Interpretation of gravity data to delineate structural features connected to low-temperature geothermal resources at Northeastern Portugal

A great number of low-temperature geothermal fields occur in Northern-Portugal related to fractured rocks. The most important superficial manifestations of these hydrothermal systems appear in pull-apart tectonic basins and are strongly conditioned by the orientation of the main fault systems in the region. This work presents the interpretation of gravity gradient maps and 3D inversion model produced from a regional gravity survey. The horizontal gradients reveal a complex fault system. The obtained 3D model of density contrast puts into evidence the main fault zone in the region and the depth distribution of the granitic bodies. Their relationship with the hydrothermal systems supports the conceptual models elaborated from hydrochemical and isotopic water analyses. This work emphasizes the importance of the role of the gravity method and analysis to better understand the connection between hydrothermal systems and the fractured rock pattern and surrounding geology. (c) 2013 Elsevier B.V. All rights reserved.

Convective patterns under the Indo-Atlantic << box >>

Using fluid mechanics, we reinterpret the mantle images obtained from global and regional tomography together with geochemical, geological and paleomagnetic observations, and attempt to unravel the pattern of convection in the Indo-Atlantic "box" and its temporal evolution over the last 260 Myr. The << box >> presently contains a) a broad slow seismic anomaly at the CMB which has a shape similar to Pangea 250 Myr ago, and which divides into several branches higher in the lower mantle, b) a "superswell, centered on the western edge of South Africa, c) at least 6 "primary hotspots" with long tracks related to traps, and d) numerous smaller hotspots. In the last 260 Myr, this mantle box has undergone 10 trap events, 7 of them related to continental breakup. Several of these past events are spatially correlated with present-day seismic anomalies and/or upwellings. Laboratory experiments show that superswells, long-lived hotspot tracks and traps may represent three evolutionary stages of the same phenomenon, i.e. episodic destabilization of a hot, chemically heterogeneous thermal boundary layer, close to the bottom of the mantle. When scaled to the Earth's mantle, its recurrence time is on the order of 100-200 Myr. At any given time, the Indo-Atlantic box should contain 3 to 9 of these instabilities at different stages of their development, in agreement with observations. The return flow of the downwelling slabs, although confined to two main << boxes >> (Indo-Atlantic and Pacific) by subduction zone geometry, may therefore not be passive, but rather take the form of active thermochemical instabilities. (c) 2005 Elsevier B.V. All rights reserved.

Aparelhos de apoio em pontes: vida útil e procedimentos de substituição

Dissertação de Natureza Científica para obtenção do grau de Mestre em Engenharia Civil Perfil Estruturas

Paralisia do VI par craniano vs. Síndrome de Duane tipo 1

O VI par craniano, é responsável pela inervação do músculo recto externo. Uma lesão que afecta o VI par irá resultar numa limitação da abdução. A Síndrome de Duane, do tipo I, caracteriza-se por limitação da abdução unilateral, em que o olho afectado não passa da linha média, por retração do globo ocular e estreitamento da fenda palpebral, em adução. O diagnóstico diferencial é de extrema importância para se proceder a um prognóstico correcto e respectivo plano terapêutico. Objectivos: Esquematizar as diversas características motoras e sensoriais da paralisia do VI par craniano comparando-as com as da Síndrome de Duane Tipo I, designando os testes de ortóptica respectivos. Identificar os testes de diagnóstico diferencial entre as duas entidades e as suas características principais, nomeadamente os exames coordimétricos e o teste das ducções forçadas.

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.

Deep structure of crust and mantle beneath Iberia and Western Mediterranean from P and S Receiver functions and SKS Waveforms

We have conducted a P and S receiver functions [PRFs and SRFs] analysis for 19 seismic stations on the Iberia and western Mediterranean. In the transition zone [TZ] the PRFs analysis reveals a band [from Gibraltar to Balearic] increased by 10-20 km relative to the standard 250 km. The TZ thickness variations are strongly correlated with the P660s times in PRFs. We interpret the variable depth of the 660-km discontinuity as an effect of subduction. Over the anomalous TZ we found a reduced velocity zone in the upper mantle. Joint inversion of PRFs and SRFs reveals a subcrustal high S velocity lid and an underlying LVZ. A reduction of the S velocity in the LVZ is less than 10%. The Gutenberg discontinuity is located at 65±5 km, but in several models sampling the Mediterranean, the lid is missing or its thickness is reduced to ~30 km. In the Gibraltar and North Africa this boundary is located at ~100 km. The lid Vp/Vs beneath Betics is reduced relative to the standard 1.8. Another evidence of the Vp/Vs anomaly is provided by S410p phase late arrivals in the SRFs. The azimuthal anisotropy analysis with a new technology was conducted at 5 stations and at 2 groups of stations. The fast direction in the uppermost mantle layer is ~90º in Iberian Massif. In Balearic is in the azimuth of ~120º. At a depth of ~60 km the direction becomes 90º. Anisotropy in the upper layer can be interpreted as frozen, whereas anisotropy in the lower layer is active, corresponding to the present-day or recent flow. The effect of the asthenosphere in the SKS splitting is much larger than the effect of the subcrustal lithosphere.

