Skip Nav Destination
Close Modal
![Discriminant diagrams for basaltoids from the Bugotak Formation, obtained by: a – Mironov [12], b – (P2O5–TiO2), c – Miyashita [13], d – Kungurtsev [14], e – Piskunov [15],f – Beccaluva [16]. For diagram a. I–VI – fields of basalts: I – mid-oceanic ridges, II – transform faults, III – back-arc spreading zones, IV – intra-oceanic islands, V – intracontinental plateaus, VI – island arcs. Contoured basaltoids of: 1–2 – basins (1) and uplifts (2) of the Sea of Japan, 3 – Mariana Trench, 4 – Lau basin and Ogasovara trough (from [11] with our supplements). For diagrams b–f. I–IV – fields of basaltoids: I – mid-oceanic ridges, II – intraplate oceanic islands (IIa – tholeiites, IIb – alkali basalts), III – island arcs, IV – back-arc spreading zones.]()
![TAS classification diagrams (a) (Na2O+K2O)–SiO2 and (b) SiO2–Nb/Y, after Winchester and Floyd (1976) for the Middle Devonian tephroid sandstones from Salair and the Kuznetsk trough. Sandstones from: 1 – the Malaya Salairka Beds; 2 – the Akarachkino Beds; 3 – the Safonovo Beds; 4 – the Bugotak Formation; 5 – dolerite-basalts from the Bugotak Formation.]()
![Distribution of Na2O, K2O, and MgO in the basaltoids of the Bugotak Formation across the strike of the Bugotak and Toguchin uplifts. 1–4 – sampling localities (see Fig. 2 and Table 1).]()
![Geological map of the Ordynskoe placer, after (Rikhvanov et al., 2001). 1, Upper Oligocene Zhuravka Formation: silts and sands (Neogene and Quaternary sediments are removed from the map); 2, Lower Oligocene Novomikhailovka Formation: clays; 3, undivided Tournaisian and Visean (Lower Carboniferous) sediments: limestones and shales; 4, undivided Upper Devonian Yurga and Pacha Formations: sandstones, shales, limestones, and siltstones; 5, Middle Devonian Bugotak Formation: tuff conglomerates, porphyrites, chlorite-albite-sericite schists, tuffaceous sandstones, and limestones; 6, geologic boundaries: actual (a) and unconformable (b); 7, faults: actual (a) and predicted (b); 8, boreholes; 9, outline of the zircon–ilmenite placer.]()
![Geological map of the region of the Filippovka buried depression without a cover of loose Cenozoic and Lower Cretaceous continental deposits. 1 — Jurassic continental deposits of the Tyumen’ Formation (Lower, Middle, and Upper series of the Jurassic in the northern part of the map; Middle Jurassic deposits within the Filippovka depression); 2–4 — Lower Carboniferous deposits: 2 — sands and clays of the Basandai Formation, 3 — carbonate-sand-clay deposits of the Visean Stage, 4 — sand-clay-carbonate deposits of the Tournaisian Stage; 5, 6 — Upper Devonian deposits: 5 — carbonate-sand-clay deposits of the Yurga Formation, 6 — clay-carbonate deposits of the Pacha Formation; 7 — Middle Devonian volcanosedimentary deposits of the Bugotak Formation; 8 — gabbroid intrusions of Upper Devonian age; 9 — faults; 10 — boreholes of the Kirza-Kargat profile and their numbers.]()
![First thumbnail for: Lithology, Geochemistry of the Middle Devonian Sed...]()
![Second thumbnail for: Lithology, Geochemistry of the Middle Devonian Sed...]()
![Third thumbnail for: Lithology, Geochemistry of the Middle Devonian Sed...]()
