Palaeomagnetic study of a subaerial volcanic ridge (São Jorge Island, Azores) for the cobb mountain subhron, volcano flank instability and tectonomagmatic implications

We present a palaeomagnetic study on 38 lava flows and 20 dykes encompassing the past 1.3 Myr on S. Jorge Island (Azores ArchipelagoNorth Atlantic Ocean). The sections sampled in the southeastern and central/western parts of the island record reversed and normal polarities, respectively. They indicate a mean palaeomagnetic pole (81.3 degrees N, 160.7 degrees E, K= 33 and A95= 3.4 degrees) with a latitude shallower than that expected from Geocentric Axial Dipole assumption, suggesting an effect of non-dipolar components of the Earth magnetic field. Virtual Geomagnetic Poles of eight flows and two dykes closely follow the contemporaneous records of the Cobb Mountain Subchron (ODP/DSDP programs) and constrain the age transition from reversed to normal polarity at ca. 1.207 +/- 0.017 Ma. Volcano flank instabilities, probably related to dyke emplacement along an NNWSSE direction, led to southwestward tilting of the lava pile towards the sea. Two spatially and temporally distinct dyke systems have been recognized on the island. The eastern is dominated by NNWSSE trending dykes emplaced before the end of the Matuyama Chron, whereas in the central/western parts the eruptive fissures oriented WNWESE controlled the westward growth of the S. Jorge Island during the Brunhes Chron. Both directions are consistent with the present-day regional stress conditions deduced from plate kinematics and tectonomorphology and suggest the emplacement of dykes along pre-existing fractures. The distinct timing and location of each dyke system likely results from a slight shift of the magmatic source.

Reconstructing the architectural evolution of volcanic islands from combined K/AR, morphologic, tectonic, and magnetic data. The Faial Island exemple (Azores)

The morpho-structural evolution of oceanic islands results from competition between volcano growth and partial destruction by mass-wasting processes. We present here a multi-disciplinary study of the successive stages of development of Faial (Azores) during the last 1 Myr. Using high-resolution digital elevation model (DEM), and new K/Ar, tectonic, and magnetic data, we reconstruct the rapidly evolving topography at successive stages, in response to complex interactions between volcanic construction and mass wasting, including the development of a graben. We show that: (1) sub-aerial evolution of the island first involved the rapid growth of a large elongated volcano at ca. 0.85 Ma, followed by its partial destruction over half a million years; (2) beginning about 360 ka a new small edifice grew on the NE of the island, and was subsequently cut by normal faults responsible for initiation of the graben; (3) after an apparent pause of ca. 250 kyr, the large Central Volcano (CV) developed on the western side of the island at ca 120 ka, accumulating a thick pile of lava flows in less than 20 kyr, which were partly channelized within the graben; (4) the period between 120 ka and 40 ka is marked by widespread deformation at the island scale, including westward propagation of faulting and associated erosion of the graben walls, which produced sedimentary deposits; subsequent growth of the CV at 40 ka was then constrained within the graben, with lava flowing onto the sediments up to the eastern shore; (5) the island evolution during the Holocene involves basaltic volcanic activity along the main southern faults and pyroclastic eruptions associated with the formation of a caldera volcano-tectonic depression. We conclude that the whole evolution of Faial Island has been characterized by successive short volcanic pulses probably controlled by brief episodes of regional deformation. Each pulse has been separated by considerable periods of volcanic inactivity during which the Faial graben gradually developed. We propose that the volume loss associated with sudden magma extraction from a shallow reservoir in different episodes triggered incremental downward graben movement, as observed historically, when immediate vertical collapse of up to 2 m was observed along the western segments of the graben at the end of the Capelinhos eruptive crises (1957-58).

Constrains on the structure of Maio Island (Cape Verde) by a three-dimensional gravity model: Imaging partially exhumed magma chambers

We propose a 3-D gravity model for the volcanic structure of the island of Maio (Cape Verde archipelago) with the objective of solving some open questions concerning the geometry and depth of the intrusive Central Igneous Complex. A gravity survey was made covering almost the entire surface of the island. The gravity data was inverted through a non-linear 3-D approach which provided a model constructed in a random growth process. The residual Bouguer gravity field shows a single positive anomaly presenting an elliptic shape with a NWSE trending long axis. This Bouguer gravity anomaly is slightly off-centred with the island but its outline is concordant with the surface exposure of the Central Igneous Complex. The gravimetric modelling shows a high-density volume whose centre of mass is about 4500 m deep. With increasing depth, and despite the restricted gravimetric resolution, the horizontal sections of the model suggest the presence of two distinct bodies, whose relative position accounts for the elongated shape of the high positive Bouguer gravity anomaly. These bodies are interpreted as magma chambers whose coeval volcanic counterparts are no longer preserved. The orientation defined by the two bodies is similar to that of other structures known in the southern group of the Cape Verde islands, thus suggesting a possible structural control constraining the location of the plutonic intrusions.

