Mar dos Açores, Mar de Portugal, Mar da Europa, aprofundar o passado para projetar o futuro

Colóquio Internacional realizado em Ponta Delgada de 27-29 de Novembro de 2014, Açores

O ensino profissional de nível secundário em Portugal, 2000-2014

O presente estudo aborda a forma como as escolas secundárias públicas com ensino profissional (cursos profissionais) de qualificação profissional de nível 4, se têm vindo a adaptar às novas configurações do sistema educativo, na integração desta oferta educativa. Esta via de ensino tem contribuído de forma expressiva para o aumento da escolarização do ensino secundário nos últimos anos em Portugal. Tendo presentes estas novas configurações institucionais que resultaram em mudanças no sistema educativo, o Estado parece agora legitimar e apelar ao comportamento competitivo, numa ação conduzida por lógicas de mercado (quase-mercado). Destacamos aspetos fundamentais como os reflexos da crise económica e financeira no desemprego e na formulação de quadros de incerteza, o reforço do regime de autonomia, a imposição de condições de administração e gestão participativa, a estrutura e organização desta via de ensino, e o planeamento da oferta formativa como contextos centrais para a reflexão e identificação da ação estratégica. Recorremos ao conceito de instituição, o qual define o ambiente organizacional como um espaço de trocas de recursos económicos e simbólicos, e enfatiza que as estruturas organizacionais são o resultado de pressões exercidas pelo ambiente institucional em que estão inseridas, e não entidades passivas, pois desenvolvem práticas e estratégias consideradas apropriadas para assegurar o seu poder, legitimidade e sobrevivência. Através da análise da evolução das ofertas de cursos às escalas nacional e regional e de entrevistas com escolas públicas e municípios da rede EXCEL, bem como de escolas privadas dos mesmos concelhos, concluímos que numa primeira fase as escolas públicas pautaram as suas ofertas por estratégias defensivas, face à dependência de recursos, à procura de estabilidade organizativa e de afetação do corpo docente instalado e à perceção duvidosa sobre a autonomia. A segunda fase, a partir de 2011, carateriza-se pelo reforço da centralidade do Estado que passou a determinar as ofertas agindo como representante único da procura pública, ao mesmo tempo que se manteve a pressão concorrencial sobre as escolas como atores da oferta, estruturando um quase-mercado aproximado a um monopsónio.

Expectativas face à vida profissional dos futuros médicos, em Portugal: estudo qualitativo

Introdução Nos últimos anos temos assistido a grandes modificações e desafios no sector da saúde, com reformas ao nível da organização cultural, reestruturação de serviços, encerramento de algumas urgências e maternidades, reduções de vencimento e grandes cortes ao nível do financiamento dos serviços. É necessário perceber, qual o impacto, que esta reforma tem provocado nas expectativas profissionais dos futuros médicos de Portugal. Sendo as expectativas um dos determinantes da motivação, estas são um factor crucial para o desempenho de um serviço de qualidade e com eficiência. Métodos Foi realizado um estudo qualitativo e a abordagem metodológica foi um estudo de caso, com uma amostra intencional por conveniência, selecionada por questões de proximidade e acessibilidade da investigadora. A informação foi recolhida através da técnica de grupos focais a internos do ano comum e da especialidade, da Administração Regional de Saúde do Alentejo, mais precisamente na cidade de Évora. Realizaram-se 4 grupos focais, onde participaram 10 internos do ano comum e 9 internos da especialidade. Os dados obtidos durante a realização dos grupos focais foram os sujeitos a análise de conteúdo e foi realizada uma breve caracterização dos indivíduos que participaram. Resultados e discussão Em todos os grupos verificou-se uma incapacidade de pensar e planear o futuro, apresentando como principal razão as constantes alterações aplicadas com a reforma no sector da saúde. Observou-se uma ausência de expectativas relativamente ao seu futuro profissional, com grande preocupação em relação ao possível desemprego médico. Os internos do ano comum pretendem na sua maioria especialidades hospitalares. Mas mantêm a preocupação relativamente à possibilidade de não conseguirem vaga para a realização da especialidade. Conclusão Estes futuros médicos necessitam de esperança e de um elementos motivadores, activadores de comportamento, que possibilite um aumento das suas expectativas e consequentemente um melhor desempenho profissional futuro.