![First thumbnail for: GEODYNAMIC COMPLEXES AND STAGES OF DEVELOPMENT OF ...]()
![Second thumbnail for: GEODYNAMIC COMPLEXES AND STAGES OF DEVELOPMENT OF ...]()
![Third thumbnail for: GEODYNAMIC COMPLEXES AND STAGES OF DEVELOPMENT OF ...]()
![Geochemical diagrams for the Middle Devonian rocks of Salair and the Kuznetsk trough. a – the classification module FM–NAM diagram for mudstones, after Yudovich and Ketris (2000); b – the diagram A(Al2O3)–CN(CaO+Na2O)–K(K2O) (in moles), after Nesbitt and Young (1982); c, d – discrimination diagrams, after Roser and Korsch (1988) and after Wronkiewicz and Condie (1987), characterizing rock compositions of the source area and admixture pyroclastics for the Middle Devonian rocks of Salair and the Kuznetsk trough. 1 – marls from the Safonovo Beds; 2 – dolerite-basalts from the Bugotak Formation; 3 – intermediate composition of the upper continental crust (Taylor and McLennan, 1985); 4 – intermediate basalt (Le Maitre, 1976); 5 – intermediate granite (Le Maitre, 1976); 6 – intermediate andesite. Other designations see in Figs. 4 and 6. I–VI – fields of clay rocks in the diagram a: I – kaolinite composition, II – with predominance of montmorillonite with admixture of kaolinite and hydromica (in the subordinate quantity); III – with predominance of chlorite and admixture of ferruginous hydromicas; IV – chlorite-hydromica composition; V – chlorite-montmorillonite-hydromica composition (mixed-layered minerals are widely developed); VI – mainly of hydromica composition with admixture of dispersed particles of feldspars; The P1, P2 and P3 fields in the diagram c correspond to clastic material; its composition approaches the original rocks of the basic, intermediate and felsic compositions, respectively. The P4 field corresponds to the mature recycled sediment. Asterisks denote intermediate compositions of igneous rocks: B – basalt, A – andesite, D – dacite, Rd – riodacite, G, Rhl – granite, rhyolite, GR – granite, TON – tonalite, TN – tholeiite, KOM – komatiite.]()
![Location of the studied objects (1–16) within the bounds of the Novosibirsk urban agglomeration (the underlying geological data after (Babin et al., 2015)). Stratigraphic subdivision: 1, Evsino Formation (N1ev); 2, Beshcheul Formation (N1bš); 3, Zhuravka Formation (₽3zr); 4, Novomikhailovka Formation (₽3nm); 5, Elbashi Formation and Lower Balakhonka Subgroup, integrated (C1–3el–bl1); 6, Evseevskii Horizon (C1–2ec); 7, Lagernyi Sad (Mil’tyush) Formation (C1ls); 8, Salamatovo and Yar formations, undifferentiated (D3–C1sm–jar); 9, Yurga Formation (D3jur); 10, Podonino Formation (D3pd); 11, Pachinskoe Formation (D3pč); 12, Ukrop Formation (D3uk); 13, Toguchin Formation (D2tg); 14, Bugotak Formation (D2bg); Barlak mesoabyssal granite–leucogranites: 15, phase II, monzoleucogranites and biotite leucogranites, medium-grained, less frequently biotite and amphibole–biotite monzogranites (ɛɤT1–2b2); 16, phase I, monzoleucogranites and biotite leucogranites, medium-grained, less frequently biotite and amphibole–biotite monzogranites (ɛɤT1–2b1); Priob’e mesoabyssal monzodiorite–granosyenite–granites: 17, phase II, monzogranites, granosyenites, granites, and amphibole granodiorites, medium-grained, porphyritic