Natural and experimental infection of planorbids from the Island of Santa Catarina (Brazil)

Studies on eight localities on the Island of Santa Catarina revealed the presence of three species of the molluscan family Planorbidae: Biomphalaria tenagophila, Drepanotrema cimex and Biomphalaria oligoza, the first one being naturally infected by Cercaria ocellifera, a furcocercaria with morphological characteristics of Cercaria caratinguensis, and by an unknown furcocercaria. Drepanotrema cimex was infected by a furcocercaria with characteristics of C. caratinguensis and by C. macrogranulosa. No natural infection was found in B. oligoza. B. tenagophila showed no susceptibility to the experimental infection by the BH-MG strain of Schistosoma mansoni from Belo Horizonte and maintained at laboratory in B. glabrata snails.

Upper crustal structure of Madeira Island revealed from ambient noise tomography

We present the first image of the Madeira upper crustal structure, using ambient seismic noise tomography. 16 months of ambient noise, recorded in a dense network of 26 seismometers deployed across Madeira, allowed reconstructing Rayleigh wave Green's functions between receivers. Dispersion analysis was performed in the short period band from 1.0 to 4.0 s. Group velocity measurements were regionalized to obtain 20 tomographic images, with a lateral resolution of 2.0 km in central Madeira. Afterwards, the dispersion curves, extracted from each cell of the 2D group velocity maps, were inverted as a function of depth to obtain a 3D shear wave velocity model of the upper crust, from the surface to a depth of 2.0 km. The obtained 3D velocity model reveals features throughout the island that correlates well with surface geology and island evolution. (C) 2015 Elsevier B.V. All rights reserved.

Upper crustal structure of Madeira Island revealed from ambient noise tomography

We present the first image of the Madeira upper crustal structure, using ambient seismic noise tomography. 16 months of ambient noise, recorded in a dense network of 26 seismometers deployed across Madeira, allowed reconstructing Rayleigh wave Green's functions between receivers. Dispersion analysis was performed in the short period band from 1.0 to 4.0 s. Group velocity measurements were regionalized to obtain 20 tomographic images, with a lateral resolution of 2.0 km in central Madeira. Afterwards, the dispersion curves, extracted from each cell of the 2D group velocity maps, were inverted as a function of depth to obtain a 3D shear wave velocity model of the upper crust, from the surface to a depth of 2.0 km. The obtained 3D velocity model reveals features throughout the island that correlates well with surface geology and island evolution. (C) 2015 Elsevier B.V. All rights reserved.

Matrizes energética e de emissões de gases com efeito de estufa no Concelho de Torres Vedras: agir localmente num problema global

Dissertação apresentada na Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa para obtenção do grau de Mestre em Engenharia do Ambiente, perfil de Gestão de Sistemas Ambientais

Processos de avaliação dos pavimentos rodoviários: Caso de estudo: reforço do pavimento em dois trechos do sublanço Enxara/Torres Vedras Sul

Relatório de Estágio Curricular para obtenção do grau de Mestre em Engenharia Civil na Área de Especialização de Vias de Comunicação e Transportes

Projeto de torres metálicas de suporte de cabos de energia elétrica - Aplicação da parte 3-1 Eurocódigo 3

Mestrado em Engenharia Civil – Ramo Estruturas

Automatização do processo de soldadura dos aros das portas das torres eólicas

Dissertação para obtenção do Grau de Mestre em Engenharia Mecânica

Treasure Island": um tesouro inesgotável"

pp. 119-160

Seroprevalence of antibodies to Venezuelan equine encephalitis complex (subtypes IAB and VI) in humans from General Belgrano Island, Formosa, Argentina

This work presents the results of the detection of antibodies (immunoglobulin G) for subtypes I and VI of VEE viruses complex (Togaviridae family) in people from the General Belgrano island, Formosa province (Argentina). The prevalence of neutralizing (NT) antibodies for subtype VI was from 30% to 70% and the prevalence of antibodies inhibitory of hemagglutination (HI) was of 0% in the first and second inquiry respectively. For the subtype IAB the prevalence of NT antibodies was from 13% to 3.6%, similar to the prevalence total for both subtypes. HI antibodies were not detected in any inquiries for any subtype. It was observed that both subtypes circulate simultaneously, while subtype VI remains constant with some peaks, subtype I was found in low level.

