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Kyzyl-Tashtyg Deposit

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Journal Article

The Kyzyl–Tashtyg Ore Deposit of Eastern Tuva—A Standard for the Ancient Volcanogenic Formation of Pyrite-Polymetallic Ores

I.V. Gaskov
Published: 01 February 2020
Russ. Geol. Geophys. (2020) 61 (2): 139–154.
DOI: https://doi.org/10.15372/RGG2019075
...I.V. Gaskov Abstract —The Kyzyl–Tashtyg deposit and the ore field of the same name are included in the Kyzyl–Tashtyg ore cluster, which is located in the southeastern part of the Ulugoi structural-metallogenic zone. The geological section of the ore field consists of lower Cambrian terrigenous...
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View PDF for article title, The <span class="search-highlight">Kyzyl</span>–<span class="search-highlight">Tashtyg</span> Ore <span class="search-highlight">Deposit</span> of Eastern Tuva—A Standard for the Ancient Volcanogenic Formation of Pyrite-Polymetallic Ores
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Image
Schematic geological map and section of the Kyzyl-Tashtyg deposit (based on the archive materials from the Tuva Geological-Survey Expedition). 1, sands, shingles, and conglomerates (Q); 2, Tapsa Formation (Є1tp): felsic and mafic lavas and tuffs, sandstones, siltstones, and limestones; 3–6, Tumat-Taiga Formation (Є1tm): 3, basaltic-andesite and basalt porphyrites with interbeds of carbonaceous-siliceous siltstones (upper member); 4, alternating dacite porphyry, basalt and basaltic-andesite porphyrites, tuffaceous mafic and felsic rocks, tuffites, and carbonaceous-siliceous and carbonaceous-siliceous-carbonate shales (ore-hosting middle member); 5, basaltic-andesite lavas and lava breccias, often with spheroidal jointing (lower member); 6, subvolcanic bodies of rhyolite and rhyolite–dacite porphyry; 7, subvolcanic bodies of diabase porphyrites; 8, hydrothermal-metasomatic quartz–sericite and quartz–chlorite–sericite rocks and quartzites; 9, 10, ores: 9, polymetallic, 10, sulfur pyrite; 11, faults.

Schematic geological map and section of the Kyzyl-Tashtyg deposit (based on...

Published: 01 November 2022
Fig. 3. Schematic geological map and section of the Kyzyl-Tashtyg deposit (based on the archive materials from the Tuva Geological-Survey Expedition). 1 , sands, shingles, and conglomerates (Q); 2 , Tapsa Formation (Є 1 tp): felsic and mafic lavas and tuffs, sandstones, siltstones
Image
General view of the open-pit quarry of the Kyzyl-Tashtyg deposit.

General view of the open-pit quarry of the Kyzyl-Tashtyg deposit.

Published: 01 February 2020
Fig. 1. General view of the open-pit quarry of the Kyzyl-Tashtyg deposit.
Image
Schematic geological map and section of the Kyzyl–Tashtyg deposit. Based on data of the Tuva Geoexploration Expedition (Lebedev, 2012a,b). 1, sands, gravel, conglomerates (Q); 2, Tapsa Formation (Є1tp): acid and basic lavas and tuffs, sandstones, siltstones and limestones; 3–6, Tumat–Taiga Formation (Є2tm): 3, basaltic andesits and basalt porphyrites with interlayers of coaly-siliceous siltstones (upper unit); 4, alternation of dacite porphyries, basaltic and basaltic andesits porphyrites with tuffogenic formations of basic and acid composition, tuffites, coaly-siliceous and coaly-siliceous-carbonaceous shales (middle ore-bearing unit); 5, lavas and lava breccias of basaltic andesits, often with spherical jointing (lower unit); 6, subvolcanic bodies of rhyolite and rhyolite-dacite porphyries; 7, subvolcanic bodies of diabase porphyrites; 8, hydrothermal-metasomatic rocks of quartz-sericite, quartz-chlorite-sericite composition, quartzites; 9, 10, ores: 9, polymetallic, 10, sulfur-pyrite; 11, faults.

Schematic geological map and section of the Kyzyl–Tashtyg deposit. Based on...