with directive textures (ɛɤР3–Т1р2); 18, phase III, biotite monzogranites, fine-grained (ɛɤР3–Т1р3); Bugotak–Toguchin rhyodacite–basalts: 19, sills and stocks of dolerites and gabbrodolerites (mvD2bt); 20, sills and stocks of quartzy diorite–porphyrites (qδπD2bt); 21, sills and stocks of quartzy diorite–porphyrites, rhyodacites, and rhyolites (λξD2bt); 22, dikes; 23, hornfels and hornblende-dominated rocks; 24, Late Cretaceous–Eocene weathering crust; 25, faults; borders of 26, Novosibirsk Region; 27, Skala Village, Kolyvan’ township, and Novosibirsk; 28, Prigorodnoe uranium deposit; lithogeochemical aureoles of distributions: 29, in loose sediments; 30, in bedrock; 31, hydrochemical aureoles. Geochemical groups of waters: 32, formation waters occupying pore spaces of a carbonate-dominated sediment cover (group I): 1, well; 33, waters of the regional fracture zone of carbonate–terrigenous host aquifer rocks (group II): Inskie springs: 2, Spring 1; 3, Spring 2; 4, Spring 3; 5, Spring 4; 6, water hole located at HC Lesnaya Strelka-1; 7, water hole located at the STU test ground; 8, water hole located at HC Lesnaya Strelka-2; 34, waters of the regional fracture zone of carbonate–terrigenous host aquifer rocks (group III): 9, Svyatoi spring, Verkh-Tula Village; 35, fissure–vein waters in granitoids (group IV): 10, water hole of the Tulinskoe deposit; 36, surface waters (group V): 11, Shebanikha River; 12, Krutikha River; 37, surface waters exposed to anthropogenic impact (group VI): 13, Inya River reach opposite Spring 4; 14, Inya River, left bank, 200 m upstream of the Krutikha River mouth; 15, Inya River, left bank, 700 m downstream of the Shebanikha River mouth; 16, Inya River, left bank, 100 m downstream of the Krutikha River mouth.]()
![First thumbnail for: Mesozoic and Cenozoic Geologic History and Surface...]()
![Second thumbnail for: Mesozoic and Cenozoic Geologic History and Surface...]()
![Third thumbnail for: Mesozoic and Cenozoic Geologic History and Surface...]()
![First thumbnail for: THE FILIPPOVKA BURIED DEPRESSION NEAR NOVOSIBIRSK:...]()
![Second thumbnail for: THE FILIPPOVKA BURIED DEPRESSION NEAR NOVOSIBIRSK:...]()
![Third thumbnail for: THE FILIPPOVKA BURIED DEPRESSION NEAR NOVOSIBIRSK:...]()
![First thumbnail for: Neotectonic Fault Pattern of the Salair Area (Sout...]()
![Second thumbnail for: Neotectonic Fault Pattern of the Salair Area (Sout...]()
![Third thumbnail for: Neotectonic Fault Pattern of the Salair Area (Sout...]()
![Local geology of the Kolyvan’–Tomsk Folded Zone and Jurassic sedimentary basins (Akhmadshchin et al., 2008; Li et al., 2008; Babin et al., 2014). 1, early–middle Paleozoic orogenic complexes of Salair and Kuznetsk Alatau, undifferentiated; 2, deformed Middle Devonian–early Carboniferous sediments in middle Paleozoic basins; 3, Middle Devonian volcanic and volcaniclastic rocks in the Kolyvan’–Tomsk Folded Zone (KTFZ), Bugotak, Toguchin, and Mitrofanovo formations; 4, Late Devonian clastic deposits of the KTFZ, Pachino and Yurga formations; 5, early Carboniferous deposits of the KTFZ, Inskaya Group; 6, Carboniferous–early Permian sediments of the Gorlovo, Zarubino, and Kuznetsk basins; 7, middle–late