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Dzhida Terrane

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ε Nd  age of clastic metasediments in Khamar-Daban and <span class="search-highlight">Dzhida</span> <span class="search-highlight">terranes</span>.  1–...
Published: 01 October 2017
Fig. 10. ε Nd age of clastic metasediments in Khamar-Daban and Dzhida terranes. 1–4 , Khamar-Daban terrane: Sludyanka Group ( 1 ), Khangarul Group ( Kovach et al., 2013 ) ( 2 ), Kornilova Formation, Khamar-Daban Group ( 3 ), Shubutui Formation, Khamar-Daban Group ( 4 ); 5 , Dzhida terrane, Zun
Journal Article
Published: 01 October 2017
Russ. Geol. Geophys. (2017) 58 (10): 1188–1198.
...Fig. 10. ε Nd age of clastic metasediments in Khamar-Daban and Dzhida terranes. 1–4 , Khamar-Daban terrane: Sludyanka Group ( 1 ), Khangarul Group ( Kovach et al., 2013 ) ( 2 ), Kornilova Formation, Khamar-Daban Group ( 3 ), Shubutui Formation, Khamar-Daban Group ( 4 ); 5 , Dzhida terrane, Zun...
FIGURES | View All (10)
Journal Article
Published: 01 January 2000
Russ. Geol. Geophys. (2000) 41 (1): 98–108.
... the Riphean Tuva-Mongolian and Caledonian Dzhida terranes. The depth at which crustal xenoliths were entrained into ascending alkali-basalt melts may have been controlled by the master fault that bounds the northern steep side of the rift valley and reaches the crust-mantle boundary beneath the Zun-Murin...
FIGURES | View All (6)
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Metamorphism in eastern surroundings of Tuva-Mongolia <span class="search-highlight">terrane</span>. Facies conto...
Published: 01 June 2003
Fig. 4. Metamorphism in eastern surroundings of Tuva-Mongolia terrane. Facies contour lines: I — garnet, II — staurolite-andalusite (central Khamar-Daban) and staurolite-disthene (Tunka and Dzhida terranes), III — sillimanite, IV — sillimanite-feldspar, V — hypersthene. Abbreviations stand
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Schematic occurrence of <span class="search-highlight">terranes</span> and metamorphism zones in the Baikal–Hövsg...
Published: 01 September 2009
Fig. 1. Schematic occurrence of terranes and metamorphism zones in the Baikal–Hövsgöl region. Isogrades of different types of metamorphism: I, garnet; II, staurolite-andalusite (Central Khamar-Daban) and staurolite-disthene (Tunka and Dzhida terranes); III, sillimanite; IV, K-feldspathic; V
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Paleotectonic reconstruction of the Cambrian evolution of the western margi...
Published: 01 April 2013
of the back part of the arc and back arc basin deposits; 8, Late Cambrian accretionary complexes; 9, spreading zones, triangles show the position of MORB in the structure of the Dzhida terrane, circles show the location of WPOIB in the structure of the Dzhida terrane, thin dots show the reconstructed
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Geodynamic zoning of Transbaikalia, modified after ( Sklyarov et al., 1997 ...
Published: 01 January 2020
belt: Late Precambrian Khamar-Daban island arc terrane ( 4 ); latest Cambrian–Cambrian Dzhida terrane ( 5 ), Barguzin microcontinent ( 6 ); Cambrian–Ordovician Eravnoe terrane; 8–10 , Mongol–Okhotsk orogenic belt: Hentiyn island arc terrane ( 8 ), mylonite gneiss domes (metamorphic core complexes) ( 9
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Variations in compositions of xenoliths across the strike of Tunka rift val...
Published: 01 January 2000
of fractional crystallization of melts beneath the steep northern shoulder of Tunka rift valley; 6 – upper crust of Dzhida terrane; 7 – zone of reduced conditions; 8 – zone of oxidized condition; 9 – crust of Tuva-Mongolian terrane (boundary between the terranes may be off the master fault); 10
Journal Article
Published: 01 June 2003
Russ. Geol. Geophys. (2003) 44 (6): 531–541.
...Fig. 4. Metamorphism in eastern surroundings of Tuva-Mongolia terrane. Facies contour lines: I — garnet, II — staurolite-andalusite (central Khamar-Daban) and staurolite-disthene (Tunka and Dzhida terranes), III — sillimanite, IV — sillimanite-feldspar, V — hypersthene. Abbreviations stand...
FIGURES | View All (4)
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Paleogeodynamic reconstructions of the Vendian–Early Paleozoic active margi...
Published: 01 January 2016
Mongolian terrane. Dark dots with arrows depict the reconstructed location and direction of movement of the Dzhida seamount on the oceanic plate toward a subduction zone at the Dzhida island arc, based on paleomagnetic data ( Gordienko and Mikhaltsov, 2001 ).
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Schematic occurrence of <span class="search-highlight">terranes</span> in the Baikal–Hövsgöl region. <span class="search-highlight">Terranes</span>: Dz...
