Physics – Geophysics
Scientific paper
Mar 1993
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993thtp.reptq....s&link_type=abstract
In MIT, Tectonic History of the Terrestrial Planets 19 p (SEE N94-31105 09-91)
Physics
Geophysics
Convective Heat Transfer, Geochemistry, Geophysics, Lithosphere, Mars (Planet), Mars Surface, Outgassing, Planetary Geology, Composition (Property), Isotopes, Meteorites, Viscosity
Scientific paper
The thermal evolution of Mars is governed by subsolidus mantle convection beneath a thick lithosphere. Models of the interior evolution are developed by parameterizing mantle convective heat transport in terms of mantle viscosity, the superadiabatic temperature rise across the mantle and mantle heat production. Geological, geophysical, and geochemical observations of the composition and structure of the interior and of the timing of major events in Martian evolution, such as global differentiation, atmospheric outgassing and the formation of the hemispherical dichotomy and Tharsis, are used to constrain the model computations. Isotope systematics of SNC meteorites suggest core formation essentially contemporaneously with the completion of accretion. Other aspects of this investigation are discussed.
Drake Michael J.
Schubert Gerald
Sleep Norman H.
Solomon Sean C.
Turcotte Donald L.
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