Tocantins Province
Mostrando 1-11 de 11 artigos, teses e dissertações.
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1. Lugar de escola e "Lugar de Fronteira": a instrução primária em Boa Vista do Tocantins em Goiás no século (1850 - 1896) / Schools place and frontiers place: the primary instruction in Boa Vista of Tocantins, in Goiás, in the 19th century (1850-1896).
A presente tese, vinculada à linha de pesquisa Estado e Políticas Educacionais do Programa de Pós-Graduação em Educação da UFG, buscou tratar do percurso histórico da instrução primária em Boa Vista do Tocantins, atual cidade de Tocantinópolis, norte do Tocantins, no período de 1850 a 1896. A análise versou pelo entendimento ao processo de cria
IBICT - Instituto Brasileiro de Informação em Ciência e Tecnologia. Publicado em: 12/06/2011
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2. Lugar de escola e "Lugar de Fronteira": a instrução primária em Boa Vista do Tocantins em Goiás no século (1850 - 1896) / Schools place and frontiers place: the primary instruction in Boa Vista of Tocantins, in Goiás, in the 19th century (1850-1896).
A presente tese, vinculada à linha de pesquisa Estado e Políticas Educacionais do Programa de Pós-Graduação em Educação da UFG, buscou tratar do percurso histórico da instrução primária em Boa Vista do Tocantins, atual cidade de Tocantinópolis, norte do Tocantins, no período de 1850 a 1896. A análise versou pelo entendimento ao processo de cria
IBICT - Instituto Brasileiro de Informação em Ciência e Tecnologia. Publicado em: 12/06/2011
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3. A influência da vegetação sobre o clima urbano de Palmas-TO / The influence of vegetation on urban climate of Palmas-TO
This study addresses the issue of urban climate. It is based on the assumption that vegetation may act to improve the microclimate conditions of cities, by reducing the temperature of the air, which is very important in warm climates. Aims to investigate the influence of vegetation on urban climate in Palmas, capital of the province of Tocantins. It was base
Publicado em: 2009
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4. Características epigenéticas do depósito de cu-au chapada, arco magmático de goiás
The Cu-Au Chapada deposit is located from 8km of Alto Horizonte-GO. The geologic picture is dominated by metavulcanic sedimentary sequences that integrate the Neoproterozoic Magmatic Arc of Mara Rosa, located in the central portion of the Tocantins Province. The framework of the deposit is represented by an antiform whose core is composed by association of t
Publicado em: 2009
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5. Geoquímica de rocha total, geocronologia de u-pb e geologia isotópica de sm-nd das rochas ortognáissicas e unidades litológicas associadas da região ipameri - Catalão (Goiás)
The part of the southern Brasília Belt, Tocantins Province, exposed in central Brazil, comprises metasedimentary rocks, metavolcano-sedimentary sequences, amphibolites and intrusive granites, and a large orthogneiss belt. These units are tectonically imbricated, and vary in metamorphic grade from lower greenschist to amphibolite facies, characterized by a 7
Publicado em: 2008
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6. Seismic tomography with P- and S-waves for the study of the upper mantle in Brazil / Tomografia sísmica com ondas P e S para o estudo do manto superior no Brasil
We used travel time seismic tomography to study the upper mantle beneath SE and Central Brazil. This method is based on the inversion of P- and S-wave relative travel time residuals (VanDecar, 1991) obtained from more than 80 stations in an area of 20 x 20 degrees. More than 11000 P and PKP residuals, and more than 8000 S, ScS, SKS, and SKKS residuals were o
Publicado em: 2008
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7. Phylogenetic Systematic of Tribu Neotropical Optatini Champion, 1907 (Coleoptera, Curculionidae, Baridinae). / SISTEMÁTICA FILOGENÉTICA DA TRIBO NEOTROPICAL OPTATINI CHAMPION, 1907 (COLEOPTERA, CURCULIONIDAE, BARIDINAE)
The tribu Optatini Champion, 1907 is composed of small to large-sized (2,3- 18,3 mm) weevils beetles, characterized by to have: rhomboidal or suboval body, covered with scales variegated, nearly everywhere of the body or forming points and spots; the mandibles toothed on the their inner edge; the prostern generally strongly grooved down the middle, and with
Publicado em: 2007
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8. "Crustal structure of central sector of Tocantins Province by using P and S waves as well as reflected phases with deep seismic refraction data" / "Estrutura crustal do setor central da província Tocantins utilizando ondas p, s e fases refletidas com dados de refração sísmica profunda"
Esta pesquisa está baseada na execução de duas linhas de refração sísmica profunda de 300 km de extensão (L1-Porangatu e L2-Cavalcante) atravessando de oeste para leste o setor central da Província Tocantins, utilizando em cada linha 120 sismógrafos digitais e explosões com tempo controlado e cargas entre 500 e 1000 kg de explosivos a cada 50 km; f
Publicado em: 2006
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9. Razão de Poisson da crosta superior da região de Porangatu, Goiás, Província Tocantins: um estudo por refração sísmica
This work presents a refined seismic model of compressional waves (Vp) showing the distribution of Poisson ratio along the upper crust of central Tocantins Province, central Brazil, based on two dimensional modelling of the Porangatu seismic refraction data. The Porangatu seismic line begins in the Araguaia Belt (FXA) and continues through the western portio
Publicado em: 2006
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10. "Estudo geológico-geocronológico dos terrenos granito-gnáissicos e sequências metavulcanossedimentares da Região do Betara (PR)" / "Geologic-geochronologic study from the granite-gnaissic terranes and metavolcanossedimentary sequences from Betara Region (PR)"
The Betara region was located at nothwest of the Curitiba City between the Campo Largo and Rio Branco do Sul municipal districts. This region includes granite-gnaissic rocks, proto to milonitics (Betara Nucleous) and metavolcanossedimentary sequences with low to intermediate metamorphic grade (Betara Formation). These terrains occur at the southern portion o
Publicado em: 2006
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11. Refração Sísmica Profunda no Setor Sudeste da Província Tocantins / Deep Seismic Refraction on Southestearn Sector of the Tocantins Province
This work to fulfil the degree of Master of Sciences is inserted among the deep seismic refraction studies of the Thematic Project Geophysical Studies and Tectonic Model of the Tocantins Province Central and Southeast Sectors, Central Brazil . Three refraction lines, of around 300 km long each, were deployed, two of them in the Central sector and the other i
Publicado em: 2000