Rock fluidization during peak-ring formation of large impact structures.

Ulrich Riller1, Michael H Poelchau2, Auriol S P Rae3

  • 1Institut für Geologie, Universität Hamburg, Hamburg, Germany. ulrich.riller@uni-hamburg.de.

Nature
|October 26, 2018
PubMed
Summary

Meteorite impacts cause rocks to drastically weaken, flow, and then regain strength to form impact rings. This study reveals acoustic fluidization as a key process in cratering mechanics.

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