Accumulations of block material in the Chuya And Katun river valleys and distribution of late pleistocene glaciation in the Altai Mountains


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Аннотация

The data presented introduce substantial changes into Quaternary stratigraphy, paleogeography, and the geological history of the Altai Mountains. The purpose of this investigation was thorough study of block accumulations in the Chuya and Katun river valleys. The new data shed light on the structure of these deposits, their composition, the geomorphological and stratigraphic position, and the morphology of blocks. The revealed morphological features of individual blocks imply their glacial origin.

Авторлар туралы

V. Zykin

Sobolev Institute of Geology and Mineralogy, Siberian Branch; Novosibirsk State University

Хат алмасуға жауапты Автор.
Email: zykin@igm.nsc.ru
Ресей, pr. Akad. Koptyuga 3, Novosibirsk, 630090; ul. Pirogova 2, Novosibirsk, 630090

V. Zykina

Sobolev Institute of Geology and Mineralogy, Siberian Branch

Email: zykin@igm.nsc.ru
Ресей, pr. Akad. Koptyuga 3, Novosibirsk, 630090

N. Sennikov

Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch; Novosibirsk State University

Email: zykin@igm.nsc.ru
Ресей, pr. Akad. Koptyuga 3, Novosibirsk, 630090; ul. Pirogova 2, Novosibirsk, 630090

A. Mistryukov

Sobolev Institute of Geology and Mineralogy, Siberian Branch

Email: zykin@igm.nsc.ru
Ресей, pr. Akad. Koptyuga 3, Novosibirsk, 630090

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© Pleiades Publishing, Ltd., 2016