Ледниковый и современный морф литогенез в Лужской губе
Аннотация
The glacial morpholithegenesis role is estimated in the modeling of the Pre-Quaternary rock surface. Non-uniform structure of the Valdai ice sheet at the find stage and during retreat of the glacier is shown to influence development of the main recoat landforms within the Luca region. Characteristic of the present-day sedimentation are inferred from the granulometry of sea floor sediments.
Рецензия
Для цитирования:
Челпанов М.Ю. Ледниковый и современный морф литогенез в Лужской губе. Геоморфология и палеогеография. 1995;(2):99-105.
For citation:
Chelpanov M.Yu. Glacial and recent morpholithogenesis in the Luga Guba bay. Geomorfologiya i Paleogeografiya. 1995;(2):99-105.
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