Permian sediments of the Gorlovo, Zarubino, and Kuznetsk basins; 8, Early–Middle Jurassic sediments of superposed basins; 9, Jurassic sediments overthrust by Paleozoic rocks of the KTFZ; 10, Cretaceous sediments; 11, Early–Middle Triassic Barlak complex; 12, late Permian Ob’ granitic complex of the KTFZ and Paleozoic granitoids of Salair, undifferentiated; 13, Cenozoic sedimentary cover of the West Siberian Basin; 14, main faults and thrusts (a) and Tomsk thrust, a frontal structure of the KTFZ (b); 15, locations of photographs in Figs. 4a,b; 16, Jurassic basins: Ulanovka (1), Doronino (2), Karaguzh (3), Bobrovka (4). Asterisks mark granitic samples for AFT dating. Inset shows location of Fig. 1 in the Central Asian Orogenic Belt.]()
![First thumbnail for: PRINCIPAL CHARACTERISTICS OF THE GEOLOGIC-GEOMORPH...]()
![Upper Precambrian and Paleozoic lithology and stratigraphy of Stepnoi Altai and its surroundings. Lithology. 1 — sandstone, 2 — siltstone, 3 — mudstone, 4 — limestone, 5 — massive limestone, 6 — clayey limestone, 7 — dolomite, 8 — dacite, 9 — liparite, 10 — andesite, 11 — basalt, 12 — tuff, 13 — conglomerate, 14 — tuffaceous conglomerate, 15 — tuffaceous sandstone, 16 — lenses, 17 — tectonic contact, 18 — unconformal bedding, 19 — conformal bedding, 20 — stratigraphic gap, 21 — facies change, 22 — stratigraphic levels of sampling. Abbreviations stand for formation names: ab — Abyshevo, al — Alambai, an — Ancheshevka (= Suenga), ar — Arinchevo, bch — Bachat (= Safatovo), bg — Bugotak, bgr — Bugryshikha, bkh — Bukhtarma, bl — Bel’gebash, br — Baragash, brt — Baratal, bs — Baskuskan, chg — Chagyrka, chm — Cheremshanka (= Pravoloktevo), chp — Cheposh, chr — Cherny Anui, chs — Chesnokovka, dv — Davydovka, el — Elanda, es — Eskonga, fm — Fominsk, grs — Gorskino, gr — Goryaevka, gv — Gavrilovka, hv — Khvoshchevka, il — Ilovaty (= Izyrak), kb — Korbalikha, kg — Kuyagan (= Kurata), kh — Khankhara, kl — Kulbich, km — Kamyshenka, kml — Kamlak, kmn — Kamenskaya, kr — Krasnoye (= El’tsovka, Chupino), krs — Karastun (= Zaichikha), ku — Kuimov, mch — Mochega, ml — Malofeevka, mln — Mel’nichnaya (= Berezovka, + Talovaya, + Shipunovo), mn — Manzherok, ob — Obukhovka, ok — Oktyabr’sky, or — Orlinaya Gora, os — Oselki (= Chumysh), pch — Pachino (= Ukrop, = Petropavlovskoye, + Sergeevka), pkh — Pikhtovka, pl — Polati, pt — Potapovo, pv — Pavlovo, sb — Sobolinoye (= Khmelevka), sh — Shashkunar, shv — Shiverta, skh — Sukhaya, sn — Snegiri, sr — Syrovaty, ss — Sosnovka, st — Suetka, tb — Tel’bess Group, td — Taidon, th — Tekhten’ (= Bulukhta, = Orlov), tl — Tolsochikha, tr — Tarkhan, ul — Ul’ba, us — Ust’-Sema, vb — Veber, (= Bobrovka, = Zyryanka), vd — Vydrikha (= Verkhtomskoye), vs — Voskresenka, vtu — Vtorye Utesy, zv — Zavodskiye (= Loktevka), yur — Yurga.]()
![First thumbnail for: The Inskie Springs: New Insights into Low-Radon Wa...]()
![Second thumbnail for: The Inskie Springs: New Insights into Low-Radon Wa...]()
![Third thumbnail for: The Inskie Springs: New Insights into Low-Radon Wa...]()
![First thumbnail for: GEODYNAMIC POSITION OF MIDDLE PALEOZOIC BASITE SER...]()
![Second thumbnail for: GEODYNAMIC POSITION OF MIDDLE PALEOZOIC BASITE SER...]()