Actas do Encontro Portugal - Galiza. Mosaicos Romanos – Fragmentos de Cultura nas Proximidades do Atlântico

Livro de actas Encontro Portugal – Galiza, dedicado ao tema “Mosaicos Romanos – Fragmentos de Cultura nas Proximidades do Atlântico”, realizado entre 6 e 7 de Julho de 2013 no Museu da Villa Romana do Rabaçal – Município de Penela, Beira Litoral, Museu D. Diogo Sousa – Direcção Regional de Cultura do Norte, e Museu Provincial de Lugo – Galiza.Livro coordenado por Miguel Pessoa, conta com colaboração de inúmeros investigadores da especialidade.

Impacto da crise no volume e perfil de internamento de doentes com VIH-SIDA em Portugal Continental : análise temporal 2001-2012

RESUMO - Contexto: O início da crise económica em Portugal no ano de 2009 colocou o país numa grave recessão económica aliada a diversas medidas de austeridade. Como consequência assistiu-se, ao nível nacional, uma diminuição do PIB, aumento do desemprego e assim como uma série de restrições orçamentais em várias áreas, nomeadamente a da saúde. Apesar de existir inúmeros estudos que avaliaram o impacto das recessões económicas na saúde os resultados são controversos e não existe um consenso quanto a esta associação. No que se refere às doenças infeciosas o número de estudos é bastante mais reduzido. O objetivo deste estudo foi o de analisar o impacto da crise atual no volume e perfil de internamento de doentes com VIH/SIDA, de forma a complementar a escassa evidência existente neste domínio. Metodologia: Foram analisados 53,296 episódios de internamento nos hospitais do SNS entre o ano de 2001 e 2012, cujo diagnóstico principal é a infeção pelo VIH/SIDA. Considerou-se o ano de 2009 como o ano inicial da crise. Através de regressões multivariadas avaliou-se o impacto da crise no volume de doentes internados, duração de internamento, número de co-morbilidades, risco de ser admitido via urgência e risco de mortalidade no internamento. Adicionalmente repetiu-se a análise por região NUTS II de Portugal Continental (Norte, Alentejo, LVT, Centro e Algarve). Resultados: A crise não teve impacto no volume de doentes internados. No entanto, após o ano de 2009, registou-se uma diminuição de 5.6% na duração de internamento; um aumento de 1.6% no número de co-morbilidades; um aumento de 11.1% no risco de ser admitido via urgência e um aumento de 8.6% do risco de mortalidade no internamento. As análises por região permitiram verificar que as regiões mais afetadas pela crise foram a região LVT e a região Norte. Conclusão: A crise em Portugal não teve impacto na incidência de internamentos por VIH/SIDA. Porém o aumento do número de co-morbilidades, do risco de ser admitido via urgência e do risco de mortalidade no internamento parece refletir um agravamento da severidade dos casos após o ano de 2009. Adicionalmente a diminuição da duração de internamento com o efeito da crise poderá refletir tanto aumento da eficiência dos cuidados prestados ou ao contrário, uma diminuição da sua qualidade.

A indústria de defesa na cooperação Brasil-Portugal

The global dynamics of alliances are strongly determined by the level of cooperation among states. This cooperation can be embodied in various aspects, but the level of defense and security cooperation becomes usually more doctrinal and lasting. By the nature of sovereignty that instills in the bilateral relationship, cooperation at defense and security level can leverages other forms of cooperation. The circumstances and relational balance between Brazil and Portugal seem to evolve towards distancing opportunities, despite they are culturally and institutionally untainted. The economic dynamics, the strategic projection in global sustainability terms, the scale and ambition of Brazilian regional leadership, contrasts with the actual context of Portugal, distancing himself both on the stage where they operate. On the other hand, the historical and cultural roots, the language, the affinity of the peoples of CPLP and some opportunities for economic niches, trend to attract both countries. The condition of Portugal in NATO and Europe, coupled with the ability to export technical and human resources to value-added for Brazil, seems also to become approaching factors. On the balance of these dynamics, there is a set of exogenous factors (economic, external global relations matrix, regional stability, among others), which are not always controlled by any of both countries. These factors call for strong capacity for foresight analysis and decision making, with the inherent risk. There is cooperation vectors that are not apparently penalized by geographic distance, or by the difference of realities. Among these vectors we shall highlight synergies in technological niches, highly tradable goods and, mostly, using the domain of dual technologies. The thirteen niches herein identified are: Monitoring, Navigation, Command and Control, Electronics, Optoelectronics, Communication and remote sensing, Information Technologies, Flight Simulation, Specialized Training, Fiber Optic Sensors, Materials Engineering, Nanotechnology and Communications. Cumulating with identified opportunities in traditional relational framework, both countries are growing (in geography and economic terms) into the Atlantic, making it a central element in the bilateral approach. By being at the same time a growing stage of disputes and which stability tends to be threatened, it will be done an analysis of these synergistic vectors, superimposed on the impact on Atlantic securitization process.