Graffiti nas edificações: identificação e resolução do problema

Trabalho final de Mestrado para obtenção do grau de Mestre em Engenharia Civil na Área de Especialização em Edificações

Uso da termografia na deteção de avarias

A civilização contemporânea, pelas suas características, é muito exigente em tudo o que diz respeito ao conforto dos edifícios, para trabalho ou habitação, e à necessidade de economizar e racionalizar o uso de energia. A térmica dos edifícios assume, por isso, uma importância acrescida na atividade profissional e no ensino. Para se conduzir ao aperfeiçoamento de soluções na envolvente dos edifícios a este nível, o trabalho aqui realizado centrou-se no estudo do funcionamento da termografia de infravermelhos e da importância da sua utilização na inspeção térmica de edifícios. Descoberta no início do século XIX e desenvolvendo os primeiros sistemas operativos desde a 1ª Guerra Mundial, a fim de determinar heterogeneidades de temperatura superficial, esta técnica não destrutiva permite identificar anomalias que não são visualizadas a olho nu. Com a análise dessas variações de temperatura é possível conhecer os problemas e a localização de irregularidades. Este trabalho baseia-se substancialmente no estudo de edifícios. A análise realizada teve como finalidade executar inspeções termográficas – visuais, com duas abordagens. Por um lado, avaliar salas pertencentes a estabelecimentos de ensino secundário, reabilitadas e não reabilitadas, todas construídas entre as décadas de 60 e 90, com o intuito de diagnosticar patologias construtivas, recorrendo à termografia. Por outro, a análise de edifícios de habitação, com a intenção de avaliar a necessidade de um equipamento complementar às inspeções termográficas – o sistema de porta ventiladora. As inspeções foram regidas pelas diretrizes da norma europeia EN 13187. A termografia é uma técnica importante na realização de ensaios in situ que requerem rapidez de execução, aliada à vantagem de disponibilizar resultados em tempo real, permitindo assim uma primeira análise das leituras no local. A inspeção termográfica complementada com o sistema de porta ventiladora permitiu, também, revelar a importância da necessidade de meios auxiliares em certos casos. A conjugação destas diferentes técnicas permite reduzir a subjetividade da análise in situ e aumentar a fiabilidade do diagnóstico.

Caracterização por optical coherence tomography (OCT) de placas coronárias sujeitas a cutting balloon: contributo das técnicas bidiomensional e tridimensional

Mestrado em Tecnologia de Diagnóstico e Intervenção Cardiovascular - Área de especialização: Intervenção cardiovascular

Epidemiologia e quadro clínico do acidente por cascavel sul-americana (Crotalus durissus)

Foram estudados 249 casos de acidentes por cascavel sul-americana (Crotalus durissus) atendidos no HVB-IB, São Paulo, Brasil, de 1974 a 1990. Os acidentes foram mais comuns no período da tarde, nos meses de janeiro a abril e de outubro a dezembro. Dentre cem serpentes classificadas quanto à subespécie 99 eram C. d. terrificus. Pertenciam ao sexo masculino 80,7% dos pacientes. Os membros inferiores e superiores foram picados em, respectivamente, 66,4% e 29,2% dos casos. As manifestações clínicas mais freqüentes foram dor (61,0%) e edema (55,0%) no local da picada, ptose palpebral (75,9%), escurecimento da urina atribuível à mioglobinúria (38,6%) e mialgia (36,1%). Nove pacientes foram submetidos a diálise devido a insuficiência renal aguda (3,6%), três apresentavam insuficiência respiratória que motivou intubação e/ou traqueostomia e um apresentou acidente vascular cerebral isquêmico. A alteração da coagulação sanguínea ocorreu em 48,1% dos pacientes. Oito amostras de sangue colhidas horas após a picada mostraram leucocitose sendo 6 com desvio a esquerda e, nos dias subseqüentes, tendência à normalização do número de leucócitos e aparecimento de eosinofilia. Atividade sérica da creatinoquinase apresentou-se aumentada em 20 dentre 21 pacientes, sendo maior no final das primeiras 24 horas após a picada, chegando a 2.377 vezes o valor de referência. A letalidade foi de 0,8%.

