Titlebook: Readings in Multiple Criteria Decision Aid; Carlos A. Bana e Costa Conference proceedings 1990 Springer-Verlag Berlin · Heidelberg 1990 En

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Anna Ostanellomean, and where they come from. Second, the Ecuadorian rights of nature contain elements that are not unique to the Ecuadorian experience, but rather shared by all rights of nature practice so far. This, as I will explain, is not incidental; there are deep reasons for why the rights of nature share

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Denis Bouyssouited Nations. This chapter will look at all of these developments in turn, starting from the municipal level up. In the process, I will analyze the basic structure of representing through rights in all of these cases and show it to be fundamentally similar to the Ecuadorian one.

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Philippe Vinckeo develop the north, the attacks and gradual erosion of the policy impacted on that ambition. Maintenance of the white Australia policy had always featured prominently in exhortations to fill the empty spaces. Could those exhortations carry conviction as the policy fell into disarray?

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Bernard Roymong other things, a tacit static assumption of trading partners remaining at more or less the same developmental stage, viz., their factor proportions do not drastically change, say through much faster capital accumulation in one trading country compared with the other. This theory got credence fro

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Jean Pierre Brans,Bertrand Mareschalhe Ponda Group..The bauxite deposits are largely confined to the Mopa-Verna tableland (palaeoplain) which consists of a thick carapace of laterite capping various other lithologies. The bauxite mineralization occurs within the lower horizons of the laterite profile..The most widespread and better de

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Benedetto Matarazzohe Ponda Group..The bauxite deposits are largely confined to the Mopa-Verna tableland (palaeoplain) which consists of a thick carapace of laterite capping various other lithologies. The bauxite mineralization occurs within the lower horizons of the laterite profile..The most widespread and better de

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of the State is placed at 85.70 Mm. of which nearly 40% goes as runoff. Irrigation accounts for 146.50 Mm. of which 112.50 Mm. is contributed by surface water and 34.00 Mm. from groundwater. The water requirement of the State is 1329 Mm.. In comparison with the water level of the previous decade (2