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Detailed Reference Information |
Sotin, C., Head, J.W. and Tobie, G. (2002). Europa: Tidal heating of upwelling thermal plumes and the origin of lenticulae and chaos melting. Geophysical Research Letters 29: doi: 10.1029/2001GL013844. issn: 0094-8276. |
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Tidal heating models are linked to thermal convection models for ice having strongly temperature dependent viscosity. In the range of ice viscosity inferred from laboratory experiments, tidal forces will heat up rising diapirs on Europa. Partial melt produced in the rising diapirs is predicted to create disruption of near-surface materials and formation of lenticulae and chaos, even if the average ice layer thickness overlying an ocean is larger than 20 km. |
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Abstract |
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Keywords
Planetology, Solar System Objects, Jovian satellites, Tectonophysics, Dynamics, convection currents and mantle plumes, Tectonophysics, Heat generation and transport, Tectonophysics, Planetary interiors (5430, 5724) |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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