1000 resultados para Portugal. Soberano (1750-1777 : José I)


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i.pp.xxxii, 415.--ii. pp. 543.

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Anhang I: "Anmerkung über die allerley Thiere die Noah in die Arche genommen hat": p. [267]-278; Anhang II: "Io. Ern. Fabri Dissertatio de animalibvs qvorvm fit mentio Zeph. II, 14": p. [279]-316.

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Este libro es producto de una iniciativa de la Comisión Económica para América Latina y el Caribe (CEPAL) y la Organización Internacional del Trabajo (OIT), destinada a contribuir al fortalecimiento del marco analítico y el debate en torno al diseño de una estrategia de desarrollo inclusivo en el Perú, así como a apoyar la formulación de políticas que impulsen la convergencia productiva, el crecimiento económico para la igualdad y la justicia social. Se trata de adoptar una estrategia renovada, con un crecimiento económico basado en una menor heterogeneidad estructural y más desarrollo productivo, cuyo dinamismo tenga efectos positivos sobre el empleo, la distribución del ingreso y la inclusión social. En la formulación de políticas consecuentes con este enfoque del desarrollo se requiere conjugar dos líneas de actuación fundamentales. Por una parte, se precisa un cambio estructural en el sistema productivo, que mejore la productividad y genere pleno empleo. Por otra, es necesario emprender iniciativas destinadas a lograr un acceso igualitario a los resultados del progreso alcanzado, que contribuyan a crear el escenario propicio para la continua mejora de las condiciones laborales, tanto salariales como no salariales, es decir, para la creación de trabajo decente.

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Several landforms found in the fold-and-thrust belt area of Central Precordillera, Pre-Andes of Argentina, which were often associated with tectonic efforts, are in fact related to non-tectonic processes or gravitational superficial structures. These second-order structures, interpreted as gravitational collapse structures, have developed in the western flank of sierras de La Dehesa and Talacasto. These include rock-slides, rock falls, wrinkle folds, slip sheets and flaps, among others; which together constitute a monoclinal fold dipping between 30º and 60º to the west. Gravity collapse structures are parallel to the regional strike of the Sierra de la Dehesa and are placed in Ordovician limestones and dolomites. Their sloping towards the west, the presence of bed planes, fractures and joints; and the lithology (limestone interbedded with incompetent argillaceous banks) would have favored their occurrence. Movement of the detached structures has been controlled by lithology characteristics, as well as by bedding and joints. Detachment and initial transport of gravity collapse structures and rockslides in the western flank of the Sierra de la Dehesa were tightly controlled by three structural elements: 1) sliding surfaces developed on parallel bedded strata when dipping >30° in the slope direction; 2) Joint’s sets constitute lateral and transverse traction cracks which release extensional stresses and 3) Discontinuities fragmenting sliding surfaces.  Some other factors that could be characterized as local (lithology, structure and topography) and as regional (high seismic activity and possibly wetter conditions during the postglacial period) were determining in favoring the steady loss of the western mountain side in the easternmost foothills of Central Precordillera.