Numerical modelling of impact melt production in porous rocks
Melting of rocks by impact is a fundamental geologic process that results from shock wave compression and subsequent release from high pressure. Shock-melted material is found in many terrestrial craters; however, most impact craters in sedimentary targets, which are typically porous, have been repo...
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Veröffentlicht in: | Earth and planetary science letters 2008-05, Vol.269 (3), p.530-539 |
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