A global data base was assembled for the study of Mars crater ejecta morphology. The craters were classified as to morhology using individual photographic prints of Viking orbiter frames. Positional and scale information were derived by fitting digitized mosaic coordinates to lattitude-longitude coordinates of surface features from the Mars geodetic control net and feature coordinates from the U.S.G.S. series of 1:5,00,000 scale shaded relief maps. Crater morphology characteristics recorded are of two classes - attributes of each ejecta deposit and other crater charactersitics. Preliminary efforts to check the data base with findings of other workers are described
Comparative planetological analyses of cratering and geomorphological processes were researched, wit...
Current research attempts to describe morphologic features seen in very high resolution Viking Orbit...
This work combines several studies related to the sedimentary rock record of Mars. Data from severa...
Impact craters are arguably the primary exogenic planetary process contributing to the surface evolu...
The most recent comprehensive database of Martian impact craters was the result of the work of impac...
The Mars Crater Morphology Consortium recommends the use of a standardized nomenclature system when ...
International audienceMartian meteorites are the only samples from the Red Planet available for in-d...
Mariner 6 and 7 pictures show that craters are the dominant landform on Mars and that their occurren...
Mars, a planet with a tenuous atmosphere and starved of surface water, is a prime location for study...
Fresh Martian impact craters display a variety of ejecta blanket morphologies. The fluidized appeara...
Double layered ejecta (DLE) craters display two distinct layers of ejecta that appear to have been e...
The Mars Crater Morphology Consortium recommends the use of a standardized nomenclature system when ...
The lobate ejecta morphology surrounding most fresh Martian impact craters can be quantitatively ana...
The impact cratering record documents the history of resurfacing events on Mars. The morphology and ...
Introduction: The population of impact craters preserved on the surface of Mars offers fundamental c...
Comparative planetological analyses of cratering and geomorphological processes were researched, wit...
Current research attempts to describe morphologic features seen in very high resolution Viking Orbit...
This work combines several studies related to the sedimentary rock record of Mars. Data from severa...
Impact craters are arguably the primary exogenic planetary process contributing to the surface evolu...
The most recent comprehensive database of Martian impact craters was the result of the work of impac...
The Mars Crater Morphology Consortium recommends the use of a standardized nomenclature system when ...
International audienceMartian meteorites are the only samples from the Red Planet available for in-d...
Mariner 6 and 7 pictures show that craters are the dominant landform on Mars and that their occurren...
Mars, a planet with a tenuous atmosphere and starved of surface water, is a prime location for study...
Fresh Martian impact craters display a variety of ejecta blanket morphologies. The fluidized appeara...
Double layered ejecta (DLE) craters display two distinct layers of ejecta that appear to have been e...
The Mars Crater Morphology Consortium recommends the use of a standardized nomenclature system when ...
The lobate ejecta morphology surrounding most fresh Martian impact craters can be quantitatively ana...
The impact cratering record documents the history of resurfacing events on Mars. The morphology and ...
Introduction: The population of impact craters preserved on the surface of Mars offers fundamental c...
Comparative planetological analyses of cratering and geomorphological processes were researched, wit...
Current research attempts to describe morphologic features seen in very high resolution Viking Orbit...
This work combines several studies related to the sedimentary rock record of Mars. Data from severa...