The Evolution of Lacustrine Environments on Mars: Is Mars Only Hydrologically Dormant?
By N. Cabrol, E. Grin. 2001
175 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Atmospheric Science
View Paper: https://www.semanticscholar.org/paper/60c38350816e105c701b023f51e78f507d9ffb71
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In Astronomy and Astrophysics
- James W. Head III
- Ralph E. Milliken
- John P. Grotzinger
- Caleb I. Fassett
- Alberto G. Fairén
- R. Wordsworth
- E. Kite
- Stuart J. Robbins
In Atmospheric Science
- James W. Head III
- Alberto G. Fairén
- Caleb I. Fassett
- Ralph E. Milliken
- S. Byrne
- R. Wordsworth
- M. Gudel
- Stuart J. Robbins
Citations in the corpus
- The Sedimentary Rock Record of Mars: Distribution, Origins, and Global Stratigraphy (2012, background): “…suggestion of volcanic ignimbrites (Scott and Tanaka 1982) or volcanic tephra (e.g., Chapman and Tanaka 2002) offset by more provocative ideas, including lacustrine deposits (Lucchitta and Ferguson 1983, Williams and Zimbelman 1994, Cabrol and Grin 2001) or even carbonates (McKay and Nedell 1988).”
- Stability of hydrous minerals on the martian surface (2003, unknown): “These minerals are also common alteration phases in terrestrial lacustrine sediments analogous to saline, alkaline lake deposits that may exist on Mars (Greeley and Williams, 1994; Forsythe and Zimbelman, 1995; Cabrol and Grin, 2001).”
- Flow discharge and sediment transport models for estimating a minimum timescale of hydrological activity and channel and delta formation on Mars (2005, unknown): “Mosangini [1998] and Cabrol and Grin [2001] also clearly E12003 KLEINHANS: WATER AND SEDIMENT IN MARTIAN CHANNELS”
- The timing of martian valley network activity : Constraints from buffered crater counting (2008, background): “The resolution and data quality of the Viking images used in these analyses might also account for fewer small craters and for the youthful basin and crater floor ages derived by Cabrol and Grin (2001).”
- Exploration of hydrothermal targets on Mars (2007, background): “…channel system, Ma'adim Vallis, drains into Gusev crater (Cabrol et al., 1998; Kuzmin et al., 2004), possibly contributing to the formation of a lake (Cabrol and Grin, 2001), though evidence may be obscured by impact cratering and windrelated activity, among other processes (Cabrol et al., 2006).”