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![Localization of granitoids of the Kukul’bei Complex within the tectonic structures of the central segment of the Mongol–Okhotsk Orogenic Belt (central and eastern Transbaikalia) [State…, 2010; Gordienko et al., 2019]. Rectangle marks the Soktui massif (the object of study). 1 – Siberian Platform; 2 – adjacent Caledonian accretion–collisional systems; collage of the Mongol–Okhotsk Orogenic Belt terranes: 3 – Aga (AG), 4 – Argun’ (AR), 5 – Hentiyn–Daurian (HD), 6 – Mongol–Okhotsk suture (MOS); 7 – borders of folded structures and terranes; 8 – massifs of the Kukul’bei granite–leucogranite complex.]()
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![First thumbnail for: Distribution of gold in igneous granitoid <span cl...]()
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![Comparative geological and geochemical schemes of granitoid magmatism of the Erzgebirge in Central Europe, Iul’tin ore district in the Chukchi province, and Sherlovy-Gory-Kukul’bei district in the Eastern Transbaikalian province. 1 – Quaternary deposits of river valleys (Iul’tin district); 2 – monzonites, syenites, granosyenites, granodiorites, and granites (Taureran rare-metal complex of the Iul’tin district and Shakhtama subrare-metal complex of Transbaikalia) ; 3 – rare-metal granites (OIC of the Erzgebirge, Iul’tin complex of the Chukchi Peninsula, and Kukul’bei complex of Transbaikalia); 4 – ultrarare-metal leucogranites (YIC of the Erzgebirge, Iul’tin complex of the Chukchi Peninsula, Kukul’bei complex of Transbaikalia); 5 – rare-metal felsites of the Erzgebirge, ultrarare-metal quartz porphyries – Transbaikalian ongonites; 6 – underground outlines of the Erzgebirge intrusion at a depth of about 3 km, hidden granite domes of the Iul’tin district down to a depth of 0.5 km; 7 – thickness of the granite-sedimentary bed in the Sherlovy-Gory-Kukul’bei district of Transbaikalia, cut at 1 km (after [28]); 8 – OIC (a) and YIC (b) granites, according to drilling data; 9 – zone of deep-seated faults of the Erzgebirge, disjunctions in the Iultin district. FRG – Federative Republic of Germany, CR – Czech Republic. Numerals stand for: Erzgebirge: I, II, III – Western, Central, and Eastern; massifs: 1 (la, 1b) – Nejdek-Eibenstock; 2 (2a, 2b) – Karlovy Vary and Slavkov woods; 3 (3a) – Kirchbergen; 4 (4a) – Teplice. Iul’tin district, massifs: 1 – Taureran, 2 – Veshkap, 3 – Metegin, 4 – Western Iul’tin, 5 – Central Iul’tin, 6 – Eastern Iul’tin; stocks (off-scale), eroded: 8 – Solnechnyi, 10 – Severnyi; hidden: 7 – Iul’tin, 9 – Svetlyi, 11 – Tenkerga. Sherlovy-Gory-Kukul’bei district, massifs: 1 – Alun-Chelon, 3 – Soktui, 3a – Antiiskii, 3b – North Soktui, 4 – Oldondo, 6 – Belukha, 10 – Kurunzulai, 11 – Alengui; stocks of amazonite granites (off-scale): 5 – Turga, 7 – Etykin, 8 – Achikan; 2 – Sherlovy-Gory dome, 2a – Bolshaya Sopka and Vysokaya Sopka (quartz porphyries – ongonites).]()
![The Zavaritskii petrochemical diagram (right part) of granitoids from the Erzgebirge, Chukchi Peninsula, and Transbaikalia (parameter b after D. S. Shteinberg, b′ = b – ba′/100, where b and a′ are given after A. N. Zavaritskii). 1 – Erzgebirge (OIC and YIC); 2 – Iu’ltin district (Taureran and Iul’tin complexes); 3 – Sherlovy-Gory-Kukul’bei district (Shakhtama and Kukul’bei complexes). Numbered figurative points correspond to columns in Table 1. Roman digits stand for fields of: I – granites, II – alkali granites, III – granodiorites, IV – granosyenites, VI – diorites, VII – earth-alkali syenites.]()
![Massifs (multiphase intrusions) of the ore-bearing Kukul’bei rare-metal granite complex (J2–J3) in the Aga structure-formational zone, eastern Transbaikalia. 1 — massifs of the Kukul’bei complex from which we sampled granites for studying REE patterns (see Table 1); 1–3, 6, 7 — massifs of the Kulinda intrusion; 2 — massifs of the Shakhtama gabbro-diorite-granodiorite complex (J2–J3); 3 — massifs of the Borshchovochnyi gneiss-granite–granite complex (J2–J3); 4 — massifs of batholith granodiorite-granite complexes: Kyra (T–J2) in the west and Unda (P2–T) in the east. Enclosing rocks: sand-shaly (T1), in the western half of the mapped area, and sand-shaly, effusive metamorphosed (PR3), and sand-shaly with effusions (C1–P2), in the eastern half.]()
