Launch of martian meteorites in oblique impacts
By N. Artemieva, B. Ivanov. 2004
187 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Atmospheric Science
View Paper: https://www.semanticscholar.org/paper/8d2570ac41c4cf05fdfd2d26d90116ebf9f6f8f7
How researchers see this paper
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In Astronomy and Astrophysics
- U. Christensen
- B. Weiss
- J. Gattacceca
- S. Stanley
- P. Rochette
- A. S. McEwen
- Edward B. Bierhaus
- Julien Aubert
In Atmospheric Science
- U. Christensen
- J. Gattacceca
- P. Rochette
- A. S. McEwen
- B. Weiss
- Edward B. Bierhaus
- Julien Aubert
- P. Olson
Citations in the corpus
- THE IMPORTANCE OF SECONDARY CRATERING TO AGE CONSTRAINTS ON PLANETARY SURFACES (2006, background): “In an oblique impact, the amount of high-velocity ejecta in the downrange direction increases by an order of magnitude (Pierazzo & Melosh 2000, Artemieva & Ivanov 2004, Yamamoto et al. 2005).”
- Paleomagnetic Records of Meteorites and Early Planetesimal Differentiation (2010, background): “On the other hand, for shock pressures above ∼40 GPa, the shock-induced temperature increase (Bischoff and Stoffler 1992; Artemieva and Ivanov 2004) is usually high enough to impart a thermoremanent magnetization (TRM) to the rock during slow cooling from postshock temperatures of ∼400–1100°C.”