Abstract
Previous analyses into viscous relaxation of impact craters on Ganymede
have predicted short characteristic relaxation times (of the order
of 100 Myr or less for larger craters), in disagreement with the
apparent great ages of Ganymede's terrains. By applying improved
understanding of theologic parameters and initial crater shapes to
a viscoelastic model, we calculate upper limit (zero heat flow) relaxation
times in excess of the age of the solar system, eliminating this
discrepancy. These very long relaxation times are not due to elastic
effects, but are simply due to the effective viscosity of water ice
at the appropriate temperatures and stresses.
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