Post-collisional Neogene magmatism of the Mediterranean Maghreb margin: a consequence of slab breakoff

A 1 200 km-long linear magmatic belt extends along the Mediterranean coast the Maghreb from Eastern Tunisia to Morocco. This belt is mainly composed of Langan calc-alkaline metaluminous to peraluminous granitoids and associated andesites/cites Central and Eastern Algeria. In Tunisia and Oranie/Western Morocco, calc alkaline activity started later (during the Serravallian) and was followed by the placement of alkali basalts and basanites since the Tortonian to the Pliocene and, in me places, the Pleistocene. Available data on the tectonic setting, petrology, age and biochemistry of this belt show that most of its striking features, e.g. (1) very low magma production rate, subduction-related geochemical imprint, extensive crustal contamination the calc-alkaline magmatism and (2) progressive magmatic change from calc-alkaline alkaline, are consistent with magma generation during a slab breakoff process as proposed Carminati et al, in 1998. The magmatism associated with this breakoff started in Central Eastern Algeria at 16 Ma, then propagated eastwards and westwards, The upward of asthenospheric enriched plume-type mantle through the tear in the downgoing first triggered melting of the overlying lithospheric mantle which had been metasomatised during a previous subduction period. Heat supply from this uprising asthenosphere may have warmed up the continental crust and made its involvement in assimilation processes easier. As the asthenosphere ascended through the `window' in the slab, partial melting occurred at the uprising boundary between asthenosphere and lithosphere, generating basalts with transitional characteristics between those of calc-alkaline and alkaline basalts. As the asthhenospheric upwelling proceeded partial:melting then occurred in the sole asthenospheric mantle, producing alkali basalts. (C) 2000 Academie des sciences Editions scientifiques et medicales Elsevier SAS.

Geological setting of the Guelb Moghrein Fe oxide-Cu-Au-Co mineralization, Akjoujt area, Mauritania

The Guelb Moghrein Fe oxide-Cu-Au-Co deposit is located at the western boundary of the West African craton in NW Mauritania. The wall rocks to the mineralization represent a meta-volcanosedimentary succession typical of Archaean greenstone belts. Two types of meta-volcanic rocks are distinguished: (1) volcanoclastic rocks of rhyodacite-dacite composition (Sainte Barbe volcanic unit), which form the stratigraphic base; (2) tholeiitic andesites-basalts (Akjoujt meta-basalt unit). The trace element signature of both types is characteristic of a volcanic arc setting. A small meta-pelitic division belongs to the Sainte Barbe volcanic unit. A meta-carbonate body, which contains the mineralization, forms a tectonic lens in the Akjoujt meta-basalt unit. It can be defined by the high X(mg) (=36) of Fe-Mg carbonate, the REE pattern and the delta(13)C values of -18 to -17 parts per thousand as a marine precipitate similar to Archaean banded iron formation (BIF). Additionally, small slices of Fe-Mg clinoamphibole-chlorite schist in the meta-carbonate show characteristics of marine shale. This assemblage, therefore, does not represent an alteration product, but represents an iron formation unit deposited on a continental shelf, which probably belongs to the Lembeitih Formation. The hydrothermal mineralization at 2492 Ma was contemporaneous with regional D(2) thrusting of the Sainte Barbe volcanic unit and imbrications of the meta-carbonate in the upper greenschist facies. This resulted in the formation of an ore breccia in the meta-carbonate, which is enriched in Fe, Ni, Co, Cu, Bi, Mo, As and Au. Massive sulphide ore breccia contains up to 20 wt% Cu. The ore fluid was aqueous-carbonic in nature and either changed its composition from a Mg-rich oxidizing to an Fe-rich reducing fluid or the two fluid types mixed at the trap site. All lithologies at Guelb Moghrein were deformed by D(3) thrusting to the east in the lower greenschist facies. The mobility of REE in the retrogressed rocks explains the formation of a second generation of hydrothermal monazite, which was dated at c. 1742 Ma. Archaean rocks of the West African craton extend to the west to Guelb Moghrein. The active continental margin was deformed and mineralized in the Late Archaean-Early Proterozoic and again reactivated in the Mid-Proterozoic and Westphalian, showing that the western boundary of the craton was reactivated several times.