![Hierarchic Q-type dendrogram of rocks of igneous complexes in the central and southwestern areas of eastern Transbaikalia. 1, Kharalga and Kukul’bei complexes: rare-metal granites and leucogranites; 2, Asakan–Shumilovka and Kyra (PAI) complexes: granites and leucogranites; 3, Kyra complex (MP): granites and granodiorites; 4, Sokhondo complex (FP): granites and granite-porphyry; 5, Sokhondo complex (MP): dacites and granodiorite-porphyry; 6, Unda complex (PAI): granites; 7, Unda complex (MP): granodiorites; 8, Shakhtama complex: gabbrodiorites, diorites, and granodiorites.]()
![Geological schemes of the Sakhanai (II), Durulgui (III), and Kulinda (IV) ore-magmatic granite systems in the Kukul’bei complex of the Aga zone. 1 — alluvial valley deposits; 2 — sand-shaly rocks: T1 — II and III, J1 — IV; 3 — metamorphic schists, R2 (IV); 4 — Shakhtama complex, diorites and granodiorites (III); 5–8 — Kukul’bei complex: 5 — fine-grained biotite monzodiorites (IV), 6 — coarse- and fine-grained biotite granites, 7 — fine- and coarse-grained two-mica granites and leucogranites, 8 — fine- and coarse-grained muscovite granites; 9 — average excess concentrations of granitophile elements (CIIE, Table 3) in various granites of intrusive systems; 10 — underground contour of the roof of concealed plutons, after gravimetric data (II and III, after [23], and IV, after [26]); 11 — contour of pegmatite fields [25]; 12 — deposits and ore occurrences: a — quartz-vein, cassiterite, wolframite, and cassiterite-wolframite; b — the same, with Be and Ta-Nb minerals (rare-metal type); c — pegmatite; d — fluorite. Roman numerals stand for intrusive systems; encircled Arabic numerals, for massifs and stocks; and Arabic numerals, for deposits: II — Sakhanai system, encircled numerals: 1 — Sakhanai massif, 2 — Zun-Undur massif, deposit: 1 — Zun-Undurskoe Sn-W-ore; III — Durulgui system, encircled numerals: 1 — western part of the Durulgui massif, 2 — eastern part (Bului valley), deposits: 1 — Dedovogorskoe W-ore, 2 — Chalotskoe Be, Ta-Nb-ore pegmatite, 3 — Imalkinskoe Sn-ore; IV — Kulinda system, encircled numerals mark unnamed massifs, except for 7 — Bogov Utes (Table 4), deposits: 1 — Malokulindinskoe Ta-Nb-ore pegmatite, 2 — Ononskoe Sn-ore (exocontact of the Bogov Utes massif).]()
![Schematic geological map of the Khangilai intrusion (I) (compiled by V.D. Kozlov after [3, 4], with simplification). 1 — alluvial deposits of valleys; 2 — metamorphosed sand-shaly and effusive rocks (PR3); 3 — sand-shaly rocks (T3); 4 — olivine diabase dikes (KZ?); 5 — granites of the Kukul’bei complex (J2–J3): a — biotite granites of the intrusion periphery (Ubzhigoi series), b — biotite, two-mica, muscovite, and amazonite rare-metal and ultrarare-metal leucogranites of the intrusion core; 6 — gabbroids and diorites of the Shakhtama complex (J2–J3); 7 — lamprophyre dikes (MZ); 8 — granite-porphyry dikes of the intrusion periphery; 9 — fracture zones; 10 — faults; 11 — contour of the roof of concealed granite pluton and places of Sn-W-ore occurrences; 12 — granite sampling localities and profiles with the numbers of samples. Encircled digits: 1 — Khangilai massif, 2 — Spokoiny dome, 3 — Orlovka dome, 4 — Ubzhigoi series of satellites.]()
![Schematic geological map of the Lugokan ore cluster, after Redin and Kozlova (2014), supplemented. 1, Quaternary deposits (Q4); 2, Turga Formation (K1tr1), conglomerates; 3, Glushkovo Formation (J3gl1), conglomerates, sandsontes, siltstones, and basalt-trachyandesitic, basalt-andesitic, andesitic, and basaltic lavas; 4, Yakovlevka Formation (D2-3jak), sandstones, siltstones, and limestones; 5, Il’dikan Formation (D1–2il), mica and quartz–mica schists; 6, Bystraya Formation (Є1bs), limestones and dolomites; 7, Kukul’bei complex (lγ1J3k), leucogranites; 8, Unda– Daya complex (J3u): a, lamprophyre and hybrid porphyry dikes, b, granite-porphyry dikes; 9, Shakhtama complex (γδπJ2–3s), granodiorite-porphyry; 10, Kutomara complex (γg2P–T1k), gneiss-granites; 11, 12, Unda complex (P1u): 11, leucocratic granites (lγ3), granites (γ2), and granodiorites (γδ2) and diorites (δ1), 12, gabbro (ν1); 13, faults: a, proved, b, predicted.]()