Princípios orientadores da formação, ao nível do 1º ciclo: a cooperação Portugal/P.A.L.O.P.'s

Os Países Africanos de Língua Oficial Portuguesa (P.A.L.O.P.'s), tal como a grande maioria de todo o continente africano, apresentam graves deficiências quanto a alfabetização das suas populações, tomando-se, assim, o ensino primário uma prioridade absoluta. De entre todas as limitações que existem ao nível dos respectivos sistemas educativos, talvez, a mais grave seja a fraca preparação científica e pedagógica que a maioria dos professores apresenta, para além, evidentemente, do seu reduzido número. Assim, a formação de professores tornou-se numa das apostas mais fortes dos P.A.L.O.P.'s, no campo da educação. Portugal, na área da cooperação com estes países, participa num Projecto de Consolidação dos Sistemas Educativos, no âmbito do qual desenvolve um programa de Acções de Formação de Formadores.

A construção social das políticas educativas: estado, educação e mudança social no Portugal contemporâneo

Tese de doutoramento em Ciências da Educação, área de Educação e Desenvolvimento

Os processos de autonomia e descentralização à luz das teorias de regulação social

Tese de Doutoramento em Ciências da Educação, área de Educação e Desenvolvimento

Pine processionary moth (Thaumetopoea pityocampa) and great tit (Parus major) in Portugal

In the present work, we studied a common outbreaking Lepidoptera species in Portuguese pine stands – Thaumetopoea pityocampa (Den. & Schiff.) - and one of its potential predators – Parus major (L.). The population dynamics of the immature stages of the Lepidoptera was studied in several types of Pinus pinaster (Aiton) plantations in three different areas: Setúbal Peninsula, Abrantes and National Pine Forest of Leiria. Location and plantation structure was the most important factors determining population density of T. pityocampa. Setubal and Abrantes was highly susceptible to attacks by the Lepidoptera, whereas Leiria had lower densities. Young and homogeneous pine stands was more susceptible to attacks than older and more heterogeneous pines stands. However, a desynchronized population of T. pityocampa, in which the larvae develops during summer instead of during winter, reached high densities also in Leiria. The impact of several mortality factors and climatic conditions on the immature stages of the insect (eggs and larvae), in normal and desynchronized populations are discussed, as well as possible evolutionary implications of the sudden appearance of the new version of T. pityocampa. The break of the pupa diapause and adult emergence times the annual life cycle of this insect. Adults from the desynchronized population emerged earlier than adults from the normal population, which in turn determined the change in the larvae development period. Different factors, potentially affecting the timing of adult emergence in both normal and abnormal populations are also discussed. To study P. Major, nest-boxes were placed in the areas of Setúbal and Leiria and they were monitored during three seasons. The nest-boxes increased the density of breeding and wintering birds in the studied pine plantations, indicating that a lack of natural holes are in fact a limiting factor for this populations. The earliest breeding start for this species was recorded in my study area, indicating that Portuguese coastal pines provide good breeding conditions earlier than in other areas of Europe and North Africa. This leads to an overlap between the end of the larvae stage of T. pityocampa and the beginning of the breeding season of P. major. Key-words: Thaumetopoea pityocampa, Parus major, Pinus pinaster, population dynamics, Portugal.

