Romantismo ingl��s : uma interpretação

Apesar de se utilizar com freq����ncia o termo ��escola rom��ntica��, apesar de ter sido poss��vel, em certos cases, marcar datas limites para o per��odo em que se desenvolveu a literatura dita rom��ntica, a verdade �� que nada disto �� mais que conven����o para facilidade de estudo. De facte, n��o h�� uma teoria rom��ntica que defina uma praxis, ��h�� tantos romantismes como rom��nticos��, segundo defini����o de um cr��tico (H. Bremend). Paul Val��ry refor��ou definitivamente esta id��ia, quando considerou que ��seria precise ter perdido todo o esp��rito de rigor para tentar definir o romantismo��. O Romantismo �� sobretudo um estado de esp��rito, que tem na base uma necessidade de afirma����o pessoal do artista, cuja inspira����o n��o cabe nos limites impostos pelos crit��rios de uma ��poca e para quem a arte �� uma realiza����o de si pr��prio e o leva a isolar-se num mundo s�� seu. Isto justifica, por exemple, que o drama seja a forma liter��ria que menos atraiu es rom��nticos.

A causa dos divertimentos

Texto justificativo para a atribui����o da Men����o Especial da Crítica 2011 ao actor Miguel Guilherme pela sua interpretação em O senhor Puntilla e o seu criado Matti, de Bertolt Brecht (enc. Jo��o Louren��o / Teatro Aberto, 2010).

Ariel o renovador: a crítica teatral de Fernando Amado como express��o de um ide��rio de teatro

�� objectivo deste artigo explorar a ideia de teatro que os textos de crítica teatral de Fernando Amado encerram ou ajudam a revelar. Para tal, importar�� dar conta do momento de renova����o c��nica e actualiza����o cultural, de que a segunda metade dos anos quarenta �� expoente, e das rela����es que o ide��rio formado por Fernando Amado, Redondo J��nior ou Gino Saviotti, entre outros, pode estabelecer com o que pela Europa Teatral se vai apelidando de teatro moderno.

Crítica teatral

Entrada sobre Crítica de Teatro.

A emerg��ncia da escrita: produ����es escritas de crian��as no jardim de inf��ncia

Relat��rio da Pr��tica Profissional Supervisionada Mestrado em Educa����o Pr��-Escolar

Mediatron : interpretação da personagem princesa P�� de Salsa : relat��rio de est��gio

Relat��rio de Est��gio submetido �� Escola Superior de Teatro e Cinema para cumprimento dos requisitos necess��rios �� obten����o do grau de Mestre em Artes Performativas - especializa����o em Interpretação

Gest��o da Qualidade: uma reflex��o crítica e actual

Pr��mio para o Melhor Artigo da Revista ���Qualidade��� da APQ-Associa����o Portuguesa para a Qualidade, 9�� Edi����o ��� 2013, ���Zulema Lopes Pereira���.

Ocorr��ncia de Taenia sp. na popula����o atendida no laborat��rio central do Instituto Adolfo Lutz, S��o Paulo, SP, Brasil (1960/1989)

Foram examinados retrospectivamente os relat��rios mensais e anuais da Se����o de Enteroparasitoses do Laborat��rio Central do Instituto Adolfo Lutz, S��o Paulo, SP, do per��odo de 1960 a 1989, perfazendo uma s��rie hist��rica de 30 anos, com 1.519.730 exames protoparasitol��gicos e 355 identifica����es de proglotes de Taenia. Pelo m��todo da sedimenta����o espont��nea foram diagnosticados 7.663 (0,5%) casos de presen��a de ovos de Taenia sp. nas fezes. Das 355 proglotes enviadas para identifica����o, 311 (87,60%) estavam em condi����es de serem especificadas, e dessas, 273 (87,80%) eram proglotes de Taenia saginata e 38 (12,22%) de T. solium.

Estratigrafia e interpretação paleogeogr��fica do Cenoz��ico continental do norte de Portugal

