The DOI matches its Crossref record; 7 of the 7 references it cites were found in a registry or an index.
Mars Global Surveyor Mars Orbiter Camera: Interplanetary cruise through primary mission
Open accessAbstract
More than 3 years of high‐resolution (1.5–20 m/pixel) photographic observations of the surface of Mars have dramatically changed our view of that planet. Among the most important observations and interpretations derived therefrom are that much of Mars, at least to depths of several kilometers, is layered; that substantial portions of the planet have experienced burial and subsequent exhumation; that layered and massive units, many kilometers thick, appear to reflect an ancient period of large‐scale erosion and deposition within what are now the ancient heavily cratered regions of Mars; and that processes previously unsuspected, including gully‐forming fluid action and burial and exhumation of large tracts of land, have operated within near‐contemporary times. These and many other attributes of the planet argue for a complex geology and complicated history.
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Christensen, P. R., Bandfield, J. L., Hamilton, V. E., Ruff, S. W., Kieffer, H. H., Titus, T. N., Malin, M. C., Morris, R. V., Lane, M. D., Clark, R. L., et al. (2001) · Journal of Geophysical Research: Planets · doi:10.1029/2000je001370 · Cited by 1,061
Self-citationAncient oceans, ice sheets and the hydrological cycle on Mars
Baker, V. R., Strom, R. G., Gulick, V. C., Kargel, J. S., Komatsu, G., & Kale, V. S. (1991) · Nature · doi:10.1038/352589a0 · Cited by 714
Carr, M. H. (1996) · doi:10.1093/oso/9780195099386.001.0001 · Cited by 551
Parker, T. J., Stephen Saunders, R., & Schneeberger, D. M. (1989) · Icarus · doi:10.1016/0019-1035(89)90027-4 · Cited by 376 · cited 3×
“The second example, Figure 125, shows a group of knobs on the northern plains near 45°N, 186°W, that was shown in Parker et al. [1993, Fig. 2b]. Each knob in the Viking image appears to have a series of concentric terraces around its base. The MOC NA image in Figure 125B shows that the concentric pattern is very subtl…”
BackgroundGeomorphic evolution of the Martian highlands through ancient fluvial processes
Craddock, R. A., & Maxwell, T. A. (1993) · Journal of Geophysical Research: Planets · doi:10.1029/92je02508 · Cited by 242
Water and processes of degradation in the Martian landscape
Milton, D. J. (1973) · Journal of Geophysical Research · doi:10.1029/jb078i020p04037 · Cited by 241
Mariner 9 evidence for wind erosion in the equatorial and mid-latitude regions of Mars
McCauley, J. F. (1973) · Journal of Geophysical Research · doi:10.1029/jb078i020p04123 · Cited by 186
Cited by
The physics of wind-blown sand and dust
Kok, J. F., Parteli, E. J. R., Michaels, T. I., & Karam, D. B. (2012) · Reports on Progress in Physics · doi:10.1088/0034-4885/75/10/106901 · Cited by 1,608
Mineralogy of the Martian Surface
Ehlmann, B. L., & Edwards, C. S. (2014) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev-earth-060313-055024 · Cited by 761
Carr, M. H., & Head, J. W. (2010) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2009.06.042 · Cited by 734
The case for rainfall on a warm, wet early Mars
Craddock, R. A., & Howard, A. D. (2002) · Journal of Geophysical Research: Planets · doi:10.1029/2001je001505 · Cited by 601
Martian cratering 8: Isochron refinement and the chronology of Mars
Hartmann, W. K. (2005) · Icarus · doi:10.1016/j.icarus.2004.11.023 · Cited by 601
Metadata
- Authors
- Malin, M. C., & Edgett, K. S.
- Venue
- Journal of Geophysical Research: Planets
- Publisher
- American Geophysical Union (AGU)
- Published
- 2001-10
- Volume
- 106
- Issue
- E10
- Pages
- 23429-23570
- ISSN
- 0148-0227 (ISSN-L)
- OpenAlex
- W2020905882
- Cited by
- 868
- References
- 7
- FWCI
- 23.42
- Type
- journal article
- Language
- en
- Open access
- bronze
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.
