996 resultados para Pernambuco Lineament


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Intraplate earthquakes in stable continental areas have been explained basically by reactivation of pre-existing zones of weakness, stress concentration, or both. Zones of weakness are usually identified as sites of the last major orogeny, provinces of recent alkaline intrusions, or stretched crust in ancient rifts. However, it is difficult to identify specific zones of weakness and intraplate fault zones are not always easily correlated with known geological features. Although Northeastern Brazil is one of the most seismically active areas in the country (magnitudes 5 roughly every 5 yr), with hypocentral depths shallower than similar to 10 km and seismic zones as long as 30-40 km, no clear relationship with the known surface geology can be usually established with confidence, and a clear identification of zones of weakness has not yet been possible. Here we present the first clear case of seismic activity occurring as reactivation of an old structure in Brazil: the Pernambuco Lineament, a major Neoproterozoic shear zone. The 2004 earthquake swarm of Belo Jardim (magnitudes up to 3.1) and the recurrent activities in the nearby towns of Sao Caetano and Caruaru (magnitudes up to 4.0 and 3.8), show that the Pernambuco Lineament is a weak zone. A local seismic network showed that the Belo Jardim swarm of 2004 November occurred by normal faulting on a North dipping, E-W oriented fault plane in close agreement with the E-W trending structures within the Pernambuco Lineament. The Belo Jardim activity was concentrated in a 1.5 km (E-W) by 2 km (downdip) fault area, and average depth of 4.5 km. The nearby Caruaru activity occurs as both strike-slip and normal faulting, also consistent with local structures of the Pernambuco Lineament. The focal mechanisms of Belo Jardim, Caruaru and S. Caetano, indicate E-W compressional and N-S extensional principal stresses. The NS extension of this stress field is larger than that predicted by numerical models such as those of Coblentz & Richardson and we propose that additional factors such as flexural stresses from the nearby Sergipe-Alagoas marginal basin could also affect the current stress field in the Pernambuco Lineament.

