Titlebook: Asteroids Impacts, Crustal Evolution and Related Mineral Systems with Special Reference to Australia; Andrew Y. Glikson,Franco Pirajno Boo

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Asteroids and Associated Mineral Systems,ent cavity and the cooling of the melt sheet and melt rocks. Most of what follows is drawn from Pirajno et al. (Aust J Earth Sci 50:775–796, 2003), Pirajno (Aust J Earth Sci 52:587–620, 2005) and Pirajno and Van Kranendonk (Aust J Earth Sci 52:329–352, 2005), particularly for the Australian examples

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https://doi.org/10.1007/978-3-030-70629-6 and the Pilbara Craton about ~3.26–3.227 Ga constitutes a primary example for the tectonic and magmatic effects of asteroid impact clusters in the Archaean, supporting Lowe and Byerly (Did the LHB end not with a bang but with a whimper? 41st Lunar Planet Science Conference 2563pdf, 2010) suggested extension of the late heavy bombardment (LHB).

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,The World’s Largest Late to Post-Archaean Asteroid Impact Structures,ter include the Vredefort and Sudbury structures. Phanerozoic mega-impacts include the Woodleigh impact structure, Warburton twin structures, Chicxulub and Popigai structures. The global tectonic consequences of some of these mega-impacts are yet to be elucidated.