Признаки «семиаридной» педипланации на Марсе
Аннотация
The ancient Martian craters evolution is shown to proceed about 3.5*109 to 3.8*109 yrs ago due to the pediplanation process (parallel slope retreat) according to the «semiarid» scheme, which is mostly under the action of sheet wash. A global planation surface of the pediplain type is shown to be formed at the time. The global scale of the «semiarid» pediplanation process on Mars during the period about 3.5*109 to 3.8*109 yrs ago suggests much denser atmosphere and higher temperature at the time than at present.
Рецензия
Для цитирования:
Полосухин В.П. Признаки «семиаридной» педипланации на Марсе. Геоморфология. 1987;(3):79-85.
For citation:
Polosukhin V.P. Signs of the «semiarid» pediplanation on Mars. Geomorfologiya. 1987;(3):79-85.
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