Palaeogeographic and tectono-sedimentary interpretation of northern Portugal, in which previous studies (geomorphology, lithostratigraphy, mineralogy, sedimentology, palaeontology, etc.) were considered, is here proposed. Cenozoic shows different features according to its morphotectonic setting in the eestern region (Tr��s-os-Montes) or near to the Atlantic coast (western region, Minho and Douro Litoral areas). Although in the eastern region the sedimentary record is considered late Neogene, in some places Paleogene (?) was identified. This oldest record, represented by alluvial deposits, was preserved from complete erosion because of its position inside Bragan��a-Vilari��a-Manteigas fault zone grabens. Later sedimentary episodes (upper Tortonian-Zanclean ?), represented by two allostratigraphical units, were interpreted as proximal fluvial braided systems of an endorheic hydrographic network, draining to the Spanish Duero Basin (eastwards); nowadays, they still remained in tectonic depressions and incised-valleys. Later on, eastern sedimentation becomes scarcer because Atlantic fluvial systems (e.g. the pre-Douro), successively, captured previous endorheic drainages. The proximal reaches of the allostratigraphic unit considered Placencian is recorded in Mirandela (western Tr��s-os-Montes) but the following fluvial episode (Gelasian-early Pleistocene ?) was already documented in east Tr��s-os-Montes, preserved in high platforms and in tectonic depressions. Placencian and Quaternary sedimentary records in the western coastal zone, mainly represented by terraces, are located in the Minho, Lima, Alver��es, C��vado and Ave large fluvial valleys and in the Oporto littoral platform. In conclusion, northern Portugal Tertiary sedimentary episodes were mainly controlled by tectonics, but later on (Placencian-Quaternary) also by eustasy.

Paleoaltera����es e cimenta����es nos dep��sitos continentais terci��rios de Portugal central: import��ncia na interpretação de processos antigos

This paper describes the palaeoweathering, cementation, clay minerals association and other closely related characteristics of central Portugal allostratigraphic Tertiary units (SLD's), that can be used for palaeoclimatic interpretation and palaeoenvironmental reconstruction. Lateral and vertical changes in palaeosols are of value for improving our understanding of the autocyclic and allocyclic controls on sediment acumulation in an alluvial basin, but they can also have stratigraphic importance. In some cases it is concluded that the geomorphological setting may have been more decisive than climatic conditions to the production of the palaeoweathering. During late Palaeogene (SLD7-8), surface and near-surface silicification were developed on tectonically stable land surfaces of minimal local relief under a semi-arid climate; groundwater flow was responsible for some eodiagenesis calcareous accumulations, with the neoformation of palygorskite. Conditions during the Miocene (SLD9-11) were favourable for the smectization of the metamorphic basement and arenization of granites. Intense rubefaction associated with basement conversion into clay (illite and kaolinite), is ascribed to internal drainage during late Messinian-Zanclean (SLD12). During Piacenzian (SLD13) intense kaolinization and hydromorphism are typical, reflecting a more humid and hot temperate climate and important Atlantic fluvial drainage. Later on (Gelasian-early Pleistocene ?; SLD14). more cold and dry conditicns are interpreted, at the beginning of the fluvial incision sage. Silica cementation is identified in the upper Eocence-Oligocene ? (SLD18; the major period of silicification), middle to upper Miocene (SLD10)and upper Tortonian-Messinian (SLD11); these occurrences are compatible with either arid or semi-arid conditions and the establishment of a flat landscape upon which a silcrete was developed.

Estratigrafia sismica do cenoz��ico na plataforma continental algarvia: interpretação do controle tect��nico da sedimenta����o

The interpretation of 64 seismic reflection profiles in the Algarve continental platform (36�� 20'-37�� 00' paralels and 7�� 20'-8�� 40' meridians) calibrated with five petroleum exploration wells, with the identification of the geometric relations between six Cenozoic seismic units (B to G) and tectonic structures, allowed the construction of sucessive time-isopach maps (twt/s) and detailed interpretation of the geologic evolution. Two major tectonic structures were identified: a) the Portim��o-Monchique fracture zone (striking N-S); b) an off-shore NW-SE fault zone, probably the S. Marcos-Quarteira fault. This accident separates two tectonic domains: the western domain (with N-S and E-W predominant structures and, secondarily, NW-SE and NE-SW) and the eastern domain (dominated by WSW-ENE, NW-SE, NE-SW, NNE-SSW and NNW-SSE structures). A persistent halokinetic activity had two major moments: a) sin-C unit; b) sin- and post-E unit. An increasing flexuration of the margin was identified, with spacial and temporal variation of the subsidence. The tectonic regime is considered as generally compressive, but the interpretation of the success��ve stress-fields is rendered dificult by the existence of tectonic sub-domains and evaporitic structures.

SIADAP : an��lise crítica

Trabalho final do Diploma de Especializa����o em Gest��o P��blica, Porto 2009/2010. Orienta����o: David Ferraz

O regime fiscal cooperativo ��� an��lise crítica e desafios

Disserta����o de Mestrado apresentada ao Instituto de Contabilidade e Administra����o do Porto para a obten����o do grau de Mestre em Contabilidade e Finan��as, sob orienta����o de Doutora Deolinda Meira e Doutora Nina Aguiar

Estudo explorat��rio da calendariza����o de m��ltiplos projectos pela cadeia crítica

Disserta����o apresentada na Faculdade de Ci��ncias e Tecnologia da Universidade Nova de Lisboa para a obten����o do grau de Mestre em Engenharia e Gest��o Industrial