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![Plutons of the Shakhtama gabbrodiorite–monzonite–granodiorite (J2–J3) and the ore-bearing Kukul’bei (J3) granite–leucogranite complexes (Aga tectonic zone, eastern Transbaikalia). 1, Kukul’bei plutons; 2, plutons and pluton groups of the Shakhtama complex; 3, plutons of the Borshchovochnyi gneissic granite–granite complex (J2–J3); 4, plutons of the batholithic granodiorite–granite complexes: Kyra (T–J2) in the west and Unda (P2–T) in the east. Host rocks: sands and schists (T1) in the west; sands, schists, and metamorphosed effusive rocks (R) as well as sands, schists, and effusive rocks (C1–P2) in the east. Squared numbers show the total granitophile-element contents of MS granitoids excessive with respect to the clarke (CI: for the Shakhtama complex, according to Table 2; for the Kukul’bei one, after (Kozlov, 2009)). Inset shows the geographical position of the Aga zone (demarcated by a dashed line).]()
![First thumbnail for: POTASSIC ALKALI BASALTOIDS AND GEOCHEMICAL SPECIAL...]()
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![Normalized REE patterns for the MS granitoids from the Shakhtama complex. Here and in what follows, the patterns are normalized to chondrite C1 (Taylor and McLennan, 1985). Here and in what follows, the pattern numbers for the Shakhtama granitoids correspond to the analysis columns in Table 1; the pattern numbers indexed with a “k” for the Kukul’bei granites correspond to the analysis columns from (Kozlov, 2009, Table 1).]()
![Ratios of outcropped areas, rare-metal abundances (a), and clarkes of concentration of Sn and W (b) in granitoids of successively intrusive complexes and stages of the Erzgebirge, Chukchi Peninsula, and Transbaikalia. 1 – Erzgebirge, 2 – Iul’tin district of the Chukchi Peninsula, 3 – Sherlovy-Gory-Kukul’bei district of Transbaikalia. Location of domes and stocks of high-ultrarare-metal granites is marked by figurative points. Symbols follow Fig. 2.]()
![Schematic map of the geologic structure of the Soktui massif, compiled from the State Geological Map [2000]. 1 – Quaternary deposits; 2–5 – host rocks: 2 – sedimentary and volcanic (K), 3 – sedimentary (J1–2), 4 – sedimentary and volcanosedimentary (P2), 5 – Urul’ga metamorphic complex (PR1); 6–10 – Kukul’bei granite-leucogranite complex (K1): 6–8 – rocks of the phase of additional intrusions (PAI) : 6 – granodiorites and quartz syenites, 7 – alkali-feldspathic granite-porphyry, 8 – alaskites; 9–10 – rocks of the major intrusive phase (MIP): 9 – microgranite dikes, 10 – monzogranite–monzoleucogranites; 11 – Shakhtama complex (J2–3), monzodiorite–granodiorite–granite; 12 – Shadoron complex (J2–3), granodiorite–porphyry, diorite–porphyrite; 13 – Chingil’tui complex (T), gabbro-diabase; 14 – greisenization zones; 15 – hornfelsing zones; 16 – proved (a) and predicted (b) faults; 17 – proved (a) and predicted (b) phase/complex boundaries; 18 – sampling localities.]()
![Schematic localization of ore fields of Pb–Zn deposits and Jurassic volcanoplutonic complexes in eastern Transbaikalia, after Sanin and Zorina (1980). 1, limestones, dolomites (PZ); 2, sandstones, siltstones (J); 3, basalts, andesite-basalts, andesites, and rhyolites of the Akatui (J2–3) and Nerchinskii Zavod (J2–3) complexes; 4, basalts, andesite-basalts, and andesites of the Shirokaya complex (J2–3); intrusive complexes (J2–3): 5, Akatui, 6, Nerchinskii Zavod, 7, Shirokaya, 8, Late Shakhtama, 9, Kukul’bei; 10, ore clusters of Pb–Zn deposits: 1, Akatui, 2, Mikhailovka, 3, Kadaya, 4, trans-Pokrovka, 5, Nerchinskii Zavod, 6, Shirokaya, 7, Shakhtama, 8, Klichka, 9, Noion-Tologoi.]()
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Journal Article
Trace-element composition and origin of granitoids from the Shakhtama complex and Kukul’bei rare-metal complex ( Aga zone, Transbaikalia ) Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 May 2011
Russ. Geol. Geophys. (2011) 52 (5): 526–536.
... that they were initially enriched in granitophile (including ore-forming) trace elements. This suggests consanguinity between the intrusions of the Shakhtama complex (J 2 –J 3 ) and the ore-bearing Kukul’bei rare-metal complex of granites and leucogranites (J 3 ) (Aga zone, Transbaikalia). Since granitophile...
