1000 resultados para Escoles secundàries -- Edificis -- Pamplona (Navarra)
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Award-winning
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Award-winning
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Mode of access: Internet.
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Escudo xilográfico en la portada.
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Escudo calcográfico en la portada.
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Escudo xilográfico en la portada.
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Escudo xilográfico en la portada.
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This investigation was made in order to develop an exporting plan of Colombian autochthonous Products target to Navarra, Spain, and then contribute with the economy and progress of Colombia, increasing the exports and the employment in the country. Thanks to the opportunity that one of the participants of this project had, it was possible to have a direct contact with the Pamplona citizens, investigating the different aspects of exporting to another country, analyzing the target, the market access, the product portfolio, and the consumer behaviour. To begin with this project, the first step was to develop a marketing research investigation, in order to determine the possibility of having a new segment of the Colombian autochthonous products, composed of Spanish and Colombian people. This was the first step to aim into a defined segment, and to learn about all the agreements and regulations between Colombian and Spain. These regulations are about food regulations, quality standards, and to remark, production chains, and distribution channels. Alter analyzing the international distribution chain to Spain, it will be found the market size, and the different enterprises that offer the same products to this country, that further more than competence, is a source of information to find the right way to sell this kind of products.
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Pérez Goyena,
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Error de paginación, repite p. 95-96.
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Frontispicio calcográfico con el escudo de Navarra, firmado: "en Pamplona. La Cruz fz."
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Escudo xilográfico en la portada.
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Escudo calcográfico en la portada.
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Fossil associations from the middle and upper Eocene (Bartonian and Priabonian) sedimentary succession of the Pamplona Basin are described. This succession was accumulated in the western part of the South Pyrenean peripheral foreland basin and extends from deep-marine turbiditic (Ezkaba Sandstone Formation) to deltaic (Pamplona Marl, Ardanatz Sandstone and Ilundain Marl formations) and marginal marine deposits (Gendulain Formation). The micropalaeontological content is high. It is dominated by foraminifera, and common ostracods and other microfossils are also present. The fossil ichnoasssemblages include at least 23 ichnogenera and 28 ichnospecies indicative of Nereites, Cruziana, Glossifungites and ?Scoyenia-Mermia ichnofacies. Body macrofossils of 78 taxa corresponding to macroforaminifera, sponges, corals, bryozoans, brachiopods, annelids, molluscs, arthropods, echinoderms and vertebrates have been identified. Both the number of ichnotaxa and of species (e. g. bryozoans, molluscs and condrichthyans) may be considerably higher. Body fossil assemblages are comparable to those from the Eocene of the Nord Pyrenean area (Basque Coast), and also to those from the Eocene of the west-central and eastern part of South Pyrenean area (Aragon and Catalonia). At the European scale, the molluscs assemblages seem endemic from the Pyrenean area, although several Tethyan (Italy and Alps) and Northern elements (Paris basin and Normandy) have been recorded. Palaeontological data of studied sedimentary units fit well with the shallowing process that throughout the middle and late Eocene occurs in the area, according to the sedimentological and stratigraphical data.