936 resultados para GEOLOGIC FORMATIONS


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Tunnel construction planning requires careful consideration of the spoil management part, as this involves environmental, economic and legal requirements. In this paper a methodological approach that considers the interaction between technical and geological factors in determining the features of the resulting muck is proposed. This gives indications about the required treatments as well as laboratory and field characterisation tests to be performed to assess muck recovery alternatives. While this reuse is an opportunity for excavations in good quality homogeneous grounds (e.g. granitic mass), it is critical for complex formation. This approach has been validated, at present, for three different geo-materials resulting from a tunnel excavation carried out with a large diameter Earth Pressure Balance Shield (EPB) through a complex geological succession. Physical parameters and technological features of the three materials have been assessed, according to their valorisation potential, for defining re-utilisation patterns. The methodology proved to be effective and the laboratory tests carried out on the three materials allowed the suitability and treatment effectiveness for each muck recovery strategy to be defined. © 2014 Elsevier Ltd.

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The reef levels of the gulf of skoura belong to the reef formation of the Upper Miocene of the South-Rifan straits. A detailed analysis of the vertical distribution of various forms of colonies has led to the establishment of precise coral morphologies zonation. This palaeoecological approach leads us to distinguish between two environments in the Skoura gulf, probably corresponding to two reef episodes. The palaeogeographical implications (relationships between the Atlantic ocean and the Mediterranean sea) will be pointed out.

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Cette thèse invite à reconceptualiser le récit dominant quant au parcours d’hommes immigrants de sexualités non normatives. Loin d’être une migration de la tradition vers la modernité, de l’oppression vers la libération, leur parcours est davantage un récit complexe de mobilité et de visibilité inscrit dans des rapports sociaux inégaux. Loin d’être un déchirement entre une «communauté ethnique» homophobe et la «communauté gaie» raciste, leur récit en est un de liens affectifs (r)établis au fil d’interactions sociales significatives. À l’intersection de normes multiples et contradictoires, on constate un processus de (re)formation de subjectivités, à la fois contraintes et habilités par ces normes. Deux corpus sont conjugués, soit l’analyse critique des représentations visuelles et textuelles de la différence ethnique et religieuse dans trois principaux magazines gais québécois et l’analyse par théorisation ancrée d’entretiens semi-dirigés. Ces entretiens ont été menés à Montréal auprès de trente hommes immigrants ayant des relations amoureuses et/ou sexuelles avec d’autres hommes. Les images analysées montrent une tendance à réduire le corps d’hommes de couleur à des objets érotiques et exotiques sur les couvertures des magazines. De plus, les textes avancent un récit de libération sexuelle par la migration qui reproduit les dichotomies dominantes. Un récit beaucoup plus complexe émerge toutefois de l’analyse des entretiens. D’une part, l’expérience de la migration est modulée par divers phénomènes sociaux au-delà de la seule libération sexuelle et l’homophobie se révèle insuffisante pour comprendre le statut des sexualités non normatives, tant dans les pays d’origine que dans les «communautés ethniques» : c’est davantage l’hétéronormativité qui a pour effet de rendre inférieures certaines pratiques de genre et de sexualités. D’autre part, l’expérience de cette visibilité contrainte ne s’exprime que très partiellement par l’idée du «placard» : ces hommes expriment plutôt le vaste potentiel d’expérience d’un espace «tacite» permettant, pour plusieurs, de vivre leur sexualité non normative sans la dire explicitement. Au contraire du rejet des accommodements religieux exprimé dans les magazines gais, les entretiens montrent finalement un réel potentiel d’accommodation du religieux et du sexuel qui, en dépit de tensions, préserve la foi religieuse ou spiritualité tout en vivant la sexualité.

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Quaternary stratigraphy of the Kerala coast and the genetic aspects of the sediments are discussed. The age of limeshells, and peaty sediments determined by radio carbon dating have been used for reconstruction of sea level changes. Evolution of red sands occurring in some parts of the coastal tract of Kerala is also discussed, based on textural parameters and quartz grain morphology.

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The main Precambrian tectonic units of Uruguay include the Piedra Alta tectonostratigraphic terrane (PATT) and Nico Perez tectonostratigraphic terrane (NPTT), separated by the Sarandi del Yi high-strain zone. Both terranes are well exposed in the Rio de La Plata craton (RPC). Although these tectonic units are geographically small, they record a wide span of geologic time. Therefore improved geological knowledge of this area provides a fuller understanding of the evolution of the core of South America. The PATT is constituted by low-to medium-grade metamorphic belts (ca. 2.1 Ga); its petrotectonic associations such as metavolcanic units, conglomerates, banded iron formations, and turbiditic deposits suggest a back-arc or a trench-basin setting. Also in the PATT, a late to post-orogenic, arc-related layered mafic complex (2.3-1.9 Ga), followed by A-type granites (2.08 Ga), and finally a taphrogenic mafic dike swarm (1.78 Ga) occur. The less thoroughly studied NPTT consists of Palaeoproterozoic high-grade metamorphic sequences (ca. 2.2 Ga), mylonites and postorogenic and rapakivi granites (1.75 Ga). The Brasiliano-Pan African orogeny affected this terrane. Neoproterozoic cover occurs in both tectonostratigraphic terranes, but is more developed in the NPTT. Over the past 15 years, new isotopic studies have improved our recognition of different tectonic events and associated processes, such as reactivation of shear zones and fluids circulation. Transamazonian and Statherian tectonic events were recognized in the RPC. Based on magmatism, deformation, basin development and metamorphism, we propose a scheme for the Precambrian tectonic evolution of Uruguay, which is summarized in the first Palaeoproterozoic tectonic map of the Rio de La Plata craton.

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The zircon mineral is widely studied in geochronology. In the case of the fission track method (FTM), the age is determined by the density of fission tracks at the zircon surface, which can be observed with an optical microscope after an appropriate chemical treatment (etching). The etching must be isotropic at the zircon grain surface to be used in the FTM, which leads those zircon grains whose etching is anisotropic to be discarded. The only reason for this discarding is the nonuniform morphology of the surface grain seen by optical microscopy, that is, no further physicochemical analysis is performed. In this work, combining micro-Raman and scanning electron microscopy (SEM) to study the etching anisotropy, it was shown that zircon grains that present at least one area at the surface where the density of fission track is uniform can be used in the FTM. The micro-Raman showed characteristic spectra of the standard zircon sample either from the areas where there are tracks or from where there are not. The only difference found was in the Raman bandwidths, which were broader for the areas with higher density of fission tracks. This suggests simply a decrease in the relative percentage of the crystalline/amorphous phases at these areas. The SEM/energy dispersive spectrometry (EDX) showed that there were no significant differences in the principal chemical composition at the areas with and without fission tracks. Copyright (c) 2008 John Wiley & Sons, Ltd.

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)