Social perceptions of floods and flood management in a Mediterranean area (Costa Brava, Spain)

Taking as an example three study cases in the Costa Brava area, this paper examines the social perceptionof floods through surveys, interviews and Focus Group sessions. Perception is then related to vulnerability, flood management, and citizen’s preferences regarding alternatives to curb flood losses in the future. The study concludes that flood awareness and the willingness to take actions regarding this hazard are clearly related to the degree of social involvement with the affairs of the local community. Furthermore, participatory settings such as Focus Group sessions appear to enable a better environment for assessing and implementing flood management options that attempt to modify human activities rather than modify natural processes as has been frequently the case in the past

Trabalhar com famílias no Programa de Saúde da Família: a prática do enfermeiro em Maringá-Paraná

O Programa de Saúde da Família (PSF) propõe-se a atender a família integralmente em seu espaço social o que requer uma nova postura profissional. Este estudo tem como objetivo conhecer a prática do trabalho realizado com famílias pelos enfermeiros que atuam no PSF em Maringá, Paraná. Foi realizado um estudo descritivo exploratório com abordagem qualitativa, utilizando, para a coleta de dados, entrevistas, observação e análise documental. Os dados foram analisados, segundo o referencial teórico de Bardin. Os resultados revelaram três categorias: atividades com indivíduos, atividades na comunidade e atividades no domicílio. Concluiu-se que, apesar de os enfermeiros considerarem a família em seu espaço domiciliar, por meio de visitas domiciliares, de coleta de dados e da educação em saúde, ainda centralizam a doença e o indivíduo, e a sua postura não tem estimulado a participação e a autonomia das famílias no que se refere à assistência e ao serviço.

Óbitos infantis investigados pelo Comitê de Prevenção da Mortalidade Infantil em região do Estado do Paraná

Este estudo teve como objetivo analisar óbitos infantis na 15ª Regional de Saúde do Paraná utilizando o resultado das investigações do Comitê de Prevenção da Mortalidade Infantil. Trata-se de um estudo descritivo exploratório, a partir do Sistema de Investigação de Mortalidade Infantil e Sistema de Informações sobre Nascidos Vivos no período de 2000 a 2006. O coeficiente de mortalidade infantil diminuiu de 13,2% para 11,6%. Dos 799 óbitos, o Comitê investigou 74,5%; destes, 56,5% no período neonatal precoce. As afecções originadas no período perinatal e as malformações congênitas foram causas principais de óbito. Foram considerados reduzíveis 70,1% dos óbitos. A redutibilidade foi maior para óbitos de mães adolescentes, recém-nascidos ≥ 2500g, parto normal, raça/cor preta, parda e indígena e mães sem consulta de pré-natal. As análises dos óbitos devem ser efetuadas mais próximas das equipes de saúde da família, que conhecem as gestantes para aprimoramento do trabalho e qualidade nas análises do Comitê.

Perfil das parturientes e seus recém-nascidos atendidos em um hospital-escola do Noroeste do Estado do Paraná

O estudo teve como objetivo traçar o perfil de parturientes e seus recém-nascidos atendidos em um hospital-escola, a partir do Sistema de Informações sobre Nascidos Vivos - SINASC. Para isso, foi realizado um estudo descritivo exploratório que identificou as características de todas parturientes e seus recém-nascidos atendidos no Hospital Universitário de Maringá - HUM no ano de 2006. Observou-se que 27,1% das parturientes eram adolescentes, 68,4% não tinham companheiro, 59,3% residiam fora de Maringá, 63,6% realizaram sete ou mais consultas de pré-natal. A proporção de parto cesárea foi de 50,4%. Os recém-nascidos, em sua maioria, apresentaram boa vitalidade ao nascer, embora 25,5% eram pré-termos e 23,6% baixo peso ao nascer. Com os resultados, foi possível traçar o perfil das parturientes e seus recém-nascidos atendidos no HUM, demonstrar a possibilidade de utilização do SINASC como um dos instrumentos de avaliação em saúde em unidade terciária e propor intervenções capazes de prevenir a morbimortalidade materno-infantil.

