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By Richard A. F. Grieve, David A. Kring (auth.), Dr. Peter T. Bobrowsky, Dr. Hans Rickman (eds.)
In 1908 an atmospheric explosion in northern Siberia published strength corresponding to 15 Mton of TNT. Can a similar or better NEO impact us back? while the subsequent NEO moves Earth will it's sufficiently big to break a urban? Will the weather switch considerably? Can archaeology and anthropology offer insights into the anticipated cultural responses with NEO interactions? Does society have a real take hold of of the particular dangers concerned? Is the good melancholy an outstanding version for the commercial cave in which may keep on with a NEO disaster? This quantity presents an important hyperlink among quite a few disciplines and comet/asteroid impacts.
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Extra info for Comet/Asteroid Impacts and Human Society: An Interdisciplinary Approach
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Nature 388:365–368 Bryant E (2004) Geological and cultural evidence for cosmogenic tsunami. Paper presented at the ICSU Workshop on Comet/Asteroid Impacts and Human Society, Tenerife, Canary Islands. Bunch TE (1968) Some characteristics of selected minerals from craters. In: French BM, Short NM (eds) Shock metamorphism of Natural Materials. Mono Book Corp, Baltimore, pp 413–432 Campins H, Swindle TD, Kring DA (2004) Evaluating comets as a source of Earth’s water. In: Seckbach J (ed) Origins: genesis, evolution and diversity of life.
Approximate rates of occurrence of impact events of a particular magnitude are indicated in orders of magnitude. The propagation of the air blast in the largest impact events may be affected by the curvature of the Earth, which was accommodated by assuming that the wave travels radially and does not produce over-the-horizon damage. Modified from Toon et al. (1997), which includes additional details. Approximate rates of occurrence of impact events of particular magnitudes are indicated at the level of orders of magnitude.
1981), or to differentiated impacting bodies, such as basaltic achondrites that are not relatively enriched in PGEs relative to terrestrial rocks. g. Koeberl et al. 1996; PeuckerEhrenbrink 2001; Farley 2001). 2 Fused Glasses and Diaplectic Glasses Shock fused glasses are characterized morphologically by flow structures and vesiculation. Peak pressures required for shock melting of single crystals are in the order of 40 to 60 GPa (Stöffler 1972, 1974). Under these conditions, the minerals in the rock melt independently after the passage of the shock wave and melting is mineral selective.