Bibliographies thématiques / Zone portuali

Littérature scientifique sur le sujet « Zone portuali »

Auteur : Grafiati
Publié le 11 mars 2023

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Articles de revues sur le sujet "Zone portuali"

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Boomer, Ian, Nigel R. Ainsworth et John Exton. « A re-examination of the Pliensbachian and Toarcian Ostracoda of Zambujal, west-central Portugal ». Journal of Micropalaeontology 17, no 1 (1 avril 1998) : 1–14. http://dx.doi.org/10.1144/jm.17.1.1.

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Abstract. Pliensbachian and Toarcian Ostracoda first described by Exton (Geological Paper, Carleton University, Ottawa, 79: 1–104 1979) from the Lusitanian Basin, west-central Portugal have been re-examined. As a result, a greater diversity in the Ostracoda (80 species) is now recognized. Two species are newly described (Eucytherura zambujalensis sp. nov., Ektyphocythere mediodepressa sp. nov.) from the marls and calcareous shales of the Maria Pares Hill section near the village of Zambujal. Poor preservation precludes a complete taxonomic review of the present material. Five ostracod zones are proposed; Gammacythere ubiquita–Ogmoconchella gruendeli Zone, Poly cope cerasia–Polycope cincinnata Zone, Liasina lanceolata–Ogmoconcha convexa Zone, Bairdiacypris rectangularis–Kinkelinella sermoisensis Zone, and Cytherella toarcensis-Kinkelinella costata Zone. Although the ostracod assemblages possess strong similarities to those described from Northwest Europe, some of the Zambujal assemblages are dominated by the genus Polycope. A marked faunal turnover, in association with the extinction of the Metacopina occurs in the lower Subzone of the tenuicostatum Zone of Lower Toarcian age. These faunal events are discussed in relation to changing environmental conditions.
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Krijger, Tom-Eric. « Extraterritorial Privacy Zone ? » TSEG - The Low Countries Journal of Social and Economic History 18, no 3 (29 novembre 2021) : 41–74. http://dx.doi.org/10.52024/tseg.11042.

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The Protestant Reformation led to a radical redrawing of the map of Europe, severely affecting international relations. An important consequence of Protestantism was the emphasis on the private dimension of religious practices, as it did away with clerical intermediaries and instead put the focus on the direct relationship between God and the believer. In this context, to facilitate diplomatic traffic between Catholic and Protestant countries, ambassadors came to enjoy the so-called Right of Chapel, allowing them to create a private place of worship and have a private chaplain at their ambassadorial residences. This right was explicitly included in two treaties that the Kingdom of Portugal and the Dutch Republic concluded with each other in the mid-seventeenth century. However, the two parties to the treaties had starkly different understandings of what was meant by ‘private’. Both of these treaties granted Dutch citizens in Portugal freedom of conscience in their own houses, but the contrasting interpretations of what ‘private’ actually meant for the Dutch and for the Portuguese resulted in serious disagreement about the exact scope of these religious rights.
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Ferreira Gomes, Luis M. « Protection Perimeter of a New Mineral Water in an Essentially Urban Environment : The Case of the São Tiago Medical Spa (Portugal) ». IOP Conference Series : Materials Science and Engineering 1203, no 2 (1 novembre 2021) : 022054. http://dx.doi.org/10.1088/1757-899x/1203/2/022054.

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Abstract São Tiago medical spa is an integrated structure in a new Health Tourism Complex, in Penamacor, Portugal, with a recent start of operation, due to the classification of a new natural mineral water in place. That medical spa bases its exploration on the natural mineral water obtained from the Well P1. Thus, to facilitate the preservation of the quality of the resource, natural mineral water, one of the fundamental instruments is the implementation of a Protection Perimeter of Well P1 and its associated aquifer system. In this sense, in this paper, after briefly presenting the basic geoenvironmental aspects that are the base for the elaboration of the Protection Perimeter, the methodology of its elaboration is explained, with the final solution, which constitutes a territory organized by three zones: Immediate Protection Zone, Intermediate Protection Zone and Extended Protection Zone. The official restrictions legally foreseen for those zones are mentioned and the official systematization of the current occupation of the territory is presented, in terms of the Municipal Master Plan (PDM), while emphasizing the potential sources of existing pollution. Finally, some comments are made about the future orientation regarding the occupation of the territory in the interior zones of the Protection Perimeter, so that the new Health Tourism complex, consisting of a medical spa, hotel, and aqualudic spaces, endures in the time, and helps the sustained economic growth of the region.
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Leandro, Sérgio Miguel, Peter Tiselius et Henrique Queiroga. « Spatial and temporal scales of environmental forcing of Acartia populations (Copepoda : Calanoida) in the Canal de Mira (Ria de Aveiro, Portugal)† ». ICES Journal of Marine Science 71, no 3 (8 février 2013) : 585–96. http://dx.doi.org/10.1093/icesjms/fst008.

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Abstract Zooplankton and hydrological data were collected from August 2000 and June 2002 at six stations distributed throughout Canal de Mira (Ria de Aveiro, Portugal). The abundance of Acartia clausi and Acartia tonsa adults and juveniles of Acartia spp. for each station and month were combined in a three-way data matrix, which was decomposed into three two-way matrices corresponding to different modes: biological, time, and space. Cluster analysis applied on the space mode revealed the existence of three different zones as a consequence of zooplankton composition. At each mode, principal component analysis showed strong seasonal variations in zones 1 and 2. A different spatial pattern was found between the periods November 2000–April 2001 and November 2001–April 2002, with the displacement of the highest abundance levels from the middle estuary to near the mouth. The congeneric populations were segregated in space: the A. clausi population was restricted to downstream stations (zone 1), whereas the A. tonsa population dominated the middle estuary. Significant correlations between hydrological parameters and copepod abundance were found to differ from zone to zone. The statistical methodology was a valuable tool to (i) discriminate spatial and seasonal distribution patterns, (ii) define estuarine sections based on the faunistic composition, and (iii) evaluate delayed effects of phytoplankton.
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XU, CHEN, RONG JIAYU, CHARLES E. MITCHELL, DAVID A. T. HARPER, FAN JUNXUAN, ZHAN RENBIN, ZHANG YUANDONG, LI RONGYU et WANG YI. « Late Ordovician to earliest Silurian graptolite and brachiopod biozonation from the Yangtze region, South China, with a global correlation ». Geological Magazine 137, no 6 (novembre 2000) : 623–50. http://dx.doi.org/10.1017/s0016756800004702.

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Late Ordovician to earliest Silurian is an important geological period marked by large geological and biological events. However, the strata and fossils of this interval are not complete in many parts of the world. Based on studies of 43 sites in South China, in particular the continuous sections on the Yangtze platform, we recognize a complete succession including seven graptolite zones and two shelly faunas. In ascending order, the graptolite zones are the Dicellograptus complanatus, Dicellograptus complexus, Paraorthograptus pacificus (including Lower Subzone, Tangyagraptus typicus Subzone and Diceratograptus mirus Subzone), Normalograptus extraordinarius–Normalograptus ojsuensis, Normalograptus persculptus, Akidograptus ascensus and Parakidograptus acuminatus zones. The shelly faunas are the Foliomena–Nankinolithus and Hirnantia faunas, which may be correlated with D. complanatus Zone and N. extraordinarius–N. ojsuensis to part of N. persculptus zones respectively. The biozonation through this interval from the Yangtze region can be correlated with that of other parts of the world such as Dob's Linn in Scotland, Spain and Portugal, Thuringia–Saxonia–Bavaria, Bohemia, Poland, Kazakhstan, Kolyma, Malaya Peninsula, Yukon, Canadian Arctic Islands, Nevada, Argentina, Niger and Victoria, Australia. The Hirnantian Substage, which has been proposed by us recently, includes the N. extraordinarius–N. ojsuensis Zone, Hirnantia fauna and N. persculptus Zone. The base of the Hirnantian Substage is marked by the First Appearance Data (FADs) of N. extraordinarius and N. ojsuensis, which have been determined to be synchronous on a global scale.
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Taveira Pinto, Francisco. « The practice of coastal zone management in Portugal ». Journal of Coastal Conservation 10, no 1 (2004) : 147. http://dx.doi.org/10.1652/1400-0350(2004)010[0147:tpoczm]2.0.co;2.