Perfil dos idosos que sofreram trauma em Londrina - Paraná

O objetivo foi caracterizar os idosos que sofreram trauma e foram internados nos três hospitais terciários, da cidade de Londrina - Paraná. Pesquisa quantitativa através de um estudo observacional, transversal, com 121 idosos de 60 a 74 anos e seus cuidadores, realizada durante um período de seis meses, por meio de entrevistas e visita domiciliar. Os resultados evidenciaram que a maioria dos idosos era do sexo masculino, com média de idade de 67,7 anos. Os traumas sofridos foram: 62,0% quedas, 25,6% acidentes de transporte e 10,4% outras causas. Como conseqüência ao trauma houveram de uma a três lesões, e 11 idosos (9,1%), foram a óbito. A queda foi a principal causa de trauma, a qual pode ser evitada observando os fatores intrínsecos e os extrínsecos que a predispõem, com o intuito de estabelecer estratégias de prevenção desse tipo de trauma.

Y-chromosome diversity in native mexicans reveals continental transition of genetic structure in the Americas

The genetic characterization of Native Mexicans is important to understand multiethnic based features influencing the medical genetics of present Mexican populations, as well as to the reconstruct the peopling of the Americas. We describe the Y-chromosome genetic diversity of 197 Native Mexicans from 11 populations and 1,044 individuals from 44 Native American populations after combining with publicly available data. We found extensive heterogeneity among Native Mexican populations and ample segregation of Q-M242* (46%) and Q-M3 (54%) haplogroups within Mexico. The northernmost sampled populations falling outside Mesoamerica (Pima and Tarahumara) showed a clear differentiation with respect to the other populations, which is in agreement with previous results from mtDNA lineages. However, our results point toward a complex genetic makeup of Native Mexicans whose maternal and paternal lineages reveal different narratives of their population history, with sex-biased continental contributions and different admixture proportions. At a continental scale, we found that Arctic populations and the northernmost groups from North America cluster together, but we did not find a clear differentiation within Mesoamerica and the rest of the continent, which coupled with the fact that the majority of individuals from Central and South American samples are restricted to the Q-M3 branch, supports the notion that most Native Americans from Mesoamerica southwards are descendants from a single wave of migration. This observation is compatible with the idea that present day Mexico might have constituted an area of transition in the diversification of paternal lineages during the colonization of the Americas.

Qualidade do Sistema de Informações de Nascidos Vivos no estado do Paraná, 2000 a 2005

Analisou-se a qualidade do Sistema de Informações de Nascidos Vivos no Estado do Paraná, de 2000 a 2005, por meio do percentual de não declaração das variáveis, utilizando banco de dados cedido pela Secretaria de Saúde de Estado. Utilizou-se a seguinte escala: excelente, percentual de não declaração < 1%; boa de 1% a 2,99%; regular de 3% a 6,99% e ruim > 7%. A qualidade do preenchimento do SINASC no Paraná foi excelente, principalmente a partir de 2003. A ocupação da mãe, classificada como regular e ruim, foi a variável de menor qualidade em todas as Macro-Regionais de Saúde. Filhos nascidos vivos, nascidos mortos e raça/cor, oscilaram de ruim a excelente qualidade. É necessário melhorar a qualidade das variáveis estado civil e número de filhos nascidos mortos em todas as Macro-Regionais de Saúde. A excelência do SINASC demonstrou a sua potencialidade como fonte de informação da saúde no Paraná.

