Mantle beneath the Gibraltar Arc from receiver functions

P and S receiver functions (PRF and SRF) from 19 seismograph stations in the Gibraltar Arc and the Iberian Massif reveal new details of the regional deep structure. Within the high-velocity mantle body below southern Spain the 660-km discontinuity is depressed by at least 20 km. The Ps phase from the 410-km discontinuity is missing at most stations in the Gibraltar Arc. A thin (similar to 50 km) low-S-velocity layer atop the 410-km discontinuity is found under the Atlantic margin. At most stations the S410p phase in the SRFs arrives 1.0-2.5 s earlier than predicted by IASP91 model, but, for the propagation paths through the upper mantle below southern Spain, the arrivals of S410p are delayed by up to +1.5 s. The early arrivals can be explained by elevated Vp/Vs ratio in the upper mantle or by a depressed 410-km discontinuity. The positive residuals are indicative of a low (similar to 1.7 versus similar to 1.8 in IASP91) Vp/Vs ratio. Previously, the low ratio was found in depleted lithosphere of Precambrian cratons. From simultaneous inversion of the PRFs and SRFs we recognize two types of the mantle: 'continental' and 'oceanic'. In the 'continental' upper mantle the S-wave velocity in the high-velocity lid is 4.4-4.5 km s(-1), the S-velocity contrast between the lid and the underlying mantle is often near the limit of resolution (0.1 km s(-1)), and the bottom of the lid is at a depth reaching 90 100 km. In the 'oceanic' domain, the S-wave velocities in the lid and the underlying mantle are typically 4.2-4.3 and similar to 4.0 km s(-1), respectively. The bottom of the lid is at a shallow depth (around 50 km), and at some locations the lid is replaced by a low S-wave velocity layer. The narrow S-N-oriented band of earthquakes at depths from 70 to 120 km in the Alboran Sea is in the 'continental' domain, near the boundary between the 'continental' and 'oceanic' domains, and the intermediate seismicity may be an effect of ongoing destruction of the continental lithosphere.

Tsunami vulnerability assessment of Casablanca-Morocco using numerical modelling and GIS tools

Earthquakes and tsunamis along Morocco's coasts have been reported since historical times. The threat posed by tsunamis must be included in coastal risk studies. This study focuses on the tsunami impact and vulnerability assessment of the Casablanca harbour and surrounding area using a combination of tsunami inundation numerical modelling, field survey data and geographic information system. The tsunami scenario used here is compatible with the 1755 Lisbon event that we considered to be the worst case tsunami scenario. Hydrodynamic modelling was performed with an adapted version of the Cornell Multigrid Coupled Tsunami Model from Cornell University. The simulation covers the eastern domain of the Azores-Gibraltar fracture zone corresponding to the largest tsunamigenic area in the North Atlantic. The proposed vulnerability model attempts to provide an insight into the tsunami vulnerability of building stock. Results in the form of a vulnerability map will be useful for decision makers and local authorities in preventing the community resiliency for tsunami hazards.

Cidade digital

A Resolução do Conselho de Ministros n.º 120/2008, de 30 de Julho, definiu como prioridade estratégica para o País, no sector das comunicações electrónicas, a promoção do investimento em redes de nova geração. Com o objectivo de dar execução às orientações estratégicas estabelecidas, o Decreto -Lei n.º 123/2009, de 21 de Maio, veio estabelecer um conjunto de obrigações aplicáveis ao Estado, às Regiões Autónomas, às autarquias locais, empresas públicas, concessionárias e, genericamente, às entidades que detenham infra-estruturas que se integrem em domínio público, de forma a garantir a todas empresas de comunicações electrónicas, o acesso às infra-estruturas aptas ao alojamento de redes de comunicações electrónicas. Em Portugal, o caminho a ser traçado até as redes de nova geração passa pela, abertura eficaz e não discriminatória de todas as condutas e outras infra-estruturas aptas ao alojamento de redes de comunicações electrónicas, elaboração de regras técnicas aplicáveis às infra-estruturas de telecomunicações em loteamentos, urbanizações e conjuntos de edifícios, adopção de soluções que eliminem ou atenuem as barreiras verticais à instalação de fibra óptica e que evitem a monopolização do acesso aos edifícios pelo primeiro operador. Neste âmbito, excluem-se, pela sua especial natureza e fins a que estão afectas, as redes privativas dos órgãos políticos de soberania, do Ministério da Defesa Nacional, das forças e serviços de segurança, de emergência e de protecção civil. Assim, este trabalho visa apresentar procedimentos aplicáveis às infra-estruturas de telecomunicações para elaboração de um cadastro de todas as infra-estruturas, públicas e privadas, aptas ao alojamento de redes de comunicações electrónicas, e propor instruções técnicas para as condições e direitos de acesso, construção e intervenção sobre estas infra-estruturas.