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The area studied forms a thin NNE-directed belt situated south of Recife town (Pernambuco state), northeastern Brazil. Geologically, it comprises the Pernambuco Basin (PB), which is limited by the Pernambuco Lineament to the north, the Maragogi high to the south and the Pernambuco Alagoas massif to the west, all of them with Precambrian age. This thesis reports the results obtained for the Cabo Magmatic Province (CMP), aiming the characterization of the geology, stratigraphy, geochronology, geochemistry and petrogenesis of the Cretaceous igneous rocks presented in the PB. The PB is composed of the Cabo Formation (rift phase) at the base (polymictic conglomerates, sandstones, shales), an intermediate unit, the Estiva Formation (marbles and argillites), and, at the top, the Algodoais Formation (monomictic conglomerates, sandstones, shales). The CMP is represented by trachytes, rhyolites, pyroclastics (ignimbrites), basalts / trachy-andesites, monzonites and alkali-feldspar granite, which occur as dykes, flows, sills, laccoliths and plugs. Field observations and well descriptions show that the majority of the magmatic rocks have intrusive contacts with the Cabo Formation, although some occurrences are also suggestive of synchronism between volcanism and siliciclastic sedimentation. 40Ar/39Ar and zircon fission tracks for the magmatic rocks indicate an average age of 102 r 1 Ma for the CMP. This age represents an expressive event in the province and is detected in all igneous dated materials. It is considered as a minimum age (Albian) for the magmatic episode and the peak of the rift phase in the PB. The 40Ar/39Ar dates are about 10-14 Ma younger than published palynologic ages for this basin. Geochemically, the CMP may be divided in two major groups; i) a transitional to alkaline suite, constituted by basalts to trachy-andesites (types with fine-grained textures and phenocrysts of sanidine and plagioclase), trachytes (porphyrytic texture, with phenocrysts of sanidine and plagioclase) and monzonites; ii) a alkaline suite, highly fractionated, acidic volcano-plutonic association, formed by four subtypes (pyroclastic flows ignimbrites, fine-to medium-grained rhyolites, a high level granite, and later rhyolites). These four types are distinguished essentially by field aspects and petrographic and textural features. Compatible versus incompatible trace element concentrations and geochemical modeling based on both major and trace elements suggest the evolution through low pressure fractional crystallization for trachytes and other acidic rocks, whereas basalts / trachy-andesites and monzonites evolved by partial melting from a mantle source. Sr and Nd isotopes reveal two distinct sources for the rocks of the CMP. Concerning the acidic ones, the high initial Sr ratios (ISr = 0.7064-1.2295) and the negative HNd (-0.43 to -3.67) indicate a crustal source with mesoproterozoic model ages (TDM from 0.92 to 1.04 Ga). On the other hand, the basic to intermediate rocks have low ISr (0.7031-0.7042) and positive HNd (+1.28 to +1.98), which requires the depleted mantle as the most probable source; their model ages are in the range 0.61-0.66 Ga. However, the light rare earth enrichment of these rocks and partial melting modeling point to an incompatible-enriched lherzolitic mantle with very low quantity of garnet (1-3%). This apparent difference between geochemical and Nd isotopes may be resolved by assuming that the metasomatizing agent did not obliterate the original isotopic characteristics of the magmas. A 2 to 5% partial melting of this mantle at approximately 14 kbar and 1269oC account very well the basalts and trachy-andesites studied. By using these pressure and temperatures estimates for the generation of the basaltic to trachy-andesitic magma, it is determined a lithospheric stretching (E) of 2.5. This E value is an appropriated estimate for the sub-crustal stretching (astenospheric or the base of the lithosphere?) region under the Pernambuco Basin, the crustal stretching probably being lower. The integration of all data obtained in this thesis permits to interpret the magmatic evolution of the PB as follows; 1st) the partial melting of a garnet-bearing lherzolite generates incompatible-enriched basaltic, trachy-andesitic and monzonitic magmas; 2nd) the underplating of these basaltic magmas at the base of the continental crust triggers the partial melting of this crust, and thus originating the acidic magmas; 3rd) concomitantly with the previous stage, trachytic magmas were produced by fractionation from a monzonitic to trachy-andesitic liquid; 4th) the emplacement of the several magmas in superficial (e.g. flows) or sub-superficial (e.g. dykes, sills, domes, laccoliths) depths was almost synchronically, at about 102 r 1 Ma, and usually crosscutting the sedimentary rocks of the Cabo Formation. The presence of garnet in the lherzolitic mantle does not agree with pressures of about 14 kbar for the generation of the basaltic magma, as calculated based on chemical parameters. This can be resolved by admitting the astenospheric uplifting under the rift, which would place deep and hot material (mantle plume?) at sub-crustal depths. The generation of the magmas and their subsequent emplacement would be coupled with the crustal rifting of the PB, the border (NNE-SSW directed) and transfer (NW-SE directed) faults serving as conduits for the magma emplacement. Based on the E parameter and the integration of 40Ar/39Ar and palynologic data it is interpreted a maximum duration of 10-14 Ma for the rift phase (Cabo Formation clastic sedimentation and basic to acidic magmatism) of the PB

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This thesis presents and discusses the results of the various seismic areas in the State of Pernambuco, with the aim of having a vision of regional seismicity and its causes. To the papers published in journals were added two new original works submitted to international journals, dealing with seismic areas located in the counties of São Caetano, Cupira, and Agrestina. All seismic areas mentioned in this thesis are located on the Pernambuco Lineament and its surroundings (both in branches or single faults within 40 km of it). The Pernambuco Lineament is a Neoproterozoic shear zone of continental-scale that deformed the Borborema Province, and presents as branches, shear zones with NE-SW direction. The new submitted papers are from the analysis of data collected by three local networks of stations that operated in the following areas: network SO07 (seismicity in the district of Santa Luzia - São Caetano, 2007), network BM10 (data from seismic areas of Serra Verde ( Cupira) and Barra do Chata (Agrestina), in 2010), network SO10 (seismicity near the urban center of São Caetano in 2010). These data were used for determining the hypocenters and focal mechanisms in order to discuss the relationship between the seismicity and geological features of the area. The new mechanisms obtained, as well as the previously published allowed the determination of the direction of the average stress in the region. The direction of stress in the region involving the various seismic areas, now or previously studied, is quite stable and approximate EW direction (SHmax). The correlation between seismicity and geological features is observed on the lineament and north of it. In the south (Cupira and Agrestina), in seismic areas nearby shear zones NE-SW, there is no correlation and seismogenic EW normal faults are active and its motion is compatible with regional stresses. It is probable that these active faults are more recent than the Neoproterozoic, probably of the Cretaceous period, when the last great movement of the Pernambuco Lineament occurred

