimetamórficas do Grupo Açungui (Formação Votuverava) e em rochas do Complexo Granítico Três Córregos. As suas rochas afloram junto à borda da Bacia do Paraná e encontram-se parcialmente encobertas por rochas sedimentares do Grupo Itararé e por sedimentos recentes da Bacia do Paraná. Suas rochas estão distribuídas na forma de um corpo alongado e paralelo a direção NE-SW das principais zonas de cisalhamento. È constituído por sienogranitos vermelhos, holo- a leucocráticos com biotita e rara hornblenda, inequigranulares de granulação média a grossa a porfiríticos e isotrópicos a levemente cataclásticos nas zonas marginais. São rochas pertencentes às séries cálcio-alcalinas alto potássio a shoshonítica ou às séries subalcalinas potássicas e caráter metaluminoso a peraluminoso. O magmatismo é compatível com os granitos do tipo A, tardi-orogênicos a anorogênicos de ambiente intraplaca, a partir da fusão de material da crosta inferior com emplacement associado à estrutura transtensiva correlacionada às zonas de cisalhamentos, em um ambiente extensional ao final do evento colisional da Orogênese Ribeira.

A Sonata de Deus e o diabolus: nacionalismo, música e o pensamento social no cinema de Glauber Rocha

Pós-graduação em Ciências Sociais - FFC

Biology of Triatoma carcavalloi Jurberg, Rocha & Lent, 1998 under laboratory conditions

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Aspectos petrográficos dos carbonatos da Formação Riachuelo - Albiano, bacia de Sergipe

The carbonatic rocks have great importance in petroleum geology, since most hydrocarbons reservoirs in the world are associated to this kind of rock. The new giant petroleum fields discovered in the Brazilian southeast Atlantic margin are directly connected to calcareous rocks, which are subjacent to the Aptian evaporite pack. This demand an increase in the number of geologists able to study such deposits. The Aptian carbonatic platform is completely exposed only in the Sergipe-Alagoas Basin. Therefore, it works as a natural laboratory to the study and understanding of this kind of rock. The Sergipe Basin is situated in the east Brazilian coast, and has its evolutional history is intimately related to the formation of the South Atlantic Ocean, through the break-up of the Gondwana supercontinent. The marine sequence of the Brazilian marginal basins is of Albian age and is marked by the development of carbonatic platforms. In doing so, this paper aims to analyze the Albian limestones from Riachuelo Formation of the Sergipe Basin. The project gave to the student the opportunity to increase his knowledge in carbonates, due to the laboratory and outdoor activities. The studied deposits, within a regional outline, were petrografically described, allowing interpretations about the evolution of the former South Atlantic Ocean. Ten points were visited where samples were collected for making of thin sheets. In this work several carbonatic facies were identified totaling 116 laminates described.

Geologia do platô N6 - província mineral de Carajás (SP)

The N6 Plateau presents an iron-ore occurence in Carajás Mineral Province, standing near to actually operating deposits. Geological mapping in 1:10,000 scale and integration of geochemical, geophysical, petrography and drilling turns possible interpretation of his geological evolution. The mapped area has lithotypes from Archean Grão Pará Group, comprising very lowgrade metamorphic basic rocks and iron formation and an Proterozoic sedimentary association of conglomeratic sandstones called as Caninana Unity. The structural geology in given by a regional scale homoclinal, where the Grão Pará Group strata dips towards SW, as a part of the Northern Limb of the Carajás Fold. Subsequent deformation associated to the installation of the Carajás Shear Zone presents as E-W fold axis. Geochemical evidence permits to consider de Parauapebas Formation as the rocks which has been hydrothermally-altered to outsourcing fluids responsible to deposition of iron formations in the oceanic system, including different signatures which can be interpreted as possible sub-embayments in the Carajás Basin. The iron ore in the area occurs in subsurface as very fine friable hematite generated by supergenous enrichment of the iron formation. The conceived geologic model differs from the current academic proposal on the fact that hydrothermal alteration has been involved on the jaspelite enrichment. Metamorphism on the Parauapebas Formation presents paragenesis considered as ocean-floor metamorphism which precedes de deformation insofar as the rocks show no tectonic fabric referring to shallow crust evolution. Geophysical methods such as magnetometry and gravimetry presents excellent results for structural interpretation in uneven exposed terrain

