О механизме формирования рельефа восточного чинка плато Устюрт
Аннотация
New data are presented on the geomorphology of the intermediate step between the eastern scarp of the Ustyurt Plateau and the western coast of the Aral Sea. The step relief formation is supposed to be result of limestone blocks detachment and extrusion of clay ridges between them. The process is a kind of diapirism. The connection of the described mechanism with tectonics and Holocene history of the Aral is pointed out.
Об авторах
В. Вад. БронгулеевРоссия
Г. Н. Пшенин
Россия
Л. Л. Розанов
Россия
Рецензия
Для цитирования:
Бронгулеев В.В., Пшенин Г.Н., Розанов Л.Л. О механизме формирования рельефа восточного чинка плато Устюрт. Геоморфология. 1978;(2):52-60.
For citation:
Bronguleyev V.V., Pshenin G.N., Rozanov L.L. On the mechanism of the formation of the eastern scarp of the Ustyurt Plateau. Geomorfologiya. 1978;(2):52-60. (In Russ.)