The first finds of skeletal fossils in the Kuk-Karauk formation of the Asha Group (Southern Urals) and their significance for determining the beginning of the Pre-Uralian-Timanian orogeny

The Bashkirian Uplift (BU) is the largest element of the southern part of the zone of the Central Ural uplift, composed predominantly of Precambrian com plexes. The Bashkirian Uplift extends for about 330 km at a width of up to 100 km (Fig. 1). In the north, west, and south, the Bashkirian Uplift is...

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Bibliographic Details
Published in:Doklady earth sciences 2011-09, Vol.440 (1), p.1239-1244
Main Authors: Kuznetsov, N. B., Shazillo, A. V.
Format: Article
Language:English
Subjects:
Earth and Environmental Science
Earth Sciences
Fossils
Geology
Orogeny
Paleozoic
Precambrian
Skeletal system
Speech therapists
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Summary:The Bashkirian Uplift (BU) is the largest element of the southern part of the zone of the Central Ural uplift, composed predominantly of Precambrian com plexes. The Bashkirian Uplift extends for about 330 km at a width of up to 100 km (Fig. 1). In the north, west, and south, the Bashkirian Uplift is bor dered by Paleozoic strata of the Western Uralian Megazone.
ISSN:1028-334X
1531-8354
DOI:10.1134/S1028334X11090261