![Third thumbnail for: GEODYNAMIC POSITION OF MIDDLE PALEOZOIC BASITE SER...]()
![First thumbnail for: PETROLEUM POTENTIAL OF MESOZOIC, PALEOZOIC AND VEN...]()
![Second thumbnail for: PETROLEUM POTENTIAL OF MESOZOIC, PALEOZOIC AND VEN...]()
![Third thumbnail for: PETROLEUM POTENTIAL OF MESOZOIC, PALEOZOIC AND VEN...]()
![First thumbnail for: Native gold in complex Ti–Zr placers of the southe...]()
![Second thumbnail for: Native gold in complex Ti–Zr placers of the southe...]()
![Third thumbnail for: Native gold in complex Ti–Zr placers of the southe...]()
![First thumbnail for: GEODYNAMIC INTERPRETATION OF ALTAI-SAYAN GEOLOGICA...]()
![Second thumbnail for: GEODYNAMIC INTERPRETATION OF ALTAI-SAYAN GEOLOGICA...]()
![Third thumbnail for: GEODYNAMIC INTERPRETATION OF ALTAI-SAYAN GEOLOGICA...]()
1-20 OF 21 RESULTS FOR
Bugotak Formation
Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account
Would you like to receive an alert when new items match your search?
1
Image
![Discriminant diagrams for basaltoids from the Bugotak Formation, obtained by: a – Mironov [12], b – (P2O5–TiO2), c – Miyashita [13], d – Kungurtsev [14], e – Piskunov [15],f – Beccaluva [16]. For diagram a. I–VI – fields of basalts: I – mid-oceanic ridges, II – transform faults, III – back-arc spreading zones, IV – intra-oceanic islands, V – intracontinental plateaus, VI – island arcs. Contoured basaltoids of: 1–2 – basins (1) and uplifts (2) of the Sea of Japan, 3 – Mariana Trench, 4 – Lau basin and Ogasovara trough (from [11] with our supplements). For diagrams b–f. I–IV – fields of basaltoids: I – mid-oceanic ridges, II – intraplate oceanic islands (IIa – tholeiites, IIb – alkali basalts), III – island arcs, IV – back-arc spreading zones.](https://gsw.silverchair-cdn.com/gsw/Content_public/Journal/rgg/39/1/rgg-03900022/1/s_rgg-1998-01_022_page_6_1.jpeg?Expires=2147483647&Signature=LQNrBpbgTNsgRVXfbLAR8dIPrbQMA6PO1BSDgBfy9o4lcj~R2F7KD9eSJuujmOPNn0-TNqq2B485n7MVXC5hECYtSaZh4dVJmXUHtVRXizf2IaeOvx-ieFbmuXn63fyA319nOOrzYQZidSSwPzkaHiLngHQ9zB7UbuSUv8NbuMfVWJN1yTnrkD-139lVEjbwebeLxqsbij~rtJgOnvDkHVcx-Z1bzYuTvYa-UYDbTEQsR6HWJkvRC8Lhno3HafwzEDcx01OURZk9V8ZaqQwrb64EXd7A5p2n10ThXeQcP1g9uYNGX51TOTjYL6vUouae2o6ICprn1Sfh5ljjm8lRuw__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA)
Discriminant diagrams for basaltoids from the Bugotak Formation, obtained b... Available to Purchase
in GEODYNAMIC COMPLEXES AND STAGES OF DEVELOPMENT OF THE KOLYVAN’-TOMSK FOLDED ZONE ( West Siberia )
> Russian Geology and Geophysics
Published: 01 January 1998
Fig. 3. Discriminant diagrams for basaltoids from the Bugotak Formation, obtained by: a – Mironov [ 12 ], b – (P 2 O 5 –TiO 2 ), c – Miyashita [ 13 ], d – Kungurtsev [ 14 ], e – Piskunov [ 15 ], f – Beccaluva [ 16 ]. For diagram a . I–VI – fields of basalts : I – mid-oceanic ridges
Image
TAS classification diagrams ( a ) (Na 2 O+K 2 O)–SiO 2 and ( b ) SiO 2 –Nb... Available to Purchase
in Lithology, Geochemistry of the Middle Devonian Sediments and the Influence of Volcanism on Sedimentation in the Southeast of West Siberia
> Russian Geology and Geophysics
Published: 01 October 2023
– the Safonovo Beds; 4 – the Bugotak Formation; 5 – dolerite-basalts from the Bugotak Formation.