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![Localization of granitoids of the Kukul’bei Complex within the tectonic structures of the central segment of the Mongol–Okhotsk Orogenic Belt (central and eastern Transbaikalia) [State…, 2010; Gordienko et al., 2019]. Rectangle marks the Soktui massif (the object of study). 1 – Siberian Platform; 2 – adjacent Caledonian accretion–collisional systems; collage of the Mongol–Okhotsk Orogenic Belt terranes: 3 – Aga (AG), 4 – Argun’ (AR), 5 – Hentiyn–Daurian (HD), 6 – Mongol–Okhotsk suture (MOS); 7 – borders of folded structures and terranes; 8 – massifs of the Kukul’bei granite–leucogranite complex.](https://gsw.silverchair-cdn.com/gsw/Content_public/Journal/rgg/66/5/10.2113_RGG20244823/1/s_naryzhnova_page_2_1.jpeg?Expires=2147483647&Signature=SEYobhL4ZkwDwy-~fbXn16sS9wcKvPCtbXW8aAPAoqfXPAzgybnknHUU1PRX0c~CFwYJLhDel4XhIPUpSeMR-SXkIUMt3At7X8VwRlV1XY6ojRSMoKeSXjg1m-8MpJCzsyY8HmGOyZwyTLjyERyFmo22lsQnvUm4f3QhvJx2Q047GSFy~Ci4SP9A80-JbGz5TW9tCngjXEvZwN9M9ly3Mrzm4Wu9X6q2uon96sd~h6r4RINgZ5wcs97b38lxt2kOd-pc8lpNrVMDo0hVtH151tF9dL6uGCrbaYf0mWXBaVFWrHpJwqaZHLQmEH0HSEUmYY5NFpNKLF7MzdoLBOLnLw__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA)
Localization of granitoids of the Kukul’bei Complex within the tectonic str... Available to Purchase
in EARLY CRETACEOUS GRANITOIDS OF THE SOKTUI MASSIF: COMPOSITION AND PETROGENESIS ( eastern Transbaikalia )
> Russian Geology and Geophysics
Published: 01 May 2025
Fig. 1. Localization of granitoids of the Kukul’bei Complex within the tectonic structures of the central segment of the Mongol–Okhotsk Orogenic Belt (central and eastern Transbaikalia) [ State…, 2010 ; Gordienko et al., 2019 ]. Rectangle marks the Soktui massif (the object of study). 1
Journal Article
Rare-earth elements as indicators of ore sources and the degree of differentiation and ore potential of rare-metal granite intrusions ( eastern Transbaikalia ) Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 January 2009
Russ. Geol. Geophys. (2009) 50 (1): 29–42.
...V.D. Kozlov Abstract The meteoritic-material-normalized REE patterns of rare-metal granite intrusions of the ore-bearing Kukul’bei complex (J2–J3), eastern Transbaikalia, were studied. It is shown that the intrusions were initially enriched in granitophile volatiles and trace elements (rare metals...
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Journal Article
GEOLOGO-GEOCHEMICAL CENTRAL STRUCTURE AND METALLOGENY OF GRANITE ORE-MAGMATIC SYSTEMS IN EASTERN TRANSBAIKALIA Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 May 2005
Russ. Geol. Geophys. (2005) 46 (5): 486–503.
...V.D. Kozlov Granites of the Late Mesozoic Kukul’bei ore-bearing complex in the Aga structure-formational zone of eastern Transbaikalia are studied. It is shown that the concentrations of incompatible trace elements in them are correlated with the domal morphology of the roof of granite intrusive...
FIGURES
Journal Article
EARLY CRETACEOUS GRANITOIDS OF THE SOKTUI MASSIF: COMPOSITION AND PETROGENESIS ( eastern Transbaikalia ) Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 May 2025
Russ. Geol. Geophys. (2025) 66 (5): 570–592.
...Fig. 1. Localization of granitoids of the Kukul’bei Complex within the tectonic structures of the central segment of the Mongol–Okhotsk Orogenic Belt (central and eastern Transbaikalia) [ State…, 2010 ; Gordienko et al., 2019 ]. Rectangle marks the Soktui massif (the object of study). 1...
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Includes: Supplemental Content
Journal Article
Distribution of gold in igneous granitoid complexes in the central and southwestern areas of eastern Transbaikalia Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 August 2010
Russ. Geol. Geophys. (2010) 51 (8): 846–856.
... Paleozoic Unda complex in the east of the study area and in the Triassic–Middle Jurassic Kyra complex in the west. The rocks of the Early–Middle Jurassic (Sokhondo) and Middle–Upper Jurassic (Shakhtama, Kharalga, and Kukul’bei) complexes have much lower Au concentrations (mainly 0.0014–0.0030 ppm...