Published: 01 February 2020
Fig. 4. Schematic geological map and section of the Kyzyl–Tashtyg deposit. Based on data of the Tuva Geoexploration Expedition ( Lebedev, 2012a , b ). 1 , sands, gravel, conglomerates (Q); 2 , Tapsa Formation (Є 1 tp): acid and basic lavas and tuffs, sandstones, siltstones and limestones; 3–6
Image
Structure of the main ore lode of the Kyzyl–Tashtyg deposit (drawing from the surface (Distanov, 1977)). 1–3, ores: 1, sulfur–pyrite, 2, copper–zinc, 3, polymetallic and baryte–polymetallic; 4–9, hydrothermal-metasomatic rocks: 4, talc-dolomite, 5, chlorite and chlorite–sericite, 6, mixed composition; 7, boudinaged quartz–sericite formations with pyrite impregnation, 8, sericite and quartz–sericite, 9, quartzites and siliceous shales; 10, faults.

Structure of the main ore lode of the Kyzyl–Tashtyg deposit (drawing from t...

Published: 01 February 2020
Fig. 5. Structure of the main ore lode of the Kyzyl–Tashtyg deposit (drawing from the surface ( Distanov, 1977 )). 1–3 , ores: 1 , sulfur–pyrite, 2 , copper–zinc, 3 , polymetallic and baryte–polymetallic; 4–9 , hydrothermal-metasomatic rocks: 4 , talc-dolomite, 5 , chlorite and chlorite
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Mineral and texture types of ores of the Kyzyl–Tashtyg deposit (half-scale). 1, sulfur–pyritic ores of massive (а), breccia-like (b) and spotted (c) texture; 2, copper–zinc ores: pocket-disseminated (а), massive-spotted (b) and striated (c) texture; 3, polymetallic ores of massive (а), banded (b) and pocket-disseminated (c) texture; 4, baryte–polymetallic ores: spotted-breccia-like (а), pocket (b) and disseminated (c) texture.

Mineral and texture types of ores of the Kyzyl–Tashtyg deposit (half-scale)...

Published: 01 February 2020
Fig. 8. Mineral and texture types of ores of the Kyzyl–Tashtyg deposit (half-scale). 1, sulfur–pyritic ores of massive ( а ), breccia-like ( b ) and spotted ( c ) texture; 2, copper–zinc ores: pocket-disseminated ( а ), massive-spotted ( b ) and striated ( c ) texture; 3, polymetallic ores
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Gold and silver content in ore grab samples of the Kyzyl-Tashtyg deposit. 1–5, ore: 1, pyrite–chalcopyrite, 2, chalcopyrite–sphalerite, 3, baryte–galena–sphalerite, 4, pyrite, 5, baryte–pyrite.

Gold and silver content in ore grab samples of the Kyzyl-Tashtyg deposit. ...

Published: 01 February 2020
Fig. 9. Gold and silver content in ore grab samples of the Kyzyl-Tashtyg deposit. 1–5 , ore: 1 , pyrite–chalcopyrite, 2 , chalcopyrite–sphalerite, 3 , baryte–galena–sphalerite, 4 , pyrite, 5 , baryte–pyrite.
Journal Article

FACTORS DETERMINING CONCENTRATION OF TRACE ELEMENTS IN ORES OF PYRITE-POLYMETALLIC DEPOSITS IN SOUTHERN SIBERIA

I.V. Gas’kov, E.G. Distanov, K.R. Kovalev
Published: 01 March 2005
Russ. Geol. Geophys. (2005) 46 (3): 303–317.
... (VHMS-type) (Kyzyl-Tashtyg deposit in Tuva; Korbalikhinskoe, Zolotushinskoe, Yubileinoe, and other deposits in Rudny Altai) and volcanosedimentary (SEDEX-type) (Kholodninskoe deposit in the northern Baikal region and Ozernoe deposit in western Transbaikalia). Comparison of major ores and ore minerals...
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View PDF for article title, FACTORS DETERMINING CONCENTRATION OF TRACE ELEMENTS IN ORES OF PYRITE-POLYMETALLIC <span class="search-highlight">DEPOSITS</span> IN SOUTHERN SIBERIA
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Journal Article

Influence of natural fulvic acids on the solubility of sulfide ores (experimental study)