The Carboniferous Baralacha La basaltic dykes (Upper Lahul, Ladakh): remnants of an early rifting event along the Indian northern plate

The Lower Carboniferous Baralacha La basaltic dykes were emplaced along transtensional faults. The basalts exhibit tholeiitic and alkaline affinities. The tholeiites are TiO2-poor, moderately enriched in light rare earth (LREE), and display Nb and Ta negative and Th positive anomalies. The alkali basalts, compared to the tholeiites, have higher TiO2, rare earth and highly incompatible trace element contents and greater LREE enrichments. The Nd and Pb isotope compositions of the Baralacha La basalts suggest that they derive from the partial melting of an enriched OIB mantle source. characterized by a HIMU component, and contaminated by the lower continental crust. The Baralacha La dyke swarm represent the remnants of an early rifting event on the northern Indian passive margin.

Dissertações produzidas no Programa de Pós-Graduação e Mestrado em Enfermagem da Universidade Federal do Paraná

Trata-se de estudo descritivo, retrospectivo e documental com objetivo de analisar as dissertações produzidas pelo Curso de Mestrado em Enfermagem do Programa de Pós-Graduação em Enfermagem da Universidade Federal do Paraná, considerando o ajustamento de suas linhas de pesquisa. Para tanto foi realizada leitura crítica dos resumos e análise da temática das dissertações e da inserção na linha de pesquisa, bem como de métodos, abordagens, sujeitos, local, instrumentos e técnicas de pesquisa. Foram analisados 64 resumos de dissertações disponíveis on-line. Das produções analisadas há predominância do enfoque qualitativo e da utilização de entrevista. Verificou-se que as dissertações têm anuência com as linhas de pesquisa do Programa do Curso de Mestrado e sua análise pode contribuir para o redimensionamento de caminhos, linhas e pesquisas que o programa tem desenvolvido.

Geological transect across the Northwestern Himalaya in eastern Ladakh and Lahul (A model for the continental collision of India and Asia)

The detailed geological mapping and structural study of a complete transect across the northwestern Himalaya allow to describe the tectonic evolution of the north Indian continental margin during the Tethys ocean opening and the Himalayan Orogeny. The Late Paleozoic Tethys rifting is associated with several tectonomagmatic events. In Upper Lahul and SE Zanskar, this extensional phase is recorded by Lower Carboniferous synsedimentary transtensional faults, a Lower Permian stratigraphic unconformity, a Lower Permian granitic intrusion and middle Permian basaltic extrusions (Panjal Traps). In eastern Ladakh, a Permian listric normal fault is also related to this phase. The scarcity of synsedimentary faults and the gradual increase of the Permian syn-rift sediment thickness towards the NE suggest a flexural type margin. The collision of India and Asia is characterized by a succession of contrasting orogenic phases. South of the Suture Zone, the initiation of the SW vergent Nyimaling-Tsarap Nappe corresponds to an early phase of continental underthrusting. To the S, in Lahul, an opposite underthrusting within the Indian plate is recorded by the NE vergent Tandi Syncline. This structure is associated with the newly defined Shikar Beh Nappe, now partly eroded, which is responsible for the high grade (amphibolite facies) regional metamorphism of South Lahul. The main thrusting of the Nyimaling-Tsarap Nappe followed the formation of the Shikar Beh Nappe. The Nyimaling-Tsarap Nappe developed by ductile shear of the upper part of the subducted Indian continental margin and is responsible for the progressive regional metamorphism of SE Zanskar, reaching amphibolite facies below the frontal part of the nappe, near Sarchu. In Upper Lahul, the frontal parts of the Nyimaling-Tsarap and Shikar Beh nappes are separated by a zone of low grade metamorphic rocks (pumpellyite-actinolite facies to lower greenschist facies). At high structural level, the Nyimaling-Tsarap Nappe is characterized by imbricate structures, which grade into a large ductile shear zone with depth. The related crustal shortening is about 87 km. The root zone and the frontal part of this nappe have been subsequently affected by two zones of dextral transpression and underthrusting: the Nyimaling Shear Zone and the Sarchu Shear Zone. These shear zones are interpreted as consequences of the counterclockwise rotation of the continental underthrusting direction of India relative to Asia, which occurred some 45 and 36 Ma ago, according to plate tectonic models. Later, a phase of NE vergent `'backfolding'' developed on these two zones of dextral transpression, creating isoclinal folds in SE Zanskar and more open folds in the Nyimaling Dome and in the Indus Molasse sediments. During a late stage of the Himalayan Orogeny, the frontal part of the Nyimaling-Tsarap Nappe underwent an extension of about 15 km. This phase is represented by two types of structures, responsible for the tectonic unroofing of the amphibolite facies rocks of the Sarchu area: the Sarchu high angle Normal Fault, cutting a first set of low angle normal faults, which have been created by reactivation of older thrust planes related to the Nyimaling-Tsarap Nappe.

