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Titlebook: Observation of the Continental Crust through Drilling I; Proceedings of the I C. Barry Raleigh Conference proceedings 1985 Springer-Verlag

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Programme on the Deep Geology of France First Year’s Resultsountries, this programme is oriented towards deep drilling, despite the fact that this does not constitute the principal objective. The main aim is to understand the deep geology of France. In this country an important part of the Paleozoic basement structures, under the sedimentary basins, is inacc
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Deep Drilling Programs in Belgiumubdivided into three main geological regions: a northern one, composed mostly by gentle dipping strata to the north, and north-east since devonian times, a southern one intensively affected by the Variscan orogeny and a central part forming the so-called (London)-Brabant Massif (Fig. 1).
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Scientific Continental Drilling Project in Japan and Scientific Goalsc characteristics. The Island Arc involves continental crust formed by the accretionary process. The continental crust is separated from the Eurasian Continent by the marginal seas with oceanic crust. Studies of the geologic history of the continental crust suggest that one should consider the conti
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Characterizing Thermal Energy and Mass Transport in Volcanic Caldera Complexes; The Role of Scientift only do they represent profound thermal anomalies in the lithosphere which potentially may be exploited for energy and economic ore deposits, they also offer grave volcanic and earthquake hazards during major eruptive phases.
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Scientific Drilling to Study the Roots and Margins of Hydrothermal Mineral Systems as well as the geochemistry of the crust and its fluids, structure and tectonics. Drilling offers opportunities for verification of the required projections, and is thus a required step in furthering crustal understanding. Like any new science, the direct observations that drilling provides commonl
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