Image
Distribution of Na 2 O, K 2 O, and MgO in the basaltoids of the Bugotak For... Available to Purchase
in GEODYNAMIC COMPLEXES AND STAGES OF DEVELOPMENT OF THE KOLYVAN’-TOMSK FOLDED ZONE ( West Siberia )
> Russian Geology and Geophysics
Published: 01 January 1998
Fig. 4. Distribution of Na 2 O, K 2 O, and MgO in the basaltoids of the Bugotak Formation across the strike of the Bugotak and Toguchin uplifts. 1–4 – sampling localities (see Fig. 2 and Table 1 ).
Image
Geological map of the Ordynskoe placer, after ( Rikhvanov et al., 2001 ). ... Available to Purchase
in Native gold in complex Ti–Zr placers of the southern West Siberian Plain
> Russian Geology and Geophysics
Published: 01 December 2013
(Lower Carboniferous) sediments: limestones and shales; 4 , undivided Upper Devonian Yurga and Pacha Formations: sandstones, shales, limestones, and siltstones; 5 , Middle Devonian Bugotak Formation: tuff conglomerates, porphyrites, chlorite-albite-sericite schists, tuffaceous sandstones
Image
Geological map of the region of the Filippovka buried depression without a ... Available to Purchase
in THE FILIPPOVKA BURIED DEPRESSION NEAR NOVOSIBIRSK: A POSSIBLE IMPACT CRATER OF TRIASSIC-EARLY JURASSIC AGE
> Russian Geology and Geophysics
Published: 01 April 2004
— carbonate-sand-clay deposits of the Yurga Formation, 6 — clay-carbonate deposits of the Pacha Formation; 7 — Middle Devonian volcanosedimentary deposits of the Bugotak Formation; 8 — gabbroid intrusions of Upper Devonian age; 9 — faults; 10 — boreholes of the Kirza-Kargat profile and their numbers.
Journal Article
Lithology, Geochemistry of the Middle Devonian Sediments and the Influence of Volcanism on Sedimentation in the Southeast of West Siberia Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 October 2023
Russ. Geol. Geophys. (2023) 64 (10): 1196–1216.
... – the Safonovo Beds; 4 – the Bugotak Formation; 5 – dolerite-basalts from the Bugotak Formation. ...
FIGURES
Journal Article
GEODYNAMIC COMPLEXES AND STAGES OF DEVELOPMENT OF THE KOLYVAN’-TOMSK FOLDED ZONE ( West Siberia ) Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 January 1998
Russ. Geol. Geophys. (1998) 39 (1): 22–34.
...Fig. 3. Discriminant diagrams for basaltoids from the Bugotak Formation, obtained by: a – Mironov [ 12 ], b – (P 2 O 5 –TiO 2 ), c – Miyashita [ 13 ], d – Kungurtsev [ 14 ], e – Piskunov [ 15 ], f – Beccaluva [ 16 ]. For diagram a . I–VI – fields of basalts : I – mid-oceanic ridges...