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Taveira Pinto, Francisco. « The practice of coastal zone management in Portugal ». Journal of Coastal Conservation 10, no 1 (janvier 2004) : 147–57. http://dx.doi.org/10.1007/bf02818951.

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Salgueiro, R., C. Inverno et A. Mateus. « Main characteristics and genesis of the Vale de Pães skarn (Cuba-Vidigueira, Ossa Morena Zone, Portugal) ». Estudios Geológicos 66, no 1 (19 mai 2010) : 65–74. http://dx.doi.org/10.3989/egeol.40150.101.

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Khenkin, S. « Spain in Zone of Turbulence ». World Economy and International Relations, no 4 (2012) : 71–81. http://dx.doi.org/10.20542/0131-2227-2012-4-71-81.

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The global financial and economic crisis abruptly changed the socio-economic and political situation in Spain. While having successfully developed in the decade before the crisis, the country became one of the most unfortunate countries in the EU (the so-called PIIGS group, which also includes Greece, Italy, Portugal and Iceland). After centuries of isolation of Spain integrated into European institutions and started to play a prominent role at the international arena. In the proposed article, the author explores the problems of internal and foreign policy, facing the modern Spain.
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Carvalho, J., E. Ramalho, R. Dias, C. Pinto et R. Ressurreição. « A Geophysical Study of the Carcavai Fault Zone, Portugal ». Pure and Applied Geophysics 169, no 1-2 (19 mai 2011) : 183–200. http://dx.doi.org/10.1007/s00024-011-0318-y.

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Thèses sur le sujet "Zone portuali"

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Virgilio, Damiano. « Studio della comunità microfitoplanctonica del Golfo di Trieste (Mare Adriatico Settentrionale) : utilizzo di una serie storica con particolare riguardo al fenomeno dell'introduzione di taxa alloctoni ». Doctoral thesis, Università degli studi di Trieste, 2008. http://hdl.handle.net/10077/2653.

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2006/2007
Le comunità planctoniche rivestono un ruolo fondamentale nel funzionamento degli ecosistemi marini, contribuendo in maniera sostanziale ai cicli biogeochimici. Il fitoplancton, in particolare, funge da primo anello della rete trofica in quanto, attraverso la fotosintesi permette l’organicazione del carbonio rendendolo disponibile all’interno delle reti trofiche marine. Questo passaggio può avvenire sia attraverso la rete trofica classica sia attraverso il microbial loop. Lo studio quindi della comunità microfitoplanctonica, sia in termini di abbondanze sia di composizione specifica, è un passaggio obbligato per poter capire ed interpretare l’intero sistema pelagico, per conoscerne le potenzialità dal punto di vista sia ecologico sia produttivo, aspetto maggiormente legato alle attività umane. Nella prima parte di questo studio è stata analizzata una serie storica (da marzo 1986 a settembre 2005) inerente la composizione quali-quantitativa della comunità microfitoplanctonica. I dati sono stati ottenuti dall’osservazione di campioni raccolti in una stazione costiera del golfo di Trieste. La serie è stata utilizzata inizialmente allo scopo di evidenziare gli andamenti stagionali della componente microfitoplanctonica ed inoltre per valutare eventuali alterazioni/ modificazioni della struttura del fitoplancton avvenute nel corso del periodo analizzato. Sono state osservate successioni stagionali influenzate principalmente dagli apporti fluviali che in golfo dipendono essenzialmente dal fiume Isonzo, che garantisce nutrienti nei periodi di fine inverno e primavera dando la possibilità alle Bacillariophyceae (o diatomee) di sviluppare le classiche fioriture, e nel periodo autunnale, quando nuovamente le Bacillariophyceae aumentano in abbondanza. Inoltre l’analisi delle serie temporale proposta in questo lavoro (con l’applicazione dell’indice IndVal) evidenzia importanti modificazioni che hanno interessato la componente microfitoplactonica nel corso dei venti anni di osservazioni. Sono stati principalmente segnalati due momenti importanti nel corso del periodo: • a metà degli anni ’90, con la riduzione delle abbondanze dei piccoli flagellati e delle grandi Dinophyceae, lo spostamento delle tipiche fioriture di Skeletonema costatum (Bacillariophyceae) da inizio primavera ad inverno, • dal 2002 la riduzione delle abbondanze delle Bacillariophyceae con la ricomparsa dei piccoli fitoflagellati e la dominanza di specie quali Prorocentrum minimum (Dinophyceae) e Cyclotella sp.p (Bacillariophyceae). L’ipotesi principale è che nel corso degli anni ci sia stato una modificazione nello stato trofico del sistema legato ad una provata riduzione degli apporti d’acqua dolce. In particolare il fosforo è uno dei nutrienti che maggiormente limitano in questa area la crescita microalgale favorendo la presenza di specie che tollerano meglio la carenza di questo nutriente. Questo studio conferma l’utilità di programmi di monitoraggio a lungo termine che rendono possibile l’osservazione delle modificazioni del sistema nel tempo. Inoltre è stato valutato se un set di dati come quello a nostra disposizione potesse tornare utile al fine di valutare l’eventuale segnalazione di nuovi taxa per il golfo di Trieste. Infatti l’alterazione dei sistemi marino costieri può anche influenzare la distribuzione delle specie e conseguentemente favorire le “invasioni biologiche”, fattore oramai considerato in continua crescita, che contribuisce al global change portando a locali alterazioni dei processi ecologici e ad una omogeneizzazione delle comunità. Dai risultati ottenuti appare evidente che il set di dati non è adatto a trarre conclusioni in tali senso, seppure nel corso dei venti anni siano stati rilevati dei taxa di nuova segnalazione che sono diventati parte integrante della comunità microfitoplanctonica del golfo. A tale scopo risulta necessario mettere a punto strategie di campionamento mirate ad una corretta e completa stima della biodiversità, ampliando l’area interessata e con metodologie di analisi che diano la possibilità di stilare liste floristiche complete. Nella seconda parte del lavoro è stata focalizzata l’attenzione sulle zone portuali in quanto prime zone interessate da un eventuale introduzione nonché punto di partenza per molti organismi. Infatti la maggior parte delle introduzioni di specie sono veicolate dalle navi attraverso le acque di zavorra delle navi. Le acque di zavorra sono utilizzate da tutte le navi al fine di mantenere la stabilità durante la navigazioni quando queste viaggiano prive di carico ed ogni giorno enormi quantità di acqua e di sedimenti provenienti da porti e mari di tutto il mondo vengono trasportate attraverso gli oceani come acque di zavorra dalle navi mercantili e scaricate in altre aree geografiche. Quest’acqua viene prelevata dalle aree portuali costiere e trasportata nel porto successivo, ove può venir rilasciata o scambiata. A questo scopo sono stati effettuati sia campionamenti di acque di zavorra (in due importanti porti italiani quali Trieste e Napoli) sia campionamenti nell’area portuale stessa (nel porto di Trieste). Nel caso delle acque di zavorra è stato valutata la comunità microalgale presente sia nell’acqua di zavorra stessa sia nei sedimenti che si accumulano sul fondo delle cisterne (con isolamento di microalghe ancora vitali) mentre nella zona portuale è stata fatta una stima qualitativa della comunità microfitoplanctonica e una stima quali-quantitativa delle forme di resistenza (tipiche degli organismi microfitoplanctonici, in particolare delle Dinophyceae) presenti nei sedimenti del porto (con esperimenti di germinazione di cisti di Dinophyceae). I risultati hanno confermato la potenziale pericolosità di trasporto di organismi microfitoplanctonici attraverso le zavorre e anche la presenza di numerose forme di resistenza nei sedimenti portuali. Sicuramente questo studio sottolinea la necessità di predisporre piani di monitoraggio estesi alle zone portuali (sia delle zavorre delle navi sia del porto stesso) al fine di evidenziare la presenza di nuovi taxa. Questo non potrà certamente permettere di evitare l’introduzione di organismi alloctoni, ma avrà la funzione di primo campanello di allerta.
XIX Ciclo
1976
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Delgado, Mariana Saraiva Mendes. « A crise económica e financeira na União Europeia : Portugal versus Polónia ». Master's thesis, Instituto Superior de Economia e Gestão, 2014. http://hdl.handle.net/10400.5/8416.

