Relevant bibliographies by topics / Val Canale

Academic literature on the topic 'Val Canale'

Author: Grafiati
Published: 11 March 2023

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Journal articles on the topic "Val Canale"

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Gelli, Annica. "Acque vive: le gore di Colle di Val d'Elsa e gli edifici andanti a acqua." STORIA URBANA, no. 125 (April 2010): 133–49. http://dx.doi.org/10.3280/su2009-125007.

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La cittŕ di Colle di Val d'Elsa deve il suo sviluppo alla presenza dell'acqua e agli opifici che potevano funzionare mediante l'energia idraulica. Nella vallata sottostante il centro medievale di Onci ricche sorgenti perenni, opportunamente incanalate, vanno a rinvigorire il fiume Elsa. Nel XII secolo l'unico modo per sfruttare tali acque fu deviarne la quasi totalitŕ in un canale artificiale, la gora, la quale seguendo il naturale dislivello morfologico del terreno arrivava fin dentro il Piano della cittŕ, una vera e propria area manifatturiera. Successive scissioni e prolungamenti dei canali corrisposero all'aumento degli edifizi andanti ad acqua, gualchiere, roterie, mulini e soprattutto cartiere. Nel Settecento la forza delle acque, regolata ed aumentata mediante delle cadute, riusciva a muovere ben diciassette opifici ma la crisi del mercato cartario amplificava le contese fra i proprietari. Č in questo secolo di declino economico che si hanno i documenti cartografici e le relazioni idrauliche piů interessanti, redatte da Ferdinando Morozzi ed altri ingegneri granducali chiamati ad intervenire direttamente dal Comune o dall'Appalto della Carta
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Prenger-Berninghoff, K., V. J. Cortes, T. Sprague, Z. C. Aye, S. Greiving, W. Głowacki, and S. Sterlacchini. "The connection between long-term and short-term risk management strategies for flood and landslide hazards: examples from land-use planning and emergency management in four European case studies." Natural Hazards and Earth System Sciences 14, no. 12 (December 5, 2014): 3261–78. http://dx.doi.org/10.5194/nhess-14-3261-2014.

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Abstract. Adaptation to complex and unforeseen events requires enhancing the links between planning and preparedness phases to reduce future risks in the most efficient way. In this context, the legal–administrative and cultural context has to be taken into account. This is why four case study areas of the CHANGES1 project (Nehoiu Valley in Romania, Ubaye Valley in France, Val Canale in Italy, and Wieprzówka catchment in Poland) serve as examples to highlight currently implemented risk management strategies for land-use planning and emergency preparedness. The focus is particularly on flood and landslide hazards. The strategies described in this paper were identified by means of exploratory and informal interviews in each study site. Results reveal that a dearth or, in very few cases, a weak link exists between spatial planners and emergency managers. Management strategies could benefit from formally intensifying coordination and cooperation between emergency services and spatial planning authorities. Moreover, limited financial funds urge for a more efficient use of resources and better coordination towards long-term activities. The research indicates potential benefits to establishing or, in some cases, strengthening this link through contextual changes, e.g., in organizational or administrative structures, that facilitate proper interaction between risk management and spatial planning. It also provides suggestions for further development in the form of information and decision support systems as a key connection point. 1 Marie Curie ITN CHANGES – Changing Hydro-meteorological Risks as Analyzed by a New Generation of European Scientists
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Prenger-Berninghoff, K., V. J. Cortes, T. Sprague, Z. C. Aye, S. Greiving, W. Głowacki, and S. Sterlacchini. "The connection between long-term and short-term risk management strategies: examples from land-use planning and emergency management in four European case studies." Natural Hazards and Earth System Sciences Discussions 2, no. 4 (April 30, 2014): 3137–82. http://dx.doi.org/10.5194/nhessd-2-3137-2014.

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Abstract. The need for continuous adaptation to complex and unforeseen events requires enhancing the links between planning and preparedness phases to reduce future risks in the most efficient way. In this context, the legal-administrative and cultural context has to be taken into account. This is why four case study areas of the CHANGES1 project (Nehoiu Valley in Romania, Ubaye Valley in France, Val Canale in Italy, and Wieprzówka catchment in Poland) serve as examples to highlight currently implemented risk management strategies for land-use planning and emergency preparedness. The strategies described in this paper were identified by means of exploratory and informal interviews in each study site. Results reveal that a dearth or, in very few cases, a weak link exists between spatial planners and emergency managers. Management strategies could benefit from formally intensifying coordination and cooperation between emergency services and spatial planning authorities. Moreover, limited financial funds urge for a more efficient use of resources and better coordination towards long-term activities. The research indicates potential benefits to establishing or, in some cases, strengthening this link and provides suggestions for further development in the form of information and decision support systems as a key connection point. Aside from the existent information systems for emergency management, it was found that a common platform, which integrates involvement of these and other relevant actors could enhance this connection and address expressed stakeholder needs. 1 Marie Curie ITN CHANGES – Changing Hydro-meteorological Risks as Analyzed by a New Generation of European Scientists.
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Singh Raju, Rajender, Panna Mangat, Saleem Azhar, and Sana. "C-Shaped canal system - A Case report." UNIVERSITY JOURNAL OF DENTAL SCIENCES 6, no. 2 (August 28, 2020): 83–85. http://dx.doi.org/10.21276/ujds.2020.6.2.12.

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ABSTRACT C-shaped canals are anatomic variants in root canal morphology. This c-shaped configuration should be diagnosed earliest as it influences the management of such cases more efficiently. They pose challenges in shaping, cleaning and obturating protocols. We require a file system which can contact and shape all possible surfaces of the c-shaped canal. Some of these file systems are XP-endo shaper files (FKG), SAF (ReDent NOVA). For cleaning, advocated systems are XP- endo finisher files (FKG), SAF, ultrasonic files like irrisafe, sonic files (endo-activator), endo-vac system. 3-D obturation should be done wih downpack and backfill technique (warm vertical or continuous wave of compaction)
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Jousseaume, Valérie, and Denis Mercier. "Processus et acteurs de l'aménagement de la zone inondable du Val nantais. Réflexions sur la prise de risque d'une société prométhéenne." Cahiers Nantais 64, no. 1 (2005): 23–42. http://dx.doi.org/10.3406/canan.2005.1155.

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Desbiens, Caroline, and Bastien Sepúlveda. "Pekedamkam: frontierism and the unearthing of indigenous landscapes in Val-d'Or, Canada." Journal of Historical Geography 65 (July 2019): 59–72. http://dx.doi.org/10.1016/j.jhg.2019.06.006.