Ambient noise tomography of the East African Rift in Mozambique

Seismic ambient noise tomography is applied to central and southern Mozambique, located in the tip of the East African Rift (EAR). The deployment of MOZART seismic network, with a total of 30 broad-band stations continuously recording for 26 months, allowed us to carry out the first tomographic study of the crust under this region, which until now remained largely unexplored at this scale. From cross-correlations extracted from coherent noise we obtained Rayleigh wave group velocity dispersion curves for the period range 5–40 s. These dispersion relations were inverted to produce group velocity maps, and 1-D shear wave velocity profiles at selected points. High group velocities are observed at all periods on the eastern edge of the Kaapvaal and Zimbabwe cratons, in agreement with the findings of previous studies. Further east, a pronounced slow anomaly is observed in central and southern Mozambique, where the rifting between southern Africa and Antarctica created a passive margin in the Mesozoic, and further rifting is currently happening as a result of the southward propagation of the EAR. In this study, we also addressed the question concerning the nature of the crust (continental versus oceanic) in the Mozambique Coastal Plains (MCP), still in debate. Our data do not support previous suggestions that the MCP are floored by oceanic crust since a shallow Moho could not be detected, and we discuss an alternative explanation for its ocean-like magnetic signature. Our velocity maps suggest that the crystalline basement of the Zimbabwe craton may extend further east well into Mozambique underneath the sediment cover, contrary to what is usually assumed, while further south the Kaapval craton passes into slow rifted crust at the Lebombo monocline as expected. The sharp passage from fast crust to slow crust on the northern part of the study area coincides with the seismically active NNE-SSW Urema rift, while further south the Mazenga graben adopts an N-S direction parallel to the eastern limit of the Kaapvaal craton. We conclude that these two extensional structures herald the southward continuation of the EAR, and infer a structural control of the transition between the two types of crust on the ongoing deformation.

Static detection of anomalies in transactional memory programs

Dissertação apresentada na Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa para a obtenção do Grau de Mestre em Engenharia Informática

Utilização de métodos ópticos de correlação de imagem para a determinação da tenacidade à fractura de adesivos estruturais

Mestrado em Engenharia Mecânica

Central nervous system paracoccidioidomycosis. Report of a case successfully treated with Itraconazol

Paracoccidioidomycosis (PCM) is a primary pulmonary infection that often disseminates to other organs and systems. Involvement of the central nervous system (CNS) is rare and due to the fact that both clinical alertness and establishment of the diagnosis are delayed, the disease progresses causing serious problems. We report here a case of neuroparacoccidioidomycosis (NPCM), observed in a 55 year-old male, who consulted due to neurological symptoms (left hemiparesis, paresthesias, right palpebral ptosis, headache, vomiting and tonic clonic seizures) of a month duration. Upon physical examination, an ulcerated granulomatous lesion was observed in the abdomen. To confirm the diagnosis a stereotactic biopsy was taken; additionally, mycological tests from the ulcerated lesion and a bronchoalveolar lavage were performed. In the latter specimens, P. brasiliensis yeast cells were visualized and later on, the brain biopsy revealed the presence of the fungus. Treatment with itraconazole (ITZ) was initiated but clinical improvement was unremarkable; due to the fact that the patient was taking sodium valproate for seizure control, drug interactions were suspected and confirmed by absence of ITZ plasma levels. The latter medication was changed to clonazepam and after several weeks, clinical improvement began to be noticed and was accompanied by diminishing P. brasiliensis antigen and antibody titers. In the PCM endemic areas, CNS involvement should be considered more often and the efficacy of itraconazole therapy should also be taken into consideration.

Snakebites by Crotalus durissus ssp in children in Campinas, São Paulo, Brazil

From January, 1984 to March, 1999, 31 children under 15 y old (ages 1-14 y, median 8 y) were admitted after being bitten by rattlesnakes (Crotalus durissus ssp). One patient was classified as "dry-bite", 3 as mild envenoming, 9 as moderate envenoming and 18 as severe envenoming. Most patients had neuromuscular manifestations, such as palpebral ptosis (27/31), myalgia (23/31) and weakness (20/31). Laboratory tests suggesting rhabdomyolysis included an increase in total blood creatine kinase (CK, 28/29) and lactate dehydrogenase (LDH, 25/25) levels and myoglobinuria (14/15). The main local signs and symptoms were slight edema (20/31) and erythema (19/31). Before antivenom (AV) administration, blood coagulation disorders were observed in 20/25 children that received AV only at our hospital (incoagulable blood in 17/25). AV early reactions were observed in 20 of these 25 cases (9/9 patients not pretreated and 11/16 patients pretreated with hydrocortisone and histamine H1 and H2 antagonists). There were no significant differences in the frequency of patients with AV early reactions between the groups that were and were not pretreated (Fisher's exact test, p = 0.12). Patients admitted less than and more than 6 h after the bite showed the same risk of developing severe envenoming (Fisher's exact test, p = 1). No children of the first group (< 6 h) showed severe complications whereas 3/6 children admitted more than 6 h post-bite developed acute renal failure. Patients bitten in the legs had a higher risk of developing severe envenoming (Fisher's exact test, p = 0.04). There was a significant association between both total CK and LDH blood enzyme levels and severity (p < 0.001 for CK and p < 0.001 for LDH; Mann-Whitney U test). No deaths were recorded.