Abstract
Three prime candidate sites for the astrobiological exploration of Mars have been identified on the basis of its hydrogeological history. Each of the sites corresponds to a major inundation phase of the global hydrological model. The Terra Meridiani site is related to the Noachian to Hesperian time, which suggest an aqueous-hydrothermal origin. The Mangala Valles relates to Late Hesperian to Early Amazonian time, where diminishing martian episodic hydrologic events over geologic time are recorded representing a later pulse of tharsis-driven hydrologic activity. The Orcus Patera site relates to Amazonian time, which is a volcanic caldera or impact crater where reduced ponded bodied of water may had existed during almost contemporary times.
Original language | English (US) |
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Pages (from-to) | 201-202 |
Number of pages | 2 |
Journal | European Space Agency, (Special Publication) ESA SP |
Issue number | 545 |
State | Published - Mar 2004 |
Event | Proceedings of the III European Workshop on Exo-Astrobiology - Madrid, Spain Duration: Nov 18 2003 → Nov 20 2003 |
ASJC Scopus subject areas
- Aerospace Engineering
- Space and Planetary Science