Physics – Geophysics
Scientific paper
May 1987
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987pggp.rept..319p&link_type=abstract
In NASA, Washington, Reports of Planetary Geology and Geophysics Program, 1986 p 319-321 (SEE N87-23341 16-91)
Physics
Geophysics
1
Canyons, Geomorphology, Mars Surface, Seas, Stratigraphy, Structural Properties (Geology), Debris, Erosion, Ground Water, Terrain, Topography
Scientific paper
The fretted terrain in west Deuteronilus Mensae consists of extensive cratered upland penninsulas or isolated plateaus cut by long, finger-like canyons typically 10 to 20 km wide and upwards of 300 km long. The longest of these canyons trend roughly north-south to north-northeast, which may reflect some local structural and/or topographic control. At least three geomorphic zones roughly parallel to the lowland/upland boundary, suggestive of increasing modification northward, can be recognized on the fretted region of the region. The southern-most zone (zone A) consists of sharply defined fretted terrain. The middle zone (zone B) consists of well defined fretted terrain in which the plateau surfaces appear smoother, with a somewhat darker and much less varied albedo surface than those of zone A. The northern-most zone (zone C) consists of rounded or softened fretted terrain. The zones were interpreted as surface exposures of successively lower stratigraphic units.
Parker Timothy J.
Pieri David C.
Saunders Stephen R.
Schneeberger Dale M.
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