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UDC 551.79:(56+55)(571.1)
FORMATION PECULIARITIES OF THE LATE PLEISTOCENE DEPOSITS WITHIN THE ELOVKA SITE (SALAIR RANGE)
N. A. Baksheev, I. V. Budnikov, M. V. Mikharevich, E. I. Fradkin, A. I. Chernykh
The article covers the formation problem of the Salair loose deposits, attributed to subaerial loess-like limons of the Elovka Formation. New data on these deposits allow their distinguishing into two members: the lower one is rudaceous, diluvial-proluvial and the upper one is silty-clay, lacustrine-swampy. According to the data studied on fossil fauna, flora and literature sources these deposits were formed in the Late Neopleistocene.
Key words: lacustrine-alluvial deposits, Late Neopleistocene, horizon, gold, tubules, vegetation, bryozoans.
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