S.P. Novikova, O.L. Gas’kova
Published: 01 May 2013
Russ. Geol. Geophys. (2013) 54 (5): 509–517.
DOI: https://doi.org/10.1016/j.rgg.2013.04.003
...S.P. Novikova; O.L. Gas’kova Abstract Model experiments were performed on the solubility of sulfide ores from the Kyzyl-Tashtyg deposit in distilled water and fulvic-acid (FA) solutions of different concentrations. It has been established that the oxidation of sulfide minerals in ores under...
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View PDF for article title, Influence of natural fulvic acids on the solubility of sulfide ores (experimental study)
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REE patterns in acid melts in inclusions. 1 — in quartz of andesite of Kyzyl-Tashtyg deposit; 2 — in quartz of rhyolite of Yubileinoe deposit (distribution field); 3 — in rhyolites of Kurilo-Kamchatkan island arc. Element contents are chondrite-normalized after [Boynton, 1984].

REE patterns in acid melts in inclusions. 1 — in quartz of andesite of Ky...

Published: 01 December 2006
Fig. 5. REE patterns in acid melts in inclusions. 1 — in quartz of andesite of Kyzyl-Tashtyg deposit; 2 — in quartz of rhyolite of Yubileinoe deposit (distribution field); 3 — in rhyolites of Kurilo-Kamchatkan island arc. Element contents are chondrite-normalized after [ Boynton, 1984 ].
Journal Article

Unique location of hydrothermal biota in the Lower Cambrian sedimentary-volcanogenic complex of the Kyzyl–Tashtyg ore field ( Eastern Tuva )

A.A. Terleev, V.A. Simonov, A.V. Kanygin, D.A. Tokarev, S.I. Stupakov, A.V. Kotlyarov
Published: 01 January 2014
Russ. Geol. Geophys. (2014) 55 (1): 54–61.
DOI: https://doi.org/10.1016/j.rgg.2013.12.004
...A.A. Terleev; V.A. Simonov; A.V. Kanygin; D.A. Tokarev; S.I. Stupakov; A.V. Kotlyarov Abstract Study of Early Cambrian sedimentary-volcanogenic complexes hosting the Kyzyl–Tashtyg pyrite deposit in Eastern Tuva has revealed cyanobacteria and algae that existed in zones of ore-forming hydrothermal...
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View PDF for article title, Unique location of hydrothermal biota in the Lower Cambrian sedimentary-volcanogenic complex of the <span class="search-highlight">Kyzyl</span>–<span class="search-highlight">Tashtyg</span> ore field ( Eastern Tuva )
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Image
Chemical components vs. SiO2 in MI in quartz from acid and normal effusions from pyrite deposits of Salair, Tuva, and the South Urals. 1 – MI in quartz from porphyries of pyrite deposits of the Salair ore field. The composition fields of MI in quartz from rocks of the Kyzyl-Tashtyg deposit, Eastern Tuva (Tu), and Verkhneural’skoe ore field, South Urals (Ur). The diagrams are compiled after our material with additional data borrowed from [18].

Chemical components vs. SiO 2 in MI in quartz from acid and normal effusio...

Published: 01 August 2001
Fig. 4. Chemical components vs. SiO 2 in MI in quartz from acid and normal effusions from pyrite deposits of Salair, Tuva, and the South Urals. 1 – MI in quartz from porphyries of pyrite deposits of the Salair ore field. The composition fields of MI in quartz from rocks of the Kyzyl-Tashtyg
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Proportions of gold and silver in ores of volcanogenic hydrothermal deposits. a — Kyzyl-Tashtyg deposit. Ore: 1 — copper, 2 — copper-zinc, 3 — barite-polymetallic, 4 — pyritic, 5 — barite-pyritic. b — deposits of Urskoe ore field. 1 — various mineral types of ores according to data of technological assay; ore (hand specimens): 2 — copper, 3 — barite-polymetallic, 4 — pyritic, 5 — barite-pyritic. c — Valentinovskoe deposit. Ore: 1 — copper, 2 — barite-polymetallic, 3 — pyritic, 4 — baritic, 5 — sulfidized rock. Some ore specimens are kindly donated by G.A. Tret’yakov.

Proportions of gold and silver in ores of volcanogenic hydrothermal deposit...