Estudo Estratigráfico e Paleontológico do Jurássico do Algarve Ocidental

Algarve Province, Southern Portugal, corresponds in part to a meso-cenozoic basin running along the coast from Cabo S. Vicente to beyond Spanish border. Structurally it is a big monocline plunging southwards much deformed mainly by two East-West longitudinal flexures. Lithostratigraphical and chronostratigraphical studies dealt specially with Jurassic formations. This and the geological mapping of the post-Hercynian sedimentary formations allow us to define the following units: Triassic-Lower Liassic Arenitos de Silves (Silves sandstones sensu P. Choffat, pro parte) - At their base the Silves sandstones (0-150m) are represented mainly by cross-bedded red sandstones. This unit is Upper Triassic (Keuper) in age, on the evidence of some Brachiopoda. Complexo margo-carbonatado de Silves (Silves marl-limestone complex=Silves sandstones sensu P. Choffat, pro parte) (80-200m) overlies the preceding, it may be reported to the Upper Triassic-Hettangian. It consists of a thick pelite-marl-dolomite-limestone series with many intercalations of greenstones. Since no fossils were found it is not possible to conclude whether it is still Hettangian or if it does correspond, in the whole or in part, already to the Sinemurian. Liassic Dolomitos e calcários dolomíticos de Espiche (Espiche dolomite-rocks and dolomitic-limestones) - The usually massive and finely crystalline or saccharoidal dolomites and dolomitic-limestones are the toughest strata of the Algarve margin giving rise to several hills. Its thickness attains in certain points 60 metres at least. Based on geometry and on lithological similarities with the carbonated complex of the northern basin of Tagus river (Peniche, São Pedro de Muel, Quiaios), this formation can be accepted as Sinemurian in age. As it happens with the carbonated complex, here also the first dolomite beds are non-isochronal throughout the region; upper time-limit of the dolomitic facies is either Lower Carixian, Lower Toarcian or even Lower Dogger. The dolomitization is secondary but not much later than sedimentation. However, between Cabo S. Vicente-Vila do Bispo there is evidence of an even later secondary dolomitization related to the regional fault complex. Calcário dolomítico com nódulos de silex da praia de Belixe (Belixe beach dolomitic-limestone with silex nodules) (50-55m) - Ascribed to Lower or Middle Carixian on the basis of Platypleuroceras sp., Metaderoceras sp. nov. and M. gr. Venarense. Calcário cristalino compacto com Protogrammoceras, Fuciniceras e ? Argutarpites de Belixe (Belixe compact crystalline limestone with Protogrammoceras, Fuciniceras and ? Argutarpites) (30m) - Ascribed to Lower Domerian. Middle and Upper Domerian are indicated but by a single specimen of ? Argutarpites. Calcários margosos e margas com Dactylioceras semicelatum e Harpoceratídeos de Armação Nova (Armação Nova marly limestones and marls with D. semicelatum and Harpoceratidae) (25m) -Ascribed to Lower Toarcian. Middle and Upper Toarcian formations are not known in the Algarve. Dogger Calcários oolíticos, c. corálicos, c. pisolíticos, c. calciclásticos, c. dolomíticos e dolomitos de Almadena (Almadena oolitic-limestones, coral-reef-limestones, pisolite-limestones, limeclastic-limestones, dolomitic-limestones and dolomite-rocks) (more than 50 metres), with lagoonal facies. Ascribed to Aalenian-Bathonian-? Callovian. Margas acinzentadas e calcários detríticos com Zoophycos da praia de Mareta (Mareta beach greyish marls and detritical limestones with Zoophycos) (40m) - Pelagic transreef facies with Upper Bajocian and Bathonian ammonites. Calcários margosos e margas da praia de Mareta (Mareta beach pelagic marly-limestones and marls) (110m) - Ascribed to the Callovian on its ammonites. Malm Near Cabo S. Vicente and Sagres the first Upper Jurassic level consists of a yellowish-brown nodular, compact, locally phosphated and ferruginous, sometimes conglomeratic, marly limestone (0,35-1,50m) containing a rich macrofauna, which includes: 1) Callovian forms unknown at Lower Oxfordian; 2) Upper Callovian forms that still survived in Lower and Middle Oxfordian; 3) Lower Oxfordian forms (Mariae and Cordatum Zones); 4) Lower and Middle Oxfordian forms (Mariae to Plicatilis Zone); 5) Middle Oxfordian forms (plicatilis Zone), and some ones appearing in Middle Oxfordian. This condensed deposit is therefore dated from Middle Oxfordian (Plicatilis Zone). The other Upper Jurassic lithostratigraphical units were also mapped but their detailed study is not presented in this work. Correlations between lithostratigraphical and chronostratigraphical scales from P. Choffat, J. Pratsch, C. Palain and from the author are stated. Further correlations are attempted between zonc scales of