Published: 01 February 2013
Fig. 1. Schematic occurrence of terranes in the Baikal–Hövsgöl region. Terranes: Dzh, Dzhida, KhD, Khamar-Daban, Tn, Tunka, Kt, Belaya–Kitoi (Kitoikin); TM, Tuva–Mongolian microcontinent; SC, Sharyshalgai uplift of the Siberian craton. The area from Fig. 2 is outlined.
Journal Article
Published: 01 June 2022
Russ. Geol. Geophys. (2022) 63 (6): 649–663.
... a large area, even beyond the study region. For example, the Cambrian sandstones of the Dzhida terrane contain representative zircon populations with ages of 580 and 630 Ma ( Reznitskii et al., 2018 ). The first data obtained in studying the Cambrian coarse-grained terrigenous rocks of the Systyg-Khem...
FIGURES | View All (10)
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Sketch map of <span class="search-highlight">terranes</span> in Baikal–Hövsgol region. Abbreviations stand for na...
Published: 01 October 2017
Fig. 1. Sketch map of terranes in Baikal–Hövsgol region. Abbreviations stand for names of tectonic units: Khamar-Daban (KhD), Tunka (Tn), Dzhida (Dzh), Olkhon (Ol), Ikat (Ik), Eravnoe (Er) terranes; Tuva–Mongolia microcontinent (TM) and Siberian craton (SC); Zun-Muren (ZM) thrust; Utulik basin
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Simplified tectonic map of <span class="search-highlight">terranes</span> in the Baikal–Hövsgöl region, with refe...
Published: 01 September 2017
Fig. 1. Simplified tectonic map of terranes in the Baikal–Hövsgöl region, with reference to ( Kuzmichev, 2004 ; Mongush et al., 2011b ). Abbreviations stand for names of tectonic units: terranes (KhS, Khemchik–Systygk-Kem; Khm, Khamsara; ET, East Tuva; Ta, Tannu-Ola; Tn, Tunka; KhD, Khamar-Daban
Journal Article
Published: 01 September 2009
Russ. Geol. Geophys. (2009) 50 (9): 779–788.
...Fig. 1. Schematic occurrence of terranes and metamorphism zones in the Baikal–Hövsgöl region. Isogrades of different types of metamorphism: I, garnet; II, staurolite-andalusite (Central Khamar-Daban) and staurolite-disthene (Tunka and Dzhida terranes); III, sillimanite; IV, K-feldspathic; V...
FIGURES | View All (11)
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A scheme of relationship of <span class="search-highlight">terranes</span> of the Baikal mountain area with the o...
Published: 01 October 2006
microcontinent: 7 — after Zonenshain et al. [ 2 ], 8 — after Belichenko et al. [ 3 ], 9 — after Khomentovsky [ 4 ]. Terranes: Dz — Dzhida, Er — Eravna, Ik — Ikat, Br — Barguzin, Ol — Ol’khon, Kh — Khamar-Daban, TM — Tuvino-Mongolian, BM — Baikal-Muya, Ok — Olokit, WS — West Stanovoi. SC — Siberian craton
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Generalized geology of Tuva-Mongolia <span class="search-highlight">terrane</span> and its surroundings.  1  — Ce...
Published: 01 June 2003
terranes surrounding Tuva-Mongolia terrane, denoted by abbreviations: DZ — Dzhida, TN — Tunka, KD — Khamar-Daban, TS — Tuva system of island arcs, WSN — West Sangilen, ST — Shutkhulai, BK — Belaya-Kitoi (Kitoikin), OZ — Ozerny; small letters denote fragments of sedimentary cover: bk — Bokson, hv — Hovsgol
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A synoptic scheme of the Tuvino-Mongolian massif and its framing.  1  — Cen...
Published: 01 October 2006
— Early Paleozoic massif-framing terranes; 7 — isotope data (Ma); 8 — overthrusts; 9 — nondifferentiated faults. Terranes: Dz — Dzhida, Tn — Tunka, Kh — Khamar-Daban, WSn — West Sangilen, Sh — Shutkhulai, BK — Belaya-Kitoi, Oz — Ozerny, TS — Tuvinian system of island arcs. Fragments of sedimentary
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Scheme of <span class="search-highlight">terranes</span> location in the southern margins of the Siberian platfor...
Published: 01 April 2021
accretionary prism (ОL); terranes: 5 , Baikal-Muya (BМ) and Dzhida (DZH); 6 , Khamar Daban–Ol’khon (KHD); 7 , Barguzin (BR); 8 , Ikat (IK); 9 , thrusts: а , established, b, projected. Encircled digits = locations of the studied rock associations: 1, Medvezhy and 2, Tyya formations, 3, Ny-urundukan
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Paleogeodynamic reconstruction of the Vendian–early Paleozoic oceanic basin...
Published: 01 March 2019
reconstruction after ( Metelkin, 2013 ). 1 , cratonal terranes (ТМ, Tuva-Mongolian; G, Gargan; B, Baikal; CM, Central Mongolian; MS, Muya-Stanovoi), 2 , Siberian continent’s platform complex; 3 , sedimentary basins of the continent’s passive margin; 4 , Neoproterozoic accretionary orogen; 5 , island-arcs