Enceladus's internal ocean and ice shell constrained from Cassini gravity, shape, and libration data

Author:

Čadek Ondřej1,Tobie Gabriel2,Van Hoolst Tim34,Massé Marion2,Choblet Gaël2,Lefèvre Axel2,Mitri Giuseppe2,Baland Rose-Marie3,Běhounková Marie1,Bourgeois Olivier2,Trinh Anthony3

Affiliation:

1. Department of Geophysics, Faculty of Mathematics and Physics; Charles University in Prague; Prague 8 Czech Republic

2. Laboratoire de Planétologie et Géodynamique, UMR-CNRS; University of Nantes; Nantes France

3. Royal Observatory of Belgium; Brussels Belgium

4. Instituut voor Sterrenkunde; KU Leuven; Leuven Belgium

Funder

European Community's Seventh Framework Programme

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference36 articles.

1. Tidally-induced melting events as the origin of South-Pole activity on Enceladus;Běhounková;Icarus,2012

2. Timing of water plume eruptions on Enceladus explained by interior viscosity structure;Běhounková;Nat. Geosci.,2015

3. Convection-driven compaction as a possible origin of Enceladus's long wavelength topography;Besserer;J. Geophys. Res. Planets,2013

4. Constraining the heat flux between Enceladus' tiger stripes: Numerical modeling of funiscular plains formation;Bland;Icarus,2015

5. Čadek , O. G. Choblet M. Běhounková G. Tobie T. Kozubek 2015 Effect of ice-shell thickness variations on the tidal deformation of Enceladus

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