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![Comparative geological and geochemical schemes of granitoid magmatism of the Erzgebirge in Central Europe, Iul’tin ore district in the Chukchi province, and Sherlovy-Gory-Kukul’bei district in the Eastern Transbaikalian province. 1 – Quaternary deposits of river valleys (Iul’tin district); 2 – monzonites, syenites, granosyenites, granodiorites, and granites (Taureran rare-metal complex of the Iul’tin district and Shakhtama subrare-metal complex of Transbaikalia) ; 3 – rare-metal granites (OIC of the Erzgebirge, Iul’tin complex of the Chukchi Peninsula, and Kukul’bei complex of Transbaikalia); 4 – ultrarare-metal leucogranites (YIC of the Erzgebirge, Iul’tin complex of the Chukchi Peninsula, Kukul’bei complex of Transbaikalia); 5 – rare-metal felsites of the Erzgebirge, ultrarare-metal quartz porphyries – Transbaikalian ongonites; 6 – underground outlines of the Erzgebirge intrusion at a depth of about 3 km, hidden granite domes of the Iul’tin district down to a depth of 0.5 km; 7 – thickness of the granite-sedimentary bed in the Sherlovy-Gory-Kukul’bei district of Transbaikalia, cut at 1 km (after [28]); 8 – OIC (a) and YIC (b) granites, according to drilling data; 9 – zone of deep-seated faults of the Erzgebirge, disjunctions in the Iultin district. FRG – Federative Republic of Germany, CR – Czech Republic. Numerals stand for: Erzgebirge: I, II, III – Western, Central, and Eastern; massifs: 1 (la, 1b) – Nejdek-Eibenstock; 2 (2a, 2b) – Karlovy Vary and Slavkov woods; 3 (3a) – Kirchbergen; 4 (4a) – Teplice. Iul’tin district, massifs: 1 – Taureran, 2 – Veshkap, 3 – Metegin, 4 – Western Iul’tin, 5 – Central Iul’tin, 6 – Eastern Iul’tin; stocks (off-scale), eroded: 8 – Solnechnyi, 10 – Severnyi; hidden: 7 – Iul’tin, 9 – Svetlyi, 11 – Tenkerga. Sherlovy-Gory-Kukul’bei district, massifs: 1 – Alun-Chelon, 3 – Soktui, 3a – Antiiskii, 3b – North Soktui, 4 – Oldondo, 6 – Belukha, 10 – Kurunzulai, 11 – Alengui; stocks of amazonite granites (off-scale): 5 – Turga, 7 – Etykin, 8 – Achikan; 2 – Sherlovy-Gory dome, 2a – Bolshaya Sopka and Vysokaya Sopka (quartz porphyries – ongonites).](https://gsw.silverchair-cdn.com/gsw/Content_public/Journal/rgg/41/6/rgg-04100830/2/s_rgg-2000-6_830_page_3_1.jpeg?Expires=2147483647&Signature=ecu36XCSBYTtcUKdwqn7JAht0en5MyQ7ldThWBs8s6QLSL1NGRVJ7DYy6V3KgPk70v9o~-Eel~VNsLgilPPFzMCGbfjgqw2oh96ASmH93FHCHPidWxr57oYELsVeISubiQLIr2f91WJtMvbI7Rkg~dpvrFBbQkj-VyBJyqVRsTvIRKbpcLrqlMJKQsh9B0EE6HOExYIPzx9aMS6PHMqSnmuAtbCDEkc3R--68UsB0VLGM8NYweVznfIsdue4KbNO22wJYnbzt3B0XwVTgcCDv5lgeNfVMVQ~x58TSylWka3RvhgdmBG290DRsyGZZ8hYWloALbtkZ58kMb1Fj3X6ZA__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA)
Comparative geological and geochemical schemes of granitoid magmatism of th... Available to Purchase
in COMPARATIVE GEOLOGICAL AND GEOCHEMICAL ASSESSMENT OF THE ORE POTENTIAL OF GRANITOIDS AND PRODUCTIVITY OF W-Sn MINERALIZATION ( Central Europe, Transbaikalia, and Chukchi Peninsula )
> Russian Geology and Geophysics
Published: 01 June 2000
district); 2 – monzonites, syenites, granosyenites, granodiorites, and granites (Taureran rare-metal complex of the Iul’tin district and Shakhtama subrare-metal complex of Transbaikalia) ; 3 – rare-metal granites (OIC of the Erzgebirge, Iul’tin complex of the Chukchi Peninsula, and Kukul’bei complex
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The Zavaritskii petrochemical diagram (right part) of granitoids from the E... Available to Purchase
in COMPARATIVE GEOLOGICAL AND GEOCHEMICAL ASSESSMENT OF THE ORE POTENTIAL OF GRANITOIDS AND PRODUCTIVITY OF W-Sn MINERALIZATION ( Central Europe, Transbaikalia, and Chukchi Peninsula )
> Russian Geology and Geophysics
Published: 01 June 2000
district (Taureran and Iul’tin complexes); 3 – Sherlovy-Gory-Kukul’bei district (Shakhtama and Kukul’bei complexes). Numbered figurative points correspond to columns in Table 1 . Roman digits stand for fields of: I – granites, II – alkali granites, III – granodiorites, IV – granosyenites, VI – diorites
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Massifs (multiphase intrusions) of the ore-bearing Kukul’bei rare-metal gra... Available to Purchase