Carixian-Lower Toarcian and Upper Bajocian-Middle Oxfordian of France, Spain (Asturias, Iberian and Betic Chains), Argel (Orania) and Portugal (northern Tagus basin and Algarve). The study of pyritous fossil assemblages common in Upper Bathonian-Lower Callovian marly levels of the praia da Mareta seems to suggest that these sediments were deposited in a bay or in an almost closed coastal re-entrance virtually without deep water circulation. Although such conditions may occur at any depth one may suppose that these ones actually correspond to an infralittoral neritic environment. The thaphocoenosis collected there are almost entirely composed of nektonic (ammonites, Belemnites) and planktonic (Bositra) faunas. The sedentary (crinoids, brachiopods) or free (sea-urchins, gastropods) epibenthonic forms are very scarce; endobenthonic forms are not known. The palaeontological study of all Nautiloids and Ammonoids of the Liassic and Dogger is presented (except Kosmoceratidae and Perisphinctaceae). Among the thirty one taxa dealt with, one is new (Metaderoceras sp. nov.) and the great majority of the others has been identified for the first time in Algarve. Some others have never been reported before in Portuguese formations. The evolution, during Jurassic times, of the sedimentary basins of the Portuguese plate margin is described. The absence of Cephalopods in the very extensive marly and dolomitic limestones, partly marine, suggests that, during Lower Liassic, palaeogeography underwent no great changes. Dolomitic-limestone with silex nodules from Cabo S. Vicente contain the first ammonites recorded at the base of the Middle Liassic. This facies, although very common in Tethys, is unknown north of the Tagus. The faunal assemblage has a mediterranean to submediterranean character. Comparisons between faunal assemblage" from Algarve with the ones known north of the Tagus show that communications between Boreal Europe and Tethys, virtually non-existent during Lower and Middle Carixian, became very easy during Lower Domerian. In earlier Pliensbachian times two distinct seas were adjacent to the Iberian plate. One, an epicontinental sea with a tethyan fauna, extended southwards from the Meseta margin. Another, was a boreal sea; during its transgressive episodes boreal faunas attained into the basin north of the Tagus. During Middle Carixian and Lower Domerian, owing to simultaneous transgressions, these two seas joined together allowing faunal exchanges along the epicontinental areas which limited the emerging hercynian chains belts. During Liassic, the Algarve belonged undoubtedly to the tethyan submediterranean province. The area north of the Tagus, on the contrary, was a complex realm where subboreal and tethyan affinities alternatively prevailed. In the Algarve the first Middle Jurassic deposits do frequently show lateral thickness reductions as well as unconformities contemporaneous with other generalized disturbances on the sedimentation processes in other parts of Europe. By this time, near Sagres, a barrier reef developed separating lagoonal or ante-reef facies from the transreef pelagic zone. The presence of tethyan fauna, the abundance of Phylloceratidae and the absence of boreal forms allow us to consider the Algarve basin as a submediterranean province. The presence of Callovian pelagic fossiliferous formations in the Loulé area shows that during Middle Jurassic the marl-limestone transreef sedimentation was not confined to the western Algarve. They would extend eastwards where they only can be seen in the core of some anticlines. This is due to the progressive sinking of the meso-cenozoic formations as we proceed towards the South of the Sagres-Algoz-Querença flexure. In the whole of the Peninsule, and as for the Middle Callovian, an important regression can be clearly recognized on the evidence of an erosion surface which strikes obliquely the Middle and Upper Callovian strata. The geographic boundaries of the different faunal provinces are not changed by the presence of many Kosmoceratidae in the phosphate nodules since they are but a minority in comparison with the tethyan forms. An abstract model can be constructed showing that in Western Europe the Kosmoceratidae may have migrated South and westwards through a channel of the sea that linked Paris basin to Poitou and Aquitaine. By migrating between the Iberian meseta and the Armorican massif this fauna reached northern Tagus basin at the beginning of Upper Callovian (Athleta Zone); this south and southwest bound migration would have proceeded, allowing such forms to reach Algarve basin only in latest Callovian times (Lamberti Zone). This migration means that during Middle Jurassic a widely spread North Atlantic sea would exist, flooding the western part of Portugal up to the Poitou.

