Formation of Impact Craters on Ganymede and Callisto as a Constraint on Ice Shell Structure
Abstract
Modeling of cratering events on Ganymede fits a broader range of data than previous work and suggest the ice shell has a conductive layer roughly 12 km thick.
- Publication:
-
49th Annual Lunar and Planetary Science Conference
- Pub Date:
- March 2018
- Bibcode:
- 2018LPI....49.1548B