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Bleck, Rainer, Howard Bluestein, Lance Bosart, W. Edward Bracken, Toby Carlson, Jeffrey Chapman, Michael Dickinson, et al. "Eighth Cyclone Workshop Scientific Summary, Val Morin, Quebec, Canada, 12–16 October 1992." Bulletin of the American Meteorological Society 74, no. 7 (July 1993): 1361–73. http://dx.doi.org/10.1175/1520-0477-74.7.1361.

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Beaudoin, Georges, and David Pitre. "Stable isotope geochemistry of the Archean Val-d‘Or (Canada) orogenic gold vein field." Mineralium Deposita 40, no. 1 (May 24, 2005): 59–75. http://dx.doi.org/10.1007/s00126-005-0474-z.

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Strain, Ellen. "Stereoscopic Visions: Touring The Panama Canal." Visual Anthropology Review 12, no. 2 (September 1996): 44–58. http://dx.doi.org/10.1525/var.1996.12.2.44.

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Boullier, Anne-Marie, and François Robert. "Palaeoseismic events recorded in Archaean gold-quartz vein networks, Val d'Or, Abitibi, Quebec, Canada." Journal of Structural Geology 14, no. 2 (February 1992): 161–79. http://dx.doi.org/10.1016/0191-8141(92)90054-z.

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Dissertations / Theses on the topic "Val Canale"

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Boccali, Chiara. "Caratterizzazione e modellazione di colate detritiche." Doctoral thesis, Università degli studi di Trieste, 2014. http://hdl.handle.net/10077/10126.

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2012/2013
La ricerca si inserisce all’interno dei numerosi lavori che da ormai qualche decennio hanno come scopo lo studio delle colate detritiche, fenomeni altamente pericolosi e distruttivi che hanno determinato e determinano la morfologia della rete idrografica secondaria, incrementando il rischio idrogeologico nei bacini montani dell’arco alpino e non solo. I bacini montani del Friuli Venezia Giulia risultano particolarmente vulnerabili dal punto di vista idrogeologico per i pesanti condizionamenti orografici, geologico-strutturali e sismici, che generano la coesistenza di tutti quei fattori negativi determinanti per l’innesco dei fenomeni di colate. Questo lavoro si è occupato del settore più orientale dell’arco alpino del Friuli Venezia Giulia: il bacino del fiume Fella e, nel dettaglio, la Val Canale, che nell’ultimo secolo è stata interessata da circa 20 eventi alluvionali “eccezionali”, con conseguente innesco di colate detritiche. Il ricordo più vivo è certamente quello dell’ultimo evento di piena, registrato a fine Agosto 2003, che dalla Val Canale al Canal del Ferro ha generato più di 1100 fenomeni franosi ed alluvionali, causando la perdita di due vite umane e danni stimati attorno al miliardo di euro. A tale disastroso evento hanno fatto seguito numerosi studi specifici da parte della Protezione Civile regionale, del Servizio Geologico e di diversi team di esperti, volti alla definizione e alla delimitazione dei fenomeni e, soprattutto, delle aree di pericolosità, nonché alla progettazione di adeguate opere di mitigazione con lo scopo di prevenire danni futuri. Proprio per l’abbondanza di dati già esistenti e per, purtroppo, l’abbondanza e la frequenza dei fenomeni di colata detritica in quest’area dell’arco alpino, è stato scelto di sviluppare la ricerca nell’ottica di individuare una metodologia valida ed adatta alla caratterizzazione dei bacini da colata e dei loro depositi. Tale metodo vorrebbe garantire la realizzazione di una modellazione numerica quanto più rispondente al vero, proprio perché compiuta a partire da dati reali e non solamente da informazioni di back analysis, che spesso vengono dedotte applicando modelli da letteratura, studiati e sviluppati in tutt’altre aree dell’arco alpino, dell’Europa e del mondo. Con tali scopi sono stati scelti sei bacini ricadenti nella Val Canale e nella Val Pontebbana, simili per il comportamento dei fenomeni alluvionali ma diversi dal punto di vista litologico e morfologico, soprattutto alla luce degli interventi di sistemazione effettuati nell’ultimo decennio. La metodologia utilizzata comprende in primo luogo un’adeguata ricerca bibliografica, volta ad acquisire una conoscenza completa del bacino e della sua “storia”. In seguito sono stati eseguiti sopralluoghi lungo le aste torrentizie, dalla zona di deposito alla zona di innesco, in funzione della morfologia degli alvei e delle sponde, nonché della stabilità dei depositi. Durante i rilievi di campagna sono stati eseguiti campionamenti di materiale detritico. La scelta dei punti di campionamento è risultata uno dei punti chiave della ricerca ed è legata all’estrema eterogeneità dei depositi da colata detritica, tipicamente mal classati e comprendenti materiale da molto fine a metrico ed oltre. Per acquisire uno spettro quanto più completo dell’andamento granulometrico dei depositi, i bacini sono stati campionati sia nella zona di innesco che in quella di deposito. Alla fase di campionamento ha fatto seguito una fase in laboratorio, comprendente analisi granulometriche, mineralogiche e reologiche. Le analisi granulometriche hanno lo scopo di risalire alla curva granulometrica dei campioni, andando ad identificare le percentuali di ciascuna classe granulometrica, e sono il primo passo per differenziare i depositi prelevati in posizioni diverse lungo l’asta torrentizia. Le analisi mineralogiche, volte al riconoscimento dei diversi minerali presenti nella frazione più fine del campione (< 4 µm), permettono di verificare l’omogeneità genetica dei depositi di uno stesso bacino e di individuare l’eventuale presenza di minerali argillosi, che possono incidere sul comportamento reologico della miscela acqua-sedimento, alla base dei fenomeni di colata. Di pari passo con la caratterizzazione granulometrica e mineralogica si è proceduto alle analisi reologiche. Scopo principale di tali analisi è la determinazione dei parametri reologici (yield stress e viscosità), i quali governano il comportamento dei fluidi e sono alla base della futura modellazione numerica. Le colate detritiche, secondo l’approccio reologico, sono considerate come fluidi omogenei e viscoelastici; si suppone cioè che il comportamento del flusso sia controllato dalle proprietà della cosiddetta matrice, ossia la miscela di acqua e particelle fini nella quale sono disperse quelle più grossolane. Date tali premesse, le analisi reologiche sui campioni prelevati nel corso di questo dottorato sono state eseguite solo sulla frazione più fine del materiale (< 62 µm) utilizzando il reometro a piatti zigrinati paralleli di diametro pari a 35 mm (Rheostress Haake RS150, Haake GmbH, Germania). I diversi campioni sono stati preparati a differenti concentrazioni volumetriche solide, la cui scelta è legata fondamentalmente alla stabilità del campione sul piatto inferiore dello strumento. I dati sperimentali sono stati quindi correlati tra loro tramite regressione esponenziale per ottenere i coefficienti reologici necessari alla futura modellazione numerica. L’ultima fase dello studio è stata dedicata alla modellazione numerica dei fenomeni di colata detritica. La modellazione fisico-matematica dei debris flow ha principalmente lo scopo di determinare la possibile area di propagazione dei fenomeni, nonché la loro velocità ed energia, con l’obiettivo finale di delimitare le aree di pericolosità e di fornire informazioni utili alla progettazione di adeguate opere di mitigazione. Nell’ambito di questo lavoro le simulazioni sono state eseguite con il modello idraulico bidimensionale FLO-2D, utilizzabile per simulare il flusso dell’acqua in corsi d’acqua anche di notevole larghezza o per la simulazione di flussi non-Newtoniani in aree di conoide. Alla luce dell’obiettivo di individuare una metodologia atta alla caratterizzazione dei bacini da colata anche in assenza di dati di back analysis, le simulazioni numeriche sono state eseguite con il duplice scopo di verificare l’effettivo areale di influenza dei fenomeni e di testare i valori dei parametri reologici derivati dai campioni prelevati lungo i rii studiati. Per ciascun bacino sono state confrontate le informazioni ricavate dalle analisi di laboratorio e dalla modellazione numerica al fine di individuare quale e/o quali caratteristiche dei depositi incidono sui risultati delle simulazioni e in che modo condizionano il comportamento del flusso detritico. In conclusione è stato possibile evidenziare pro e contro della metodologia sperimentale e definirne l’applicabilità allo studio delle colate detritiche.
XXVI Ciclo
1985
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Souza, Eliel Pereira de. "Canal do Valo Grande: Governança das águas estuarinas na perspectiva da aprendizagem social." Universidade de São Paulo, 2012. http://www.teses.usp.br/teses/disponiveis/90/90131/tde-20082012-085559/.

