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Selenga-Stanovoy Terrane

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Tectonic map of the southeastern margin of the North Asian craton. Data by ...
Published: 01 July 2018
fold belt; 7 , Cenozoic loose sediments; 8 , major faults. Letters indicate tectonic blocks (terranes) in superterranes of the Central Asian Fold Belt. SelengaStanovoi superterrane: AG, Amazar–Gilyui; MG, Mogocha; TN, Tungir. Dzhugdzur–Stanovoi superterrane: BR, Bryanta; DM, Dambuki; IL, Ilikan; KP
Image
Schematic occurrence of layered ultrabasic-basic massifs in the <span class="search-highlight">Selenga</span>-Sta...
Published: 10 December 2007
massifs; 2 — Dzhugdzhur-Stanovoy superterrane; 3 , 4 — Selenga-Stanovoy (West Stanovoy) superterrane: 3 — Mogocha block, 4 — Urkan block; 5 — Dzheltulak suture zone; 6 — Kerulen-Argun-Mamyn terrane; 7 — Mongolo-Okhotsk fold belt; 8 — faults: a — major, b — subsidiary; massifs: 1
Journal Article
Published: 01 March 2004
Russ. Geol. Geophys. (2004) 45 (3): 347–362.
...M.E. Kazimirovsky Detailed petrochemical characteristics of Paleozoic (Cambrian(?)-Silurian and Carboniferous) granitoids of the West Stanovoy structure-formational zone (SFZ) (central Selenga-Stanovoy mountain area (SSMA), Transbaikalia) are presented. The Early Paleozoic granitoids...
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Journal Article
Published: 01 March 2020
Russ. Geol. Geophys. (2020) 61 (3): 286–302.
... , V.P. , Sal’nikova , E.B. , Yarmolyuk , V.V. , Velikoslavinskii , S.D. , Yakovleva , S.Z. , Plotkina , Yu.V. , 2015 . Granitoids of the Olekma Complex in the SelengaStanovoi super-terrane of the central Asian mobile belt: Age and tectonic position . Dokl. Earth Sci. 464 ( 1...
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Journal Article
Published: 01 July 2018
Russ. Geol. Geophys. (2018) 59 (7): 709–717.
... fold belt; 7 , Cenozoic loose sediments; 8 , major faults. Letters indicate tectonic blocks (terranes) in superterranes of the Central Asian Fold Belt. SelengaStanovoi superterrane: AG, Amazar–Gilyui; MG, Mogocha; TN, Tungir. Dzhugdzur–Stanovoi superterrane: BR, Bryanta; DM, Dambuki; IL, Ilikan; KP...
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Journal Article
Published: 01 October 2013
Russ. Geol. Geophys. (2013) 54 (10): 1236–1249.
... of the Siberian Platform ( Fig. 1 ). The CAFB and the investigated part of the framing of the Siberian Platform to the west and south include the Caledonian SelengaStanovoi, Late Paleozoic–Early Cretaceous Mongol-Okhotsk orogenic belts and the Argun–Mamyn microcontinent (Karsakov and Zhao Chunjing, 2001...
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Journal Article
Published: 01 March 2014
Russ. Geol. Geophys. (2014) 55 (3): 335–348.
... of the granitoids of the Amudzhikan complex (134–132 Ma) located within the SelengaStanovoy superterrane is the same as the age of the granitoids of the Upper Amur and Burinda complexes (140– 127 Ma) widespread within the Argun terrane ( Sorokin et al., 2004 , 2009 , 2010a ). The wide occurrence of the Late...
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Journal Article
Published: 01 December 2016
Russ. Geol. Geophys. (2016) 57 (12): 1688–1695.
... . Early Cretaceous collisional granitoids of the Drevnestanovoi complex from the SelengaStanovoi superterrane of the Central Asian Mobile Belt . Dokl. Earth Sci. 456 ( 2 ), 649 – 654 . Kravchinsky , V.A. , Sorokin , A.A. , 2001 . Paleomagnetism of Devonian rocks in the Ol’doi terrane...
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Journal Article
Published: 01 October 2016
Russ. Geol. Geophys. (2016) 57 (10): 1389–1397.
..., upon the granitoids of the Tynda–Bakaran complex, and upon the Precambrian metamorphic rocks of the Zverevo block of the Stanovoi structural suture. This suture separates the Aldan Shield of the Siberian craton from the Dzhugdzhur–Stanovoi and SelengaStanovoi superterranes in the Central Asian...
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Journal Article
Published: 10 December 2007
Russ. Geol. Geophys. (2007) 48 (12): 1026–1036.
... massifs; 2 — Dzhugdzhur-Stanovoy superterrane; 3 , 4 — Selenga-Stanovoy (West Stanovoy) superterrane: 3 — Mogocha block, 4 — Urkan block; 5 — Dzheltulak suture zone; 6 — Kerulen-Argun-Mamyn terrane; 7 — Mongolo-Okhotsk fold belt; 8 — faults: a — major, b — subsidiary; massifs: 1...
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Image
Schematic map of metamorphic-core complexes in western Transbaikalia ( a ),...
Published: 01 November 2016
, Zagan, M, Malkhan, S(U-U), Selenga (Ulan-Ude), Ya, Yablonovyi. b : 1 , Siberian Platform; 2–6 , terranes of the Central Asian Orogenic Belt: 2 , island-arc terranes, 3 , backarc-basin terranes, 4 , metamorphic terranes, 5 , turbidite basin terranes, 6 , accretionary-wedge terranes; 7 , Mongol
Journal Article
Published: 01 February 2022
Russ. Geol. Geophys. (2022) 63 (2): 184–192.
.../S0016852113050026 . Kotov , A.B. , Larin , A.M. , Sal’nikova , E.B. , Velikoslavinskii , S.D. , Glebovitskii , V.A. , Sorokin , A.A. , Yakovleva , S.Z. , Anisimova , I.V. , 2014 . Early Cretaceous collisional granitoids of the Drevnestanovoi complex from the Selenga-Stanovoi...
FIGURES
Journal Article
Published: 01 May 2010
Russ. Geol. Geophys. (2010) 51 (5): 461–481.
... the Yablonovyi–Malkhan and West Stanovoi zones of metamorphic and cratonic terranes. The latter, in turn, border the Mongolia–Okhotsk suture in the southeast and the associated large shear zones that separate the terranes from the Argun cratonic terrane and from the belt of Middle–Late Paleozoic turbidite...
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Journal Article
Published: 01 July 2012
Russ. Geol. Geophys. (2012) 53 (7): 636–648.
...I.V. Buchko; A.A. Sorokin; V.A. Ponomarchuk; A.E. