Topographic profiles and depth-diameter ratios from the crater Camelot and craters of the central cluster in the Apollo 17 landing area suggest that these craters are of the same age. Therefore, layers that can be recognized in the deep-drill core and that can be identified as ejecta deposits from Camelot or from the cluster craters should yield similar emplacement ages.
Relative age of Camelot crater and crater clusters near the Apollo 17 landing site
Icarus ; 37
1979-01-01
Miscellaneous
No indication
English
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