Mathematics – Logic
Scientific paper
Oct 1991
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1991avest..25..515z&link_type=abstract
Astronomicheskii Vestnik (ISSN 0320-930X), vol. 25, Sept.-Oct. 1991, p. 515-547. In Russian.
Mathematics
Logic
7
Gravitational Fields, Mars (Planet), Planetary Composition, Planetary Structure, Chemical Composition, Green'S Functions, Petrology, Planetary Cores, Planetary Crusts, Planetary Mantles
Scientific paper
Various aspects of the interior structure of Mars, including the chemical composition and a petrological model of the planet, are considered. This model of Mars is divided into three basic regions: the crust, the mantle, and the core. The crust thickness may approach 150-200 km. The depth of the core-mantle boundary is 1600 +/- 200 km. The Martian core may be in a liquid state. The Green function method is used to interpret the gravitational field. The stress level in the Martian lithosphere is several hundred bars. The value of the stresses in the mantle is about 30 bars.
Koshliakov E. M.
Marchenkov Konstantin I.
Zharkov Vladimir Naumovich
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