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In this dissertation we studied the seismic activity in the São Caetano county, Pernambuco State, Northeastern Brazil, located near the Pernambuco Lineament. The Pernambuco Lineament is a one of Neoproterozoic continental-scale shear zones that deforms the Borborema province. The seismicity estudied occurred in a NE trending branch of Pernambuco Lineament. The seismic activity in São Caetano started in 2006 and in May 20th, 2006 a 4,0 mb earthquake hit there. This was the largest earthquake ever reported in Pernambuco State. This dissertation is the result of a campaign done in the period from Februay 1th 2007 to July 31 th 2007. In this campaign up to nine three-component digital seismographic stations were deployed and the collected data was used to determine hypocenters and focal mechanism. A total of 214 earthquakes, recorded at least by three stations, were analyzed. To determine hypocenters and time origin the HYPO71 program was used assuming a half-space model with parameters : VP (P-wave velocity) equal to 5.90 km/s and the ratio VP/VS 1.70, where VS is the S-wave velocity. The earthquakes hypocentral distribution was approximately 4 km long and agrees with the NE-SW direction of the Pernambuco Lineamento branch. Hypocentres depth range from 2 to 8 km. The composed focal mechanism was made from a group of 14 selected earthquakes. We try firstly to find the fault plane solution matching the polarity distribution at stations, using the FPFIT program. The result was 43 deg ± 15 deg for strike, 59 deg ± 9 deg for dip and -142 deg ± 15 deg for rake. We also fitted a plane using the hypocentral distribution to obtain the dip and azimuth of the hypocentral distribution. The results obtained by this fit were 58 deg for the azimuth, 55 deg for the dip and -155 deg for rake. This result shows a mechanism of a strike-slip dextral fault with a normal component. This dissertation shows, once more, that there is a good correlation between the seismic activity and geological features in the region near the Pernambuco Lineament and its NE branches

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OBJECTIVE: To characterize the behavior of premature newborns in the first year of chronological age. METHODS: This is a cross-sectional descriptive study, bound to a longitudinal study titled: Comparison of visual behavior on the first quarter of year of life of premature nursling born at two maternities of Recife/PE. The sample was composed by 52 premature newborns selected from June, 2007 to June, 2008 from the Maternity of the Federal University of Pernambuco (UFPE). Biological, socioeconomic and demographic data was collected through medical records and interviews with progeny. Newborns were evaluated by the Assessment Guide of Visual Ability in Infants. RESULTS: Most of the newborns were male at a gestational period between 33 weeks and 36 weeks and 6 days, showed a good visual behavior development for the age researched, and most of the families showed good socioeconomical and demographic profile. Besides, it was possible to detect ocular signs in 19% of sample, that were referred to an Ophthalmology Service. CONCLUSION: This study results point out the method like an important key in the early detection and visual screening for premature nursling since the first month of life and it led us to believe that clinical view for occupational therapy intervention must be focused not only on biological risks but also at the influence environment in newborn performance.

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The karyotype of Amphisbaena ridleyi, an endemic species of the archipelago of Fernando de Noronha, in State of Pernambuco, Brazil, is described after conventional staining, Ag-NOR impregnation and fluorescence in situ hybridization (FISH) with a telomeric probe. The diploid number is 46, with nine pairs of macrochromosomes (three metacentrics, four subtelocentrics and two acrocentrics) and 14 pairs of microchromosomes. The Ag-NOR is located in the telomeric region of the long arm of metacentric chromosome 2 and FISH revealed signals only in the telomeric region of all chromosomes. Further cytogenetic data on other amphisbaenians as well as a robust phylogenetic hypothesis of this clade is needed in order to understand the evolutionary changes on amphisbaenian karyotypes.

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Considerando a importância do Sistema de Informações sobre Orçamentos Públicos em Saúde (SIOPS) como ferramenta para o planejamento, gestão e controle social dos gastos públicos em saúde, este trabalho teve como objetivo avaliar a relação entre a regularidade na alimentação do SIOPS e o conhecimento e uso do Sistema pelos gestores municipais do Estado de Pernambuco, Brasil. Foram selecionados dez municípios distribuídos nas cinco mesorregiões do estado, sendo cinco regulares e cinco irregulares na alimentação do Sistema, e aplicada uma entrevista semi-estruturada entre os secretários de saúde dos respectivos municípios. Com base na análise dos dados, foi identificado que o domínio de informática e o conhecimento do Sistema não interferem na regularidade da alimentação, em função do distanciamento entre os gestores das Secretarias de Saúde e o SIOPS, em geral alimentado por serviços terceirizados. Constata-se que as informações geradas não têm sido exploradas potencialmente pelos gestores enquanto instrumento de gestão.