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A publicação da lei 9.433 de 1997, que institucionaliza a Política Nacional de Recursos Hídricos no Brasil, abriu a perspectiva de uma gestão integrada, participativa e descentralizada dos recursos hídricos. A integração da gestão de bacias hidrográficas com a gestão da zona costeira é uma diretriz dessa política e a participação social é pressuposto para medidas de gestão mais sustentáveis e legítimas. A qualidade dos processos participativos está ligada à incorporação de diferentes atores, com perspectivas distintas em relação à bacia hidrográfica, em processos de grupo que permitam reflexão e aprendizado, sobre o próprio grupo e sobre o ambiente natural e institucional da bacia. O presente trabalho é um estudo de caso sobre a gestão da bacia do rio Ribeira de Iguape, no litoral sul de São Paulo. Na porção terminal desse rio, uma obra hidráulica construída no século XIX, conhecida como Valo Grande, retificou seu curso, desestabilizando o sistema estuarino adjacente pelo aporte de água e sedimentos em região abrigada. Desde a década de 70, houve uma série de ações governamentais no sentido de recuperara essa região do estuário, o que gerou tensão e conflito com os atores a montante da bacia. Em resposta, o assunto foi debatido e negociado em diferentes fóruns criados a partir da década de 80. O presente trabalho analisa o processo decisório sobre o canal, buscando identificar elementos que favorecem ou inibem a transformação da participação em aprendizagem social. Os resultados revelam que a aprendizagem social não é um processo espontâneo, e, apesar da forte interdependência entre os atores envolvidos, espaços de convergência e consenso são prejudicados por fatores como a falta de liderança pró-ativa, representação desproporcional dos atores, ausência de redes de cooperação e coalizões, além da falta de implementação de medidas negociadas.
The launch of the Law 9.433 of 1997, wich institutionalizes the National Policy of Water Resources, opened the prospect of an integrated, participatory and decentralized management of the water resources. The integration of the watershed management with the management of the coastal zone is a guideline of this policy and social participation is prerequisite for more sustainable and legitimate. The quality of participatory process is linked to the incorporation of different actors, with distinctive perspectives in relation to the catchment area, in a group process that enable reflection and learning, about the own group itself and about the natural and institutional framework of the basin. The present study is a case study on the management of river basin of Ribeira de Iguape, on the southern coast of São Paulo State. In the terminal part of this river, a hydraulic work was built in the nineteenth century, known as Valo Grande, rectify its course, destabilizing the adjacent estuary system by the input of water and sediments in a sheltered area. Since the 70s, there was a series of government in order to recover this region of estuary, wich created tension and conflict with the upstream actors of the basin. In response, the matter was discussed and negotiated in different decision-makers forums created since the 80s. The present work examines the decision process on the channel, in order to identify factors that promote or inhibit the transformation of participation in social learning. The results show that the social learning is not a spontaneous process, and despite the strong interdependency among the actors envolved, areas of convergence and consensus are affected by aspects like the lack of a proactive leadership, disproportionate representation of actors, lack of networks of cooperation and coalition, and the lack of implementation of negotiated measures.
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Trevisan, Carlos Alberto. "Canal de marketing : um estudo em vinícolas da indicação geográfica vale dos vinhedos." reponame:Repositório Institucional da UCS, 2014. https://repositorio.ucs.br/handle/11338/917.

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Submitted by Ana Guimarães Pereira (agpereir@ucs.br) on 2015-03-17T17:39:07Z No. of bitstreams: 1 Dissertacao Carlos Alberto Trevisan.pdf: 309066 bytes, checksum: f9279e699675454f91983c223d696e0e (MD5)
Made available in DSpace on 2015-03-17T17:39:07Z (GMT). No. of bitstreams: 1 Dissertacao Carlos Alberto Trevisan.pdf: 309066 bytes, checksum: f9279e699675454f91983c223d696e0e (MD5)
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Carneiro, Rafaelle Rocha Souza. "A pesca da manjuba (Anchoviella lepidentostole) e o canal do Valo Grande: uma relação de (des)continuidades em Iguape-SP." Universidade de São Paulo, 2006. http://www.teses.usp.br/teses/disponiveis/8/8136/tde-16072007-120634/.

