The Transition from Complex Craters to Multi-Ringed Basins on Terrestrial Planetary Bodies: The Scale-Dependent Role of the Expanding Melt Cavity and Progressive Interaction with the Displaced Zone

Details The Transition from Complex Craters to Multi-Ringed Basins on Terrestrial Planetary Bodies: The Scale-Dependent Role of the Expanding Melt Cavity and Progressive Interaction with the Displaced Zone The Transition from Complex Craters to Multi-Ringed Basins on Terrestrial Planetary Bodies: The Scale-Dependent Role of the Expanding Melt Cavity and Progressive Interaction with the Displaced Zone

Mar 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpi....41.1029h&link_type=abstract

41st Lunar and Planetary Science Conference, held March 1-5, 2010 in The Woodlands, Texas. LPI Contribution No. 1533, p.1029

Computer Science

1

Scientific paper

The "nested melt-cavity" model combines main components of the cratering
process (transient cavity, displaced zone, melt cavity) and provides a
basis for understanding the characteristics of the transition from
complex craters to multi-ringed basins.

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