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Anuy River

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Geoelectric section through the <span class="search-highlight">Anuy</span> <span class="search-highlight">River</span> valley, Altai. I, channel placer...
Published: 01 January 2022
Fig. 7. Geoelectric section through the Anuy River valley, Altai. I, channel placer; II, valley placer; 1 , alluvium; 2 , clay shale; 3 , intensely weathered and fractured main bottom; 4 , base of alluvial deposits (bedrock top); 5 , boundaries of the promising placer mining site.
Image
Example organic buildups in Late Ordovician–early Silurian Altai basins. Pa...
Published: 01 March 2023
along Anui River (length about 10 km, width >1 km); Panel 12: fragment of carbonate platform near Ust’-Chagyrka and Ust’-Pustynka villages (length about 10 km, width >3 km) composed of Katian, Hirnantian, Telychian, Sheinwoodian, Lochkovian, and Pragian reef deposits. Panels 1–5, 10, 11 are based
Journal Article
Published: 01 January 2022
Russ. Geol. Geophys. (2022) 63 (1): 98–108.
...Fig. 7. Geoelectric section through the Anuy River valley, Altai. I, channel placer; II, valley placer; 1 , alluvium; 2 , clay shale; 3 , intensely weathered and fractured main bottom; 4 , base of alluvial deposits (bedrock top); 5 , boundaries of the promising placer mining site. ...
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Journal Article
Published: 01 November 2021
Russ. Geol. Geophys. (2021) 62 (11): 1269–1284.
... of the Stratigraphic Code ( 2019 ) saying that a formation can be divided into subformations in one area but can remain undifferentiated in another area. For the recent decade, we have documented in detail the Kuimov and Cherny Anui formations in a number of sections in the upper reaches of the Anui River, near...
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Journal Article
Published: 01 June 2024
Russ. Geol. Geophys. (2024) 65 (6): 737–755.
... (western, central, and southern Altai), Uimen’-Lebed’ (eastern Altai), and Teletskoe (southeastern Altai) terranes ( Buslov, 2011 ). As shown by geodynamic reconstructions ( Dobretsov, 2003 ), the western and northwestern Gorny Altai territory, including the Charysh–Inya and Anui–Chuya facies zones ( Fig...
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Typical gas chromatogram of saturated hydrocarbons (steranes,  m/z  = 217),...
Published: 01 June 2005
Fig. 5. Typical gas chromatogram of saturated hydrocarbons (steranes, m/z = 217), bitumen from Paleozoic sediments in Altai (example of bitumen from limestone sampled in Shinok River outcrop, D 1 e, Baragash Formation, Kuvash beds, Anui-Chuya zone).
Journal Article
Published: 01 March 2023
Russ. Geol. Geophys. (2023) 64 (3): 292–305.
... along Anui River (length about 10 km, width >1 km); Panel 12: fragment of carbonate platform near Ust’-Chagyrka and Ust’-Pustynka villages (length about 10 km, width >3 km) composed of Katian, Hirnantian, Telychian, Sheinwoodian, Lochkovian, and Pragian reef deposits. Panels 1–5, 10, 11 are based...
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Image
Typical gas chromatogram of saturated hydrocarbons (alkanes), bitumen from ...
Published: 01 June 2005
Fig. 4. Typical gas chromatogram of saturated hydrocarbons (alkanes), bitumen from Paleozoic sediments in Altai (example of bitumen from limestone sampled in Shinok River outcrop, D 1 e, Baragash Formation, Kuvash beds, Anui-Chuya zone). 1 — normal alkanes, 2 — isoprenoids.
Journal Article
Published: 01 April 2019
Russ. Geol. Geophys. (2019) 60 (4): 451–471.
... defined based on graptolite and conodont faunas. The stratotype section of the Kuimov Formation is at the Tigirek Village ( Fig. 1 ), near the Kuimov Creek, the right tributary of the Inya River) and in the vicinity of the former Komsomolets Settlement ( Kul’kov, 1966 , 1967 ; Yolkin et al., 1974...
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Typical gas chromatogram of saturated hydrocarbons (terpanes,  m/z  = 191),...
Published: 01 June 2005
Fig. 7. Typical gas chromatogram of saturated hydrocarbons (terpanes, m/z = 191), bitumens from Paleozoic sediments in Altai (example of bitumen from limestone sampled in Shinok River outcrop, D 1 e, Baragash Formation, Kuvash beds, Anui-Chuya zone). Hydrocarbons: T n — tricyclanes, M n
Journal Article
Published: 01 January 2003
Russ. Geol. Geophys. (2003) 44 (1-2): 156–171.