in Rare-earth elements as indicators of ore sources and the degree of differentiation and ore potential of rare-metal granite intrusions ( eastern Transbaikalia )
> Russian Geology and Geophysics
Published: 01 January 2009
Fig. 1. Massifs (multiphase intrusions) of the ore-bearing Kukul’bei rare-metal granite complex (J 2 –J 3 ) in the Aga structure-formational zone, eastern Transbaikalia. 1 — massifs of the Kukul’bei complex from which we sampled granites for studying REE patterns (see Table 1 ); 1–3, 6, 7
Image
Hierarchic Q -type dendrogram of rocks of igneous complexes in the central... Available to Purchase
in Distribution of gold in igneous granitoid complexes in the central and southwestern areas of eastern Transbaikalia
> Russian Geology and Geophysics
Published: 01 August 2010
Fig. 3. Hierarchic Q -type dendrogram of rocks of igneous complexes in the central and southwestern areas of eastern Transbaikalia. 1 , Kharalga and Kukul’bei complexes: rare-metal granites and leucogranites; 2 , Asakan–Shumilovka and Kyra (PAI) complexes: granites and leucogranites; 3 , Kyra
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![Geological schemes of the Sakhanai (II), Durulgui (III), and Kulinda (IV) ore-magmatic granite systems in the Kukul’bei complex of the Aga zone. 1 — alluvial valley deposits; 2 — sand-shaly rocks: T1 — II and III, J1 — IV; 3 — metamorphic schists, R2 (IV); 4 — Shakhtama complex, diorites and granodiorites (III); 5–8 — Kukul’bei complex: 5 — fine-grained biotite monzodiorites (IV), 6 — coarse- and fine-grained biotite granites, 7 — fine- and coarse-grained two-mica granites and leucogranites, 8 — fine- and coarse-grained muscovite granites; 9 — average excess concentrations of granitophile elements (CIIE, Table 3) in various granites of intrusive systems; 10 — underground contour of the roof of concealed plutons, after gravimetric data (II and III, after [23], and IV, after [26]); 11 — contour of pegmatite fields [25]; 12 — deposits and ore occurrences: a — quartz-vein, cassiterite, wolframite, and cassiterite-wolframite; b — the same, with Be and Ta-Nb minerals (rare-metal type); c — pegmatite; d — fluorite. Roman numerals stand for intrusive systems; encircled Arabic numerals, for massifs and stocks; and Arabic numerals, for deposits: II — Sakhanai system, encircled numerals: 1 — Sakhanai massif, 2 — Zun-Undur massif, deposit: 1 — Zun-Undurskoe Sn-W-ore; III — Durulgui system, encircled numerals: 1 — western part of the Durulgui massif, 2 — eastern part (Bului valley), deposits: 1 — Dedovogorskoe W-ore, 2 — Chalotskoe Be, Ta-Nb-ore pegmatite, 3 — Imalkinskoe Sn-ore; IV — Kulinda system, encircled numerals mark unnamed massifs, except for 7 — Bogov Utes (Table 4), deposits: 1 — Malokulindinskoe Ta-Nb-ore pegmatite, 2 — Ononskoe Sn-ore (exocontact of the Bogov Utes massif).](https://gsw.silverchair-cdn.com/gsw/Content_public/Journal/rgg/46/5/rgg-460486/2/s_s02may05_page_13_1.jpeg?Expires=2147483647&Signature=MGmocfo42x3DNgoIzTiSrDFR~ps2ljRxJ6ABiOS97exEGs6X1YbYCJGhM00PmexUrw6YpexYJvQTmhXriXlzQttHP6cd6GGfPk-1AZFpa~fTmRtpJbPuVEGE~Y7msEw7VPqQOoWJAcTWDHRlrCAoxJaHt4omOxEaY9xGgxTwKYPMqfLeyybUresljpet81LF9fg4s9ZMn4zGk~O5yp5JYnT1PV3vNTwb~8A3DnSkUo3wN2xWV82KRRqD6TuljUFXIIwyOvkRBwx0Lbt3ztnkKlCh3R3~Y7~uwet2DscoI-w3amiuH5WBFirNN1w8V5uLz2x8T8yDWXwQdRi8xga6AQ__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA)
Geological schemes of the Sakhanai (II), Durulgui (III), and Kulinda (IV) o... Available to Purchase
in GEOLOGO-GEOCHEMICAL CENTRAL STRUCTURE AND METALLOGENY OF GRANITE ORE-MAGMATIC SYSTEMS IN EASTERN TRANSBAIKALIA
> Russian Geology and Geophysics
Published: 01 May 2005
Fig. 5. Geological schemes of the Sakhanai (II), Durulgui (III), and Kulinda (IV) ore-magmatic granite systems in the Kukul’bei complex of the Aga zone. 1 — alluvial valley deposits; 2 — sand-shaly rocks: T 1 — II and III, J 1 — IV; 3 — metamorphic schists, R 2 (IV); 4 — Shakhtama