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Mestrado em Economia Internacional e Estudos Europeus
A crise da dívida pública europeia, que se seguiu à crise financeira internacional de 2008, ditou o rumo das políticas económicas dos seus países. Através do estudo a dois Estados-membro da União Europeia, Portugal e Polónia, simbolizando respectivamente, a zona euro e os países não pertencentes à UEM, analisam-se, no período entre 2008 e 2013, as respectivas evoluções económicas e as características macroeconómicas prevalecentes. Assim, pretende-se responder aos objectivos propostos, procedendo a: (i) contextualização histórica da crise económica e financeira actual, (ii) revisão da teoria das Zonas Monetárias Óptimas, (iii) análise de indicadores macroeconómicos. As evoluções das economias portuguesa e polaca (2008-2013) demonstram o modo como os dois países, que se encontram em diferentes estágios de maturação económica e de integração europeia, reagiram à crise internacional de 2008. A economia portuguesa, apresentando fortes desequilíbrios macroeconómicos, prosseguiu com um programa de assistência económica e financeira, apresentando a partir de 2013, uma recuperação económica gradual. Por sua vez, a Polónia foi, não só a única grande economia na Europa a evitar uma recessão durante a crise financeira, como apresentou a maior taxa de crescimento dentro da União Europeia - mais de 20%, em termos cumulativos entre 2008 e 2013.
The European sovereign debt crisis, which followed the global financial crisis of 2008, dictated the direction of the economic policies of their countries. Through the analysis of two EU Member States, Portugal and Poland, respectively symbolizing the eurozone countries and non-EMU, are analyzed in the period between 2008 and 2013, their economic developments and the prevailing macroeconomic characteristics of that period. Thus, it is intended to meet the proposed objectives, expressed: (i) historical context of the current economic and financial crisis, (ii) review of the theory of Optimal Monetary zones, (iii) analysis of macroeconomic indicators. The evolutions of the Portuguese and Polish (2008-2013) economies demonstrate how the two countries, which are at different stages of economic maturity and European integration, reacted to the international crisis of 2008. The Portuguese economy with strong macroeconomic imbalances continued with a program of economic and financial assistance, presenting from 2013, a gradual economic recovery. In turn, Poland was not only the only major economy in Europe to avoid a recession during the financial crisis, as had the highest growth rate in the European Union - more than 20% in cumulative terms between 2008 and 2013.
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Mullane, Eta. « The geochemistry of the south Portuguese zone, Spain and Portugal ». Thesis, University of Southampton, 1998. https://eprints.soton.ac.uk/42142/.

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Mass balance calculations illustrate that the incorporation of silicate within sulphide analysis has a variable impact on the REE profiles, depending upon the degree of contamination and the REE characteristics of the silicate phases. Manganiferous Chert Deposits Manganiferous cherts are dominantly biogenic, produced from radiolarian tests, with only minor participation of hydrothermal and hydrogenous sources. Reduced detrital input is necessary for a thriving radiolarian population, and as the depositional basins were compartmentalised and separated by small ridges, this suggests that the surface area of sediment source areas was diminished. Absence of radiolarian tests is attributed to recrystallisation, as tests initially comprise amorphous silica. Chert REE and Nd-isotope geochemistry is variable and this is attributed to the presence or absence of detrital and/or volcanic material, which overprints the initial hydrothermal characteristics. This variation in signature is dominantly controlled by the spatial location of the chert, within the depositional basin., Genetically, both the massive sulphides and chert deposits are independent, the cherts being biogenic and sulphides being hydrothermal. Additionally, both may be precipitated concurrently. It has been previously suggested that sulphides were preserved and oxidation hindered, by the presence of siliceous gel cap. This is not necessary if bottom-hugging brines were present. This factor explains why sulphides are preserved in the absence of a capping horizon.
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Medeiros, Pedro Jorge de Castro Ferreira. « Portugal na Zona Euro : ajustamentos e convergência ». Master's thesis, Instituto Superior de Economia e Gestão, 2008. http://hdl.handle.net/10400.5/994.

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Mestrado em Economia e Estudos Europeus
Decorridos oito anos desde da adesão de Portugal à terceira fase da União Económica e Monetária (UEM), existem já elementos que nos permitem avaliar o impacto dessa adesão no desempenho da economia portuguesa. Assim sendo, a presente tese pretende dar um pequeno contributo na compreensão do fenómeno da UEM, analisando o comportamento da economia portuguesa na Zona Euro face a possíveis choques assimétricos, dentro da temática da Teoria das Zonas Monetárias Óptimas (ZMO). Com base na análise dos dados recolhidos e tratados, facilmente podemos constatar que, segundo os principais critérios da Teoria das ZMO's, Portugal melhorou os seus resultados na maioria dos indicadores, entre o 2.° e o 3.° períodos, sugerindo uma maior consistência na actuação de mecanismos de ajustamento capazes de actuar na eventualidade de virem a ocorrer choques assimétricos. Não obstante os restantes resultados menos favoráveis para Portugal no período 1999¬2005, assistiu-se a uma aproximação económica com a UE, ao nível da correlação nas taxas de crescimento real do PIB, da correlação nas taxas de crescimento do Emprego, da flexibilidade dos salários reais e preços, da variabilidade das taxas de câmbio, do grau de abertura da economia ao exterior e da tendência convergente da estrutura produtiva das exportações com a Zona Euro, permitindo concluir que Portugal encontra¬se numa posição mais solidificada e integrada com a UE, após a sua adesão à Zona Euro.
Eight years have passed since Portugal joined the third phase of Economic and Monetary Union (EMU), which is time enough to give a preliminary evaluation on the Portuguese economy's performance. Thus, the present essay intends to give a small contribution on the comprehension of EMU's event, by analyzing the Portuguese economy's behaviour in the Euro Area, concerning the Optimum Currency Area (OCA)'s theory. Based on the results of data collection and its statistical analyses, we can conclude that, according to the main criteria of the OCA's theory, Portugal presents better results on most of the indicators, between the 2.nd and the 3.rd period, suggesting more consistency of the automatic mechanisms activities to accommodate possible asymmetric shocks. Despite the remaining results less favorable for Portugal between 1999 to 2005, it indicates an approximation of the Portuguese economy to the EU, specially in terms of the correlation on the GDP's real growth rate, of the correlation on growth rate, of the flexibility on the real wages and prices, of the exchange rate's variability, of the degree of economic openness and of the convergent trend on the productive structure of exportation with the EU, showing a more solidified and integrated economy after joining the Euro Area.
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Pereira, Nair dos Santos. « A política monetária não convencional do Banco Central Europeu face à crise na zona euro e a sua Influência na crise económica em Portugal ». Master's thesis, Instituto Superior de Economia e Gestão, 2014. http://hdl.handle.net/10400.5/7793.

