Physics
Scientific paper
Apr 1985
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1985pggp.rept..204p&link_type=abstract
In NASA, Washington Repts. of Planetary Geol. and Geophys. Program 1984 p 204-205 (SEE N85-23474 13-91)
Physics
Ejecta, Flow Distribution, Geomorphology, Impactors, Meteorite Craters, Planetary Geology, Terraces (Landforms), Mapping, Planetary Craters, Solar Blankets, Structural Basins, Topology
Scientific paper
The evidence of interaction between impact flow ejecta blankets and pre-existing landforms such as craters, scarps, and wrinkle ridges may yield important clues as to the nature of the ejecta emplacement process. The morphology of flow ejecta blankets and the interactions of these blankets with pre-emplacement impact craters were characterized. About 80 small satellite craters on or in 3 well-expressed low ejecta parent impact craters were recognized. Interaction of the blanket with pre-existing structures was studied, and several types were described. These are: (1) infilling; (2) encroachment; (3) overflow; and (4) breaching. Examination of the overall morphology of three ejecta blankets reveals a range of thickness, from depths sufficient to completely bury craters in the 5 km diameter range in distal areas of the blankets, to very thin blankets which allow subtle pre-existing topography to be visible within a half the diameter of the parent crater. Radial and azimuthal symmetries appear to exist within the blankets over a range of morphologies. It also appears that there is a weak linear correlation between the diameter of craters with nearly 100% infilling and distance from the center of the parent crater.
Baloga Stephen M.
Hurick M.
Pieri David C.
No associations
LandOfFree
Interaction of Martian flow ejecta blankets with pre-existing impact craters: Morphological observations does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.
If you have personal experience with Interaction of Martian flow ejecta blankets with pre-existing impact craters: Morphological observations, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Interaction of Martian flow ejecta blankets with pre-existing impact craters: Morphological observations will most certainly appreciate the feedback.
Profile ID: LFWR-SCP-O-1290016