Развитие низовьев р. Колымы в плейстоцене
Аннотация
Five stages of the Kolyma Lowland formation can be identified on the base of the geomorphic interpretation of large-scale aerial photographs as well as field studies conducted by the author at the lower reaches of the Kolyma River. The stages are as follows: Neogene-Early Pleistocene (N-Q1), Middle Pleistocene (Q21+2), two stage during Late Pleistocene (Q31+2 and Q33+4) and recent - Holocene (Q4). Each stage left relicts of ancient valleys and deltas of the Kolyma River at the modern topography. The relicts show evidence that during the Quaternary a series of block subsidences along fault lines resulted in the river migration eastward (until it took its present position), the distance of the migration being 135 kilometers.
Об авторах
И. Ю. БайронСССР
В. Г. Миллер
Россия
В. Д. Минченок
Россия
Рецензия
Для цитирования:
Байрон И.Ю., Миллер В.Г., Минченок В.Д. Развитие низовьев р. Колымы в плейстоцене. Геоморфология. 1977;(2):44-51.
For citation:
Byron I.Yu., Miller V.G., Minchenok V.D. Lower Kolyma River development during Pleistocene. Geomorfologiya. 1977;(2):44-51. (In Russ.)