Published: 01 October 2004
Fig. 2. Proportions of gold and silver in ores of volcanogenic hydrothermal deposits. a — Kyzyl-Tashtyg deposit. Ore: 1 — copper, 2 — copper-zinc, 3 — barite-polymetallic, 4 — pyritic, 5 — barite-pyritic. b — deposits of Urskoe ore field. 1 — various mineral types of ores
Journal Article

EVOLUTION OF PHYSICOCHEMICAL PARAMETERS AND GEOCHEMICAL CHARACTERISTICS OF MAGMAS DURING THE DEVELOPMENT OF ORE-MAGMATIC PYRITE SYSTEMS OF RUDNY ALTAI AND TUVA

I.V. Gas’kov, V.A. Simonov, S.V. Kovyazin
Published: 01 December 2006
Russ. Geol. Geophys. (2006) 47 (12): 1360–1370.
...Fig. 5. REE patterns in acid melts in inclusions. 1 — in quartz of andesite of Kyzyl-Tashtyg deposit; 2 — in quartz of rhyolite of Yubileinoe deposit (distribution field); 3 — in rhyolites of Kurilo-Kamchatkan island arc. Element contents are chondrite-normalized after [ Boynton, 1984 ]. ...
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View PDF for article title, EVOLUTION OF PHYSICOCHEMICAL PARAMETERS AND GEOCHEMICAL CHARACTERISTICS OF MAGMAS DURING THE DEVELOPMENT OF ORE-MAGMATIC PYRITE SYSTEMS OF RUDNY ALTAI AND TUVA
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Image
Stratigraphic column of the Kyzyl-Tashtyg pyrite-polymetallic deposit. 1–5 — deposits of the Tumat-Taiga Formation (Є1t): 1 — coal-siliceous and carbonate-clay-siliceous siltstones, 2 — volcanomict sandstones and tuffs of dacite composition, 3 — amygdaloidal basalts and basic tuffs, 4 — andesite basalts and intermediate tuffs, 5 — lavas and acidic tuffs; 6, 7 — subvolcanic bodies (Є1): 6 — dacitic, 7 — rhyolitic; 8 — pyrite-polymetallic orebodies.

Stratigraphic column of the Kyzyl-Tashtyg pyrite-polymetallic deposit. 1 –...

Published: 01 December 2006
Fig. 4. Stratigraphic column of the Kyzyl-Tashtyg pyrite-polymetallic deposit. 1 – 5 — deposits of the Tumat-Taiga Formation (Є 1 t): 1 — coal-siliceous and carbonate-clay-siliceous siltstones, 2 — volcanomict sandstones and tuffs of dacite composition, 3 — amygdaloidal basalts and basic
Journal Article

GOLD AND SILVER IN ORES OF VOLCANOGENIC HYDROTHERMAL AND HYDROTHERMAL-SEDIMENTARY PYRITE-POLYMETALLIC DEPOSITS OF SIBERIA

K.R. Kovalev, E.G. Distanov, G.N. Anoshin, I.V. Gas’kov, V.A. Akimtsev, M.V. Baulina
Published: 01 October 2004
Russ. Geol. Geophys. (2004) 45 (10): 1171–1185.
...Fig. 2. Proportions of gold and silver in ores of volcanogenic hydrothermal deposits. a — Kyzyl-Tashtyg deposit. Ore: 1 — copper, 2 — copper-zinc, 3 — barite-polymetallic, 4 — pyritic, 5 — barite-pyritic. b — deposits of Urskoe ore field. 1 — various mineral types of ores...
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View PDF for article title, GOLD AND SILVER IN ORES OF VOLCANOGENIC HYDROTHERMAL AND HYDROTHERMAL-SEDIMENTARY PYRITE-POLYMETALLIC <span class="search-highlight">DEPOSITS</span> OF SIBERIA
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Journal Article

