931 resultados para Six types of Play
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After four rounds of the European Semester process of EU economic coordination, Belgium has done relatively little to comply with EU recommendations. This brief substantiates and confirms this claim after clarifying the meaning of these recommendations. While the challenges underlined by the European Commission still lie ahead, Belgium’s ownership of the recommendations for reforms has been low. Not only do coordination processes remain bureaucratic and technocratic, but many of the recommendations’ concerns – external competitiveness, social security reforms, market reforms – are not traditionally defended by the political left in Belgium. The controversy surrounding the recommendations for national structural reforms owes much to their supply-side orientation, which contrasts with the inability of the EU to pursue demand-side policies. But despite this disequilibrium, the recommendations highlight relevant issues that ought to be addressed, and indicate where scope for national debate exists.
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Total contents of carbohydrates were determined in samples of natural sediments of various genetic types. Analyses were made on board. Deep-sea pelagic sediments (red clays of various types including zeolite clays, and also radiolarian and carbonate oozes) were the main types of sediments studied. Contents of carbohydrates in pelagic oozes of the Central Pacific ranged from 214 to 1605 ppm, averaging 602 ppm of air-dried sediment. Organic matter of the group studied is a diagenetically stable complex, with polysaccharides apparently predominating.
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Nineteen samples of the Cape Roberts-1 drillcore were taken from Miocene- age deposits, from 90.25 - 146.50 metres below seafloor (mbsf) for thin section and laser grain-size analysis. Using the grain-size distribution, detailed core logging, X-radiography and thin-section analysis of microstructures, coupled with a statistical grouping of the grain-size data, three main styles of gravity-flow sedimentation were revealed. Thin (centimetre-scale) muddy debris-flow deposits are the most common and are possibly tirggered by debris rain-out from sea-ice These deposits are characterised by very poorly sorted, faintly laminated muddy sandstones with coarse granules toward their base. Contacts are gradational to sharp. Variations on this style of mass-wasting deposit are rhythmically stacked sequences of pebbly-coarse sandstones representing successive thin debris-flow events. These suggest very high sedimentation rates on an unstable slope in a shallow-water proximal glacimarine environment. Sandy-silty turbidites appear more common in the lower sections of the core, below approximately 141.00 mbsf, although they occur occasionally with the debris flow deposits The turbidites are characterised by inversely to normally graded, well-laminated siltstones with occasional lonestones, and represent a more distal shallow-water glacimarine environment.
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"B-212809"--Prelim. p. [1].
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Mode of access: Internet.
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Mode of access: Internet.
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Mode of access: Internet.
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National Highway Traffic Safety Administration, Washington, D.C.
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Mode of access: Internet.
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