Mantle differentiation and the crustal dichotomy of Mars

Planetary and Space Science

Volumn 41, Issue 4, 1993, Pages 269-283

  Breuer, D ^a   Spohn, T ^a   Wullner U ^a  

^a UNIVERSITY OF MÜNSTER   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 38249001396     PISSN: 00320633     EISSN: None     Source Type: Journal    
DOI: 10.1016/0032-0633(93)90022-T     Document Type: Article

References (69)

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6. Influence of heating mode on three-dimensional mantle convection
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9. 3-D convection with variable viscosity
10. Mars thickness of the lithosphere from the tectonic response to volcanic loads
11. Mars, a volatile rich planet
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13. Large impact basins and the megaimpact origin for the crustal dichotomy on Mars
14. A widespread common age resurfacing event in the highland-lowland transition zone in eastern Mars
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19. The destruction of geochemical heterogeneities by differential fluid motions during mantle convection
20. The dependence of convection platform on mode of heating
21. Chronology of SNC meteorites
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23. Water in SNC meteorites—evidence for a Martian hydrosphere
24. Chemical systematics of the Shergotty meteorite and the composition of its parent body (Mars)
25. Magmatic processes on Mars: insights from SNC meteorites (abstract)
26. What SNC meteorites tell us about Martian magmatism (abstract)
27. Geologic evidence supporting an endogenic origin for the Martian crustal dichotomy
28. SNC meteorites: clues to Martian petrologic evolution?
29. Origin and evolution of the Nakhla meteorite inferred from Sm-Nd and U-Pb systematics and REE, Ba, Sr, Rb abundances
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32. Do oblique impacts produce Martian meteorites?
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34. Phenocryst-matrix partition coefficients for K, Rb, Sr, and Ba, with applications to anorthosite and basalt genesis
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43. A thermal history for the Earth with parameterized convection
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58. The resurfacing history of Mars: a synthesis of digitized, Viking-based geology
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63. The Martian hemispherical dichotomy may be due to a giant impact
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