Author/Authors :
Rodriguez، نويسنده , , J. Alexis P. and Leonard، نويسنده , , Gregory J. and Platz، نويسنده , , Thomas and Tanaka، نويسنده , , Kenneth L. and Kargel، نويسنده , , Jeffrey S. and Fairén، نويسنده , , Alberto G. and Gulick، نويسنده , , Virginia and Baker، نويسنده , , Victor R. and Glines، نويسنده , , Natalie and Miyamoto، نويسنده , , Hideaki and Jianguo، نويسنده , , Yan and Oguma، نويسنده , , Midori، نويسنده ,
Abstract :
The martian south polar plateau, Planum Australe, comprises the largest known water–ice surface deposit on the planet. Here, we present evidence for an episode of extensive polar plateau retreat during the Late Amazonian, which affected regions flanking circum-polar terrains located between Cavi Angusti and Sisyphi Montes.
Keywords :
Mars , polar geology , ICES , polar caps
