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Tuva-Mongolian Massif

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Journal Article
Published: 01 December 2011
Russ. Geol. Geophys. (2011) 52 (12): 1662–1671.
... sedimentary basin localized on the margin of the TuvaMongolian massif in the setting of an island-arc system. The carbonate formation proceeding in the passive tectonic regime was interrupted in the second half of the Late Riphean, after the origin of an active continental margin near the TuvaMongolian...
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a , Simplified geological map of the <span class="search-highlight">Tuva</span>–<span class="search-highlight">Mongolian</span> <span class="search-highlight">massif</span> (TMM) and the Tu...
Published: 01 August 2022
Fig. 1. a , Simplified geological map of the TuvaMongolian massif (TMM) and the Tunka terrane, after Kuz’michev ( 2004 ): 1 , Riphean folded strata of the TMM; 2 , Kitoi zone; 3 , Vendian–Cambrian carbonate rocks of the TMM; 4 , Riphean carbonate rocks; 5 , Archean granite-gneisses
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Schematic geological map of the northern <span class="search-highlight">Tuva</span>–<span class="search-highlight">Mongolian</span> <span class="search-highlight">massif</span>.  1 , schist...
Published: 01 January 2013
Fig. 1. Schematic geological map of the northern TuvaMongolian massif. 1 , schists of the Gargan block; 2, Neoproterozoic cover of the Gargan block; 3 , Dunzhugur island arc (mainly basement rocks); 4 , sedimentary complexes associated with the Dunzhugur arc; 5 , volcanic and sedimentary
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Schematic geologic structure of the <span class="search-highlight">Tuva</span>–<span class="search-highlight">Mongolian</span> <span class="search-highlight">massif</span>, compiled after  ...
Published: 01 December 2011
Fig. 1. Schematic geologic structure of the TuvaMongolian massif, compiled after Kuz’michev (2004) with supplements. 1 , Vendian–Cambrian deposits of the Khamsara, Dzhida, Khamar-Daban, and Tunka terranes; 2 , Vendian–Cambrian carbonate deposits of the Bokson and Hövsgöl Groups; 3
Journal Article
Published: 01 August 2022
Russ. Geol. Geophys. (2022) 63 (8): 901–914.
...Fig. 1. a , Simplified geological map of the TuvaMongolian massif (TMM) and the Tunka terrane, after Kuz’michev ( 2004 ): 1 , Riphean folded strata of the TMM; 2 , Kitoi zone; 3 , Vendian–Cambrian carbonate rocks of the TMM; 4 , Riphean carbonate rocks; 5 , Archean granite-gneisses...
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Journal Article
Published: 01 July 2019
Russ. Geol. Geophys. (2019) 60 (7): 720–734.
...I.V. Karmysheva; V.G. Vladimirov; R.A. Shelepaev; S.N. Rudnev; V.A. Yakovlev; D.V. Semenova Abstract —The Bayan-Kol gabbro–granite association has been recognized within the West Sangilen fragment of collision zone in the northwestern framing of the TuvaMongolian massif, and its composition, age...
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Journal Article
Published: 01 December 2018
Russ. Geol. Geophys. (2018) 59 (12): 1660–1678.
... that they formed during the Early Paleozoic collisional orogeny in the TuvaMongolian massif at the Cambrian–Ordovician boundary. The granites of the Kystarys complex are moderately alkaline high-K rocks and are enriched in Zr, Nb, Y, and REE; therefore, they are classified as postcollisional, transitional...
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Journal Article
Published: 01 June 2018
Russ. Geol. Geophys. (2018) 59 (6): 652–672.
... of sedimentation, and provenances of metaterrigenous-carbonate complexes of the Derba block (Sayan Group), West Sangilen block of the TuvaMongolian massif (Erzin and Moren complexes), and the Khamar-Daban terrane (Slyudyanka Group) suggests that these structures were a single Vendian continental margin...
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Series: Geological Society, London, Memoirs
Published: 01 January 2011
DOI: 10.1144/M36.23
EISBN: 9781862394117
... Abstract The Bokson Group (Gr.) forms the platform cover in northern part of the Tuva-Mongolian Massif, south of the East Sayan Mountains. Widespread diamictites occur in the lower part of the Bokson Gr., in the Zabit Formation (Fm.). These contain erratic, faceted and striated stones along...
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Schematic occurrence of the Tunka terrane metavolcanics.  1 , Cenozoic depo...
