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Titlebook: Basement Tectonics 11 Europe and Other Regions; Proceedings of the E O. Oncken,C. Janssen Conference proceedings 1996 Springer Science+Busi

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期刊全称Basement Tectonics 11 Europe and Other Regions
期刊简称Proceedings of the E
影响因子2023O. Oncken,C. Janssen
视频video
学科分类Proceedings of the International Conferences on Basement Tectonics
图书封面Titlebook: Basement Tectonics 11 Europe and Other Regions; Proceedings of the E O. Oncken,C. Janssen Conference proceedings 1996 Springer Science+Busi
影响因子The Eleventh International Conference on Basement Tectonics was held at the GeoForschungsZentrum Potsdam in Germany 25-29 July 1994. It was the first time that a meeting of this series took place in the centre of Europe and the first such meeting in this area after the recent political changes in eastern Europe. Consequently, the main theme of the meeting focussed on the structure and history of the entire European continent. Further themes were grouped around topics of current interest. Keynote lectures on these topics were given by A. Berthelsen, St. Mueller, A. Green, and D. Fountain. The technical sessions were arranged with support of the Scientific Committee on the following topics: 1. Continental scale features of basement rocks of phanerozoic cratons - with emphasis on Europe 2. Extrapolation and correlation of geological and geophysical data from basement rocks: an assessment 3. Mechanisms of basement exhumation in the evolution of orogenic belts 4. Structure and intraplate deformation of the North-American craton Papers submitted to this volume have however all been collected in one part since all of them deal with different aspects of deformation of the continental basem
Pindex Conference proceedings 1996
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Hegels Interpretation dieser Welt,iferous burial and exhumation history at a major Variscan suture zone in Central Europe. Modeling suggests that during Late Viséan to Early Namurian times convergence rates between two of the main tectono-metamorphic units of the Variscan fold belt, Saxothuringian and Rhenohercynian, exceeded 30 mm/
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Die erste Generation nach Hegelm monzonite to granodiorite. This batholith intruded upper Proterozoic to lower Paleozoic anchizonal to greenschist facies, multiply deformed metasediments during which a narrow (.004 to.16 batholith radii) structural aureole formed in the country rock. The structural characteristics of this aureole
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The Metamorphoses of EmpiricismStructurally upwards these are: (1) Izera-Karkonosze (gneisses and mica schists), (2) South Karkonosze (phyllites and metabasites), and (3) Leszczyniec (metabasites and gneisses) units. All three units experienced contrasting metamorphic paths..Three ductile deformation events (D., D., D.) have been
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Martinus Nijhoff Philosophy Libraryites with seismic velocities as high as P.=6.35–7.05 km/s, densities of 2.85–3.08 g/cm. (Meissner, 1986) and radioactive heat productions of A=0.48–0.53 µW/m. (Rudnick, 1992, Kremenetsky et al., 1986). In contrast the upper crust is enriched with highly radioactive granite batholiths and granite-mig
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Observation of Organic Nature (A)rocks (Hirata et al, 1987; Sammis and Biegel, 1989) because it provides the simplest nontrivial description of scale invariance of physical systems. Computer simulation of quasi-static fracture in solids that incorporates lattice models (Louis and Guinea, 1989; Hassold and Srolovitz, 1989) also gene
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Hegel—From Foundation to System western Alps). Small-scale textural variations in migmatites, which can be observed in hand-sample and outcrop scale, closely resemble the overall structural style and kilometer-scale distribution of texturally distinct migmatites within the Argentera basement. Three-dimensional contouring of textu
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