Early geochemical environment of Mars as determined from thermodynamics of phyllosilicates
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/nature05961.pdf
Reference29 articles.
1. Malin, M. C. & Edgett, K. S. Evidence for persistent flow and aqueous sedimentation on early Mars. Science 302, 1931–1934 (2003)
2. Poulet, F. et al. Phyllosilicates on Mars and implications for the early Mars history. Nature 481, 623–627 (2005)
3. Bibring, J.-P. et al. Mars surface diversity as revealed by the OMEGA/Mars Express observations. Science 307, 1576–1581 (2005)
4. Meunier, A. & El Albani, A. The glauconite–Fe-illite–Fe-smectite problem: a critical review. Terra Nova 19, 95–104 (2006)
5. Bibring, J. P. et al. Global mineralogical and aqueous Mars history derived from OMEGA/Mars express data. Science 312, 400–404 (2006)
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