Implicações da formação continuada na prática pedagógica do(a) professor(a) no âmbito da cultura corporal do movimento

Pós-graduação em Ciências da Motricidade - IBRC

Geologia, geomorfologia e morfotectônica da região de Marabá - PA

Pós-graduação em Geologia Regional - IGCE

Caracterização geológica do município de Assis: a importância do estudo das coberturas cenozóicas

Pós-graduação em Geologia Regional - IGCE

Gestão democrática escolar em Cuiabá: estudo de caso

Pós-graduação em Educação - FFC

Avaliação da erodibilidade pelo método Inderbitzen em solo não saturado da região de Bauru - SP

Pós-graduação em Engenharia Civil e Ambiental - FEB

Estudo da inflexão da Serra do Garrote e sua influência na zona de falha de Vazante (MG)

The Vazante Fault Zone (VFZ), located northwestward of Minas Gerais, host the largest zinc deposit known in the Brazilian territory. This structure is hosted in Vazante’s Group rocks, a metassedimentary sequence of marine environment. Near Vazante is situated the south end of the VFZ. To the west, occur the Serra do Garrote inflexion, characterized by a curvature in the contact of Formations Serra do Garrote and Serra do Poço Verde. This structure is through the analysis of aerial imagery of the region and represented in the published geological maps. The objective of this work is to understand what causes this inflexion and determine whether it affects the VZF, causing a shift in the same, and possibly, in the mineralization as well. To this end, it was done a mapping work in the region covering the Serra do Garrote inflexion and the south end of the VFZ, in 1:25.000 scale, supplemented by petrographic description of thin section and geologic sections, with cooperated to the understanding of the structural evolution of the region. Data analysis allowed the identification of six deformation phases. The D1 an D2 phases generated the main foliation. The D3 phase generate kink bands folds, with NS axis and vertical axial plane. The fourth phase is responsible for generating the Vazante Fault Zone. The fifth phase produces low angle folds and shear zones, subparallel to S1//S2. The last phase generates folds with NW axis and vertical axial plane, with causes the inflection of lithologic contactas. Field observations also make possible the conclusion that the Vazante Fault Zone presents a south continuation, which is affected by deformation associated to D6 phase attributing to the trace of the VFZ a curved geometry, similar to that exhibited by lithologic contacts between units of the map

Mapeamento geológico, caracterização litoquímica e potencial econômico do corpo de cromitito de Cedrolina, Santa Terezinha de Goiás - GO

Studies of mafic-ultramafic bodies have been carried out through the years due to their great use on the interpretation of geochemical and geotectonic processes that took place in Earth's history. Amongst them, chromitites are notably recognized for being excellent indicators of their parental magma chemistry and of different geotectonic environments, as well for frequently containing associated noble metals mineralization. Thus the investigation of one of this ultramafic bodies that occurs inside the Pilar de Goiás Greenstone Belt was proposed, resulting in a detailed map of the chromitites and country rocks, as well as innumerous new data on the chemistry of chromite and associated matrix and accessory minerals. These studies were based upon geological field observations, optic and Scanning Electron Microscope (SEM), besides electron microprobe and cathodoluminescence analysis performed at the “Eugen F. Stumpfl Laboratory” of the Montanuniversität Institute of Resource Mineralogy, University of Leoben - Leoben, Austria. The chromitites are composed of 40-70% in volume of chromite (~50% on average), 14-55% of talc (~30% on average), 3-60% of chromium rich chlorite (~20% on average), traces to 4% of iron hydroxides and traces to 3% of rutile (1,5% on average). The chromite occurs as large spherical aggregates or as fine grained subhedral crystals disseminated in the matrix. This aggregates have diameters of 0.3-1.5 cm (1 cm on average) and are extremely well rounded, massive to intensively fractured, and commonly deformed to ellipsoids. When observed under the microscope, these aggregates show well rounded to slightly irregular borders, but on their interiors, these structures are represented by fine to medium grained euhedral to subhedral chromite crystals that have sharp contacts between themselves. The rock's matrix is basically made of chlorite and talc that define a metamorphic foliation (Sn), being the talc an alteration product ...

O brinquedo na educação infantil: algumas reflexões do uso do brinquedo à luz da sociedade disciplinar foucaultiana

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Área de vida e biologia reprodutiva da maria-da-restinga (Phylloscartes kronei) (Aves, Tyrannidae)

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

Os objetos lúdicos em salas de aula com crianças de ensino fundamental de 1º ao 5º ano

The playful objects challenge and support the child to the playful action. These actions leverage the use of imagination and fantasy, necessary skills throughout our life. These objects are ways to create situations and play day by day. Games and toys are also augmenting resources of learning processes in various areas of knowledge. However, this process does not occur spontaneously, there is a need of scientific knowledge for selection and use of these resources in educational formal processes, especially in schools. The objective of this study was to identify, classify and analyze the play material performance of a primary school of the Municipal System of Education from Bauru-SP. To attain the goal, became a literature review in indexed data bases and printed materials. Subsequently, based on the theoretical references, tools for collection and analysis of data were developed, enabling the triangulation of data collected and analyzed for the closest to the reality studied. The instruments for collecting and analyzing data: a) survey and identification of playful collection based on COL (KOBAYSHI, 2009), b) questionnaire with school teachers and c) field observations. The survey results and the triangulation of sources allowed better characterization of the collection available at the school and their uses as resources and education and recreation procedures

Contradições no uso de tecnologias em contexto de estágio de um curso de Letras: o professor de inglês em formação inicial no ensino superior

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

Contexto deposicional da sequência Balbuena III (Maastrichtiano/ Daniano) da formação Yacoraite na sub-bacia metán-alemania, na região de Salta, Argentina

Pós-graduação em Geologia Regional - IGCE

Recolhimento mecanizado do café em função do manejo do solo e da declividade do terreno

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Pollination of Anemopaegma album (Bignoniaceae) with focus on floral nectar as the mediator of interactions with mutualistic and antagonistic bees

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Species composition and spatial distribution of a stream fish assemblage in the east coast of Brazil: comparison of two field study methodologies

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)