Records of Myodopsylla wolffsohni wolffsohni (Rothschild, 1903) (Siphonaptera, Ischnopsyllidae) on Myotis nigricans Schinz, 1821 (Chiroptera, Vespertilionidae), from the State of Paraná, Southern Brazil

The flea, Myodopsylla wolffsohni wolffsohni (Rothschild, 1903), had been recorded for the first time in the State of Paraná in 1940, on the bat, Myotis levis (I. Geoffroy, 1824). Previously, this species of flea had only been recorded on Myotis nigricans, in the Amazonian region. This is the second record of M. w. wolffsohni on M. nigricans in Brazil, and the first in the State of Paraná. Although this flea has been found on undetermined Chiroptera in the State of Santa Catarina, the present record represents the meridional limit of geographic distribution for the infestation on M. nigricans.

Análise faunística de Braconidae (Hymenoptera) em três áreas de mata nativa do Estado do Paraná, Brasil

The material studied comes from three of the several natural environments which still occur in Paraná State. The samples were collected during the project PROFAUPAR, developed by Departamento de Zoologia, Universidade Federal do Paraná. The selected sites were: Antonina (in the coastal plain), São José dos Pinhais (in the coastal mountain range) and Telêmaco Borba (in the second plateau). During one year of the project, 2,106 specimens of Braconidae were collected with light trap. These wasps represented 21 subfamilies and 1,966 specimens were identified in 85 genera. Hormiinae, Rogadinae, Microgastrinae, Alysiinae, Doryctinae and Meteorinae were the most frequent subfamilies. Indices of diversity and evenness were used to discuss richness and dominance of genera in each locality. Statistical analyses indicated that the asymptote of actual genera richness have been approached only to Antonina and Telêmaco Borba.

Fauna de Muscidae (Diptera) em três localidades do Estado do Paraná, Brasil, capturada por armadilha Malaise

During two years, from August 1986 to July 1988, the entomofauna of some preserved areas of Parana State, southern Brazil, was sampled in a project called "Levantamento da Fauna Entomológica no Estado do Paraná (PROFAUPAR)". Specimens of Muscidae (Diptera) were sorted out from the material collected using Malaise traps in three of the eight sites sampled (Colombo, Ponta Grossa and Guarapuava) in the first year (August 1986 to July 1987). A total of 7,014 specimens of Muscidae was captured and 91 species were identified. Neodexiopsis flavipalpis Albuquerque was the most abundant species in Ponta Grossa (672 specimens) and in Guarapuava (332 specimens). For Colombo, the most abundant species was Neodexiopsis vulgaris Couri & Albuquerque (172 specimens). The highest richness of species and abundance were observed in Ponta Grossa (77 and 3,559 respectively). The total number of specimens and means values of capture were analyzed. Indices of diversity and evenness were used to discuss richness and dominance of species in each locality. Besides using ecological indices, species richness estimators were also used.