Published: 01 September 2009
-Daban terrane: 9 , 10 , Khangarul Group: 9 , Bezymyanskaya Formation, 10 , Kharagol Formation, 11 , Slyudyanka Group; 12 , TuvaMongolian massif; 13 , thrust boundary of the Tunka terrane and TuvaMongolian massif; 14 , predicted boundary of the Tunka and Khamar-Daban terranes; 15 , sampling
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Schematic occurrence of metavolcanics of the Tunka terrane.  1 , Cenozoic d...
Published: 01 February 2013
– 11 , Khamar-Daban terrane: 9 – 10 , Khangarul Group: 9 , Bezymyanskaya Formation, 10 , Kharagol Formation, 11 , Slyudyanka Group; 12 , TuvaMongolian massif; 13 , thrust boundary between the Tunka terrane and the TuvaMongolian massif; 14 , predicted boundary between the Tunka and Khamar-Daban
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Localization of gold deposits in geologic structures of eastern <span class="search-highlight">Tuva</span>.  1 , ...
Published: 01 December 2008
Fig. 1. Localization of gold deposits in geologic structures of eastern Tuva. 1 , 2 — volcanosedimentary deposits: 1 — D–C, 2 — (Є–S; 3 — volcanoterrigenous-car-bonate deposits of the Tuva-Mongolian massif, V–(Є; 4 — intrusive rocks of the Kaa-Khem batholith; 5 — faults of: a — Kaa
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Structure-geologic position of the Despen volcanic rocks.  1 , Cenozoic sed...
Published: 01 June 2021
deposits of the Serlig and Irbitei formations, 7 , native-copper occurrence of the Sook–Sair group of occurrences, 8 , faults, 9 , section line. Inset a : Schematic map of the tectonic structure of eastern Tuva, compiled after Kuz’michev ( 2004 ) and Mongush et al. ( 2011 ). 1 , TuvaMongolian massif
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Schematic geologic structure of the Oka prism in the basin of the Yakhoshop...
Published: 01 January 2013
of the TuvaMongolian massif; 8 , faults; 9 , sampling localities; 10 , Quaternary deposits.
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ε Nd –age diagram for Late Vendian–Early Paleozoic granitoid associations o...
Published: 01 September 2015
; 3 , evolution field for the Nd isotope composition of rocks from the Tannu-Ola zone of Eastern Tuva, after Mongush et al. (2011) ; 4 , evolution field for the Nd isotope composition of supracrustal complexes of the TuvaMongolian massif, after Kozakov et al. (2003) ; 5 , evolution trend
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The regularities of manifestation of the Devonian within-plate magmatism on...
Published: 01 August 2010
triple junction); 3 , faults; 4 , Siberian Platform; 5 , Paleoasian ocean; 6 , outlines of the TuvaMongolian massif (T-Mm), after Kuz’michev (2004) . Rectangle marks the area of Devonian magmatism in the Kropotkin Ridge region (see Figs. 2 and 3 ).
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Schematic geological map of western Sangilen (southeastern <span class="search-highlight">Tuva</span>), after Vla...
Published: 01 July 2019
), Kokmolgarga (ko); 10 , Agardag suture; 11 , boundaries of nappes; 12 , faults; 13 , objects of study: 1, Bayan-Kol gabbro–granite pluton, 2, areas of mingling dikes. Inset: 1 , Siberian craton; 2 , Precambrian terranes: 1, TuvaMongolian massif, 2, Dzavhan massif, 3, Tarbagatai massif); 3 , Paleozoids
Journal Article
Published: 01 January 2013
Russ. Geol. Geophys. (2013) 54 (1): 34–43.
...Fig. 1. Schematic geological map of the northern TuvaMongolian massif. 1 , schists of the Gargan block; 2, Neoproterozoic cover of the Gargan block; 3 , Dunzhugur island arc (mainly basement rocks); 4 , sedimentary complexes associated with the Dunzhugur arc; 5 , volcanic and sedimentary...
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Journal Article
Published: 01 October 2020
Russ. Geol. Geophys. (2020) 61 (10): 1088–1108.
... in their composition were due to the melting of thick crust, whose isotopic heterogeneity was caused by the different contributions of a more ancient crustal source. The crust of the TuvaMongolian terrane made the main contribution to the formation of the potassic granitoids of the Bren’ massif (450 Ma), marking...
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Journal Article
Published: 01 July 2011
Russ. Geol. Geophys. (2011) 52 (7): 685–700.
... parts of the TuvaMongolian and Dzavhan massifs. The ~1500 km long Sarkhoi–Dzavhan volcanic belt is a fragment of the Neoproterozoic active continental margin separated from the continent. In the Middle Neoproterozoic, the geodynamic system also included the Oka accretionary prism joining the Sarkhoi...
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