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The aim of this article is to discuss conexions between Pernambuco and Rio de la Plata around the year 1817. In a more general sense, it offers a large pattern of comprehension of the indepdendences of Luso and Spanish America in terms of its mutual relationships.

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Sera from 269 rodents obtained during the routine surveillance operations in plague areas of Rio de Janeiro and Pernambuco states, Brazil were tested by ELISA for specific IgG antibodies against a recombinant nucleocapsid (N) protein of Araraquara hantavirus. ELISA-positive sera were submitted to reverse transcriptase-polymerase chain reaction (RT-PCR) for amplification of the virus genome and later sequencing for identification of the viral variant. The samples from the state of Pernambuco were antibody negative, and although four from Rio de Janeiro were ELISA-positive, they failed to yield viral cDNA by RT-PCR. This is the first report of the presence of antibodies to a hantavirus among rodents from Rio de Janeiro and suggests the possibility of human cases of hantavirus pulmonary syndrome (HPS) in that state, although no case has yet been reported. (C) 2008 Elsevier B.V. All rights reserved.

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A partir de 1998, teve in??cio, na Secretaria da Fazenda do Estado de Pernambuco, o Programa de Moderniza????o Fazend??ria (Promofaz), que promoveu diversas mudan??as organizacionais, concentrando esfor??os em projetos estruturadores, incluindo investimentos no planejamento de tecnologia da informa????o (TI). Dentre os projetos de TI, destacou-se a elabora????o das arquiteturas de sistemas e tecnol??gicas. Neste trabalho, foi realizada uma revis??o dos processos organizacionais da moderniza????o fazend??ria, abrangendo aspectos de cultura, mudan??a e aprendizagem organizacionais, confrontados com referenciais hist??ricos e te??ricos, e maior enfoque na ??rea de tecnologia da informa????o. Apesar das dificuldades, o processo de informatiza????o tem provocado fortes impactos nos componentes culturais da institui????o. Sem a utiliza????o da tecnologia da informa????o como ferramenta, provavelmente n??o se implantariam os novos modelos de gest??o adotados pela Sefaz, mas se observou que a tecnologia, sozinha, n??o faz o milagre da mudan??a, sendo necess??rio todo um conjunto de esfor??os e um trabalho paralelo com outros fatores de mudan??a.

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O acesso universal e igualitário às ações e serviços públicos garantido através da Constituição de 1988 tornou mais acessível o diagnóstico precoce da deficiência auditiva. Desta forma, por meio do Sistema Único de Saúde (SUS), prestadores públicos e privados de serviços proporcionam essa cobertura a toda população, nos diferentes níveis de complexidade. OBJETIVO: O trabalho tem como objetivo estudar a oferta de serviços de diagnóstico da Deficiência Auditiva na média complexidade em Pernambuco no 1º semestre de 2003. MATERIAL E MÉTODO: Através de um estudo de séries foram analisados 17669 procedimentos e 372 profissionais da área de diagnóstico da deficiência auditiva nos 185 municípios do estado de Pernambuco, dados retirados do Sistema de Informação Ambulatorial do Ministério da Saúde. RESULTADOS: Os resultados mostraram que os procedimentos estão sendo realizados em apenas cinco municípios, a maioria em unidades geridas pela esfera municipal. Também, identificou-se uma distribuição não-eqüitativa da oferta dos procedimentos de diagnóstico. CONCLUSÃO: Concluiu-se que muito ainda precisa ser feito para que o acesso e oferta do diagnóstico da deficiência auditiva ocorram de forma horizontal, respeitando as diferenças da comunidade através de um modelo universal, integrativo e eficiente como propõe o Sistema Único de Saúde.

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A laringe é considerada o sítio de maior ocorrência de neoplasias na região de cabeça e pescoço, e para os estudos do câncer a mortalidade constitui-se um dos indicadores de saúde mais confiáveis OBJETIVO: Estudar a mortalidade por câncer de laringe em Pernambuco no período 2000-2004. FORMA DE ESTUDO: Estudo de coorte contemporânea com corte transversal. MATERIAL E MÉTODOS: Considerou-se o universo dos óbitos por câncer de laringe, em residentes do estado de Pernambuco entre 2000 e 2004, extraídos do Sistema de Informações sobre Mortalidade (SIM/SUS). A análise dos dados foi realizada através de estatística descritiva com resultados expressos em tabelas, gráficos e mapa, utilizando o software Excel versão 2000 e o software EpiInfo, versão 6.04b. RESULTADOS: Existiu pouca variação do coeficiente de mortalidade entre os anos estudados. A mesorregião do Sertão concentrou o agregado com o maior número de óbitos e Fernando de Noronha apresentou a maior taxa de mortalidade. O perfil encontrado foi de homens entre 60-69 anos, pardos, casados, com baixo grau de escolaridade, cujo óbito aconteceu em ambiente hospitalar. CONCLUSÃO: Ocorreu estabilidade da mortalidade e heterogeneidade entre os municípios. O perfil da mortalidade segundo variáveis sociais corrobora com outros estados brasileiros, exceto pela raça/cor.

