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- W330825345 abstract "We have applied the model to simulate induced stresses in the presence of a subsurface ocean underneath the ice shell of Jovian moon Europa and to correlate these stresses with the shape of the lineaments of cracks and ridges observed on the surface. Stresses at the surface might be induced by several different mechanisms, from which only the two most important are analyzed: the eccentricity tide acting on Europa and non-synchronous rotation (NSR) of the ice shell. The eccentricity-tide forcing induces a highly variable stress field that explains the formation of cycloidal features without taking into account NSR stresses. The NSR mechanism induces a nearly static stress field that explains the formation of both regional slightly-curved and global lineaments. As both types of lineaments exist on the surface of Europa, the strength of NSR stresses should have changed throughout the geological history of Europa. Such a change can be driven by a variable rate of non-synchronous rotation, which can be the result of thickness variations in the ice shell." @default.
- W330825345 created "2016-06-24" @default.
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- W330825345 date "2010-05-01" @default.
- W330825345 modified "2023-09-24" @default.
- W330825345 title "State of Stresses at the Icy Surface of Europa: A Strong Case for the Existence of a Subsurface Ocean" @default.
- W330825345 hasPublicationYear "2010" @default.
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