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G. Smeetsenic processes (those within the Earth´s crust), called tectonics. These images and the processes that they document show that continents are shifting, mountains are uplifting, and ocean bottoms may sink deeper978-94-024-0625-2978-94-017-9713-9
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Conference proceedings 1995res of the 19th International Symposium on Shock Waves held in Marseille in 1993. They are published in four topical volumes, each containing papers on related topics, and preceded by an overview written by a leading international expert. The volumes may be purchased independently.
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Interaction of Thermal Protection Materials with the High-Enthalpy Flow of the Arc-Heated Wind Tunneum processes in the nozzle flow coupled with frozen or equilibrium shock solutions. Spectroscopic analyses of the material composition of the samples tested in the air atmosphere indicate the development of a protective SiO.-layer.
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A Life with Shock Waves (Ernst Mach Memorial Lecture)rst motivation was to use the shock tube as a short-duration aerodynamic test facility, a goal to be belately achieved, with results on e.g. hypersonic flow around flared bodies, or transonic motion of permeable airfoils. In the meantime, two shock tubes and a large facility, combining the shock- an
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Computational Analysis on Generic Forms in European Hypersonic Facilities: Standard Model Electre anElectre whose purpose is to serve as a standard model in hypersonic wind tunnel testing. The second form is a hyperboloid flare for the study of the separation and reattachment of the boundary layer in front of a deflected control flap. The Electre standard model does not only serve to improve the f