Model constraints on the opening rates of bands on Europa |
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Authors: | Michelle M Stempel Robert T Pappalardo |
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Institution: | Laboratory for Atmospheric and Space Physics, University of Colorado at Boulder, Campus Box 392, Boulder, CO 80309-0392, USA |
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Abstract: | A mid-ocean-ridge spreading analog is used to constrain the opening rates and brittle-ductile transition depths for two axisymmetric ridged bands on Europa. Estimates of brittle-ductile transition depth based on the morphologies of Yelland and Ino Lineae are combined with a conductive cooling model based on a mid-ocean ridge analog to estimate the opening rates and active lifetimes of the bands. This model limits local strain rates to ∼10−15-10−12 s−1, opening rates to 0.2-40 mm yr−1, and active lifetimes of the bands to 0.1-30 Myr. If the observed structures in the outer portions of ridged bands are indeed normal faults, the estimated range for the tensile strength of ice on Europa is 0.4-2 MPa, consistent with nonsynchronous rotation as the dominant driving mechanism for band opening. |
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Keywords: | Europa Geological processes Geophysics Satellites of Jupiter Tectonics |
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