... of this group (formation) in the Charysh (Charysh-Inya) and Talitsa structural zones of Gorny Altai, a series of these sections was discovered and investigated on the Marcheta River in the Anui-Chuya (Anui) zone of Gorny Altai. Until recently, it was believed that the Zasur’ya unit was in contact only...
FIGURES
Journal Article
Published: 01 November 2017
Russ. Geol. Geophys. (2017) 58 (11): 1277–1288.
... rocks of the Anui–Chuya basin in the Gorny Altai terrane. The inferred source areas of zircon hosts are igneous rocks of the Precambrian craton basement and the Vendian–Early Ordovician Kuznetsk–Altai island arc. Early Neoproterozoic (1.00–0.75 Ma) detrital zircons are abundant in the Early Paleozoic...
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Journal Article
Published: 01 June 2005
Russ. Geol. Geophys. (2005) 46 (6): 652–666.
...Fig. 5. Typical gas chromatogram of saturated hydrocarbons (steranes, m/z = 217), bitumen from Paleozoic sediments in Altai (example of bitumen from limestone sampled in Shinok River outcrop, D 1 e, Baragash Formation, Kuvash beds, Anui-Chuya zone). ...
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Journal Article
Published: 01 August 2014
Russ. Geol. Geophys. (2014) 55 (8): 971–988.
... of the sections of the Bugryshikha and Khankhara Formations—the Ebogon section in the Anui–Chuya structure-facies zone of Gorny Altai. See legend in Fig. 3 . In the Uimen’–Lebed’ zone of Gorny Altai, the Tuloy Formation (including the stratotype of the Lebed’ Horizon near the Lebed’ River) is overlain...
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Journal Article
Published: 01 November 2003
Russ. Geol. Geophys. (2003) 44 (11): 1206–1213.
... ] and produced a rugged surface topography, most contrasting in Siberia, with deeply incised river valleys and elevated plateaus at 2000–3000 m asl. The structural pattern is dominated by strike-slip faults [ 12 ], oriented mostly in the SE direction in the western part and varying in strike from W-E to N-S...
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Journal Article
Published: 01 August 2018
Russ. Geol. Geophys. (2018) 59 (8): 1010–1021.
...@igm.nsc.ru (I.V. Gaskov) 12 4 2017 2 8 2017 © 2018, IGM, Siberian Branch of the RAS 2018 IGM, Siberian Branch of the RAS metallogeny mineral deposits mineralization magmatism Gorny Altai Rudny Altai The Anui–Chuya zone occupies a basin of the same name and extends...
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Journal Article
Published: 01 June 2002
Russ. Geol. Geophys. (2002) 43 (6): 567–578.
..., Pospelikha, Charysh, Anui rivers, etc), and the Terekta-Sumul’ta domal uplift. Most of the analyzed structures evolve upon the Rudny Altai stable block bounded by the Irtysh fault in the northwest and the Northeastern shear zone in the northeast. In the north the block joins the Barnaul block along...
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Journal Article
Published: 01 January 2003
Russ. Geol. Geophys. (2003) 44 (1-2): 49–75.
..., % K-Ar age, Ma Ar-Ar Age, Ma Kurai metamorphic complex, southeastern Gorny Altai 1 Block in mylonites of shear zone, upper Kurai River Amphibolite 92-27802 Amph, Bt, Pl, Qtz Amph 0.921 ± 0.018 394 ± 8   2 » Upper Kuyakhtanar River Crystalline schist 95-7-1 Amph, Bt, Pl, Qtz...
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Journal Article
Published: 01 May 2010
Russ. Geol. Geophys. (2010) 51 (5): 431–446.
... (Peschanka strata): 30, sandstone, 31, siltstone; 32, 33, metasedimentary rocks from the Uimon Formation; 34–44, sedimentary rocks from the Cambrian–Ordovician turbidite megabasin: 34, 35, Gorny Altai Group of the Anui–Chuya block (34, sandstone, 35, siltstone); 36, 37, Katun’ Formation of the Altai...
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Journal Article
Published: 01 August 2006
Russ. Geol. Geophys. (2006) 47 (8): 923–937.
... (TUNZ) 5200′46.51″ 8628′14.51″ 266.9 2001 12 Ust’-Ulagan (ULAG) 5030'01.01″ 8739′13.58″ 2039.3 2000 13 Ust’-Kan (USTK) 5056′22.20″ 8446′08.00″ 999.4 2000 14 Ukok (UKOK) 4933′43.37″ 8813′54.92″ 2323.9 2001 15 Anui (ANUI) 5221′24.42″ 8446′06.52″ 183.0 2001 16...
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