Mathematics – Logic
Scientific paper
Dec 2002
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002agufm.p22a0385g&link_type=abstract
American Geophysical Union, Fall Meeting 2002, abstract #P22A-0385
Mathematics
Logic
6225 Mars
Scientific paper
Gusev will be an outstanding candidate to achieve the 2003 MER mission goals. The crater has collected sediments from a diversity of parent rocks in the vast Maadim Vallis watershed over a period of three billion years. Because of the interaction between Gusev and Maadim, it has been proposed that a significant volume of the sedimentary material in the crater is of aqueous origin. Mars Odyssey has shown that the hydrogen abundance in the Gusev region is higher than average at corresponding latitudes. This observation could be consistent with a past long lived aqueous activity. The presence of aqueous material is central to the MER mission because it can provide clues about the past water history, climate changes, and the potential habitability of Mars. However, while Gusev is recognized as a primary site because of its past fluvio lacustrine activity, the geological diversity and history of its immediate surroundings makes it exceptional and provides the foundation for an exciting exploration leading to key discoveries. In addition to aqueous, many other processes can have contributed to the material in the crater basin: volcanic, Apollinaris patera is only 200 km away, aeolian, glacial, and global airfall processes. How to identify the signature of each process? What was their succession in time? Do we see the evolution from perennial to more episodic lakes? Do we see interaction between volcanic, glacial, aeolian and lacustrine processes? What was the recurrence of dry episodes? What type of measurements can provide a definitive answer for each of these questions in the 600 m traverse range that the rover will accomplish? What diversity can we also expect in this range? Finally, the uniqueness and potential of Gusev does not reside only in this exceptional diversity. As there is evidence for long lived lake episodes, Gusev also offers the unique possibility to study for the first time the results of the in situ formation of aqueous sediments and minerals in their geological context. This chance was denied in all previous landed missions located in grab bag regions of short lived flows.
Barlow Nadine
Cabrol Nathalie A.
Carr Michael
de Goursac Olivier
Des Marais David
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