Channel morphometry, sediment transport, and implications for tectonic activity and surficial ages of Titan basins

Details Channel morphometry, sediment transport, and implications for tectonic activity and surficial ages of Titan basins Channel morphometry, sediment transport, and implications for tectonic activity and surficial ages of Titan basins

Aug 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011icar..214..561c&link_type=abstract

Icarus, Volume 214, Issue 2, p. 561-570.

Physics

1

Scientific paper

We evaluate networks and bifurcation ratios for five Titan and three terrestrial basins. Three Titan basins are dendritic with bifurcation ratios below the terrestrial range. Two Titan basins display patterns suggestive of potential tectonic influence. We use sediment transport rates to generate a timescale for lowering a Titan basin. The denudation timescale ranges from ˜60 Kyr to 470 Myr, depending on model inputs.

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