... of the Upper Yenisei megaflood sediments are localized in topographic lows of the Tuva and Minusa depressions. Beyond the Altai–Sayan mountainous area, the megaflood sediments of the Upper Yenisei sequence compose high terraces of the Yenisei, Chulym, Chet’, and Kiya rivers in the southern Chulym plain...

...I.V. Korovnikov; D.A. Tokarev; N.V. Novozhilova; A.A. Terleev Abstract The lower Ust’-Kundat Formation has been studied in detail in a section along the Kiya River (Kuznetsk Alatau, Altai–Sayan folded area). The section was deposited during the Tommotian stage and is a stratotype for the Lower...

... and back-arc basin environments. These basalts were sampled on the right side of the Belyi Iyus River, south of Efremkino Village (Efremkino locality 54.45° N 89.48° E), where one of the representative sections of the formation is located. The stratigraphic position of the unit, corresponding...

... River; 7–10 — Kuznetsk Alatau: 7 — Kiya River downstream from the mouth of the Kundat Brook, 8 — Azyrtal Ridge, Kuten’-Buluk ravine, Mt. Charyshtag, 9 — Belyi Iyus River basin, Kharatas Brook, Synnig ravine, Mt. Amar, 10 — Son River basin (Podtemny ravine); 11 — Gorny Altai, Katun’ and Edigan Rivers; 12...

..., 1989 )). The Nikolaevskoe placer is localized in the southwestern Chulym–Yenisei basin, on the right bank of the Serta River—the right tributary of the Kiya River, ~30 km from the Kuznetsk Alatau ( Figs. 1 , 2 ). The placer consists of rhythmic sandy-gravel-pebble deposits ( Table 4 ) confined...

... in the northwestern East Sayans (Mana trough), Gornaya Shoria, Kuznetsk Alatau (Kiya basin, Azyrtal Range, Bateny Ridge, Belyi Iyus basin), and Gorny Altai (northern Katun’ anticlinorium). The northwestern East Sayans (Mana trough) (see Fig. 1 , I, II). There, the volcanosedimentary formations of the Upper...

... (undifferentiated, NP); BT , Bateni (back arc basin, V–Є); CM , Chulyshman (accretionary prism, mainly oceanic, V–Є); CU , Chagan-Uzun (accretionary prism, mainly oceanic, V–Є); DZ , Dzhida (undifferentiated, V–Є); KI , Kiya (island arc, V–Є); KK , Kizir–Kazir (undifferentiated, V–Є); KM , Khamsara (island...

... arkheacyatovykh gorizontov Sibiri. Doklady Akademii nauk SSSR] . Zhuravleva I.T. ( 1959 ). – Archaeocyaths of Bazaikha horizon of the Kiya River . – Reports Academy of Sciences USSR , 124 , 2 , 424 – 427 [Arkheocyaty bazaikhskogo gorizonta reki Kiya] . Zybin V.A. ( 2006...

..., Sukharikha River; 9–12 – Northern Siberia; 13 – northeastern Siberia, Chekurovka village; 14 – eastern Siberia, Selinde River; 15 – Kuznetsky Alatau, Kiya River; 16 – Transbaikal, Georgievka village; 17 – western Mongolia, Zavkhan Basin; 18 – southern China, Meishucun village; 19 – South Australia, Flinders...

... in the eastern part of the territory, extending from north to south between the rivers Kiya, Yaya, Kitat, Tom’, Chulym, and others, occupying the whole territory of Stepnoi Altai and the western part of the Novosibirsk Region (area of Lake Chany and rivers Bagan and Karasuk). The most widely spread substrate...

... of the Osinovo Massif in the near-mouth part of the Nogata River and a series of veined bodies of potassic granites in the basins of the Uvolga, Nogata, and Indola Rivers. The skarns in the contact aureole of biotite-tourmaline leucogranites of the Osinovo Massif contain bodies of magnetite ores, rare-earth...

... of Siberian Platform and to the east of Yenisei Range; however, whether they also occur in the Fore-Yenisei Basin remains unclear. Seismic data indicate that the Vendian strata extend 200–300 km to the west of the Yenisei River and the Yenisei Range ( Kontorovich et al., 2006 ) and that the boreholes...

... and alkaline rocks in the Kuznetsk Alatau and Minusa basin. 1 , gabbro, theralite, mafic foidolites, and nepheline syenite of the Upper Petropavlovka pluton; 2 , urtites of the Kiya-Shaltyr’ pluton ( Gertner et al., 2002 ); 3 , Devonian subalkalic mafic rocks of the Minusa basin ( Vorontsov et al., 2011...

... the Upper Jurassic and lower beds of the Lower Cretaceous deposits J 3 -K 1 bg). The producing horizon is overlapped by the 50–110 m thick red-colored clays of the Ilek Formation. The above-lying deposits of the Kiya and Simonovsky Formations, 20–100 m thick, are represented by rocks of alluvial...

... (Berikul’ Formation in the middle reaches of the Kiya River upstream from Makaraksky Village ( Fig. 4 ) to strike-slip-collision stage in the Early Ordovician (Smirnov Formation on the right bank of the Kiya River opposite Chumai Village (see Fig. 3 ). Average coordinates of the region under study...

.... , 1956 . The age and form of granitoid intrusions of the middle reach of the Agul River basin (East Sayan) , in: Materials on Regional Geology [in Russian] . Gosgeolizdat , Moscow , Vol. 2 , pp. 96 – 97 . Zonenshain , L.P. , Kuz’min , M.I...

.... They found archaeocyathids in the basin of the Bolshaya Oldynda River and the northern part of the Eravninsky district. Rocks containing this fauna were recognized as the Oldynda Formation of the Lower Cambrian. In the late 1950s I. T. Zhuravleva established there analogs of the Bazaikha and Sanashtykgol...