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Titlebook: High-Pressure Shock Compression of Solids V; Shock Chemistry with Lee Davison,Yasuyuki Horie,Toshimori Sekine Book 2003 Springer Science+Bu

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Redistribution of Radiogenic Lead in Plagioclase during Shock Metamorphism,ad in plagioclase during shock metamorphism. Almost all of the samples recovered from the Apollo and Luna missions have experienced shock metamorphism. With increasing shock intensity, plagioclase converts to the isotropic glass, “maskelynite,” which is ubiquitously observed in highland rocks and mare basalts.
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Impact Processes of Ice in the Solar System,n of the solar system. This chapter concentrates on impact processes of ices at various impact velocities, and shows how the various impact phenomena are related to the origin and evolution of icy planets in the solar system.
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Book 2003f civili­ zation, shock phenomena have been subjects of continuing interest, speculation, and enquiry. The interdisciplinary aspects of investigations of shock phenomena are especially noteworthy, and these investigations have been pursued by scien­ tists and engineers from a broad range of discipli
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Experimental Techniques for the Simulation of Shock Metamorphism: A Case Study on Calcite,effects of these still ongoing collisions are visible from the megascopic down to the submicroscopic length scale, i.e., they range from large impact craters and their ejecta blankets down to shock-metamorphic effects in minerals [2–4]. These effects form as a result of the interaction of strong shock waves with the affected solid matter.
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Structural Evolution of Quartz and Feldspar Crystals and their Glasses by Shock Compression, several impact craters on the present earth where we find shock-wave deformation textures and high-pressure minerals formed by shock-wave effects. Especially, stishovite is one of the best known shock products in nature [3]. Diaplectic glasses transformed from mineral crystals by shock metamorphism
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