Les Hipparion du Portugal

This paper is concerned with Hipparion from Ribatejo, Portugal, and with the stratigraphy of the Neogene series of this region. The first two chapters are an introduction and an historical review. Paleontological study includes both a revision of the specimens accounted by ROMAN (1907) and the description of new material. Two forms were recognized, an early H. cf. primigenium, lower Vallesian in age, NM 9 mammal unit (from Archino, Vila Nova da Rainha, Aveiras de Cima), and a more advanced H. primigenium cf. melendezi. Upper Vallesian, NM 10 (possibly lowermost Turolian, NM 11) (at Azambujeira and Marmeleira). A synthesis of Middle and Upper Miocene from Ribatejo is also presented. Levels with H. p. cf. melendezi are somewhat older than «Upper Pontian», as it was previously acknowledged, they attain at the best the lowermost Turolian (approximately corresponding to «Upper Pontian»). Even higher levels may be Turolian in age, though they are not yet accurately dated. Almost all the localities are shown (tableau 11) according to its stratigraphical position; age, correspondance to mammal units from NM 5 to NM 10 (and may be also from NM 11 to NM 12), and correlation with marine formations near Lisbon are also taken in account. The stratigraphical position of localities such as Póvoa de Santarém, Quinta do Marmelal, Pero Filho, Azambujeira (lower levels), and Fonte do Pinheiro was revised; the stratigraphical position of Marmeleira was ascertained. The localities so far known correspond to NM 5 (?), NM 6, NM 8, NM 9, NM 10 and possibly to NM II and NM 12. A new interpretation (M. T. ANTUNES) of localities with oysters from Ribatejo allows a better correlation with vertebrate localities. Relationships with Serravallian transgression seem well established. Only two localities, Vila Nova da Rainha and Foz do Alviela, may possibly be correlated to V-b division of Lisbon (Langhian) with «Hispanotherium fauna». All the other localities are younger than Serravallian oyster beds. Undirect correlation shows that NM 6 localities are somewhat younger than the apogee ef Serravallian transgression (corresponding approximately to Blow's N 11 to N 13 zones based on planctonic foraminifera).

Sobre a ocorrência de copiapite na orla meso-cenozóica occidental de Portugal

The occurrence of a copiapite in the Paleogenic (?) formations of Vale Furado (South of S. Pedro de Muel, Portugal) is described, X-ray, DTA and TGA data and a chemical analysis of this mineral are presented.

Evolução tectónica mesozóica da Bacia Lusitaniana

The evolution of the Lusitanian Basin, localized on the western Iberian margin, is closely associated with the first opening phases of the North Atlantic. It persisted from the Late Triassic to the Early Cretaceous, more precisely until the end of the Early Aptian, and its evolution was conditioned by inherited structures from the variscan basement. The part played by the faults that establish its boundaries, as regards the geometric and kinematic evolution and the organization of the sedimentary bodies, is discussed here, as well as with respect to important faults transversal to the Basin. A basin evolution model is proposed consisting of four rifting episodes which show: i) periods of symmetrical (horst and graben organization) and asymmetrical (half graben organization) geometric evolution; ii) diachronous fracturing; iii) rotation of the main extensional direction; iv) rooting in the variscan basement of the main faults of the basin (predominantly thick skinned style). The analysis and regional comparison, particularly with the Algarve Basin, of the time intervals represented by important basin scale hiatuses near to the renovation of the rifting episodes, have led to assume the occurrence of early tectonic inversions (Callovian–Oxfordian and Tithonian–Berriasian). The latter, however, had a subsequent evolution distinct from the first: there is no subsidence renovation, which is discussed here, and it is related to a magmatic event. Although the Lusitanian Basin is located on a rift margin which is considered non-volcanic, the three magmatic cycles as defined by many authors, particularly the second (approx. 130 to 110 My ?), performed a fundamental part in the mobilization of the Hettangian evaporites, resulting in the main diapiric events of the Lusitanian Basin. The manner and time in which the basin definitely ends its evolution (Early Aptian) is discussed here. Comparisons are established with other west Iberian margin basins and with Newfoundland basins. A model of oceanization of this area of the North Atlantic is also presented, consisting of two events separated by approximately 10 My, and of distinct areas separated by the Nazaré fault. The elaboration of this synthesis was based on: - information contained in previously published papers (1990 – 2000); - field-work carried out over the last years, the results of which have not yet been published; - information gathered from the reinterpretation of geological mapping and geophysical (seismic and well logs) elements, and from generic literature concerning the Mesozoic of the west iberian margin.