Rift processes at Valles Marineris, Mars - Rate dependent strength evolution versus necking

Details Rift processes at Valles Marineris, Mars - Rate dependent strength evolution versus necking Rift processes at Valles Marineris, Mars - Rate dependent strength evolution versus necking

Mar 1997

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1997lpi....28...35a&link_type=abstract

Conference Paper, 28th Annual Lunar and Planetary Science Conference, p. .35.

Other

Mars Surface, Planetary Evolution, Lithosphere, Planetary Structure, Time Dependence, Mathematical Models

Scientific paper

Analytical models for extensional processes that either incorporate the evolution of lithospheric strength as a function of time or are based on the necking instabilities are presently applied to Valles Marineris, comparing the lithospheric structure predicted by each model as being necessary for the formation of the observed troughs. It is noted that the strength-evolution models are not fully 2D, while necking models do not address the evolution of the geotherm with time and finite extension.

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