Estudo dos flebótomos (Diptera, Phlebotominae), vectores de Leishmania sp. No Concelho de Torres Novas, Portugal

Estudo dos flebótomos (Diptera, Phlebotominae), vectores de Leishmania sp. no Concelho de Torres Novas, Portugal. Sofia Isabel Martins Branco PALAVRAS-CHAVE: flebótomos, bioecologia, Leishmania, Torres Novas, Portugal. Os flebótomos são insectos vectores de vários agentes patogénicos, dos quais se destacam os protozoários do Género Leishmania. Em Portugal, as leishmanioses, canina e humana, são causadas por L. infantum, sendo o cão o principal reservatório e Phlebotomus perniciosus e P. ariasi os vectores comprovados do parasita. São conhecidos três focos de doença, mas casos de leishmaniose canina têm sido reportados em outras regiões nas quais se desconhecem as espécies flebotomínicas presentes e respectivas taxas de infecção. Neste trabalho, efectuou-se a primeira prospecção flebotomínica no Concelho de Torres Novas, Distrito de Santarém, localizado na região Centro de Portugal. Os principais objectivos foram determinar a fauna flebotomínica do Concelho, os aspectos bioecológicos, as taxas de infecção por Leishmania e os factores de risco para a transmissão vectorial. De Junho a Novembro de 2010, 275 biótopos foram prospectados com armadilhas CDC. As capturas foram realizadas em 91 localidades, nas 17 freguesias do Concelho, e incluíram habitats domésticos, peridomésticos e silváticos. Os exemplares capturados foram identificados morfologicamente, as fêmeas utilizadas para detecção molecular de DNA de Leishmania e identificação das refeições sanguíneas. Análises de regressão simples e múltipla foram utilizadas para avaliação dos factores de risco para a presença das várias espécies flebotomínicas. Testes não paramétricos foram usados para comparar densidades. Dos 1262 flebótomos capturados, quatro espécies foram assinaladas com as seguintes abundâncias relativas: P. perniciosus 73,69%, P. ariasi 8,16%, P. sergenti 6,58% e Sergentomyia minuta 11,57%. Em 82% das localidades prospectadas foi detectada pelo menos uma espécie flebotomínica e em 71,4% destas foi capturada pelo menos uma das espécies comprovadamente vectoras de L. infantum. P. perniciosus foi assinalado em todas as 17 freguesias do Concelho. Os factores de risco identificados foram: temperaturas elevadas e humidades relativas baixas, locais abrigados e ausência de vento forte, presença de pinheiros como vegetação dominante, biótopos peridomésticos, particularmente currais de ovelhas e coelheiras, ou na proximidade de ovelhas, aves de capoeira e ninhos com andorinhas. A taxa de infecção flebotomínica por L. infantum foi de 4% para P. ariasi e de 0,32% para o total de fêmeas capturadas. A maioria das fêmeas para as quais se identificou a origem da refeição sanguínea pertencia a P. perniciosus. Esta espécie apresentou um comportamento oportunista, alimentando-se numa grande variedade de hospedeiros vertebrados. A elevada abundância e distribuição das espécies vectoras, juntamente com a seroprevalência de Leishmania nos cães do Distrito (5-10%), e a captura de uma fêmea grávida de P. ariasi (infectante), sugerem que o Concelho de Torres Novas é um foco de leishmaniose no país. A maior abundância relativa de P. sergenti, comparando com prospecções realizadas noutras áreas da região Centro de Portugal, sugere que este potencial vector esteja a expandir-se para latitudes mais elevadas, aumentando o risco de introdução de L. tropica no território, por contacto com imigrantes ou viajantes infectados de áreas endémicas. A monitorização flebotomínica, e dos hospedeiros vertebrados, deverá ser continuada no Concelho para que medidas eficazes de controlo possam ser definidas e implementadas.

Caracterização da paleta de Diogo de Torres. Quatro pinturas Retabulares do séc. XVI. Estudo da descoloração do azul de esmalte

Dissertação para obtenção do Grau de Mestre em Conservação e Restauro

Metodologias em Educação Ambiental – o exemplo do Centro de Educação Ambiental de Torres Vedras

Relatório de Estágio apresentado para cumprimento dos requisitos necessários à obtenção do grau de Mestre em Ambiente e Recursos Naturais