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Mestrado em Economia Internacional e Estudos Europeus
Face à crise económico-financeira internacional, eclodida em 2008, que assolou profundamente a Europa, tendo abalado os alicerces desta, o BCE, a atuar no contexto de um «choque assimétrico» (a crise das dívidas soberanas, despontada em 2010, na Zona Euro), teve de reformular as suas funções e tomar medidas de cariz não convencional. Desde a tradicional movimentação das taxas de juro, foi necessário ceder liquidez em quantidades avultadas e, in extremis, intervir no mercado secundário de títulos de dívida. Portugal, enquanto uma das economias mais fragilizadas por este choque, assistiu ao resvalar da sua economia para uma profunda recessão, situação que levou a que o país tivesse de pedir um resgate financeiro. Desta forma, a análise do caso português torna-se pertinente. Averigua-se que a ação do BCE, conjugada com o Programa de Assistência Económica e Financeira, constituiu-se como crucial para impedir o completo desmoronamento da economia portuguesa. A resposta do BCE foi um tanto ou quanto tardia, mas não falhou. Não obstante a incerteza do futuro, almeja-se uma recuperação de Portugal e, em caso de sobrevivência do Euro a esta intempérie, a União Europeia sairá fortalecida em todas as suas vertentes.
Regarding the international economic and financial crisis, that began in 2008, which has deeply strucked Europe, having shaked its foundations, the ECB, acting in a context of an «asymmetric shock» (the sovereign debt crisis emerged in 2010, in the Euro Zone) had to reformulate its functions and to take unconventional measures. Since the traditional movement of the interest rates, it was necessary to provide liquidity in considerable amounts and, in extremis, to intervene in the secondary market of debt securities. Portugal, as one of the economies that had suffered most damage with this shock, has seen its economy plunging into a great recession, a situation which has led the country to ask for a financial bailout. Thus, the analysis of the portuguese case becomes relevant. It can be noticed that the action of the ECB, combined with the Economic and Financial Assistance Programme, was crucial to prevent the complete collapse of the portuguese economy. The response of the ECB was somewhat late, but it hasn?t failed. Despite the uncertainty of the future, it is aimed a full recovery of Portugal and, if the Euro survives this storm, the European Union will be strengthened in all its dimensions.
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Curtis, Michael L. « The structural and kinematic evolution of an upper crustal transpression zone : the Lusitanian Basin, Portugal ». Thesis, Durham University, 1993. http://etheses.dur.ac.uk/5680/.

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The Lusitanian Basin forms a long (250km), narrow (50-100km), NE-SW trending outcrop of inverted Mesozoic carbonates and elastics. The outcrop of the Mesozoic sequence is flanked by two Neogene sub-basins, the contact between which is commonly faulted indicating that the Lusitanian basin underwent inversion during the Miocene. This inversion was achieved by reactivation of Jurassic extensional faults, which were originally formed above reactivated Hercynian basement faults during the Atlantic rifting event. The Serra de Montejunto/Candeeiros fault system (SMCF) forms the eastern boundary to this inverted zone, and is dominated by the NNE trending Serra dos Candeeiros fault (SCF). Towards the northern end of this fault system is a complex, uplifted, 15x20km fault bounded block, the Candeeiros block. At the southern termination of the SMCF, the fault orientation changes abruptly from NNE to ENE. This change in fault orientation coincides with the Serra de Montejunto mountain range, a narrow zone of tectonic uplift. Detailed studies of the main fault zones and adjacent wall rock deformation, allows the kinematics and strain to be characterised. These studies have revealed a complex history of Miocene to Recent reactivation along the boundaries of the Candeeiros block. Initial reactivation of the cross-faults of the block was synthetic to the sinistral SCF. Initial sinistral motion along the cross-faults was superimposed by a late period of dextral transpression, as evidenced by the inverted Alvados pull-apart basin preserved along the Alvados/Minde cross-faults. Dextral transpressive strains along the cross faults of the Candeeiros block, appear to be intimately related to the southerly directed extrusion and anti-clockwise rotation of the block. Structural relationships suggest up to 30 of rotation has occurred. Rotation of the Candeeiros Block is believed to be associated with the change from sinistral simple shear to sinistral transpression along the SCF, during the Late Miocene. The Serra de Montejunto region also displays a complex kinematic history, initiated by N-S shortening across the range, which was superseded by a late stage of sinistral transpression. This transpressive phase manifests itself as both simple and complex transpressive strains. The overall structural geometry of the region is that of a flower structure, formed in a major restraining bend at the termination of the SMCF. The kinematic and deformation style of the early Miocene reactivation in both the Candeeiros and Montejunto regions are consistent with the application of a N-S regional shortening direction, or σ(_1), on the pre-existing Jurassic age structure of the areas. This initial phase of deformation is overprinted by a distinct late phase of deformation related to sinistral transpression along the SCF, which was probably responsible for the inversion of the Lusitanian Basin. The orientation, and chronology of the regional shortening directions responsible for the evolution of the SMCF are in agreement with the relative plate motion history for Africa-Europe (Dewey et al., 1989).A comparison of instrumental seismicity and neotectonic surface faults associated with the SMCF, suggests that the basin is undergoing basement driven sinistral deformation, which is decoupled from the cover sequence by a thick evaporate sequence. The sinistral displacement along the proposed concealed, steep, basement faults appears to be transferred laterally along the sub-horizontal evaporite horizon, for up to 20km, to the steep cover faults of the SMCF.
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Girão, Cristina Josefina Malheiro de Sousa Faria. « Portugal e a UEM : Uma Perspectiva Socioeconómica ». Master's thesis, Instituto Superior de Economia e Gestão, 2012. http://hdl.handle.net/10400.5/10895.

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Mestrado em Desenvolvimento e Cooperação Internacional
No âmbito do Mestrado em Desenvolvimento e Cooperação Internacional, propusemo-nos compreender a situação de Portugal na última década numa perspetiva socioeconómica, beneficiando assim de uma visão retrospetiva respeitante ao processo de integração europeu. Este ensaio não visa prever como irá estar o país daqui a dez ou vinte anos, mas antes contribuir para perceber o que aconteceu desde a entrada em vigor da nova moeda. Está dividido em três partes: A integração económica; O caso português na última década; Hipóteses Futuras.
Under the Master in Development and International Cooperation, we set out to understand the situation of Portugal in the last decade in a socio-economic perspective, thus offering a retrospective view concerning the European integration process. This essay is not intended to predict how the country will be in ten or twenty years, but rather contribute to realize what has happened since the entry into force of the new currency. It is divided into three parts: economic integration, the Portuguese case in the last decade; Hypotheses of the Future.
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Mendes, Maria Helena Acciaioli Homem. « Processos metamórficos variscos na serra da Freita : zona Centro-Ibérica, Portugal ». Doctoral thesis, Universidade de Aveiro, 1997. http://hdl.handle.net/10773/16952.

