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On the comparative evolution of Ganymede and CallistoThe paper examines the differences in the apparent ages of the surfaces of Ganymede and Callisto revealed by Voyager images. The differences could be due to the persistence of tectonic activity on Ganymede beyond the time of early, heavy bombardment. The slightly greater radioactive content expected in Ganymede could prolong such activity by 0.5 million years beyond the cessation of endogenic surface activity on Callisto. It is concluded that if the different ages of the surfaces of Ganymede and Callisto are due to differences in internal evolution, the slightly higher radioactive content of Ganymede is the most likely cause; tidal dissipation could not have been important for Ganymede for more than 10 to the 8th power years, and it was never important for Callisto.
Document ID
19800043910
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Cassen, P.
(NASA Headquarters Washington, DC United States)
Reynolds, R. T.
(NASA Ames Research Center Theoretical and Planetary Studies Branch, Moffett Field, Calif., United States)
Peale, S. J.
(California, University Santa Barbara, Calif., United States)
Date Acquired
August 10, 2013
Publication Date
February 1, 1980
Publication Information
Publication: Icarus
Volume: 41
Subject Category
Lunar And Planetary Exploration
Accession Number
80A28080
Funding Number(s)
CONTRACT_GRANT: NGR-05-010-062
CONTRACT_GRANT: NCA2-OR-680-805
Distribution Limits
Public
Copyright
Other

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