Metallogeny of Endogenous Gold in Tuva

I.V. Gaskov, S.G. Prudnikov
Published: 01 November 2022
Russ. Geol. Geophys. (2022) 63 (11): 1300–1312.
DOI: https://doi.org/10.2113/RGG20204299
...Fig. 3. Schematic geological map and section of the Kyzyl-Tashtyg deposit (based on the archive materials from the Tuva Geological-Survey Expedition). 1 , sands, shingles, and conglomerates (Q); 2 , Tapsa Formation (Є 1 tp): felsic and mafic lavas and tuffs, sandstones, siltstones...
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Geology of the Ulugoy sulfide zone; composed by Zaikov (2006) using materials of the Tuva Geoexploration Expedition. 1, metamorphosed volcanogenic-sedimentary Meso-Neoproterozoic deposits; 2–4, Tumat–Taiga rhyolite–dacite–basalt complex, lower Cambrian, Aldan stage (Є1tm): 2, lower basalt unit, 3, upper rhyolite–dacite–basalt unit, 4, undifferentiated deposits (effusives and tuffs of basic and acid composition); 5, 6, Tapsa (Syynak) basalt–andesite–rhyolite complex, lower Cambrian, Lena stage (Є1tр): 5, carbonaceous–siliceous–terrigenous–volcanogenic unit, 6, basalt–andesite–rhyolite unit; 7, carbonate–terrigenous deposits of the Tashtyghem Formation (Є3th); 8, Tannu-Ola tonalite–diorite–granite complex (Є2); 9, Bren’ granite–granosyenite complex (D2); 10, deposits and ore occurrences of pyrite–polymetallic formation (1, Kyzyl–Tashtyg; 2, Dal’nee; 3, Piritovoe; 4, Yuzhnoe); 11, faults; 12, outline of ore regions (I, Kyzyl–Tashtyg, II, Ottug–Taiga); 13, outline of the Kyzyl–Tashtyg ore field.

Geology of the Ulugoy sulfide zone; composed by Zaikov ( 2006 ) using mater...

Published: 01 February 2020
, basalt–andesite–rhyolite unit; 7 , carbonate–terrigenous deposits of the Tashtyghem Formation (Є 3 th); 8 , Tannu-Ola tonalite–diorite–granite complex (Є 2 ); 9 , Bren’ granite–granosyenite complex (D 2 ); 10 , deposits and ore occurrences of pyrite–polymetallic formation (1, Kyzyl–Tashtyg; 2
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Schematic occurrence of Au-Cu deposits in the Altai-Sayan folded area. 1 — Cu-skarn: 1 — Murzinskoe, 2 — Sinyukhinskoe, 3 — Choiskoe, 4 — Maisko-Lebedskoe, 5 — Fedorovskoe, 6 — Natal’evskoe, 7 — Tardanskoe, 8 — Khopto; 2 — porphyry Cu-Mo: 1 — Kyzyl-Chadr, 2 — Aksug, 3 — Sora, 4 — Kul’bich; 3 — pyrite-polymetallic: 1 — NE Rudny Altai (Korbalikhinskoe, Rubtsovskoe, Zolotushinskoe, Zarechenskoe, etc.), 2 — Kyzyl-Tashtyg ore field (Kyzyl-Tashtyg, Dal’nee), 3 — Salair ore field (Kvartsitovaya coniform hill, Pervomaiskoe, Aleksandrovskoe, etc.), 4 — Ursk ore field (Novourskoe, Beloklyuchevskoe, etc.).

Schematic occurrence of Au-Cu deposits in the Altai-Sayan folded area. 1 ...

Published: 01 September 2006
Fig. 1. Schematic occurrence of Au-Cu deposits in the Altai-Sayan folded area. 1 — Cu-skarn: 1 — Murzinskoe, 2 — Sinyukhinskoe, 3 — Choiskoe, 4 — Maisko-Lebedskoe, 5 — Fedorovskoe, 6 — Natal’evskoe, 7 — Tardanskoe, 8 — Khopto; 2 — porphyry Cu-Mo: 1 — Kyzyl-Chadr, 2 — Aksug, 3 — Sora, 4
Image
Location of pyrite-polymetallic deposits. 1 — Yubileinoe, 2 — Korbalikhinskoe, 3 — Zakharovskoe, 4 — Kyzyl-Tashtyg, 5 — Kholodninskoe, 6 — Ozernoe.

Location of pyrite-polymetallic deposits. 1 — Yubileinoe, 2 — Korbalikhinsk...

Published: 01 March 2005
Fig. 1. Location of pyrite-polymetallic deposits. 1 — Yubileinoe, 2 — Korbalikhinskoe, 3 — Zakharovskoe, 4 — Kyzyl-Tashtyg, 5 — Kholodninskoe, 6 — Ozernoe.