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![Schematic geological map of the Khangilai intrusion (I) (compiled by V.D. Kozlov after [3, 4], with simplification). 1 — alluvial deposits of valleys; 2 — metamorphosed sand-shaly and effusive rocks (PR3); 3 — sand-shaly rocks (T3); 4 — olivine diabase dikes (KZ?); 5 — granites of the Kukul’bei complex (J2–J3): a — biotite granites of the intrusion periphery (Ubzhigoi series), b — biotite, two-mica, muscovite, and amazonite rare-metal and ultrarare-metal leucogranites of the intrusion core; 6 — gabbroids and diorites of the Shakhtama complex (J2–J3); 7 — lamprophyre dikes (MZ); 8 — granite-porphyry dikes of the intrusion periphery; 9 — fracture zones; 10 — faults; 11 — contour of the roof of concealed granite pluton and places of Sn-W-ore occurrences; 12 — granite sampling localities and profiles with the numbers of samples. Encircled digits: 1 — Khangilai massif, 2 — Spokoiny dome, 3 — Orlovka dome, 4 — Ubzhigoi series of satellites.](https://gsw.silverchair-cdn.com/gsw/Content_public/Journal/rgg/46/5/rgg-460486/2/s_s02may05_page_3_1.jpeg?Expires=2147483647&Signature=ZixtH1N5heIa6Njeke-Lf8zyowf-dLQQKNUBpDybsjuyCLKDHk9U6OaxUM1fIwrq7g~xgrncE7AAxor4XVdHF1IeagiKscPtTCinNLMQCu1YXzE~4As~JMXUMIb03xK9Wv6L1JWrZx7SEALfVJ7WbFSvHTYmj3jCmLyfF78yAGDTLPUQaJamgpm6cfS112ZAj9oiCo-zdXXjDYlUhZ-yncCXHi9xv9FCrA~-WkhWuSGGcf62k-sylrUAz7oBpDgVwFi2ZgwMK9tGkPVLnlJWl7iAFDs~Uf1vduNV3k3QjImjg5zD~2OVMYhHm8C23Dlvp-LUGAmTbfd3Z55p8E5ScQ__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA)
Schematic geological map of the Khangilai intrusion (I) (compiled by V.D. K... Available to Purchase
in GEOLOGO-GEOCHEMICAL CENTRAL STRUCTURE AND METALLOGENY OF GRANITE ORE-MAGMATIC SYSTEMS IN EASTERN TRANSBAIKALIA
> Russian Geology and Geophysics
Published: 01 May 2005
— granites of the Kukul’bei complex (J 2 –J 3 ): a — biotite granites of the intrusion periphery (Ubzhigoi series), b — biotite, two-mica, muscovite, and amazonite rare-metal and ultrarare-metal leucogranites of the intrusion core; 6 — gabbroids and diorites of the Shakhtama complex (J 2 –J 3 ); 7
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Schematic geological map of the Lugokan ore cluster, after Redin and Kozlov... Available to Purchase
in The Lukoganskoe Au–Cu Skarn Deposit (Eastern Transbaikalia): Mineral Composition, Age, and Formation Conditions
> Russian Geology and Geophysics
Published: 01 February 2020
, basalt-andesitic, andesitic, and basaltic lavas; 4 , Yakovlevka Formation (D 2-3 jak), sandstones, siltstones, and limestones; 5 , Il’dikan Formation (D 1–2 il), mica and quartz–mica schists; 6 , Bystraya Formation (Є 1 bs), limestones and dolomites; 7 , Kukul’bei complex (lγ 1 J 3 k), leucogranites
Journal Article
COMPARATIVE GEOLOGICAL AND GEOCHEMICAL ASSESSMENT OF THE ORE POTENTIAL OF GRANITOIDS AND PRODUCTIVITY OF W-Sn MINERALIZATION ( Central Europe, Transbaikalia, and Chukchi Peninsula ) Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 June 2000
Russ. Geol. Geophys. (2000) 41 (6): 830–841.
... district); 2 – monzonites, syenites, granosyenites, granodiorites, and granites (Taureran rare-metal complex of the Iul’tin district and Shakhtama subrare-metal complex of Transbaikalia) ; 3 – rare-metal granites (OIC of the Erzgebirge, Iul’tin complex of the Chukchi Peninsula, and Kukul’bei complex...
FIGURES
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Plutons of the Shakhtama gabbrodiorite–monzonite–granodiorite (J 2 –J 3 ) a... Available to Purchase
in Trace-element composition and origin of granitoids from the Shakhtama complex and Kukul’bei rare-metal complex ( Aga zone, Transbaikalia )
> Russian Geology and Geophysics
Published: 01 May 2011
Fig. 1. Plutons of the Shakhtama gabbrodiorite–monzonite–granodiorite (J 2 –J 3 ) and the ore-bearing Kukul’bei (J 3 ) granite–leucogranite complexes (Aga tectonic zone, eastern Transbaikalia). 1 , Kukul’bei plutons; 2 , plutons and pluton groups of the Shakhtama complex; 3 , plutons
Journal Article
POTASSIC ALKALI BASALTOIDS AND GEOCHEMICAL SPECIALIZATION OF ASSOCIATED RARE-METAL GRANITES Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 July 1999
Russ. Geol. Geophys. (1999) 40 (7): 973–985.
... granite magmatism of Eastern Transbaikalia is represented in Table 1 by the Kukul’bei complex (146–135 Ma [ 18 ]). The average composition of plumasite rare-metal granites of the main phase was calculated from the compositions of three massifs which are spatially associated with the above-mentioned...