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O presente estudo procurou compreender como se efetua a pesca da manjuba em Iguape-SP e qual a sua relação com o canal do Valo Grande: quais as modificações sofridas pela atividade pesqueira no município, antes, durante e após a construção da barragem no dito canal, e como os pescadores passaram a se organizar após essa interferência no meio ambiente. Objetivou compreender o modo de vida do pescador, através dos seus saberes tradicionais, e como esse modo de vida ainda resiste nos dias atuais, onde a tônica é pescar mais e mais, a fim de se obter uma renda maior. Enfim objetivou-se, mediante o diálogo entre teoria e conhecimento tradicional, mostrar como um pescador artesanal resiste num campo tão competitivo, como é a pesca da manjuba
The present study searched to understand a how to make the manjuba\'s angling in Iguape/SP and wich your relation with the Valo Grande\'s strait: with the modifications suffer the fishing grounds atictivities in the country, before, during and after the structure of the dam in the strait, and how the fisherman have been organized after these interferation in the environment. Objectified to understand the life mode of the fisherman, through of the their traditionals aware, and how this life mode still stard of the present time, where the tonic is fish more to more, in order to have more rent. After all objectified, by means of the dialogue between the theory and traditional knowledge to show how the fisherman resiste in the field so competition, how is the manjuba\'s fish
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Girault, Michel. "Pétrographie et géochimie de volcanites archéennes polymétamorphiques : reconstitution de l'histoire pétrologique (zone minière Manitou-Louvem, Val d'Or, Québec)." Phd thesis, Grenoble 1, 1986. http://tel.archives-ouvertes.fr/tel-00739836.

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La zone Manitou-Louvem, à minéralisations de sulfures massifs, comporte une série volcanique sous-marine (laves, pyroclastites et siIls) appartenant, pour l'essentiel, à la formation de Val d'Or. A la base, des basaltes à amphiboles et boules d'épidote dérivent, par faible fusion partielle, d'une source mantellique enrichie en éléments hygromagmaphiles légers. Vient ensuite l'intime association de laves intermédiaires et felsiques, de pyroclastites grossières généralement felsiques et monogéniques, et de filon-couches hypovolcaniques de diorite. Toutes ces roches sont comagmatiques, et liées aux basaltes de la base. Les filon-couches font la transition entre la diorite de Bourlamaque qui noyaute le complexe volcanique central de Val d'Or, et le volcanisme effusif. Le cachet géochimique est calcoalcalin, mais les tendances d'évolution (cristallisation fractionnée anhydre) sont tholéiitiques : elles varient selon la stratigraphie, par évolution des modalités de fractionnement et appauvrissement de la source mantellique. Au sommet, la formation de Héva, avec des basaltes évolués hyperalumineux d'affinité tholéiitique plus franche, marque le retour progressif au volcanisme abyssal, après celui d'arc insulaire (formation de Val d'Or) : ils proviennent d'un centre éruptif et d'une lignée d'évolution différents. Un modèle de bassin marginal permettrait de concilier tous ces caractères et pourrait expliquer la contradiction tholéiitique. calcoalcalÎn, qui mériterait une étude détaillée. La minéralogie est issue des altérations et métamorphismes successifs, que l'on caractérise grâce à une étude précise de minéraux secondaires: spi!itisation, métasomatoses liées ou non aux minéralisations, métamorphisme régional. Celui-ci est du faciès des schistes verts (zone à biotite). Les problèmes d'interprétation pour la minéralogie des " roches vertes" (termes abusivement banalisé) sont examinés en détail. L'auteur estime que la prospection minière devrait tirer profit de telles études, qu'elle devrait intégrer à ses méthodes comme un élément supplémentaire de reconnaissance des milieux minéralisés par opposition aux zones stériles.
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Lemarchand, Jérémie. "Les minéralisations filoniennes aurifères du pluton de Bourlamaque (Val d'Or, Abitibi) : synthèse structurale et apports de la datation ⁴⁰Ar/³⁹Ar." Thèse, Rennes 1, 2012. http://www.theses.fr/2012REN1S130.

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Le pluton de Bourlamaque encaisse une dizaine de gisements filoniens aurifères post-métamorphiques matérialisés par des veines de quartz-tourmaline-carbonates-sulfutes associées à des zones de cisaillement mylonitique inverses. La minéralisation s'organise selon des réseaux compatibles avec un modèle de type Riedel, centrés sur des structures mylonitiques est-ouest à fort pendage. Plusieurs structures stériles à pendage nord ont été également reconnues et sont interprétées comme liées à un épisode structural post-minéralisation. L'interprétation des données ⁴⁰Ar/³⁹Ar suggère que les premières traces de fluides liés à la minéralisation sont enregistrées par les amphiboles du pluton de Bourlamaque vers 2650 Ma, lors d'une phase d'exhumation régionale. La géométrie des spectres d'âges des zones mylonitiques traduit une recristallisation dynamique compatible avec les indications de circulations hydrothermales associées aux veines aurifères et se poursuivant possiblement jusque vers 2505 Ma. La cyclicité des pics de densité de probabilité des âges plateaux de l'ensemble de smicas blancs et le décalage entre les spectres des veines de quartz et des mylonites sont compatibles avec une activité hydrothermale cyclique de type fault-valve. Au final la datation ⁴⁰Ar/³⁹Ar conjointe de l'intrusion de Bourlamaque ainsi que des veines minéralisées et de la déformation mylonitique associée offre de nouvelles perspectives d'interprétation et apporte de nouveaux éléments de compréhension concernant le contexte de mise en place des minéralisations filonniennes aurifères de la région de Val d'Or
The Bourlamaque pluto contains about ten post-metamorphic load gold deposits, formed by quartz-tourmaline-carbonate-sulphide veins in association with reverse mylonitic shear zones. The mineralization corresponds to a Riedel type shear zones network evolving from steeply dipping structures. Several north-dipping barren structures have been also recognized and interpreted as being related to a post-mineralization structural event. Interpretation of the ⁴⁰Ar/³⁹Ar data set suggests that the first fluids related to the mineralization are recorded by the amphibole of the Bourlamaque plutonic rock at ca. . 2605 Ma, synchronously with a regional exhumation phase. Geometry of age spectra from mylonitic shear zones is typical of dynamic recrstallization and consistent with indications of hydrothermal circulations possibly extending until ca. 2505 Ma in the gold veins themselves. The cyclicity of the plateau ages frequency peaks from white micas and the delay between quartz veins and mylonitic shear zones spectra are consistent with a fault-valve hydrothermal activity. Finally, ⁴⁰Ar/³⁹Ar dating of the Bourlamaque plutonic rock together with auriferous quartz veins and related mylonitic shear zones provides renewed perspective and elements for a better understanding of the global context of load gold deposits in the Val d'Or area
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Morency, Jenna L. "Outcast Men: American Citizens in Upper Canada and Van Dieman's Land." Fogler Library, University of Maine, 2011. http://www.library.umaine.edu/theses/pdf/MorencyJL2011.pdf.