FIGURES
Image
Geochemical diagrams for the Middle Devonian rocks of Salair and the Kuznet... Available to Purchase
in Lithology, Geochemistry of the Middle Devonian Sediments and the Influence of Volcanism on Sedimentation in the Southeast of West Siberia
> Russian Geology and Geophysics
Published: 01 October 2023
-basalts from the Bugotak Formation; 3 – intermediate composition of the upper continental crust ( Taylor and McLennan, 1985 ); 4 – intermediate basalt ( Le Maitre, 1976 ); 5 – intermediate granite ( Le Maitre, 1976 ); 6 – intermediate andesite. Other designations see in Figs. 4 and 6 . I–VI
Image
Location of the studied objects (1–16) within the bounds of the Novosibirsk... Available to Purchase
Published: 01 December 2022
, Podonino Formation (D 3 pd); 11 , Pachinskoe Formation (D 3 pč); 12 , Ukrop Formation (D 3 uk); 13 , Toguchin Formation (D 2 tg); 14 , Bugotak Formation (D 2 bg); Barlak mesoabyssal granite–leucogranites: 15 , phase II, monzoleucogranites and biotite leucogranites, medium-grained, less frequently
Journal Article
Mesozoic and Cenozoic Geologic History and Surface Topography of the Northwestern Altai–Sayan Area Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 July 2019
Russ. Geol. Geophys. (2019) 60 (7): 781–792.
... watershed areas. Peneplain in the part of the Bugotak–Sokur upland we studied makes the base of broad (up to 10–15 km) watersheds under 50 m thick loess of the Pleistocene Bachat and Elovka Formations. ( Belyaev and Nechaev, 1999 ). There are buried planation surfaces at 220–230 and 260–290 m asl separated...
FIGURES
Journal Article
THE FILIPPOVKA BURIED DEPRESSION NEAR NOVOSIBIRSK: A POSSIBLE IMPACT CRATER OF TRIASSIC-EARLY JURASSIC AGE Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 April 2004
Russ. Geol. Geophys. (2004) 45 (4): 525–529.
... — carbonate-sand-clay deposits of the Yurga Formation, 6 — clay-carbonate deposits of the Pacha Formation; 7 — Middle Devonian volcanosedimentary deposits of the Bugotak Formation; 8 — gabbroid intrusions of Upper Devonian age; 9 — faults; 10 — boreholes of the Kirza-Kargat profile and their numbers. ...
FIGURES
Journal Article
Neotectonic Fault Pattern of the Salair Area (Southern West Siberia): Relation with the Pre-Cenozoic Tectonic Framework Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 January 2022
Russ. Geol. Geophys. (2022) 63 (1): 1–12.
... ( Vail et al., 1977 ; Haq et al., 1987 ; Haq and Al-Qahtani, 2005 ; Miller et al., 2011 ) and by geochronological constrains on the onset of neotectonic activity in the Salair Ridge ( Novikov and Sokol, 2007 ). Correspondingly, the formation of the stepped peneplain profiles has an alternative...
FIGURES
Image
Local geology of the Kolyvan’–Tomsk Folded Zone and Jurassic sedimentary ba... Available to Purchase
in Mesozoic Intracontinental Orogeny in the Tectonic History of the Kolyvan’– Tomsk Folded Zone (Southern Siberia): a Synthesis of Geological Data and results of Apatite Fission Track Analysis
> Russian Geology and Geophysics
Published: 01 September 2021
Carboniferous sediments in middle Paleozoic basins; 3 , Middle Devonian volcanic and volcaniclastic rocks in the Kolyvan’–Tomsk Folded Zone (KTFZ), Bugotak, Toguchin, and Mitrofanovo formations; 4 , Late Devonian clastic deposits of the KTFZ, Pachino and Yurga formations; 5 , early Carboniferous deposits
Journal Article
PRINCIPAL CHARACTERISTICS OF THE GEOLOGIC-GEOMORPHOLOGICAL BASES OF THE LANDSCAPES OF THE NOVOSIBIRSK REGION Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 February 1996
Russ. Geol. Geophys. (1996) 37 (2): 68–77.
... ]. They were of importance, but no zoning of geological formations as components of natural landscapes has been carried out. This work is the first experiment of this kind. The natural conditions and landscapes of the Novosibirsk Region are quite diverse. To understand properly the reasons...