Design of a sea-level tsunami detection network for the Gulf of Cadiz

The devastating impact of the Sumatra tsunami of 26 December 2004, raised the question for scientists of how to forecast a tsunami threat. In 2005, the IOC-UNESCO XXIII assembly decided to implement a global tsunami warning system to cover the regions that were not yet protected, namely the Indian Ocean, the Caribbean and the North East Atlantic, the Mediterranean and connected seas (the NEAM region). Within NEAM, the Gulf of Cadiz is the more sensitive area, with an important record of devastating historical events. The objective of this paper is to present a preliminary design for a reliable tsunami detection network for the Gulf of Cadiz, based on a network of sea-level observatories. The tsunamigenic potential of this region has been revised in order to define the active tectonic structures. Tsunami hydrodynamic modeling and GIS technology have been used to identify the appropriate locations for the minimum number of sea-level stations. Results show that 3 tsunameters are required as the minimum number of stations necessary to assure an acceptable protection to the large coastal population in the Gulf of Cadiz. In addition, 29 tide gauge stations could be necessary to fully assess the effects of a tsunami along the affected coasts of Portugal, Spain and Morocco.

Escola a tempo inteiro: medidas de política educativa e debate parlamentar

O conteúdo da presente comunicação resulta de uma investigação sobre as medidas de política educativa desenvolvidas em Portugal pelo Ministério de Educação com o objectivo de promover a “Escola a Tempo Inteiro” no âmbito do 1.º ciclo do ensino básico, através da formulação e implementação dos programas de generalização das actividades de enriquecimento curricular (AEC) e do alargamento do horário de funcionamento das escolas. A “análise especulativa” (Woods, 1999) decorrente da evolução do estudo revelou a emergência de uma diversidade de “cenas” (Delvaux, 2007) e de actores intervenientes no processo, tendo em conta que as políticas educativas devem ser entendidas “como espaços comunicacionais e sociais nos quais se exprimem e interagem diferentes concepções e modos de relação com o mundo educacional” (Barroso, et al., 2007). Por conseguinte, “têm de ser observadas a partir de múltiplos pontos de sua produção e ancoragem”. A presente comunicação focaliza-se apenas num desses pontos, nomeadamente, no debate parlamentar, considerando a Assembleia da República como produtora de políticas e palco de escrutínio de posições em confronto e de lógicas de argumentação diversas e, como tal, uma importante agência cuja acção contribui para a compreensão das políticas públicas de educação. Procura-se, então, descrever, compreender e analisar a forma como este órgão de soberania tratou a questão da escola tempo inteiro, particularmente, o que diz respeito aos programas de generalização das AEC (inicialmente com o ensino do inglês) e ao alargamento do horário no 1.º ciclo do ensino básico. A partir da análise das iniciativas parlamentares e das dinâmicas que lhes estão subjacentes, explicitadas nos Diários da Assembleia da República, procura-se: dar conta da forma como as medidas políticas em estudo são introduzidas nos assuntos e nas actividades parlamentares e como são contextualizadas, integradas ou articuladas com outras medidas; identificar os actores e interpretar as respectivas posições e estratégias face às medidas; evidenciar e problematizar as principais controvérsias, convergências e divergências estabelecidas face às medidas, bem como as lógicas de justificação subjacentes às posições dos actores, quer em termos de mobilização de conhecimento, quer em termos de defesa explícita ou implícita de valores, princípios, ideologias e interesses; problematizar os possíveis efeitos directos ou indirectos da actividade parlamentar nas medidas políticas, ao nível do processo de formulação da política em análise

O desafio do digital no século XXI: a análise à estratégia de Comunicação da Presidência da República

Temos assistido, especialmente ao longo dos últimos dois anos,a um progressivo aumento da utilização das redes sociais por parte da Presidência da República Portuguesa, com destaque para o Facebook. Tal repete a tendência registada a nível mundial, com especial destaque para os EUA e para o seu actual presidente, Barack Obama. No caso português, a Presidência da República, órgão de soberania liderado pelo Prof. Cavaco Silva,é um dos mais activos nesta frente, procurando utilizar as redes sociais como um barómetro sobre a forma como os portugueses sentem a democracia e o estado da nação.

