Тенденции кайнозойского морфолитогенеза в Западном Приохотье
Аннотация
A composite section of loose deposits of Western Okhotsk region has been compiled, and environments of sedimentation determined. A transition of graded topography with extensive weathering crusts and fine sediments towards rugged topography (low and medium-height mountains), with associated coarse - pebble and cobble - deposits, is recognized as the main trend in the Cenozoic morpholithogenesis. Most abrupt change falls on the middle Pliocene.
Рецензия
Для цитирования:
Каревская И.А., Лебедева Е.В., Куликов О.А. Тенденции кайнозойского морфолитогенеза в Западном Приохотье. Геоморфология. 1994;(2):115-124.
For citation:
Karevskaya I.A., Lebedeva E.V., Kulikov O.A. Trends in the Cenozoic morpholithogenesis in Western Okhotsk region. Geomorfologiya. 1994;(2):115-124.