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Grzela, Donald. "Chemical composition of indicator minerals from orogenic gold deposits and glacial sediments of the Val-d'Or district (Québec, Canada)." Master's thesis, Université Laval, 2017. http://hdl.handle.net/20.500.11794/27588.

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Les tourmalines, les scheelites et les magnétites provenant des gisements aurifères de type orogénique (n=22) et des sédiments glaciaires (n=5) du district minier de Val-d’Or (Québec, Canada) ont été investiguées à la microsonde électronique (EPMA) et par ablation laser et spectrométrie de masse à plasma à couplage inductif (LA-ICP-MS) afin de déterminer leur signature chimique et d’évaluer leur potentiel en tant que minéraux indicateurs pour l’exploration aurifère. Les tourmalines de Type I provenant de dépôts aurifères de type orogénique encaissés dans des roches felsiques et intermédiaires calco-alcalines montrent de faibles teneurs en V, Cr, Mn, Fe, Co, Ni, Zn et Sn et une teneur élevée en Mg par rapport aux tourmalines de Type II provenant de dépôts aurifères de type orogénique encaissés dans des roches mafiques tholéiitiques. Les tourmalines de Type III provenant de dépôts aurifères de type orogénique situés au contact entre des roches mafiques volcaniques et métasédimentaires montrent une chimie similaire aux tourmalines de Type I avec des teneurs en Li, Mn et Pb légèrement plus élevées. Les tourmalines des gisements aurifères de type orogénique sont caractérisées par des teneurs en Zn, Cu, Sn et Pb plus faibles que les tourmalines associées aux miniéralisations de type Cu-Zn, Pb-Zn-Cu et Sn. Les tourmalines récupérées dans le till portent la signature chimique des tourmalines provenant des gisements aurifères de type orogénique avec une majorité portant la signature des tourmalines de Type I. Les scheelites provenant de dépôts aurifères de type orogénique encaissés dans des intrusions calco-alcalines de composition intermédiaire sont caractérisées par des teneurs en Na, ÉTR et Y plus élevées que les scheelites provenant de dépôts aurifères encaissés dans des roches sédimentaires ou mafiques. Les scheelites récupérées dans le till portent la signature chimique des scheelites provenant des gisements aurifères de type orogénique. Les magnétites sont rare dans les dépôts aurifères de type orogénique du district de Val-d’Or. Les magnétites d’origine hydrothermale provenant des veines aurifères sont caractérisées par des teneurs plus élevées en Cr, Zn, Mn, K, Ca, Ti et Al que les magnétites d’origine magmatique retrouvées dans les roches encaissantes de composition dioritique ou gabbroique. Les magnétites associées à la minéralisation aurifère forment des grains fins disséminés (< 0,05 mm), ce qui suggère que les magnétites grossières récupérées dans le till ne proviennent probablement pas des veines de quartz aurifères.
Tourmalines, scheelites and magnetites from orogenic gold deposits (n=22) and glacial sediments (n=5) of the Val-d’Or mining district (Québec, Canada) were investigated by Electron Probe Micro-Analyzer (EPMA) and Laser Ablation Inductively Coupled Plasma Mass Spectrometry (LA-ICP-MS) in order to determine their chemical signature and to assess their potential as indicator minerals for gold exploration. Type I tourmalines from orogenic gold deposits hosted in felsic and intermediate calc-alkaline rocks have low contents of V, Cr, Mn, Fe, Co, Ni, Zn, and Sn and a high content of Mg compared to Type II tourmalines from orogenic gold deposits hosted in mafic tholeiitic rocks. Type III tourmalines from orogenic gold deposits located at the contact between mafic volcanic and metasedimentary rocks show a chemistry similar to Type I tourmalines with slightly higher Li, Mn, and Pb contents. Tourmalines from orogenic gold deposits are characterized by lower contents of Zn, Cu, Sn, and Pb than tourmalines associated to Cu-Zn, Pb-Zn-Cu, and Sn mineralizations. Till tourmalines carry the chemical signature of tourmalines from orogenic gold deposits with a majority carrying the signature of Type I tourmalines. Scheelites from orogenic gold deposits of the Val-d’Or district hosted in calc-alkaline intrusions of intermediate composition are characterized by high Na, REE, and Y contents compared to scheelites from sediment- or mafic-hosted gold deposits. Till scheelites carry the chemical signature of scheelites from orogenic gold deposits. Magnetites are rare in orogenic gold deposits of the Val-d’Or district. Magnetites of hydrothermal origin occuring in gold veins are characterized by higher contents of Cr, Zn, Mn, K, Ca, Ti, and Al than magnetites of magmatic origin found in the dioritic or gabbroic host rocks. Magnetites associated to the gold mineralization form fine disseminated grains (< 0.05 mm), which suggests that the coarse magnetites recovered in the till probably do not originate from the gold-bearing quartz veins.
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LATIL, ISABELLE. "Le medecin generaliste face au syndrome du canal carpien : discussion autour de 193 cas recenses chez des omnipraticiens des alpes-maritimes et du var." Nice, 1990. http://www.theses.fr/1990NICE6553.

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Walsh, Mark James. "Strategic political positioning and tax policy : recent VAT policy changes in Canada and Germany." Thesis, University of British Columbia, 2008. http://hdl.handle.net/2429/5504.

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During the twenty-first century, why have some welfare state governments shifted their tax system towards a greater dependence upon consumption taxes, while other governments have chosen to move away from this dependence? This paper addresses that question by examining the contemporary politics of taxation in Canada and Germany. It analyzes what causes a government to choose employ specific tax policy instruments. This paper contends that, if a government is insecure and in need of enlarging its support base, it will largely ignore fiscal policies that predominantly focus on improving aggregate economic conditions in favour of policies which provide fiscal benefits to necessary constituencies, unless both dire economic conditions and adequate blame avoidance opportunities exists. While Canada chose to shift its tax burden away from consumption taxes because these necessary conditions did not exist, Germany chose to shift its tax burden towards consumption taxes because these conditions did exist.
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Books on the topic "Val Canale"

1

Gariup, Mario. Il santuario di Monte Lussari in Val Canale. Cividale del Friuli: Dom, 1991.

