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Hesperian Age for Western Medusae Fossae Formation, Mars

Catalog Data

Author:
Scheidt, Stephen P.  Search this
Zimbelman, James R.  Search this
Object Type:
Smithsonian staff publication
Electronic document
Year:
2012
Abstract:
The Medusae Fossae Formation (MFF) on Mars is an intensely eroded deposit north of the cratered highlands. It is widely thought that MFF materials were emplaced through ignimbrite eruptions. Recent geologic mapping of western MFF identified outliers of MFF materials well beyond the previously mapped western extent for the deposit, including outliers close to Gale crater. We report counts of impact craters on the MFF units that have implications for our understanding of the general history of MFF and the uppermost layered materials on the Gale crater mound.
Doi:
10.1126/science.1221094
Citation:
Zimbelman, James R. and Scheidt, Stephen P. 2012. Hesperian Age for Western Medusae Fossae Formation, Mars. <i>Science<i>, 336(6089): 1683 doi:10.1126/science.1221094
Topic:
Flight  Search this
Aeronautics  Search this
Space sciences  Search this
Flight  Search this
Data source:
Smithsonian Libraries
EDAN-URL:
edanmdm:SILSRO_111649