A review of Martian impact crater ejecta structures and their implications for target properties
By N. Barlow. 2005
149 citations recorded by the source corpus.
Subfields: Aerospace Engineering, Astronomy and Astrophysics
View Paper: https://www.semanticscholar.org/paper/862ea29e3bcf151ca0ae0ff4551b5fea921cd2f6
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In Aerospace Engineering
In Astronomy and Astrophysics
- A. S. McEwen
- Nicolas Gonzalez Thomas
- Hirise Team
- Nicolas Mangold
- S. Conway
- B. Langlais
- V. Ansan
- S. Adeli
Citations in the corpus
- A chronology of early Mars climatic evolution from impact crater degradation (2012, background): “This map shows that these ejecta extend about two to three crater radii (2R to 3R) from the crater center, typical for this size of crater [e.g., Barlow, 2005].”
- Mars Reconnaissance Orbiter's High Resolution Imaging Science Experiment (HiRISE) (2007, background): “…cratering has played a large role in sculpting the surface [Strom et al., 1992], but it is unclear whether subtle differences in pristine morphology may reflect the influence of the atmosphere and/or subsurface volatiles during formation [Schultz and Gault, 1979; Schultz, 1992; Barlow, 2005].”