Abstract Global geologic mapping of Mars was originally accomplished following acquisition of orbital spacecraft images from the Mariner 9 mission. The mapping program represented a joint enterprise by the U.S. Geological Survey and other planetary scientists from universities in the United States and Europe. Many of the Mariner photographs had low resolution or poor albedo contrast caused by atmospheric haze and high-sun angles. Some of the early geologic maps reflect these deficiencies in their poor discrimination and subdivision of rock units. New geologic maps made from higher resolution and better quality Viking images also represent a cooperative effort, by geologists from the U.S. Geological Survey, Arizona State University, and the University of London. This second series of global maps consists of three parts: 1) western equatorial region, 2) eastern equatorial region, and 3) north and south polar regions. These maps, at 1:15 million scale, show more than 60 individual rock-stratigraphic units assigned to three Martian time-stratigraphic systems. The first completed map of the series covers the western equatorial region of Mars. Accompanying the map is a description of the sequence and distribution of major tectonic, volcanic, and fluvial episodes as recorded in the stratigraphic record.
Global geologic mapping of Mars: The western equatorial region
Advances in Space Research ; 5 , 8 ; 71-82
1985-01-01
12 pages
Article (Journal)
Electronic Resource
English
Mars Global Geologic Mapping: Amazonian Results
NTRS | 2008
|Mars Global Geologic Mapping: About Half Way Done
NTRS | 2009
|Geologic Mapping in Mars Rover Operations
AIAA | 2010
|Geologic Mapping in Mars Rover Operations
British Library Conference Proceedings | 2010
|Geologic Mapping in Mars Rover Operations
AIAA | 2011
|