Large impact basins and the mega‐impact origin for the crustal dichotomy on Mars

Geophysical Research Letters

Volumn 15, Issue 3, 1988, Pages 229-232

  Frey, Herbert ^a   Schultz, Richard A ^b  

^a NASA GODDARD SPACE FLIGHT CENTER   (United States)

^b PURDUE UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0023774859     PISSN: 00948276     EISSN: 19448007     Source Type: Journal    
DOI: 10.1029/GL015i003p00229     Document Type: Article

References (17)

1. The evolution of impact basins; cooling, subsidence and thermal stress
2. Global and regional ridge patterns on Mars
3. Crustal evolution of the early Earth: The role of major impacts
4. The martian crustal dichotomy: product of accretion and not a specific event? (abstract)
5. Crater counts in the transition zone in eastern Mars : evidence for common resurfacing events (abstract)
6. A widespread common age resurfacing event in the highland‐lowland transition zone in eastern Mars
7. Considerations of large scale impact and the early Earth (abstract)
8. Martian ages
9. Impact basin control of volcanic and tectonic provinces on Mars (abstract)
10. The structure and evolution of ancient impact basins on Mars
11. Assessment of global and regional tectonic models for faulting in the ancient terrains of Mars
12. Characteristic structures of the highland boundary on Mars; evidence against a single mega‐impact event? (abstract)
13. The evolution of impact basins: viscous relaxation of topographic relief
14. Martian impact basins: morphology differences and tectonic provinces (abstract)
15. The martian hemispherical dichotomy may be due to a giant impact
16. Tectonic evolution of Mars