2021
DOI: 10.5800/gt-2021-12-1-0517 View full text |Buy / Rent full text
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Ф. И. Жимулев,
Е. В. Поспеева,
И. С. Новиков
et al.

Abstract: The Salair fold-nappe terrane (a.k.a. Salair orogen, Salair) is the northwestern part of the Altai-Sayan folded area of the Central Asian Orogenic Belt. It is composed of Cambrian – Early Ordovician volcanic rocks and island-arc sedimentary deposits. In plan, Salair is a horseshoe-shaped structure with the northeast-facing convex side, which is formed by the outcrops of the Early Paleozoic folded basement. Its inner part is the Khmelev basin composed of Upper Devonian – Lower Carboniferous sandstones and silts… Show more

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