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editor, Strassoldo Marzio, ed. Castelli e fortificazioni del Canal del Ferro e della Val Canale. Udine: Forum, 2014.

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Scroccaro, Mauro. Dall'aquila bicipite alla croce uncinata: L'Italia e le opzioni nelle nuove provincie Trentino, Sudtirolo, Val Canale (1919-1939). Trento: Museo storico in Trento, 2000.

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Scroccaro, Mauro. Dall'aquila bicipite alla croce uncinata: L'Italia e le opzioni nelle nuove provincie Trentino, Sudtirolo, Val Canale, 1919-1939. Trento: Museo storico in Trento, 2000.

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Tone, Kralj, and Sclauzero Carlo photographer, eds. Tone Kralj: Cerkvene poslikave na Tržaškem, Goriškem in v Kanalski dolini = le pitture murali nelle chiese dell'area Triestina, del Goriziano e della Val Canale. Gorica: Goriška Mohorjeva, 2018.

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Ravnik, Mojca. Na žegen!: Žegnanje in drugi prazniki z rekruti v Ukvah v Kanalski dolini = Venite alla sagra! : la sagra e altre feste con i coscritti nel paese di Ugovizza nella Val Canale. Ljubljana: Inštitut za slovensko narodopisje ZRC SAZU, 2015.

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Desroches, Frederick J. Force & fear: Robbery in Canada. Toronto: Nelson Canada, 1995.

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Damsté, Willem Sinninghe. Het Noordzeekanaal 1863-1883: De geschiedenis van een concessie = The North Sea Canal 1863-1883 : the history of a concession. Nijmegen: Ars Aequi Libri, 2001.

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Vedder, Jan. Het Apeldoorns Kanaal: Monument van de plattelandsgeschiedenis van de Oost-Veluwe (1800-1850). Utrecht: Matrijs, 2001.

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Desroches, Frederick J. Force & fear: Robbery in Canada. Toronto: Canadian Scholars' Press, 2002.

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Book chapters on the topic "Val Canale"

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Boccali, C., C. Calligaris, L. Zini, F. Cucchi, and R. Lapasin. "Comparison of Scenarios After Ten Years: The Influence of Input Parameters in Val Canale Valley (Friuli Venezia Giulia, Italy)." In Engineering Geology for Society and Territory - Volume 2, 525–29. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-09057-3_87.

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Dion, Kenneth L. "Canada." In Encyclopedia of psychology, Vol. 2., 5–12. Washington: American Psychological Association, 2000. http://dx.doi.org/10.1037/10517-004.

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Thang, Simon. "Loan Intermediary Services: Canada." In VAT and Financial Services, 87–108. Singapore: Springer Singapore, 2017. http://dx.doi.org/10.1007/978-981-10-3465-7_6.

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Ritchie, Pierre L. J. "Regional psychological associations: In Canada." In Encyclopedia of psychology, Vol. 7., 22–24. Washington: American Psychological Association, 2000. http://dx.doi.org/10.1037/10522-010.

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Rocard, M. "Canadian Woman’s ‘Ultimate Frontier’ in Aritha van Herk’s Fictional World." In Canada on the Threshold of the 21st Century, 323. Amsterdam: John Benjamins Publishing Company, 1991. http://dx.doi.org/10.1075/z.52.46roc.

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Canalis-Durand, Mireille. "Formal expansion of van der pol equation canard solutions are gevrey." In Lecture Notes in Mathematics, 29–39. Berlin, Heidelberg: Springer Berlin Heidelberg, 1991. http://dx.doi.org/10.1007/bfb0085022.

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Ferkous, K., and A. Tremblay. "Thrust-related gold-bearing tourmaline-quartz veins: The Wrightbar mine, Val d'Or mining camp (Abitibi, Canada)." In Mineral Deposits at the Beginning of the 21st Century, 735–38. London: CRC Press, 2022. http://dx.doi.org/10.1201/9781003077503-187.

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MacGregor, J. "In the Lake—Strange Swell—A Storm—Submerged Ruins—The “Herd of Swine ”—Samakh Village—Hippos—High Sea,—Vale of Doves— Long Last Look—Cana—Nazareth—Old Sights—Sights Unseen— Plain Words." In A Canoe Cruise in Palestine, Egypt and the Waters of Damascus, 375–91. 1.MacGregor, J. - Journeys - Middle East 2.Rob Roy (Canoe) 3.Canoes and canoeing- Middle East - History- 19th century 4.Jordan River - Description and travel 5.Middle East - Description and travel: Routledge, 2019. http://dx.doi.org/10.4324/9781315828664-23.

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MacGregor, J. "Rukleh—Bust of Baal—Mount Hermon—Kefr Kuk—Rasheya—Search for Jordan—Earliest Spring—Jordan’s Eye—Sad Loss—Leeches — The Hasbany—Wady Et Teim—Hasbany Source—First Bridge— Start on Jordan—Coloured Cascade—Pitch Pits—Jordan Vale—The Litany—Storm—Dripping Bedroom." In A Canoe Cruise in Palestine, Egypt and the Waters of Damascus, 162–83. 1.MacGregor, J. - Journeys - Middle East 2.Rob Roy (Canoe) 3.Canoes and canoeing- Middle East - History- 19th century 4.Jordan River - Description and travel 5.Middle East - Description and travel: Routledge, 2019. http://dx.doi.org/10.4324/9781315828664-12.

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Van Glabbeek, Francis, and Jacqueline Vons. "Dissection and representation of muscles in Vesalius, Canano, Sagemolen." In Quatre atlas de myologie de Van Horne et Sagemolen. Université Paris Cité, 2022. http://dx.doi.org/10.53480/van-horne.647e17.

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The recently discovered drawings of Sagemolen (ca. 1660) and the anatomical works published 100 years earlier by Giovanni Battista Canano in 1542 (Muscularum humani corporis picturata dissectio) and by Andreas Vesalius in 1543 (De humani corporis fabrica) represent the illustrations of human anatomical dissections. Vesalius depictions are very precisely explained by an accompanying text, not only discussing the illustrated anatomical structures but also justifying his choices in representing them. Canano describes in detail the dissection of the muscles of the upper limb. His illustrations are drawn by a well-known Ferrarese artist. We will investigate the role of Vesalius and Canani who might have influenced Van Horne and Sagemolen in preparing their marvelous anatomical work.
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Conference papers on the topic "Val Canale"

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Calligaris, C., L. Zini, and F. Cucchi. "Debris flow rainfall thresholds in Val Canale Valley: first steps into their redefinition." In DEBRIS FLOWS. Southampton, UK: WIT Press, 2012. http://dx.doi.org/10.2495/deb120051.