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Doutoramento em Geociências
Esta tese consiste no estudo de metassedimentos da Serra da Freita. Estes metassedimentos fazem parte do "C.X.Gn. ante - ordovicico e foram intnii'dos por granitos sina tardi e pós D3. Os dados de campo, petrográficos e de química mineral conjugados com conhecimentos prévios, permitiram concluir que o metamorfismo decorreu essencialmente no período final da D2 sin a tardi D3, sendo do tipo de baixa pressão, com paragéneses contendo andaluzite nas zonas de grau médio e alto, prógrado e praticamente isobárico. Localmente, geraram-se associações ricas de distem: estas associações são particularmente importantes nos locais que evidenciam uma intensa circulação de fluidos (grande densidade de veios de quartzo; minerais hidratados); este facto, complementarmente ao reconhecimento da distena ser posterior ao polimorfo de mais baixa pressão, sugere que o aumento de ductilidade (provocado pela hidratação por fluidos metamórficos ascendentes a partir da zona da silimanite) tenha causado aumento local da tensão média, criando-se assim condições que favoreciam a transformação andaluzite-distem. Em zonas subjacentes a este domínio metamórfico foram encontradas, ao longo de uma direcção, paragéneses minerais rnarcadas pela coexistência em equilíírio de cristais de andaluzite de distena e de silimanite. Esta inwlgar ocorrência de associações de ponto triplo foi, provavelmente, resultado da intervenção de dois factores: (a) presença de solução sólida FeA1Si05 nas fases de A12Si05 e (b) o aumento de variância de um grau induzido pela presença adicional de um componente químico - o ferro. O padrão geométrico das isógradas sugerindo "dobramento" é encarado como resultando de várias fases de evolução metamórfica e tectónica: ocorreu inicialmente uma estruturação das superiíces isográdicas durante o metamoriísmo sinD2, a que se sobrepuseram os episódios de deformação, metamorfismo e relaxamento térmico posteriores. Os planos isográdicos foram considerados como superfícies de reajustamento químico sujeitos a uma evolução contínua durante a imposição de regime metamórfico varisco e não como descontinuidades físicas criadas em episódios pontuais.
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Peres, Maria Elisabete. « A solidão dos idosos na zona intra-muros de Évora : estudo exploratório ». Master's thesis, Universidade de Évora, 2000. http://hdl.handle.net/10174/15370.

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Introdução - Confrontada com a necessidade de escolher um tema para dissertação do Mestrado em Sociologia, decidi-me pela "Solidão dos Idosos na zona intra- muros de Évora". As razões de tal escolha são fundamentalmente três: em primeiro lugar a relevância científica e social do tema enquanto indicador da integração e solidariedade sociais; em seguida, o facto de exercer a minha actividade profissional num organismo de Segurança Social a que compete executar as políticas dos governos relativas aos idosos e por fim, a exequibilidade da pesquisa dado o trabalho de campo se ir processar na cidade de Évora, onde vivo, e não implicar a mobilização de recursos financeiros para mim incomportáveis. Fixado o problema a investigar - a solidão - e delimitada a unidade de análise - as pessoas com 65 ou mais anos que vivem "sós" na zona intra-muros da cidade de Évora também designada "Centro Histórico", procurei formular uma ideia orientadora do trabalho subsequente. Após leitura de estudos afins e de contacto com as estatísticas demográficas formulei a seguinte hipótese de trabalho: "a solidão dos idosos depende da teia de relações que estes mantêm com o meio e com a Sociedade em geral". No que respeita aos objectivos Geral e Específico que me proponho são respectivamente: 1-averiguar até que ponto os idosos que vivem isolados no centro histórico de Évora são afectados pelo sentimento de solidão; 2 - avaliar o contributo que as políticas sociais dirigidas aos idosos contribuem para afastar ou diminuir esse mesmo sentimento. Da natureza do assunto a investigar decorreu, natural, a escolha dos métodos a usar - pesquisa documental, entrevista semi-estruturada e observação directa, Toda a informação recolhida foi estruturada em cinco capítulos, procedendo em cada um deles a uma revisão bibliográfica. No primeiro, que intitulo O Envelhecimento Demográfico., fixo a emergência histórica deste fenómeno e sua difusão diferencial no espaço e ponho em evidência o aumento contínuo da percentagem de pessoas que vivem "sós" No segundo capítulo caracterizo o Envelhecimento Individual da perspectiva fisica, psíquica e social e detenho-me a conceptualizar a solidão, dado ser o principal conceito estruturante da minha pesquisa. Clarificados os conceitos de envelhecimento e solidão, descrevo no capítulo terceiro as Metodologias a aplicar no trabalho de campo ou seja, a entrevista semi-estruturada e a observação directa. No capítulo quarto, que constitui o núcleo deste estudo, analiso a informação provocada na entrevista e que procurei completar com a observação directa efectuada no processo da mesma. No capítulo final, o quinto, intitulado Políticas de velhice e solidão intento, de algum modo, aferir se a solidariedade oferecida aos idosos, sob as mais diversas formas, é apta para imunizar ou pelo menos atenuar o sentimento de solidão que ronda o seu isolamento. Mais do que com uma conclusão, termino com a síntese dos conhecimentos adquiridos e com a sugestão de pesquisas futuras neste âmbito, uma vez que os resultados obtidos não poderão ser extrapolados para outro universo.
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Maylle, Gamarra Franklin. « Variabilidad hidrográfica en la zona de operaciones del Terminal Portuario de Salaverry ». Bachelor's thesis, Universidad Nacional Mayor de San Marcos, 2018. https://hdl.handle.net/20.500.12672/7807.

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Publicación a texto completo no autorizada por el autor
Determinar la variabilidad hidrográfica en la zona de operaciones del Terminal Portuario de Salaverry (TPS). Para este fin se realizó el levantamiento hidrográfico en la zona de estudio. Se aplicó diferentes dispositivos de acústica submarina y sensores complementarios para lograr y cumplir con el objetivo propuesto. El estudio examina diferentes datos históricos de profundidad recolectados de diferentes fuentes y la estimación de cálculo de volúmenes de los sedimentos ingresados en las áreas acuáticas de interés por la empresa de Puertos ENAPU S. A., y de acuerdo a los resultados obtenidos garantizar la operatividad eficiente de dicho puerto para el ingreso y salida de buques con calados de hasta 10 m. Los variable temperatura, salinidad y presión son trascendentes para la medición de profundidad, estos parámetros físicos influyen directamente a la propagación de velocidad de sonido, cuantificando que no se encontró variaciones significativas en estos parámetros durante los levantamientos hidrográficos, (ver figura 1 y 2). Las profundidades en las áreas acuáticas del TPS oscilan entre 9 y 11 m en el centro de las áreas de amarradero, atraque y canal de ingreso, mientras que en las cercanías de los muelles 1A, 2A, 1B, 2B, cabezos del muelle y cerca al litoral costero oscilan entre los 5 y 8 m. de profundidad. El resultado de estimación del ingreso de sedimento con datos de hidrográfico registró un valor de 828’205.6 m3/año con un error de - 0.19 % con respecto al estudio realizado por Maldonado (2009), en el lugar y - 3.33 % con respecto a lo determinado por Castro (2015).
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Livres sur le sujet "Zone portuali"

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Nardi, Carla. Il Tevere e la città : L'antica magistratura portuale nei secoli XVI-XIX. Roma : Multigrafica, 1989.

