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- W65440088 abstract "For nearly three decades researchers have suggested that Ganymede’s ubiquitous grooves formed via periodic extensional necking of the ice lithosphere [e.g., 1,2,3]. While analytical and numerical models have indicated that the necking mechanism is feasible [4,5], successful models of groove formation that include large strains, random initial topography, and realistic lithospheric strength profiles have not yet been achieved. Here we present new numerical models of extensional deformation in an ice lithosphere that successfully produce periodic, large-amplitude, groove-like features under more physically realistic conditions." @default.
- W65440088 created "2016-06-24" @default.
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- W65440088 date "2009-09-01" @default.
- W65440088 modified "2023-09-23" @default.
- W65440088 title "The formation of Ganymede's grooved terrain" @default.
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- W65440088 hasPublicationYear "2009" @default.
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