Деструктивный рельеф Гобийского пенеплена в Юго-Восточной Монголии
Аннотация
The paper contains an analysis of the Neogene-Quaternary relief modelled by the wind and water erosion and denudation at the margins of Dariganga volcanic area (SE Mongolia). The author obtained new data on the structure of denudational-deflational plains and various landforms developed on the surface of the Late Cretaceous-Paleogene Gobi peneplain (dry river valleys with hanging mouth, waterfalls and giant's kettles, large deflation hollows within the Miocene-Pliocene sedimentary basins, etc.). First established are evidences of paleo-seismic dislocations, such as longitudinal trenches in dry valley sides on grants, and «wild flysch» in rhythmically bedded sequences.
Рецензия
Для цитирования:
Чичагов В.П. Деструктивный рельеф Гобийского пенеплена в Юго-Восточной Монголии. Геоморфология и палеогеография. 1994;(4):85-99.
For citation:
Chichagov V.P. Destructional relief of the Gobi peneplain in South-Eastern Mongolia. Geomorfologiya. 1994;(4):85-99.
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