961 resultados para Petrologia - Amazonas


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AIM: The aim of this survey was to assess the prevalence of AC in riverine population in countryside of Amazonas, northern Brazil. MATERIAL AND METHODS: Patients answered a questionnaire and were examined between January and December of 2008. Data were gathered on the following participant’s characteristics: 1) age group; 2) gender; 3) ethnicity 4) outdoor activities (sunlight exposure); 5) smoking habits; 6) drinking habits; and 7) access to oral health services (the last dental visit). Clinical observation of the lips for determination of AC presence was used. Patients who presented clinical manifestation of moderate and severe AC were submitted to incisional biopsy to confirm the diagnosis. In case of a positive result after histopathological examination, patients were advised and appropriate treatment was offered. All patients received information about AC and its'prevention. RESULTS: Among the 200 participants that were examined, the prevalence of AC was 2% (4 cases). Of all patients surveyed, women were the majority totalizing 124 patients (72.0%). According to age, 48 (24.0%) people were 20g34 yeargold; 42 (21.0%) were 35g44gyeargold; 50 (25.0%) were 45g60gyeargold; and 60 (30.0%) were 61 or older. CONCLUSION: Even though AC was present in a low prevalence rate, an epidemiological variety is expected, once geographic and ethnic differences should be considered.

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This work deals with the historical survey of the class for the Devonian layers, general characteristics of the group and taphonomic preservation standards associated with the group. It was analyzed specimens of scientific collections from brazilian museums and universities. The taxonomic group is represented by four genera in the basins of Parana, Parnaiba and Amazon: Tentaculites, Homoctenus, Styliolina and Volynites. The tentaculitids occur from Ordovician to the Devonian, having its peak in the Middle Devonian. The class has three known orders: Tentaculitida, animals of benthic habit, Homoctenida and Dacryoconarida, animals of habit planktonic. It was also noticed the presence of two patterns of taphonomic conservation: isolated and grouped specimens.

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Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

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The region Indiara (GO) is located in southwestern of São Francisco Craton in the Internal Zone of the Brasília Belt, western part of the Tocantins Province. In this locality outcrop rocks of the Goiás Magmatic Arc. These rocks are muscovite gneiss with biotite, muscovite-biotite gneiss, biotite gneiss with muscovite and garnet, biotite-muscovite gneiss, muscovite porfiroclastic gneiss, biotite porfiroclastic gneiss, muscovite-quartz schists, garnetquartz schists, and metamafic rock (hornblende schists) as metric or kilometric lenses. The gneisses have granodioritic composition, granoblastic texture, with some portions with lepidoblastic texture, constituting a discontinuous centimeter to millimeter banding; the structure is anisotropic, marked by the preferred orientation of all the minerals. These gneisses are leucocratic, generally are inequigranular and fine to medium grained. The hornblende schists have nematoblastic texture, are inequigranular and fine to medium grained and have anisotropic structure that is given by a foliation, marked by a strong preferential orientation of the crystals of amphibole and other minerals present in the rock. The gneisses of the area are composed of plagioclase (oligoclase/andesine), quartz, microcline, muscovite, biotite, epidote, apatite, zircon, garnet, kyanite, oxides and hydroxides of iron and opaque minerals. And the metamafic rocks of Indiara region are composed mainly of amphibole, plagioclase (oligoclase/andesine), quartz, titanite, biotite, allanite, garnet, oxides and hydroxides of iron, apatite, epidote, rutile, muscovite and opaque minerals. At least three phases of deformation were observed in the rocks of area of study (Dn-1, Dn and Dn +1). The Dn phase and represented by a well-marked foliation Sn having low dip angle (average dip of 20 °) and dip direction to SW (210/21) and to NE (18/20); the Dn-1 phase is represented by a compositional banding (Sn- 1), this banding is generally...

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The towns of Castro Alves and Rafael Jambeiro, central-east of Bahia state, are located in the east of São Francisco Craton, in granulite terrains of Salvador-Curaçá Belt, formed in Paleoproterozoic. The region of study contains ortognaisses of Caraíba Complex, metamafic and metaultramafic rocks of São José do Jacuípe Suite, metasedimentary rocks of Tanque Novo-Ipirá Complex, granitoids, pegmatites and alkaline rocks. The study carried out regional and detailed geological mapping in addition to petrographical and geochemical characterization of six areas in the search for targets of feldspar and white diopside, minerals used in ceramic industry. The areas consist of granitic ortognaisses interspersed with lenses of mafic granulite rocks, calc-silicate rock, banded iron formations, paragnaisses, quartzites, and bodies of quartz-feldspar or feldspar pegmatites and alkaline rocks that fill discontinuities. The region of study contains four deformations phases, with a predominance of ductile structures. The foliation Sn has N30E to N70W direction, high angle of dip and is characterized by compositional banding of granoblastic and felsic bands interspersed with nematoblastic or lepidoblastic mafic bands. A mineral or stretching lineation Ln is associated with Sn and has trend of S55E to S72E. The rocks have been suffered a regional metamorphism with granulite facies peak and partial retrogression to greenschist facies. Geochemical studies indicate that the green coloring calc-silicate rocks have lower SiO2, MgO and higher Fe2O3 content compared with white calcssilicate rocks. The alkaline rocks of the studied area have higher Na2O, SiO2 and lower K2O, Fe2O3 content compared with others Paleoproterozoic alkaline rocks of Bahia state. The targets of diopside are associated with white calc-silicate rocks, while the targets of feldspar are associated with paragnaisses, pegmatites and alkaline rocks

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

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Lentinus strigosus (Schwein.) Fr. is an exploitable edible mushroom occurring in the Brazilian Amazon, being part of a huge diversity of edible mushrooms which are little grown. The use of regional waste is recommended to reduce production costs of any kind of edible mushroom. Thus, the mycelial growth of L. strigosus in culture media based on regional wood waste extract by using substrates based on Protium puncticulatum, Cariniana micrantha and Caryocar glabum sawdust, supplemented with 20% of wheat bran (Triticum aestivum), corn bran (Zea sp.) or rice bran (Oryza sp.) was observed. Eucalyptus (Eucaliptus sp.) sawdust was used for comparison with the other wood wastes because it is commonly used in the cultivation of edible fungi. The experimental design employed was totally randomized, in 4 x 3 factorial scheme (sawdust x bran), adding up 12 treatments with 5 repetitions, being that each repetition corresponded to a Petri dish, totalizing 60 dishes, incubated at 35 ºC. The diameter of the colony was daily evaluated until the fungus reached the borders of the Petri dish in one of the treatments. After that period, the media based on P. puncticulatum sawdust obtained thebest results of mycelial growth, showing potential to be used as an alternative residuein a future production of L. strigosus in the state of Amazonas.

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Pós-graduação em Geociências e Meio Ambiente - IGCE

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O presente estudo visa demonstrar a utilização do diário de campo em pesquisas realizadas em contexto natural sob a perspectiva do modelo bioecológico de Bronfenbrenner. Para efeito de ilustração, são apresentados dados que fizeram parte da pesquisa de mestrado da primeira autora sobre as percepções de uma família com uma criança com deficiência intelectual no contexto ribeirinho amazônico. Após a coleta das informações, os dados foram organizados com base nos conceitos propostos por Bronfenbrenner. O diário de campo permitiu o aprofundamento das análises em que foram contemplados tanto os aspectos contextuais (cultura ribeirinha amazônica), como os pessoais (características biossociopsicológicas da criança/pais) e os processuais (relações, papéis familiares e atividades compartilhadas). Os dados são discutidos considerando a contribuição do diário de campo nas pesquisas que investigam famílias em seu contexto.