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![Scheme of the geologic structure of the northern Kundusuyul pluton, modified and supplemented from Rudnev et al. (2006). 1 – carbonateterrigenous-volcanic deposits, V–Є1; 2 – dolomites, limestones, shales, and metavolcanic rocks, R2–3; 3 – granosyenites of the Chebula alkali granite–granite complex, D1–2; 4 – tonalites and plagiogranites, R3; 5, 6 – Kundusuyul gabbro–diabase complex, R3? (5 – diabase dikes, 6 – gabbro and diorites, undivided); 7, 8 – Moskovka peridotite–pyroxenite–gabbro complex, R3? (7 – gabbroids, 8 – peridotites and pyroxenites, undivided); 9 – faults; 10 – dips and strikes (deg); 11 – localities of sampling for U–Pb isotope zircon dating. Massifs: G – Gremyachikha, Gl – Glukhovka, M – Moskovka, NG – North Gremyachikha, K – Kundusuyul.]()
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![Scheme of the geologic structure of northern Kuznetsk Alatau, modified and supplemented from Rudnev et al. (2008). Stratified deposits: 1 – Meso–Cenozoic deposits of the Chulym–Yenisei basin; 2 – volcanic deposits of the Uchulen–Kazankol and Palatninsk–Belaya Osipovka complexes, undivided, D1; 3 – volcanic deposits of the Bazyr–Apshan complex of the Nazarovka basin, undivided, D1; 4 – terrigenous-carbonate deposits of the Taimen Formation, O1; 5 – Berikul’ rhyodacite–basalt–trachybasalt complex, Є2; 6 – terrigenous-carbonate deposits of the Usa Formation, Є1; 7 – volcanic deposits of the Ust’-Anzas trachyte–trachybasalt–basalt complex, Є1; 8 – volcanic deposits of the Chumai plagiorhyolite–basalt complex, V– Є1; 9 – calcareous and carbonate–clayey deposits of the Malyi Rastai Formation and clay–silica–calcareous deposits of the Prokop’evo Formation, R3?–V. Intrusive deposits, undivided: 10 – Tel’bes monzodiorite–granodiorite–melanogranite complex, D1; 11 – Goryachegorsk alkali gabbroid complex, D1; 12 – Chebula alkali granite–granite complex, D1; 13 – Karadat alkali syenite complex, D1; 14 – Martaiga(?) quartz diorite–granodiorite (tonalite)–granite complex, О1; 15 – Karnayul’ granosyenite–melanogranite complex, О1; 16–18 – Malyi Dudet monzogabbro–monzodiorite complex, Є3–O1 (16 – syenites and quartz syenites, 17 – monzodiorites, 18 – monzogabbro); 19 – Upper Petropavlovka alkali gabbroid complex, Є3–O1; 20 – Krasnyi Kamen’ leucomonzodiorite–leucomonzonite–granosyenite complex, Є3–O1; 21 – Martaiga quartz diorite–granodiorite (tonalite)–granite complex, Є3–O1; 22 – Taskyl pyroxenite–gabbro complex, Є2; 23 – early Cambrian plagiogranite complex, Є1; 24 – Tylin (Lavrenovo) diorite–tonalite–plagiogranite complex, Є1; 25 – early Cambrian pyroxenites and gabbro, Є1; 26 – Barkhat dunite–harzburgite complex, R3–Є1; 27 – tonalite–plagiogranite association, R3; 28 – Kundusuyul gabbro–diorite–dolerite complex, R3?; 29 – Moskovka peridotite–pyroxenite–gabbro complex, R3?; 30 – faults; 31 – results of U–Pb isotope dating, age, Ma (Vrublevskii et al., 2003; Rudnev et al., 2006, 2008), parenthesized is the number of the massif (1 – Tylin, 2 – Kozhukh, 3 – Krasnyi Kamen’, 4 – Malyi Dudet, 5 – Kaidalovo, 6 – Udarnaya, 7 – Karnayul, 8 – Tsentral’nyi, 9 – Upper Petropavlovka, 10 – Karadat, 11 – Gremyachikha, 12 – North Gremyachikha, in the Kundusuyul pluton). Roman numerals in squares denote batholiths (I – Kozhukh, II – Dudet, and III – Tsentral’nyi). Inset shows a scheme of geological and structural regionalization of northern Kuznetsk Alatau, after Shokal’skii et al. (2000): PZU – Pezas–Zolotoi Kitat uplift, IU – Iyus uplift, AU – Azyrtal uplift, ChB – Chumai block, KB – Kanym block, TBB – Talanovka–Bogorodkaii block, TB – Tom’ block, TG – Taidon graben, RG – Rastai graben, SG – Sargaya graben, PVB – Palatnaya volcanic basin, NB – Nazarovka basin, NMB – North Minusa basin. Rectangle outlines the study area.]()
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Scheme of the geologic structure of the northern Kundusuyul pluton, modifie...
in Conditions of Formation and Sources of Melts of Early Neoproterozoic Granites in Northern Kuznetsk Alatau
> Russian Geology and Geophysics
Published: 01 February 2023
Fig. 2. Scheme of the geologic structure of the northern Kundusuyul pluton, modified and supplemented from Rudnev et al. ( 2006 ). 1 – carbonateterrigenous-volcanic deposits, V–Є 1 ; 2 – dolomites, limestones, shales, and metavolcanic rocks, R 2–3 ; 3 – granosyenites of the Chebula alkali
Journal Article
Conditions of Formation and Sources of Melts of Early Neoproterozoic Granites in Northern Kuznetsk Alatau
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 February 2023
Russ. Geol. Geophys. (2023) 64 (2): 133–147.
...Fig. 2. Scheme of the geologic structure of the northern Kundusuyul pluton, modified and supplemented from Rudnev et al. ( 2006 ). 1 – carbonateterrigenous-volcanic deposits, V–Є 1 ; 2 – dolomites, limestones, shales, and metavolcanic rocks, R 2–3 ; 3 – granosyenites of the Chebula alkali...
FIGURES
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Image
Scheme of the geologic structure of northern Kuznetsk Alatau, modified and ...
in Conditions of Formation and Sources of Melts of Early Neoproterozoic Granites in Northern Kuznetsk Alatau
> Russian Geology and Geophysics
Published: 01 February 2023
, 10 – Karadat, 11 – Gremyachikha, 12 – North Gremyachikha, in the Kundusuyul pluton). Roman numerals in squares denote batholiths (I – Kozhukh, II – Dudet, and III – Tsentral’nyi). Inset shows a scheme of geological and structural regionalization of northern Kuznetsk Alatau, after Shokal’skii et al
Journal Article
EARLY PALEOZOIC GRANITOID ASSOCIATIONS OF THE ALTAI-SAYAN FOLDED AREA: THEIR TYPES AND ROLE IN PALEOGEODYNAMIC RECONSTRUCTIONS
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 September 2000
Russ. Geol. Geophys. (2000) 41 (9): 1202–1213.
... is plagiogranitic and tonalite-plagiogranitic, occasionally with porphyry varieties of rocks in the margin of plutons. Plagiogranites were not dated radiologically and the available age estimates average 530–550 Ma [ 22 ]. These are, for example, the Kundusuyul’ and Lavrenev complexes in Kuznetsk Alatau [ 23 , 24...
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