...N.I. Akulov; I.M. Mashchuk Abstract Devonian and Lower Carboniferous continental deposits in the south of the Siberian Platform formed in eight sedimentary basins localized within stable ancient land Angarida (Angaraland). Interbasin correlation of the stratigraphic units of these deposits...

...A.G. Klets Data on stratigraphy of Carboniferous and Permian deposits formed in marginal seas of Angarida, which is the ancient Siberian continent covering the territory of Siberia and Far East, have been generalized. The biostratigraphic base of interregional correlation consists of: zonal faunal...

... the submeridional occurrence of the paleolandscapes, dwindled in the Famennian and was only a subordinate provenance for the marine water areas. The Angarida continent, as in the Frasnian, was outside the eastern part of the West Siberian sea. Its western boundary passed along the right bank of the Yenisei River...

...). Another Devonian-Carboniferous peninsular land source from the side of the Siberian craton was reconstructed ( Matukhin, 1991 ) at the northeastern end of Angarida, a Late Paleozoic continent ( Klets, 2005 ). The clastic transport of that provenance was presumably ( Matukhin, 1991 ) into the Northern...

.... During the Carboniferous, the Kuznetsk Basin was part of the Angarida megaplate, situated in high latitudes and associated with low temperatures [ Kalvoda, 2002 ]. The late middle Tournaisian was characterized by a sea-level drop associated to a global cooling. It was followed during the beginning...

... . Stratigraphy and Formation Conditions of the Kol’chugino Group in the Kuzbass, in: The Kuzbass as a Key Region for Stratigraphy of the Late Paleozoic of Angarida [in Russian]. SNIIGGiMS , Novosibirsk , Vol. 1 , pp. 104 – 115 . Boulter , C.A...

... seas around the Angarida paleocontinent ( Klets, 2005 ) traceable in different areas of Siberia. The Verkhoyansk clastic deposition was induced by a late Visean collision of the Kara terrane with the northern margin of the Siberian paleocontinent ( Vernikovsky, 1996 ; Metelkin et al., 2005 , 2012...

... island-arc system (Baikal-Vitim median massif) beneath the Riphean Baikalides surrounding the Siberian Platform in the south and west. This caused a general uplifting of the adjacent part of the Siberian Platform (sea regression) and the emergence of a land, Angarida, at its surface. This was accompanied...

... tectonic regime, which in places led to enrichment of the deposits with volcanogenic material [ 6 ]. Closer to the Siberian continent, between Angarida and Kazakhstania, a narrow, elongate in meridional direction, trough with carbonate-carbonaceous-clayey sediments has been revealed...

... of Angarida : Bulletin of Geosciences , v. 89 , p. 645 – 678 . Bardashev , I.A. , and Ziegler , W. , 1992 , Conodont biostratigraphy of Lower Devonian deposits of the Shishkat section (southern Tien-Shan, Middle Asia) : Courier Forschungsinstitut Senckenberg , v. 154 , p. 1 – 29...

... this megazone was remote both from the East European continent and from Kazakhstan and Angarida ( Fig. 2 ) and limestone strata formed on an isolated carbonate platform (according to the classification by Read (1985) . This platform formed on the margin of the Ural Ocean in the Middle Devonian ( Mizens et al...

... basins and subsequent formation of an extensive land area (the Angarida paleocontinent) overgrown with subtropical vegetation ( Malich, 1975 ). The characterization of the Chukotka terrane was largely complemented by B. Natal’in et al. ( 1999 ). They divided it into two tectonic zones (Chegetun...