A Large Paleoseismodislocation in the Southeastern Part of the Cherskii Seismic Belt, Northern Priokhotye
- Авторы: Smirnov V.N.1, Kondratyev M.N.1, Kolegov P.P.1
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Учреждения:
- Northeastern Complex Research Institute, Far East Branch
- Выпуск: Том 479, № 2 (2018)
- Страницы: 425-428
- Раздел: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/192674
- DOI: https://doi.org/10.1134/S1028334X18040104
- ID: 192674
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Аннотация
The structure of a large paleoseismodislocation located on the southeastern flank of the Cherskii seismic belt, in the upper reaches of the Ola River, 125 km NNE of Magadan, is studied. Detailed morphologic, morphometric, and structural descriptions of this paleoseismodislocation are made. The main parameters of the landslide body and the dammed lake formed by it are determined. The correlating deposits formed in the dammed lake and upon the surface of rupture are studied, and their radiocarbon age is determined.
Об авторах
V. Smirnov
Northeastern Complex Research Institute, Far East Branch
Автор, ответственный за переписку.
Email: smirnov@neisri.ru
Россия, Magadan, 685000
M. Kondratyev
Northeastern Complex Research Institute, Far East Branch
Email: smirnov@neisri.ru
Россия, Magadan, 685000
P. Kolegov
Northeastern Complex Research Institute, Far East Branch
Email: smirnov@neisri.ru
Россия, Magadan, 685000
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