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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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.

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V. Zykin

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

编辑信件的主要联系方式.
Email: zykin@igm.nsc.ru
俄罗斯联邦, 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
俄罗斯联邦, 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
俄罗斯联邦, 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
俄罗斯联邦, pr. Akad. Koptyuga 3, Novosibirsk, 630090

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