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Neste artigo procura-se associar os estudos teóricos relacionados à temática centro-periferia, multi-level governance, federalismo cooperativo e positive and negative integration à realidade empírica das unidades subnacionais no seio do Mercosul. São ainda efetuadas pesquisas de campo junto a atores políticos e representações de agentes econômicos a fim de privilegiar fontes primárias de informação e desta forma analisar comparativamente os impactos do Mercado Comum do Sul na economia política dos estados de Pernambuco, Bahia, São Paulo e Rio Grande do Sul, assim como em suas respectivas capitais.

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Em Pernambuco, a disponibilidade de P é avaliada sem se considerarem características físicas, químicas, ou, mineralógicas dos solos. Este trabalho teve como objetivos determinar os níveis críticos de P em diferentes solos, utilizando-se diferentes extratores químicos, considerando-se a quantidade e a qualidade da fração argila e relacionar as características físicas, químicas e mineralógicas dos solos com os níveis críticos de P. Os solos foram classificados como: Argissolo Amarelo distrocoeso (PAdx); Latossolo Amarelo distrófico (LAd); Argissolo Amarelo distrófico (PAd); Gleissolo háplico eutrófico (GXve) e Espodossolo cárbico duripânico (EKo). Os tratamentos consistiram em sete doses de P, determinadas de acordo com a capacidade máxima de adsorção de P (CMAP). O delineamento experimental foi em blocos ao acaso, com quatro repetições. Foram coletadas amostras de solo na área útil das parcelas. Essa amostragem foi realizada 30 dias após o plantio e aplicação das doses de P, numa profundidade de 0,0-0,2 m. Nessas amostras, determinaram-se o teor de P pelos extratores Mehlich-1, Mehlich-3, Bray-1 e Resina de Troca Iônica (RTA). Com os teores de P no solo e a produção agrícola, determinaram-se os níveis críticos de P no solo. A RTA extraiu mais P independentemente do tipo de solo. Os níveis críticos de P no solo foram dependentes da CMAP, da quantidade de argila e do P remanescente (P-rem), quando o extrator para avaliação do P disponível foi o Mehlich-1. Os níveis críticos no solo determinados pela RTA não foram dependentes de nenhuma característica química e, ou, física dos solos.

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As diferentes respostas dos genótipos de cana-de-açúcar (Saccharum spp.), em relação à produtividade, quando submetidos a mudanças nos diferentes ciclos de colheita, representam problema para os agricultores e grande desafio para os melhoristas, sendo de interesse comum a identificação e obtenção de variedades que apresentem como características alta produtividade agroindustrial, ampla estabilidade, longevidade e excelente viabilidade econômica em sua exploração comercial. Objetivou-se, com este trabalho, avaliar o desempenho agroindustrial de 11 clones e 15 variedades de cana-de-açúcar, na microrregião canavieira da Zona Centro de Pernambuco, considerando-se os cultivos de cana planta, soca e ressoca, e eleger os genótipos mais produtivos. O experimento foi conduzido na área agrícola da Usina Petribú, município de Lagoa de Itaenga. Utilizou-se o delineamento experimental de blocos casualizados, com quatro repetições. Foram avaliadas as variáveis toneladas de pol por hectare (TPH), toneladas de cana por hectare (TCH), fibra (FIB), pol % corrigida (PCC), pureza (PZA), teor de sólidos solúveis (BRIX) e açúcar total recuperável (ATR). Pela análise de variância, foram detectadas diferenças significativas entre os genótipos, indicando variabilidade genética. A alta estimativa da herdabilidade média para a variável TCH indicou elevada possibilidade de êxito na seleção, baseando-se neste importante componente de produção. Por meio da análise econômica, constata-se que as variedades RB92579 e RB93509 apresentam melhor desempenho para colheita no início da safra.