Sedimentary textures formed by aqueous processes, Erebus crater, Meridiani Planum, Mars

@article{Grotzinger2006SedimentaryTF,
  title={Sedimentary textures formed by aqueous processes, Erebus crater, Meridiani Planum, Mars},
  author={J. Grotzinger and J. Bell and K. Herkenhoff and Jeffrey B. Johnson and A. Knoll and E. McCartney and S. McLennan and J. Metz and J. Moore and S. Squyres and R. Sullivan and O. Ahronson and R. Arvidson and B. L. Joliff and M. Golombek and K. Lewis and T. Parker and J. Soderblom},
  journal={Geology},
  year={2006},
  volume={34},
  pages={1085-1088}
}
New observations at Erebus crater (Olympia outcrop) by the Mars Exploration Rover Opportunity between sols 671 and 735 (a sol is a martian day) indicate that a diverse suite of primary and penecontemporaneous sedimentary structures is preserved in sulfate-rich bedrock. Centimeter-scale trough (festoon) cross-lamination is abundant, and is better expressed and thicker than previously described examples. Postdepositional shrinkage cracks in the same outcrop are interpreted to have formed in… Expand

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