Auxílios de Estado sob a forma fiscal: O caso Açores - Proc. C-88/03

Mestrado em Fiscalidade

Tsunamigenic earthquakes in the Gulf of Cadiz: fault model and recurrence

The Gulf of Cadiz, as part of the Azores-Gibraltar plate boundary, is recognized as a potential source of big earthquakes and tsunamis that may affect the bordering countries, as occurred on 1 November 1755. Preparing for the future, Portugal is establishing a national tsunami warning system in which the threat caused by any large-magnitude earthquake in the area is estimated from a comprehensive database of scenarios. In this paper we summarize the knowledge about the active tectonics in the Gulf of Cadiz and integrate the available seismological information in order to propose the generation model of destructive tsunamis to be applied in tsunami warnings. The fault model derived is then used to estimate the recurrence of large earthquakes using the fault slip rates obtained by Cunha et al. (2012) from thin-sheet neotectonic modelling. Finally we evaluate the consistency of seismicity rates derived from historical and instrumental catalogues with the convergence rates between Eurasia and Nubia given by plate kinematic models.

Seismic imaging of the western Iberian crust using ambient noise: Boundaries and internal structure of the Iberian Massif

We present new Rayleigh-wave dispersion maps of the western Iberian Peninsula for periods between 8 and 30 s, obtained from correlations of seismic ambient noise, following the recent increase in seismic broadband network density in Portugal and Spain. Group velocities have been computed for each station pair using the empirical Green's functions generated by cross-correlating one-day-length seismic ambient-noise records. The resulting high-path density allows us to obtain lateral variations of the group velocities as a function of period in cells of 0.5 degrees x 0.5 degrees with an unprecedented resolution. As a result we were able to address some of the unknowns regarding the lithospheric structure beneath SW Iberia. The dispersion maps allow the imaging of the major structural units, namely the Iberian Massif, and the Lusitanian and Algarve Meso-Cenozoic basins. The Cadiz Gulf/Gibraltar Strait area corresponds to a strong low-velocity anomaly, which can be followed to the largest period inverted, although slightly shifted to the east at longer periods. Within the Iberian Massif, second-order perturbations in the group velocities are consistent with the transitions between tectonic units composing the massif. (C) 2013 Elsevier B.V. All rights reserved.

Narrativas da transição: um olhar sobre a transferência de poderes de Macau vista pelo jornal Ponto Final: 1996-2001

Dissertação apresentada à Escola Superior de Comunicação Social como parte dos requisitos para obtenção de grau de mestre em Jornalismo.

Centro de Informação ao Cidadão e Relações Públicas da Assembleia da República: plano de ação estratégica para o desenvolvimento da área educativa

Relatório de estágio apresentado à Escola Superior de Comunicação Social como parte dos requisitos para obtenção de grau de mestre em Gestão Estratégica das Relações Públicas.

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.

From the Bay of Biscay to the High Atlas: completing the anisotropic characterization of the upper mantle beneath the westernmost Mediterranean region

The knowledge of the anisotropic properties beneath the Iberian Peninsula and Northern Morocco has been dramatically improved since late 2007 with the analysis of the data provided by the dense TopoIberia broadband seismic network, the increasing number of permanent stations operating in Morocco, Portugal and Spain, and the contribution of smaller scale/higher resolution experiments. Results from the two first TopoIberia deployments have evidenced a spectacular rotation of the fast polarization direction (FPD) along the Gibraltar Arc, interpreted as an evidence of mantle flow deflected around the high velocity slab beneath the Alboran Sea, and a rather uniform N100 degrees E FPD beneath the central Iberian Variscan Massif, consistent with global mantle flow models taking into account contributions of surface plate motion, density variations and net lithosphere rotation. The results from the last Iberarray deployment presented here, covering the northern part of the Iberian Peninsula, also show a rather uniform FPD orientation close to N100 degrees E, thus confirming the previous interpretation globally relating the anisotropic parameters to the LPO of mantle minerals generated by mantle flow at asthenospheric depths. However, the degree of anisotropy varies significantly, from delay time values of around 0.5 s beneath NW Iberia to values reaching 2.0 sin its NE comer. The anisotropic parameters retrieved from single events providing high quality data also show significant differences for stations located in the Variscan units of NW Iberia, suggesting that the region includes multiple anisotropic layers or complex anisotropy systems. These results allow to complete the map of the anisotropic properties of the westernmost Mediterranean region, which can now be considered as one of best constrained regions worldwide, with more than 300 sites investigated over an area extending from the Bay of Biscay to the Sahara platform. (C) 2015 Elsevier B.V. All rights reserved.