Corpos intrusivos básicos na coluna sedimentar Permo-Carbonífera no vale do rio Corumbataí

As rochas intrusivas básicas associadas a Formação Serra Geral na porção sul do município de Rio Claro e norte de Piracicaba configuram geometrias na forma de diques e soleiras. Estes corpos estão associados à uma parte da Bacia Sedimentar do Paraná que foi deformada por eventos tectônico que resultaram em trends preferencias NW-SE, condicionando a estratigrafia, a intrusão e geometria dos corpos de diabásio e formação da estrutura domática do alto de Pitanga. Os corpos intrusivos tem em sua maioria a forma de soleiras e em menor quantidade a forma de diques. A compreensão destes corpos é importante para o entendimento da estratigrafia da área conhecida como domo de Pitanga na região de Rio e Piracicaba

Caracterização tectono-sedimentar do Grupo Lagoa Feia (Eocretáceo) no Campo de Pampo, sudoeste da Bacia de Campos

The Lagoa Feia Group (Early Cretaceous) is widely distributed around the Campos Basin, forming deep prospects in the basin. It has two large coquinas platforms shellfish, and the lower deck constituent important reservoir in the southwestern of this basin, a producer of oil in the trend-Badejo-Linguado-Pampo. Due to the rising national energy demand is necessary to see the incorporation of technical knowledge and training of human resources in the knowledge of petroleum reservoirs. In this sense, the Pampo Field, as well as other fields of the trend, fall as interesting target area for study. Accumulations of hydrocarbons are partitioning structural - stratigraphic only for the three fields. They are mixed origin of traps, with influence of structural, stratigraphic and diagenetic. With the development of catchment areas of the latter condition has manifested itself in such a way to verify parts with nonproducing wells, which are observed in the intervals coquinas are closed, with reduced thickness and / or low quality porous. The understanding of these accumulations, by testing structural, stratigraphic and reservoir and the use of geological and geophysical techniques, will bring a better understanding of the portions relating to economic accumulation or subeconomic development of hydrocarbons in this region, contributing to the scientific knowledge of the Pampo Field.

Caracterização magnetométrica de Sill de diabásio na região de Limeira - SP

Pós-graduação em Geologia Regional - IGCE

Análise da relação filogenética entre Triatoma carcavalloi Jurberg, Rocha; Lent, 1998; Triatoma circummaculata Stal, 1859; Triatoma klugi Carcavallo, Jurberg, Lent; Galvão, 2001 e Triatoma rubrovaria Blanchard, 1843 (Hemiptera, Reduviidae) baseada no sequenciamento de genes do DNA mitocondrial e nuclear

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Fonte alternativa de K obtida da produção de KCl a partir da rocha silicática potássica (verdete) na cultura de milho

Para produzir o termopotássio e, até mesmo, o KCl, a rocha silicática potássica (verdete) passa pelo processo de calcinação. Neste processo é gerado um resíduo denominado coproduto que contém em sua composição química 3% a 4% de K2O, Ca, Mg e Si e apresenta baixa solubilidade em água. O presente trabalho objetivou testar a hipótese de que doses de K2O na forma de coproduto fornecem potássio para as plantas de milho em menor quantidade do que as mesmas doses na forma de KCl, inclusive no estudo do efeito residual, e que o potássio extraído do solo pela resina trocadora de íons tem maior correlação com as quantidades de potássio absorvida pela planta de milho do que com o potássio extraído pela solução extratora de Mehlich-1. O experimento foi conduzido em casa de vegetação, onde foram realizados dois cultivos consecutivos de milho em amostras de Neossolo Quartizarênico órtico. O delineamento foi em blocos casualizados com duas fontes de K (KCl e coproduto), três doses de K2O (0, 200 e 400 kg ha-1) e quatro repetições, totalizando 24 unidades experimentais. Foram determinados os teores de potássio extraído da amostra de solo pela solução extratora de Mehlich-1 e resina trocadora de íons, a produção de matéria seca da parte aérea das plantas de milho, os teores e o acumulo de potássio nas plantas após o primeiro e o segundo cultivo. Em dois cultivos consecutivos das plantas de milho, a aplicação de 200 e 400 kg ha-1 de K2O na forma de KCl proporcionou o acumulo de potássio na parte aérea das plantas de 77 e 84% maior do que aplicação dessas mesmas doses de K2O na forma de coproduto, respectivamente. A aplicação de 200 e 400 kg ha-1 de K2O na forma de coproduto proporcionou aumentos no acumulo de potássio da parte aérea das plantas de milho de 66 e 75% em relação ao controle (sem K2O), respectivamente. A recuperação de potássio pelas plantas de milho tratadas com KCl foi de 92% e as plantas...