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Belas-Artes, Academia Nacional de. Inventário artístico de Portugal. : Zona de Nordeste. Lisboa : Academia Nacional de Belas-Artes, 1991.

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Pinto, A. Mendonça. Política económica, em Portugal e na Zona Euro. Cascais : Principia, 1999.

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Matos, João (João X.), author, Fernandes, Paulo (Paulo Manuel Carvalho), author et Oliveira J. T. author, dir. Palynostratigraphy and systematic palynology of the Devonian and Carboniferous successions of the South Portuguese Zone, PORTUGAL. Lisboa : Ministério da Economia e da Inovação, SECRETARIA DE ESTADO DA INDÚSTRIA E DA INOVAÇÃO, INSTITUTO NACIONAL DE ENGENHARIA, TECNOLOGIA E INOVAÇÃO, 2008.

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López, Norberto Aurelio. Relevamiento de la zona portuaria de la ciudad de Buenos Aires, 1536-1987. Buenos Aires : Junta de Estudios Históricos del Puerto Nuestra Señora Santa María de Buen Ayre, 1987.

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Histórico, Portugal Arquivo, Aomen ji jin hui, Guangdong Sheng li Zhongshan tu shu guan et Aomen da xue. Tu shu guan, dir. Putaoya Wai jiao bu cang Puguo zhu Guangzhou zong ling shi guan dang an : Qing dai bu fen, Zhong wen. Guangzhou Shi : Guangdong jiao yu chu ban she, 2009.

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Leão, Cláudio Carvalho. Marginalisation et développement des zones de montagnes méditerranéennes : Le cas de la commune de Soajo au Portugal. Montpellier : Institut agronomique méditerranéen de Montpellier, 1986.

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Cong Guangzhou tou shi zhan zheng : Putaoya zhu Guangzhou zong ling shi Mojiadu guan yu Zhong Ri zhan zheng de bao gao. Shanghai : Shanghai she hui ke xue yuan chu ban she, 2000.

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Eduardo, Calvo Rojas, et García Pérez Marta, dir. La ordenación urbanística y la Ley de puertos : Jornadas de Estudio celebradas en el Consorcio por a Zona Franca, Vigo, 15 y 16 de junio de 1994. [Vigo] : Consorcio da Zona Franca de Vigo, 1994.

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Thompson, William R., et Leila Zakhirova. The Netherlands : Not Quite the First Modern Economy. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780190699680.003.0006.

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In this chapter, we look at four cases: Genoa, Venice, Portugal, and the Netherlands. Genoa, Venice, and Portugal acted as transitional agents over a five- to six-hundred-year period, creating sea power and trading regimes to move Asian commodities and innovations to and from European markets. While Genoa and Venice were primarily Mediterranean-centric, Portugal led the breakthrough from the constraints of the inland sea and inaugurated Europe’s Atlantic focus. None of these actors possessed the power of China nor subsequent global actors, but for their age, they were critical technological leaders, providing a technological bridge from the eastern zone of Eurasia to the western zone. The Netherlands fits into this narrative by combining Baltic and Atlantic activities to construct a European trade regime that greatly overshadowed the earlier transitional efforts. Buttressed by the development of agrarian and industrial technology and a heavy reliance on peat and wind as energy sources, the Dutch case seems idiosyncratic. Most critically, its energy transition was only partial. Although the Netherlands made clear advances in some power-driven machinery and technological innovation , the heat and energy that were expended remained constrained by the inherent limitations of the energy sources.
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Chapitres de livres sur le sujet "Zone portuali"

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Correia, Paulo V. D., et Inês Calor. « Portugal ». Dans Regulating Coastal Zones, 127–46. New York : Routledge, 2020. | Series : Urban planning and environment : Routledge, 2020. http://dx.doi.org/10.4324/9780429432699-7.

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Carvalho, José Martins, Maria José Afonso, José Teixeira, Liliana Freitas, Ana Rita Lopes, Rosário Jesus, Sofia Batista, Rosário Carvalho et Helder I. Chaminé. « Groundwater Favourable Infiltration Zones on Granitic Areas (Central Portugal) ». Dans Advances in Sustainable and Environmental Hydrology, Hydrogeology, Hydrochemistry and Water Resources, 317–19. Cham : Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01572-5_75.

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Oliveira, D. P. S. de, L. J. Robb et C. M. C. Inverno. « The São Martinho gold occurrence, NE Ossa Morena Zone, Portugal : Geological setting and ore genesis ». Dans Mineral Deposits at the Beginning of the 21st Century, 791–93. London : CRC Press, 2022. http://dx.doi.org/10.1201/9781003077503-201.

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Sá, A. A., J. C. Gutiérrez-Marco, C. A. Meireles, D. C. García-Bellido et I. Rábano. « A Revised Correlation of Lower Ordovician Sedimentary Rocks in the Central Iberian Zone (Portugal and Spain) ». Dans Springer Geology, 441–45. Cham : Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_85.

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Zeferino, Joel, Maria Rosário Carvalho, Tânia Ferreira, Maria Catarina Silva, Maria José Afonso, Liliana Freitas, Ana Rita Lopes et al. « Forecasting and Mass Transport Modelling of Nitrates in the Esposende–Vila Do Conde Nitrate Vulnerable Zone (Portugal) ». Dans Advances in Sustainable and Environmental Hydrology, Hydrogeology, Hydrochemistry and Water Resources, 95–98. Cham : Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01572-5_23.

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« Portugal ». Dans Entrepreneurship and SMEs in the Euro-Zone, 166–80. PUBLISHED BY IMPERIAL COLLEGE PRESS AND DISTRIBUTED BY WORLD SCIENTIFIC PUBLISHING CO., 2006. http://dx.doi.org/10.1142/9781860948077_0012.

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« Coastal Zone Management ». Dans OECD Environmental Performance Reviews : Portugal 2011, 147–67. OECD, 2011. http://dx.doi.org/10.1787/9789264097896-10-en.

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Ugalde, Esther Gimeno. « Paradoxes and Mediation Pitfalls of the Translational Contact Zone ». Dans Iberian and Translation Studies, 21–48. Liverpool University Press, 2021. http://dx.doi.org/10.3828/liverpool/9781800856905.003.0002.

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By assuming the intersection between Iberian and translation studies to be a new, fruitful disciplinary contact zone, this chapter contends that Iberian studies’ polycentric and multidirectional approach opens up the possibility for new modes of rethinking and analyzing intra-Iberian literary translation, overcoming a dualistic propensity that more often than not distorts our perspective and prevents us from discovering subtle and veiled power dynamics. Based on a study of Catalan novels translated in twenty-first-century Portugal (2000–19), it explores multiple phenomena arising from this specific contact zone, including literary biliterariness, (opaque) self-translation, and indirect translation. Ultimately, the chapter aims to examine the consequences and paradoxes resulting from the complexity of the Catalan literary landscape that become more visible when Catalan literature is translated into Portuguese.
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Silva de Oliveira, Aline, Joaquim Sande Silva, José Gaspar, Nuno R. G. Nunes Guiomar et Paulo M. Fernandes. « Is native forest an alternative to prevent wildfire in the WUI in Central Portugal ? » Dans Geografia, Riscos e Proteção Civil. Homenagem ao Professor Doutor Luciano Lourenço. Volume 2, 67–77. RISCOS - Associação Portuguesa de Riscos, Prevenção e Segurança, 2021. http://dx.doi.org/10.34037/978-989-9053-06-9_1.2_05.