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Castañé Sanmartín, Marta. "El (Ter)annà d’un territori industrialitzat: dels molins a les grans colònies industrials." In Seminario Internacional de Investigación en Urbanismo. Barcelona: Maestría en Planeación Urbana y Regional. Pontificia Universidad Javeriana de Bogotá, 2014. http://dx.doi.org/10.5821/siiu.6048.

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Al 1824 es té constància a Torelló del primer molí hidràulic per a moldre el blat que canvia la seva concessió de l’aigua per a utilitzar-la per cardar la llana i el cotó. Aquell mateix any ja es troben diferents concessions per utilitzar les aigües per a una fàbrica tèxtil a Roda de Ter i a Manlleu. És a partir d’aquest moment quan durant els pròxims 150 anys, el Ter passa a ser colonitzat en tot el seu recorregut per fàbriques que acabarien transformant el territori i el paisatge. La industrialització del Ter va comportar unes 29 colònies industrials i 37 fàbriques tèxtils (BAYON 2005), a més de noves vies de comunicació, el ferrocarril, nous habitatges, ponts i canals, que van transformar i canviar un territori eminentment rural. El resultat és un dels rius més densificats i amb una distribució en el territori de petites taques disperses. La conca fluvial del Ter, des de l’edat mitjana ja era una vall poblada i treballada per pagesos i camperols. Quan la indústria vol implantar-se a la vall, no es troba amb un territori erm. L’agricultura deixa unes preexistències que condicionaran la posició de les noves fàbriques. Per tant, un projecte territorial basat en l’ús de l’aigua i el rendiment econòmic que s’inicia amb la posició d’aquestes preexistències de l’agricultura en el territori del Ter. Un patrimoni que també s’ha de tenir present en la història de la indústria. Tot aquest patrimoni, ja no té una funció industrial; no és només un rastre de la història i de la identitat del lloc, sinó que és també una oportunitat per a seguir construint un futur per al territori. Aquest article forma part d’una investigació que pretén explicar com van succeir aquests canvis i perquè en el Ter tenen un tarannà diferent. In 1824 there is evidence in Torelló of the first hydraulic mill to grind wheat that changes water’s concession to use it for carding wool and cotton. That same year, different concessions to use the water for a textile plant are found in Roda de Ter and Manlleu. From that moment, and during 150 Ter River would be colonized in its entire itinerary by plants that would end up transforming the territory and the landscape. The industrialization of the Ter River implied around 29 industrial colonies and 37 textile plants (BAYON 2005),, as well as new communication routes, the railway, new housing, bridges and canals that transformed and changed the existent rural territory. The result is one of the most densified rivers with a territorial distribution of small disperse patches. Since middle age the Ter river basin was a populated area cultivated by farmers. Tracks left by agriculture will influence industry settlement, affecting the location of the new plants location. In fact, this regional project, based on the water as a energy and the economical benefits, starts on the watermills. This heritage has to be in the industrial history. All this heritage, which has not industrial function, is currently not just a track from the history and identity of the place, but also an opportunity to keep building a future for the territory. This paper is part of a research that expects to explain how these changes took place and why do they have a different character (tarannà) in the Ter river.
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Barot, Hemant, Lake Singh, and Rajiv K. Varma. "Operational experience with Static var Compensators in Ontario, Canada." In 2014 IEEE Power & Energy Society General Meeting. IEEE, 2014. http://dx.doi.org/10.1109/pesgm.2014.6939525.

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Cilip, Christopher M., Jonathan P. Jarow, and Nathaniel M. Fried. "Noninvasive laser coagulation of the canine vas deferens, ex vivo." In SPIE BiOS: Biomedical Optics, edited by Nikiforos Kollias, Bernard Choi, Haishan Zeng, Reza S. Malek, Brian J. Wong, Justus F. R. Ilgner, Kenton W. Gregory, et al. SPIE, 2009. http://dx.doi.org/10.1117/12.807495.

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Cilip, Christopher M., Ashley E. Ross, Jonathan P. Jarow, and Nathaniel M. Fried. "Noninvasive laser coagulation of the canine vas deferens, in vivo." In BiOS, edited by Nikiforos Kollias, Bernard Choi, Haishan Zeng, Reza S. Malek, Brian J. Wong, Justus F. R. Ilgner, Kenton W. Gregory, et al. SPIE, 2010. http://dx.doi.org/10.1117/12.839601.

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Zhai, Beibei, Anne Steino, Jeffrey Bacha, Dennis Brown, and Mads Daugaard. "Abstract B15: Dissecting the molecular mechanism of dianhydrogalactitol (VAL-083) activity in cancer treatment." In Abstracts: AACR Special Conference on DNA Repair: Tumor Development and Therapeutic Response; November 2-5, 2016; Montreal, QC, Canada. American Association for Cancer Research, 2017. http://dx.doi.org/10.1158/1557-3125.dnarepair16-b15.

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Daver, Lucille Marie. "HETEROGENEITY IN THE ARCHETYPE OF MESOTHERMAL DEPOSITS IN THE VAL D’OR MINING DISTRICT, QUEBEC, CANADA: MINERALOGICAL ASSOCIATION OF TOURMALINE-PYRITE." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-286512.

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Sugimoto, Jugo, Pin-Yu Huang, Shota Okutani, and Yuichi Kado. "Bidirectional Isolated Ripple Cancel Dual Active Bridge Modular Multile vel DC-DC Converter." In 2020 IEEE Applied Power Electronics Conference and Exposition (APEC). IEEE, 2020. http://dx.doi.org/10.1109/apec39645.2020.9124429.

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Cilip, Christopher M., Mohamad E. Allaf, and Nathaniel M. Fried. "Optical coherence tomography vs. high-frequency ultrasound during noninvasive laser coagulation of the canine vas deferens." In SPIE BiOS. SPIE, 2012. http://dx.doi.org/10.1117/12.905259.

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Cilip, Christopher M., Gino R. Schweinsberger, and Nathaniel M. Fried. "Comparison of 808, 980, and 1075nm lasers for noninvasive thermal coagulation of the canine vas deferens, ex vivo." In SPIE BiOS. SPIE, 2011. http://dx.doi.org/10.1117/12.873293.