A crítica cultural do jovem Glauber Rocha no suplemento dominical do jornal do Brasil: impasses e estratégias adotados na chegada ao Rio de Janeiro

Glauber Rocha’s arrival at Rio de Janeiro can be considered a milestone for the Brazilian Cinema Novo movement in the early 1960s. In 1959, Glauber starts his collaborations in the Suplemento Dominical do Jornal do Brasil. This paper examines Rocha’s major contributions in this newspaper for the purpose of pointing out the strategies and formulations of the young intellectual from Bahia to promote a debate on the forms of modern Brazilian cinema and its relationship to other art forms in the 1960s.

Glauber Rocha e a dimensão do confronto de ideias na cena midiática: estudo das estratégias do jovem crítico de cinema no Jornal da Bahia no final dos anos 1950

In late 1950, the young Glauber Rocha, still without having directed any of his films, becomes the main cultural critic of the Jornal da Bahia in Salvador, Bahia. His film critic activity falls within the symbolic local disputes and his texts published become an active voice in the cultural field of Bahia. With a considerable apparatus of the press in his favor, the performance of the young critic Glauber Rocha allows to discuss: the role of public intellectual and media production and dissemination of ideas by the newspapers at the turn of the 1950s to the 1960s, a time of intense political, social and cultural changes in Brazil.

Glauber Rocha e a crítica de cinema no Diário de Notícias: periferia e resistência

In the early 1960s, after his experience as a film critic in the Jornal da Bahia, the young Glauber Rocha began his collaboration in the Suplemento Artes e Letras of Diário de Notícias in Salvador. Inserting itself the symbolic disputes in defense of a film art of authentic Brazilian nuance, the activity of the critic Glauber Rocha represents a voice that demarcates the internal tensions of the field of cinema in Bahia and outlines, in the form of genesis, his most famous manifesto, “An esthetic of hunger” (1965). For this analysis were focused mainly two critics: “Experiência ‘Barravento’: confissão sem moldura”, published December 25-26, 1960, and “Luz Atlântica, 1962”, published in December 31, 1961.

Geoquímica de perfis lateríticos na chapada sedimentar do Triângulo Mineiro

The ferruginous sandstone (Serra da Galga member) from Marilia formation present in sedimentary mining triangle plateaus - MG (southeast Brazil) is still not properly characterized, as well as the presence of a rich layer Fe nodules which is not properly understood, as are the alteration products of this material that may be linked to the presence of refractory clays which are characterized by intimate relationship between Fe and Al. Aluminum is widely present on top of these plateaus. This course conclusion paper characterized the mineralogy and distribution of smaller elements both rust sandstone evolved as soil above this sandstone. The characterization has been done by using X-ray fluorescence techniques (XRF), the iron was removed by using the CBD method (dithionito-citratebicarbonate), and X-ray diffraction (XRD) and analysis of the products extracted by the CBD method by ICP- OES were made to characterize the material. The results of the XRF show great variation of Al and Si, Fe with almost constant behavior in the average depth of 110 cm, where it has the highest concentration levels. Fe appear associated with the V and Ce. CDB results show a clear relation of Fe with Al. Al does not have in this case compared with Cr or any other item. The concentration of extracted Al was always below the concentration of Fe. In the region, the formation of this Latosols- Gleysols system is subject to topography and its influence on local water regime, a regime that has direct influence on the formation of supergene accumulations as in the area and results in aluminum accumulation in refractory clays exploited by IBAR mining

Mapeamento geológico-geotécnico por meio de análise integrada no Parque Estadual do Juquery - Franco da Rocha-SP

Pós-graduação em Geociências e Meio Ambiente - IGCE