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he expansion of the 2017 mega-fires in Portugal was observed to be locally halted by native forest patches. Here we present spatial simulation scenarios of fire behaviour to assess whether native forest cover mitigates fire spread during extreme wildfire conditions in wildland-urban interface (WUI) areas around Industrial Zones (IZs). Our results suggest that broadleaved forest cover can reduce fireline intensity and rate of spread around IZs up to 20 and 8 times, respectively, on average. Thus, our results support the need to discuss forest management in Portugal to better prevent WUI fires.
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NDOUR, Issa. « Les Luso-africains de la Sénégambie ». Dans Les Annales du Sud, No. 1, 99–112. Editions des archives contemporaines, 2023. http://dx.doi.org/10.17184/eac.7239.

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Entre les XVIe et XVIIe siècles s’étaient développés sur la Petite-côte de nombreux comptoirs notamment à Rufisque et à Portudal qui devinrent de véritables zones de brassages culturels entre Européens et Africains. Dans ces lieux de traite s’étaient établis des Luso-africains appelés Lançados qui, de par leur implication dans le commerce de l’ivoire, des peaux, du cuir et des esclaves, eurent une influence économique considérable. Grâce à une forte présence sur la côte et un monopole de fait sur les transactions, ils étaient devenus les intermédiaires incontournables dans le commerce entre les traitants européens et les fournisseurs africains. En effet, installés par petits groupes, les Lançados étaient en rapport les uns des autres, étendant sur tout le littoral un vaste réseau commercial. Leur poids économique grandissant suscita l’hostilité du Portugal qui promulgua une législation visant à enrayer cette communauté, mais cette entreprise n'eut jamais le succès escompté. Car ces Luso-africains entretenaient des relations privilégiées avec les souverains des royaumes côtiers du Kajoor, du Bawol et du Siin dans lesquels ils résidaient. Toutefois, la perte du monopole commercial par les Portugais et les relations souvent conflictuelles avec certains chefs africains vont réduire de manière sensible leur nombre sur le littoral de la Sénégambie septentrionale à la fin du XVIIe siècle.
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Actes de conférences sur le sujet "Zone portuali"

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Jiang, Shan, Laura Viña-Arias, Christopher Zegras, Joseph Ferreira et Marta Gonzalez. « Calling for validation : demonstrating the use of mobile phone data to validate integrated land use transportation models ». Dans Virtual cities and territories. Coimbra : Department of Civil Engineering of the University of Coimbra and e-GEO, Research Center in Geography and Regional Planning of the Faculty of Social Sciences and Humanities of the Nova University of Lisbon, 2011. http://dx.doi.org/10.5821/ctv.7696.

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In this paper we demonstrate the use of a particular source of ICT data, Mobile phones, generated and provided by a mobile phone service provider, to help validate an integrated land use transportation (LUT) model calibrated for the Lisbon, Portugal, metropolitan area (hereafter LMA). Specifically, we use 1 month of anonymous data provided by a private cell phone network operator. These data allowed us to identify, for each phone, all phone activity, localized to the nearest cellular telephone tower (601 towers in LMA). We use the cellular phone towers to generate analysis zones consistent with existing statistical and administrative boundaries (i.e., census blocks and civil parishes). We also infer, for each cell phone tower analysis zone, the number of phones that “reside” and/or “work” in that zone, based on the phone activity profile generated over the observed month.
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Granja, Helena, et Eduardo Loureiro. « Why Are Shingle Beaches Replacing Sandy Beaches ? (Coastal Zone of NW Portugal) ». Dans Sixth International Symposium on Coastal Engineering and Science of Coastal Sediment Process. Reston, VA : American Society of Civil Engineers, 2007. http://dx.doi.org/10.1061/40926(239)41.

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Oliveira, Antonio, Helena Brites et Fernando Noronha. « PETROGRAPHY AND WHOLE-ROCK GEOCHEMISTRY OF VAUGNERITES FROM NW PORTUGAL (CENTRAL IBERIAN ZONE) ». Dans 20th SGEM International Multidisciplinary Scientific GeoConference Proceedings 2020. STEF92 Technology, 2020. http://dx.doi.org/10.5593/sgem2020/1.1/s01.029.

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Fidalgo, Paulo, Rui Almeida, Elsa Caetano, Álvaro Cunha et Paulo Cachim. « Tree Top Walk at Serralves Park, Portugal ». Dans Footbridge 2022 (Madrid) : Creating Experience. Madrid, Spain : Asociación Española de Ingeniería Estructural, 2021. http://dx.doi.org/10.24904/footbridge2022.184.

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<p>The current paper describes the structure and the dynamic behaviour of a footbridge built in Serralves Park at Porto, Portugal. The footbridge, named Tree Top Walk, is located in a slope in the park at the height of the top of the trees. Because it is in a slope, the footbridge develops with an irregular U-shape at a constant level. The total length of the footbridge is approximately 250 m. At its highest level, the height is 15 m.</p><p>Approximately at one third of the course there is a passage between the two branches of the U. At this zone, there is a staircase that allows to reach the footbridge at the middle of its course, from the woods and a small amphitheatre at a level of 14 m. The structure of the deck is made with timber while the columns are made with steel covered with timber across their height and the connection between the columns and the deck is performed with timber struts placed in the longitudinal and transversal directions. Three of the columns are made with a circular profile, while the others are 4-foot tubes connected at the top by a circular tube with</p><p>2.35 m length. The deck is made with four longitudinal girders with a cross section of 8x52 cm. Spans have different lengths, ranging from 5 to 14,34 m. In total there are 23 spans and 22 columns. In the structural analysis, dead loads, live loads, wind and earthquake actions were considered. To assess the dynamic behaviour of the structure, dynamic tests have been carried out. The performed tests include an ambient vibration test, the determination of the damping level and tests with pedestrians.</p>
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Stojkov, Stefan, Emilija Beker Pucar, Olgica Glavaški et Marina Beljić. « Exchange Rate Pass-Through Asymmetry : The Case of the Euro-Zone ». Dans 27th International Scientific Conference Strategic Management and Decision Support Systems in Strategic Management. University of Novi Sad, Faculty of Economics in Subotica, 2022. http://dx.doi.org/10.46541/978-86-7233-406-7_218.

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An essential aspect of deepening the level of economic integration between European economies is the reduction of mutual economic disparities, which is especially emphasized by the formation of the supranational monetary authority of the Euro-zone member states. However, fixing the currency for the euro and losing monetary sovereignty in the circumstances of a structurally heterogeneous system meant that the same monetary policy provoked different repercussions for member states. This research aims to point out the differences in the exchange rate transmission mechanism between the representatives of two groups of Euro-zone member states: the core of the EZ (Germany, Finland, Belgium, and France) and the periphery of the EZ (Greece, Spain, Portugal, Ireland), in the 1999M1-2021M1 time horizon. Empirical findings are based on estimates of the VAR model, i.e. derived impulse response functions in the circumstances of shock transmission (nominal effective exchange rate) to inflation (consumer price index). The results of the research indicate the asymmetry of the exchange rate transmission mechanism in terms of a more pronounced and longer degree of exposure of peripheral economies to shocks of the nominal exchange rate compared to the representatives of the core of the Euro-zone. Empirical findings confirm the asymmetry of the exchange rate transmission mechanism as one of the indicators of the weakness of the Euro-zone, given the inflationary diversity and the consequent anomalies of the monetary union with heterogeneous membership.
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Oliveira, Antonio, Helena Brites et Helena Sant Ovaia. « INSIGHTS INTO THE FELSIC VEIN MAGMATISM IN NORTHERN PORTUGAL (CENTRAL IBERIAN ZONE) : AN INTEGRATED GEOCHEMICAL AND PETROPHYSICAL STUDY ». Dans 20th SGEM International Multidisciplinary Scientific GeoConference Proceedings 2020. STEF92 Technology, 2020. http://dx.doi.org/10.5593/sgem2020/1.1/s01.018.