FIGURES
Image
Upper Precambrian and Paleozoic lithology and stratigraphy of Stepnoi Altai... Available to Purchase
in PETROLEUM POTENTIAL OF MESOZOIC, PALEOZOIC AND VENDIAN DEPOSITS IN STEPNOI ALTAI AND THE SURROUNDING MOUNTAINS: GEOCHEMICAL EVIDENCE
> Russian Geology and Geophysics
Published: 01 June 2005
. Abbreviations stand for formation names: ab — Abyshevo, al — Alambai, an — Ancheshevka (= Suenga), ar — Arinchevo, bch — Bachat (= Safatovo), bg — Bugotak, bgr — Bugryshikha, bkh — Bukhtarma, bl — Bel’gebash, br — Baragash, brt — Baratal, bs — Baskuskan, chg — Chagyrka, chm — Cheremshanka (= Pravoloktevo), chp
Journal Article
The Inskie Springs: New Insights into Low-Radon Waters Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 December 2022
Russ. Geol. Geophys. (2022) 63 (12): 1424–1441.
... , Podonino Formation (D 3 pd); 11 , Pachinskoe Formation (D 3 pč); 12 , Ukrop Formation (D 3 uk); 13 , Toguchin Formation (D 2 tg); 14 , Bugotak Formation (D 2 bg); Barlak mesoabyssal granite–leucogranites: 15 , phase II, monzoleucogranites and biotite leucogranites, medium-grained, less frequently...
FIGURES
Journal Article
GEODYNAMIC POSITION OF MIDDLE PALEOZOIC BASITE SERIES OF THE ALTAI, EXEMPLIFIED BY THE KARAOYUK AND TEREKTA COMPLEXES Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 February 2004
Russ. Geol. Geophys. (2004) 45 (2): 212–221.
... of the complexes. It is supposed that the dike complexes have their own intrusive “roots” exposed in the Altai geologic structures, which are erroneously considered part of other igneous complexes of the region. The formation of the explored dike complexes is related to the functioning of a mantle column...
FIGURES
Journal Article
PETROLEUM POTENTIAL OF MESOZOIC, PALEOZOIC AND VENDIAN DEPOSITS IN STEPNOI ALTAI AND THE SURROUNDING MOUNTAINS: GEOCHEMICAL EVIDENCE Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 June 2005
Russ. Geol. Geophys. (2005) 46 (6): 652–666.
.... Abbreviations stand for formation names: ab — Abyshevo, al — Alambai, an — Ancheshevka (= Suenga), ar — Arinchevo, bch — Bachat (= Safatovo), bg — Bugotak, bgr — Bugryshikha, bkh — Bukhtarma, bl — Bel’gebash, br — Baragash, brt — Baratal, bs — Baskuskan, chg — Chagyrka, chm — Cheremshanka (= Pravoloktevo), chp...
FIGURES
Journal Article
Native gold in complex Ti–Zr placers of the southern West Siberian Plain Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 December 2013
Russ. Geol. Geophys. (2013) 54 (12): 1484–1498.
... (Lower Carboniferous) sediments: limestones and shales; 4 , undivided Upper Devonian Yurga and Pacha Formations: sandstones, shales, limestones, and siltstones; 5 , Middle Devonian Bugotak Formation: tuff conglomerates, porphyrites, chlorite-albite-sericite schists, tuffaceous sandstones...
FIGURES
Journal Article
GEODYNAMIC INTERPRETATION OF ALTAI-SAYAN GEOLOGICAL COMPLEXES Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 January 1996
Russ. Geol. Geophys. (1996) 37 (1): 56–73.
... in this paper. Here we describe only the complexes related to the formation, development, and closure of the Paleoasian Ocean. The complexes recognized are rift, oceanic, passive and active continental margins, island-arc and collisional ( Figs. 1 , 2 ). 17 05 1995 © 1996 by Allerton Press, Inc...
FIGURES
1
