Geração automática de código ANSI C a partir de Redes de Petri IOPT - PNML2C -

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

C'est là que l'on joue la comédie: les casa da opera en Amérique Portugaise (1719-1819)

La présente thèse doctorale propose l’étude de l’activité théâtrale développée dans les théâtres permanents construits en Amérique Portugaise au long du XVIIIe et dans la première décennie du XIXe siècle, en mettant l’accent sur les idéalisateurs des Casas da Ópera et les moyens de financement utilisés dans l’édification et l’entretien de celles-ci, le répertoire mis en scène, les artistes composant les compagnies théâtrales, les spectateurs et les possibilités de sociabilité établies dans l’espace théâtrale et les modèles architectoniques qui ont inspiré la construction des bâtiments théâtraux au cours de la période mentionnée. Ces cinq axes principaux soulignent l’approche interdisciplinaire qui a orienté nos études, dans un souci de contribution à une plus complète compréhension de notre sujet de recherche. Mots clés : Théâtres, Amérique Portugaise, Comédiens Mulâtres, Théâtre Éphémère, Comédies Portugaises, Architecture théâtrale luso-américaine, Casa da Ópera de Vila Rica/Ouro Preto.

C&SIG na delimitação da estrutura ecológica municipal: aplicação ao município de Cascais

Trabalho de projecto apresentada como requisito parcial para obtenção do grau de Mestre em Ciência e Sistemas de Informação Geográfica.

Tectónica da região de Sintra

Photo-interpretation of aerial stereopairs of the Sintra region on the approx. 1/32 000 scale together with field work allowed the production of the present Tectonic Map of the Sintra region. It is now possible to separate structures which resulted from two different tectonic events: one, corresponding to the intrusion of the Late Cretaceous Sintra igneous diapir, and the other the Miocene compressive event, the most important tectonic inversion phase of the Lusitanian Basin. The former are present to the south, southeast and east of the intrusion and within the intrusion itself, affecting the peripheral granites and their contacts with the gabbro-syenite core. These structures comprehend: i) faults and conical fractures striking parallel to the massif boundary, which were intruded by dykes, ii) vertical faults and fractures of two conjugate sets, dextral NNW-SSE and sinistral NNE-SSW. These faults are certainly associated with the E-W striking massif's northwards directed thrust and indicate a N-S oriented horizontal maximum compressive stress. The Miocene compressive event reactivated most of the inherited structures as follows. The NNWSSE faults located on the Sintra southern platform were reactivated as dextral strike slip faults and the E-W thrust along the northern boundary of the massif was also reactivated. This thrust propagated to the east. It also enhanced the asymmetry of the rim-syncline, uplifted the massif and reactivated the NNE-SSW faults as sinistral lateral ramps, which also accommodated vertical throw. The present Tectonic Map of Sintra together with the available geophysical data (MOREIRA, 1984, KULLBERG et al., 1991, SILVA & MIRANDA, 1994) allowed reassessment of the models proposed for the emplacement of the Sintra, Sines and Monchique igneous massifs, which intruded during Late Cretaceous times along the deep dextral NNW-SSE oriented strike slip fault (RIBEIRO et al., 1979; TERRINHA, 1998; TERRINHA & KULLBERG, 1998).

Dynamic and interaction of cytochrome c with Pf1 virus

Dissertação apresentada na Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa para obtenção do grau de Mestre em BioOrgânica