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Reports on the topic "Val Canale"

1

Desrochers, A., and B. Beauchamp. Ufinian-Kazanian (Lower and Upper Permian) stratigraphy (Van Hauen and Degerböls formations), Hvitland Peninsula and adjacent areas, northwestern Ellesmere Island, Arctic Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1995. http://dx.doi.org/10.4095/202797.

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Russo, Margherita, Fabrizio Alboni, Jorge Carreto Sanginés, Manlio De Domenico, Giuseppe Mangioni, Simone Righi, and Annamaria Simonazzi. The Changing Shape of the World Automobile Industry: A Multilayer Network Analysis of International Trade in Components and Parts. Institute for New Economic Thinking Working Paper Series, January 2022. http://dx.doi.org/10.36687/inetwp173.

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In 2018, after 25 years of the North America Trade Agreement (NAFTA), the United States requested new rules which, among other requirements, increased the regional con-tent in the production of automotive components and parts traded between the three part-ner countries, United States, Canada and Mexico. Signed by all three countries, the new trade agreement, USMCA, is to go into force in 2022. Nonetheless, after the 2020 Presi-dential election, the new treaty's future is under discussion, and its impact on the automo-tive industry is not entirely defined. Another significant shift in this industry – the acceler-ated rise of electric vehicles – also occurred in 2020: while the COVID-19 pandemic largely halted most plants in the automotive value chain all over the world, at the reopen-ing, the tide is now running against internal combustion engine vehicles, at least in the an-nouncements and in some large investments planned in Europe, Asia and the US. The definition of the pre-pandemic situation is a very helpful starting point for the analysis of the possible repercussions of the technological and geo-political transition, which has been accelerated by the epidemic, on geographical clusters and sectorial special-isations of the main regions and countries. This paper analyses the trade networks emerg-ing in the past 25 years in a new analytical framework. In the economic literature on inter-national trade, the study of the automotive global value chains has been addressed by us-ing network analysis, focusing on the centrality of geographical regions and countries while largely overlooking the contribution of countries' bilateral trading in components and parts as structuring forces of the subnetwork of countries and their specific position in the overall trade network. The paper focuses on such subnetworks as meso-level structures emerging in trade network over the last 25 years. Using the Infomap multilayer clustering algorithm, we are able to identify clusters of countries and their specific trades in the automotive internation-al trade network and to highlight the relative importance of each cluster, the interconnec-tions between them, and the contribution of countries and of components and parts in the clusters. We draw the data from the UN Comtrade database of directed export and import flows of 30 automotive components and parts among 42 countries (accounting for 98% of world trade flows of those items). The paper highlights the changes that occurred over 25 years in the geography of the trade relations, with particular with regard to denser and more hierarchical network gener-ated by Germany’s trade relations within EU countries and by the US preferential trade agreements with Canada and Mexico, and the upsurge of China. With a similar overall va-riety of traded components and parts within the main clusters (dominated respectively by Germany, US and Japan-China), the Infomap multilayer analysis singles out which com-ponents and parts determined the relative positions of countries in the various clusters and the changes over time in the relative positions of countries and their specialisations in mul-tilateral trades. Connections between clusters increase over time, while the relative im-portance of the main clusters and of some individual countries change significantly. The focus on US and Mexico and on Germany and Central Eastern European countries (Czech Republic, Hungary, Poland, Slovakia) will drive the comparative analysis.
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Reporte de Infraestructura Financiera 2022. Banco de la República de Colombia, July 2022. http://dx.doi.org/10.32468/rept-infr-finan.2022.

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La labor de seguimiento a la infraestructura financiera local es un aporte adicional del Banco de la República a la estabilidad financiera del país. Uno de los productos de dicho seguimiento ha sido el Reporte de Sistemas de Pago, que a partir de esta edición cambia de nombre a Reporte de Infraestructura Financiera, con el objetivo de que refleje de manera amplia los temas que aquí se abordan. En esta edición 2022 se incluyen varios cambios, producto de un estudio comparativo realizado frente a reportes de infraestructura financiera elaborados por otros bancos centrales. Dichos cambios buscan hacer más fluida y liviana la lectura del reporte, incluyendo los mensajes principales y las cifras clave para los diferentes grupos de interés a los cuales va dirigido. En el reporte se muestra que la infraestructura financiera mantuvo sus servicios de forma continua, dando muestra general de su buen funcionamiento en el 2021. Adicionalmente, se validó la resiliencia de la Cámara de Riesgo Central de Contraparte (CRCC) y del Sistema de Pagos de Alto Valor (CUD) ante eventos extremos, con base en pruebas de estrés con estándares internacionales (enfocadas en el riesgo de liquidez y de crédito). En cuanto a los pagos al por menor, de acuerdo con información transaccional, el uso en valor de los instrumentos electrónicos aumentó durante 2021 frente al año 2020 (tarjetas crédito y débito, cheque y transferencias). El empleo de las tarjetas débito y crédito en pagos aumentó a niveles similares a los alcanzados en el año prepandemia. Por su parte, las transferencias electrónicas continuaron en crecimiento. Aunque los resultados de la encuesta BR 2022 muestran que el efectivo continúa siendo el instrumento más utilizado por el público para los pagos habituales (comportamiento similar al de otros países), la percepción de su uso disminuyó significativamente al 75 % (87 % en 2019). También para el comercio, el efectivo fue el instrumento preferido por sus clientes. Sin embargo, en esta medición varios canales de comercio como peluquerías, droguerías y restaurantes se sumaron al grupo que tradicionalmente viene recibiendo pagos electrónicos por un valor superior al 10 % de sus ventas (hipermercados y estaciones de servicio). Asimismo, para cerca del 50 % de la población los pagos en efectivo son menores a los que realizaron antes de la pandemia, lo cual es consecuente con el incremento transaccional de los instrumentos de pago electrónicos que se registró en el año 2021. El Banrep continúa monitoreando los desarrollos tecnológicos que han ampliado y modernizado la oferta en el mercado de pagos internacional y local, ya que son temas de interés para la industria que presta servicios de compensación y liquidación de pagos. En este reporte se presenta el caso PIX en Brasil para pagos inmediatos, los proyectos que se llevan a cabo sobre la posible emisión de moneda digital por parte de los bancos centrales (CBDC, por sus siglas en inglés) para pagos transfronterizos, así como una aproximación al ecosistema Fintech en Colombia con énfasis en las empresas que prestan servicios de pagos. Leonardo Villar Gerente General
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