FIGURES
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Normalized REE patterns for the MS granitoids from the Shakhtama complex. H... Available to Purchase
in Trace-element composition and origin of granitoids from the Shakhtama complex and Kukul’bei rare-metal complex ( Aga zone, Transbaikalia )
> Russian Geology and Geophysics
Published: 01 May 2011
Fig. 2. Normalized REE patterns for the MS granitoids from the Shakhtama complex. Here and in what follows, the patterns are normalized to chondrite C 1 ( Taylor and McLennan, 1985 ). Here and in what follows, the pattern numbers for the Shakhtama granitoids correspond to the analysis columns
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Ratios of outcropped areas, rare-metal abundances ( a ), and clarkes of con... Available to Purchase
in COMPARATIVE GEOLOGICAL AND GEOCHEMICAL ASSESSMENT OF THE ORE POTENTIAL OF GRANITOIDS AND PRODUCTIVITY OF W-Sn MINERALIZATION ( Central Europe, Transbaikalia, and Chukchi Peninsula )
> Russian Geology and Geophysics
Published: 01 June 2000
Fig. 3. Ratios of outcropped areas, rare-metal abundances ( a ), and clarkes of concentration of Sn and W ( b ) in granitoids of successively intrusive complexes and stages of the Erzgebirge, Chukchi Peninsula, and Transbaikalia. 1 – Erzgebirge, 2 – Iul’tin district of the Chukchi Peninsula
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![Schematic map of the geologic structure of the Soktui massif, compiled from the State Geological Map [2000]. 1 – Quaternary deposits; 2–5 – host rocks: 2 – sedimentary and volcanic (K), 3 – sedimentary (J1–2), 4 – sedimentary and volcanosedimentary (P2), 5 – Urul’ga metamorphic complex (PR1); 6–10 – Kukul’bei granite-leucogranite complex (K1): 6–8 – rocks of the phase of additional intrusions (PAI) : 6 – granodiorites and quartz syenites, 7 – alkali-feldspathic granite-porphyry, 8 – alaskites; 9–10 – rocks of the major intrusive phase (MIP): 9 – microgranite dikes, 10 – monzogranite–monzoleucogranites; 11 – Shakhtama complex (J2–3), monzodiorite–granodiorite–granite; 12 – Shadoron complex (J2–3), granodiorite–porphyry, diorite–porphyrite; 13 – Chingil’tui complex (T), gabbro-diabase; 14 – greisenization zones; 15 – hornfelsing zones; 16 – proved (a) and predicted (b) faults; 17 – proved (a) and predicted (b) phase/complex boundaries; 18 – sampling localities.](https://gsw.silverchair-cdn.com/gsw/Content_public/Journal/rgg/66/5/10.2113_RGG20244823/1/s_naryzhnova_page_3_1.jpeg?Expires=2147483647&Signature=3QAJb~sYTNSk1wMcQvgLcDKa5gAvTgEbPwtFz72PqhHUPPyWOGlCbZl9yuoXQOh7XzfkCeO1UNzqv4K6bkFb6IfGP9cz5jCKPnMWG2qLuH~dWUTBilr8w0JO5XptQTP0jcQaEGnU6orEpXdZacaAXkohi71eJIsAahy~5b8q5UdSyX5KfiHwNzJvirH9iODVQe2N-3sQaaKtU8uD8OVI45uKjXllNdzcGSBGKnfhFNnrXh8O8oS2C9JUJI5GZKYaR48~rEVoZBv4C7MHvwmmkeMzpNmbeGH6g8XIsylprQgN9M4HlGqMrclda6skx83Fd3C6xsANb9QUFOQR6kPzmA__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA)
Schematic map of the geologic structure of the Soktui massif, compiled from... Available to Purchase
in EARLY CRETACEOUS GRANITOIDS OF THE SOKTUI MASSIF: COMPOSITION AND PETROGENESIS ( eastern Transbaikalia )
> Russian Geology and Geophysics
Published: 01 May 2025
metamorphic complex (PR 1 ); 6 – 10 – Kukul’bei granite-leucogranite complex (K 1 ): 6 – 8 – rocks of the phase of additional intrusions (PAI) : 6 – granodiorites and quartz syenites, 7 – alkali-feldspathic granite-porphyry, 8 – alaskites; 9 – 10 – rocks of the major intrusive phase (MIP): 9
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Schematic localization of ore fields of Pb–Zn deposits and Jurassic volcano... Available to Purchase
in The Noion-Tologoi polymetallic deposit: formation conditions and petrogeochemical peculiarities of rocks and ores ( eastern Transbaikalia )
> Russian Geology and Geophysics
Published: 01 February 2017
(J 2–3 ) and Nerchinskii Zavod (J 2–3 ) complexes; 4 , basalts, andesite-basalts, and andesites of the Shirokaya complex (J 2–3 ); intrusive complexes (J 2–3 ): 5 , Akatui, 6 , Nerchinskii Zavod, 7 , Shirokaya, 8 , Late Shakhtama, 9 , Kukul’bei; 10 , ore clusters of Pb–Zn deposits: 1 , Akatui
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