| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 1773994 | Icarus | 2011 | 22 Pages |
Abstract
⺠Diurnal stresses are not always virtually elastic. ⺠A strongly dissipative warm ice layer causes a westward shift of diurnal stress patterns. ⺠A small obliquity substantially influences the orientation of diurnal stresses. ⺠Relaxation of ocean-ice boundary is only important for NSR if the ice shell behaves elastically. ⺠The large diversity of surface lineaments on Europa suggests variations in the rate of NSR.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Space and Planetary Science
Authors
Hermes M. Jara-Orué, Bert L.A. Vermeersen,