955 resultados para Developments on North Indian Scripts


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During the first section of the "Meteor" cruise No. 2 a profile was run from the Azores to the south across the flanks of the Mid-Atlantic Ridge with a chain of seamounts. The profile extended between the Cruiser (living) and the Hyeres seamounts, which, according to our soundings, form a connected massif, and across the centre of the Grosse Meteor Bank (30°N, 28.5 °W). These seamounts rise from a depth of more than 4000 m up till close to the surface of the sea forming there a large almost flat plateau. In the case of the Grosse Meteor Bank, this plateau has a N-S extension of approx. 30 nautical miles and an E-W extension of approx. 20 nautical miles and reaches a height of 275 m in water depth. The gravity measurements yielded a density of the topographic masses of 2.6 g/cm**3 for the Grosse Meteor Bank. Magnitude and shape of the measured free-air anomaly are very well shown in a model computation with this density. The theoretical gravity effects of the seismically detected swell of cristalline rock and of the Moho depression (mountain root) are not indicated by the observational data. It can, therefore, be assumed that the latter two neutralize each other. It seems, accordingly, that there is no local isostatic compensation of the topographic masses. Hence, the density of 2.6 g/cm**3 obtained would be about the true density of rock. In connection with the mean velocity of P waves (Aric et al., 1968) obtained by seismic refraction methods it must be concluded that the material of the 1200-4000 m thick surface layer of the Grosse Meteor Bank consists of consolidated sediments. This finding is supported by the total intensity of the Earth's magnetic field over the Grosse Meteor Bank. On the assumption of a homogeneous magnetization in the direction of the present Earth's field, the computed anomaly of the massif deviates considerably from the measured anomaly while the magnetic field of the seismically detected crystalline body is capable of interpreting the observed data. Deviating from the prevailing interpretation of the seamounts' plateau as a volcanic cone with submarine abrasion, the Grosse Meteor Bank and the seamounts in the vicinity are assumed to be of continental origin. The questions whether these seamounts submerged later on or whether the sealevel has risen subsequently are, therefore, largely nonexistent.

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Recently, there has been a surge in bilateral and regional trade arrangements between developed and developing countries, which are known as North-South RTAs. Under the current legal system of the WTO, North-South RTAs are governed by Article XXIV of the GATT or Article V of the GATS, which means such RTAs must be reciprocal and must cover substantially all the trade. On the other hand, there is another category of rules on RTAs based on the so-called Enabling Clause, which, in exceptional circumstances, provides special and differential treatment (SDT) for RTAs among developing countries. This paper considers the applicability of the SDT concept to North-South RTAs by examining why rules on RTAs and the concept of SDT were incorporated into the GATT/WTO legal framework so as to permit the derogation of most-favored-nation (MFN) obligations.

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In the present study the geometry of cups is experimentally studied through anemometer performance. This performance is analyzed in two different ways. On the one hand the anemometer transfer function between cases is compared. On the other hand the stationary rotation speed is decomposed into constant and harmonic terms, the comparison being established between the last ones. Results indicate that some cup shapes can improve the uniformity of anemometer rotation, this fact being important to reduce degradation due to ageing.

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This research explores the policy implications of the approval of three wind energy projects on the Oak Ridges Moraine, and their impact on the Coordinated Land Use Planning Review process. Specifically, it focuses on the involvement of First Nations and environmental non-governmental organizations (ENGOs). This research was conducted through analyzing submissions to the Coordinated Land Use Planning Review, related legislation and policy, Environmental Review Tribunal hearing documents, and interviews with key informants. This research culminates in a number of recommendations to the Coordinated Review informed by the analysis.

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The results of parliamentary elections in seven German federal states, ongoing since early 2011, show the collapse of the existing order on the German political scene, both on a national level and on the level of the individual federal states. So far, the federal states have been governed by one of the catch-all parties1 – i.e. the Christian Democrats or Social Democrats – in coalitions with smaller partners – the FDP and the Greens, respectively2. This year’s elections have fully revealed the extent of social transformation in Germany and its impact on voting preferences and the hitherto stable party system in this country. The largest and most popular parties so far – the CDU and the SPD – are losing the voters’ confidence and support, whereas the parties associated with protest movements (such as the Greens) are gaining prominence. Moreover, the German political scene is undergoing increasing fragmentation, as new small, local groups are appearing who have no political aspirations at the federal level but who are attractive to voters acting as successful groups of common cause. The changes in the existing balance of power on the German political scene are being sped up by the specific features of the federal system. Elections to the parliaments of the federal states are held at regular intervals which increasingly affects policies on the national level. The key decisions that concern domestic and foreign affairs are made under the pressure of constant election campaigns.