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Tyrkanda District

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Scheme of the Inagli massif (a) with the layout of ore districts within the Chara–Aldan metallogenic zone of the Aldan–Stanovoi Shield (b) with geochronological data (geological plot based on (Dzevanovskii et al., 1972), ore districts are shown based on (Parfenov and Kuz’min, 2001)). 1, shield base; 2, cover rocks: I, Proterozoic sandstones and Cambrian limestones, II, Jurassic sandstones, III, Cretaceous sandstones; 3, Mesozoic igneous rocks; 4, faults; 5, outlines of ore districts associated with Mesozoic alkaline magmatism: CAD, Central Aldan district; TD, Tyrkanda district; KKD, Ket-Kap district. Geochronological data are obtained using U–Pb and Ar–Ar methods (Borisenko et al., 2011; Polin et al., 2012; Prokopyev et al., 2018).
Published: 01 January 2019
)). 1 , shield base; 2 , cover rocks: I, Proterozoic sandstones and Cambrian limestones, II, Jurassic sandstones, III, Cretaceous sandstones; 3 , Mesozoic igneous rocks; 4 , faults; 5 , outlines of ore districts associated with Mesozoic alkaline magmatism: CAD, Central Aldan district; TD, Tyrkanda
Journal Article
Published: 01 February 2023
Russ. Geol. Geophys. (2023) 64 (2): 175–191.
.... Magmatism of this stage was of limited occurrence in the CAOD and did not produce alkali syenites, monzonite–syenites, and ores. At the same time, rocks with an age of 121.1 ± 1.3—115.5 ± 1.6 Ma are widespread in the large (120 km 2 ) Dzheltula ring massif of the Tyrkanda ore district, located east...
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Journal Article
Published: 01 January 2019
Russ. Geol. Geophys. (2019) 60 (1): 33–44.
... )). 1 , shield base; 2 , cover rocks: I, Proterozoic sandstones and Cambrian limestones, II, Jurassic sandstones, III, Cretaceous sandstones; 3 , Mesozoic igneous rocks; 4 , faults; 5 , outlines of ore districts associated with Mesozoic alkaline magmatism: CAD, Central Aldan district; TD, Tyrkanda...
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Journal Article
Published: 01 June 2010
Russ. Geol. Geophys. (2010) 51 (6): 661–671.
...V.G. Khomich; N.G. Boriskina Abstract Gold ore districts in the Siberian (North Asian) craton and bordering terranes have been studied. Studies showed the long duration of gold concentration processes (Early Cambrian to Late Mesozoic and Cenozoic) and the influence of structural geological...
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Journal Article
Published: 01 December 2011
Russ. Geol. Geophys. (2011) 52 (12): 1672–1679.
.... Siberian Platform. Aldan granulite–gneiss zone: 1 , Early Archean blocks (Aldanides): Chg, Chuga; Gon, Gonam; Id, Idzhek; Ie, Iengra; Nm, Nimnyr; S, Seim; T, Timpton; Tr, Tyrkanda; 2 , Late Archean blocks, graben–synclinorium structures: F, Fedorovskii trough; Sun, Sunnagino; Un, Ungra graben; 3...
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Image
Geological-metallogenic sketch map of the Central Aldan superterrane, after (Kazanskii, 2004; Parfenov and Kuz’min, 2001), with some modifications. Terranes: ANM, Nimnyr, granulite–orthogneiss, AST, Sutam, granulite–paragneiss. 1, Siberian Platform cover: a, Jurassic terrigenous (epiplatform), b, Vendian–Cambrian, predominantly carbonate; 2, amphibole, biotite–amphibole, diopside–amphibole, two-pyroxene–amphibole plagiogneisses, more rarely schists interbedded and interlensed with diopsides, phlogopite–diopsides, and calciphyres (Fedorovka Formation); 3, quartzites and high-alumina gneisses interlensed with calciphyres, argillaceous and diopside quartzites (Kurumkan Formation), granitic gneisses; 4, garnet–biotite gneisses and plagiogneisses, hypersthene–biotite, two-pyroxene, and diopside–amphibole plagiogneisses (Seim Formation); 5, granitic, charnockitic, and enderbitic gneisses interlensed with two-pyroxene mafic granulites; 6, mélange zones: am, Amga, kl, Kalar, tr, Tyrkanda; 7, high-angle faults (a) and thrusts (b) (SM, Seim); 8, El’kon (Yakokut–Yllymakh) granitization field; 9, boundary of the Central Aldan superterrane and large Mesozoic calc–alkali and alkalic massifs; 10, 11, deposits: 10, magnetite, 11, phlogopite; 12–15, major gold ore clusters and fields in the Aldan district: 12, El’kon (Au–U), 13, Lebedinoe (Au), 14, Kuranakh (Au), 15, Ryabinovoe (Au, Mo);16, boundaries of the Seligdar–Kavakta fragment of the Seligdar–Upper Timpton gravity gradient zone.