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Goncalves, Ana. « IDENTIFICATION OF HYDROTHERMAL ALTERATION ZONES IN GRANITIC AREAS USING MAGNETIC SUSCEPTIBILITY. AN EXAMPLE IN NW PORTUGAL ». Dans 17th International Multidisciplinary Scientific GeoConference SGEM2017. Stef92 Technology, 2017. http://dx.doi.org/10.5593/sgem2017/13/s03.049.

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Gamito, Margarida, et Fernando Moreira Da Silva. « UrbanCroma : Chromatic Methodology applied to Oeiras Municipality, Portugal ». Dans 13th International Conference on Applied Human Factors and Ergonomics (AHFE 2022). AHFE International, 2022. http://dx.doi.org/10.54941/ahfe1001997.

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This paper presents a research work, inserted in the post-Doctoral applied investigation which aims to test and validate this new methodology. UrbanCroma, the chromatic planning methodology for urban furniture which was applied in Oeiras Municipality, is part of a theoretical and practical work carried out during the research for a PhD thesis, in which the present methodology was developed. Thus, UrbanCroma is mainly intended to be applied into the elaboration of chromatic plans for urban furniture, whose needs do not completely correspond to those proposed by other existing methodologies, destined almost exclusively to be applied to the built environment, i.e., to architecture. These chromatic plans, allow the full performance of Urban Furniture functions, improving its use, and transforming it in a factor of inclusivity, as its elements will become more visible and legible as they stand out from the surrounding environment, whether being built or landscape. Likewise, this methodology has an identification and orientation function, since its elements will constitute harmonic chromatic sets that, although they establish a strong contrast with the surrounding environment, respect the local chromatic traditions, identify the neighborhoods or urban areas and, by their variation, constitute orientation landmarks throughout the city. In this case study ─ Oeiras Municipality ─ that have settlements both on the interior and on the sea front, and is at the same time a miscellanea of old and contemporary, were chosen three different localities: Laje, Carnaxide Historic Center, and a new urban area of Carnaxide. These locals, that encompass social neighborhoods, traditional settlements and modern building urbanizations, inevitably have several characteristics that allow the application of this methodology to a wide range of neighborhoods. So, UrbanCroma application starts by choosing samples areas, which will encompass the case study most representative zones, applying there the new methodology to all furniture elements, in order to increase their potentiality as relevant issues for city color planning. In all these intervention areas, all the colors present in the environment are recorded, being it built or landscape, taking in account all the changes due to climatic variations and the non-permanent colors, whose presence has enough importance to be considered as environmental colours. All these colors were, then, registered in files and maps, in order to create a data-base allowing the identification of all environmental colors. The set of these colors permitted the establishment of the local dominant colors and, these ones, along with the contribute of the local history and culture, constitute the scientific basis upon which, it was established a very comprehensive urban furniture chromatic plan, with scientific rigor, for Oeiras Municipality case study.
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Álvarez, Juan Camilo. « Mis manos limpias previenen enfermedades y salvan vidas ». Dans Encuentros Diseño Social RAD 2020. Bogotá, Colombia : Red Académica de Diseño - RAD, 2021. http://dx.doi.org/10.53972/rad.etrads.2020.1.154.

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El agua es el recurso más valioso para el desarrollo de la vida. En un país como Colombia el agua es abundante. En efecto, Colombia es uno de los países con más fuentes de agua dulce del mundo y el río Magdalena es un ejemplo de ello. Este es el río más grande del territorio nacional. Por ello mismo, a lo largo y ancho de sus riberas residen muchas poblaciones. Entre ellas está el corregimiento de Palermo del municipio Sitionuevo. El acceso a servicios públicos como el agua potable es fundamental para un desarrollo social digno. Paradójicamente, a pesar de su ubicación, dicho corregimiento no cuenta con servicio de acueducto y agua potable. Aunque no posea agua potable, el municipio de Palermo cuenta con un puerto, una sociedad portuaria y una zona franca. Entre las empresas que conforman la zona franca está la Fundación Buenamar del grupo Coremar, que se encarga de la enseñanza de deportes y artes para los niños del corregimiento.
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Carvalho, Ana, Ricardo Ribeiro, Rui Moura et Alexandre Lima. « GEOPHYSICAL EXPLORATION OF ANTIMONY MINERALIZATIONS : ALTO DO SOBRIDO AND RIBEIRO DA SERRA MINES (PORTUGAL) ». Dans 22nd SGEM International Multidisciplinary Scientific GeoConference 2022. STEF92 Technology, 2022. http://dx.doi.org/10.5593/sgem2022/1.1/s03.033.

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The Alto do Sobrido and Ribeiro da Serra Mines, are two antimony-gold mines located in Gondomar, Portugal, and are part of the Durico-Beirao Mining District (DBMD). In this work, we use four geophysical methods, such as gravity, radiometry, magnetic and electromagnetic, to improve the knowledge about these mineralizations and the lithologies and structures associated with them. These four methods allowed us to study these mineralizations through different physical properties. The gravimetric method allowed us to add more data to the hypothesis that the goldantimony mineralizations of the DBMD could be genetically associated with a nonoutcropping granite intrusion, which functioned either as a heat engine that promoted the circulation of fluids and/or as a source of fluids and metals itself. A 2D model was proposed, created with both modelling and inversion, to show that the presence of this granite could indeed fit the response of the negative anomalies found in the residual anomaly. The radiometric method was used mainly as a mapping tool, where we were able to distinguish between some of the lithologies of the area, like the Lower Ordovician quartzites and the metasediments of the Middle Ordovician to the Carboniferous, but also to observe different element concentrations within the Pre-Ordovician SchistGreywacke Complex (SGC). These variations within the SGC lithology don�t have a clear explanation as to why they occur. Still, we believe that they could occur due to the influence of the abovementioned non-outcropping granite. With the very low frequency (VLF) electromagnetic method, it was possible to locate areas of lower resistivities that correspond to the location of several known mineralized veins, as well as the probable location for a new vein. It was also possible to observe some weathered rocks near faults and fractures associated with the Durico-Beirao Shear Zone (DBSZ). With the magnetic method, it is possible to contribute to areas with the prevalence of lithologies and minerals with higher magnetic susceptibilities. Several magnetic anomalies found near the Alto do Sobrido mining works correspond to the mineralized veins paragenesis. Other anomalies appear to be related to the location of faults and fractures associated with the DBSZ. The use of all these methods allowed us to observe the mineralization responses and its associated lithologies and structures through the different geophysical properties while adding knowledge about the genesis of these mineralizations and possibly the location of new mineralized veins.
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Rapports d'organisations sur le sujet "Zone portuali"

1

Romano, M. Lower To Middle Ordovician Trace Fossils From the Central Iberian Zone of Portugal and Spain. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132188.

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