COLOR AND ALBEDO OF THE SOUTH POLAR LAYERED DEPOSITS ON MARS

被引:33
作者
HERKENHOFF, KE
MURRAY, BC
机构
[1] Division of Geological & Planetary Sciences, California Institute of Technology, Pasadena
来源
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS | 1990年 / 95卷 / B2期
关键词
D O I
10.1029/JB095iB02p01343
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Five color/albedo units, including polar frost, have been recognized and mapped in the southern layered deposits on Mars. The layered deposits appear to be mantled by red dust, except where eolian stripping has exposed the underlying bedrock. Frost and bare ground are mixed below the resolution of the images in many areas adjacent to the polar cap, some of which appear to be younger than the surrounding layered terrain. Dark material has been deposited in topographic depressions in much of the south polar region, including the layered deposits. The available observational data suggest that the layered deposits are composed of bright dust, ice, and a small amount of dark material. If the dark material is sand, a periodic change in polar winds seems required in order to transport the sand poleward into the layered terrain. -from Authors
引用
收藏
页码:1343 / 1358
页数:16
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