Published: 01 June 2010
, and enderbitic gneisses interlensed with two-pyroxene mafic granulites; 6 , mélange zones: am, Amga, kl, Kalar, tr, Tyrkanda; 7 , high-angle faults ( a ) and thrusts ( b ) (SM, Seim); 8 , El’kon (Yakokut–Yllymakh) granitization field; 9 , boundary of the Central Aldan superterrane and large Mesozoic calc
Journal Article
Published: 01 March 2024
Russ. Geol. Geophys. (2024) 65 (3): 425–444.
...-melange zones (am – Amga, kl – Kalar, tr – Tyrkanda); 7 – faults (dzh – Dzheltulak, ts – Taksakanda); 8 – thrusts; 9 – deposits and ore occurrences (1 – Kuranakhskoe, 2 – Ryabinovoe, 3 – El’kon group deposits, 4 – Lebedinskoe, 5 – Samolazovskoe, 6 – P. Pinigin, 7 – Kolchedannyi Utes; 8 – Ledyanoe; 9...
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Journal Article
Published: 01 October 2013
Russ. Geol. Geophys. (2013) 54 (10): 1236–1249.
... metallogenic epoch are found in 14 ore districts and districts, which have a potential for hosting ore deposits: El’kon (U, Au, Mo), Kuranakh (Au), Lebedinsk (asbestos, fluorite, Au), Apsakan-Nagornensky (Au, Ag, Mo), Khaikta (Mo, Au), Solov’ev (Au, Sb), Kabakta (Au), Tyrkanda (Au, Mo, W), Gonam (Au, Mo, W...
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Journal Article
Published: 01 July 2006
Russ. Geol. Geophys. (2006) 47 (7): 850–864.
... clusters and districts. The largest and most commercially important of them is the Central Aldan ore district, which is considered a regional ore-magmatic system (ROMS) within the Aldan Shield, a specific ore-magmatic province. The Aldan complex is a polychronous and polyfacies association composed...
FIGURES
Journal Article
Published: 01 April 2025
Russ. Geol. Geophys. (2025) 66 (4): 424–449.
... – Kalar mélange zone; tr – Tyrkanda mélange zone; mineragenic regions: UAR – Upper Amga; CAR – Central Aldan; TR – Tyrkanda; KKR – Ket–Kap. 1 – granite–greenstone terranes; 2 – tonalite–trondhjemite–gneiss terranes; 3 – granulite–orthogneiss terranes; 4 – granulite–paragneiss terranes; 5 – belts...
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Journal Article
Published: 01 March 2025
Russ. Geol. Geophys. (2025) 66 (3): 290–298.
.... Two large blocks separated by the Tyrkanda fault zone are traditionally distinguished therein: Central Aldan and East Aldan. Granitoid orthogneisses are widespread among the rocks of the Central Aldan block, and varying quantities of primary sedimentary rocks are identified. The structural plan...
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Journal Article
Published: 01 March 2024
Russ. Geol. Geophys. (2024) 65 (3): 302–325.
... of the shield from one side (Ket-Kap–Yuna and Tyrkanda magmatic provinces) and in its Center and in the northwest (Central Aldan, Upper Amga and Chara-Tokka magmatic provinces) from another, significantly differ in time its beginning: approximately 15 Myr ( Polin et al., 2022 ). This fact alone, if taken...
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Journal Article
Published: 01 August 2004
Russ. Geol. Geophys. (2004) 45 (8): 992–1007.
...L.V. Buzlukova; V.S. Shatsky; N.V. Sobolev Study has addressed xenoliths of the crustal rocks from the Zagadochnaya kimberlite pipe, in the Daldyn-Alakit diamondiferous district of the Yakutian kimberlite province. Most xenoliths are represented by garnet granulites (60% of the bulk of xenoliths...
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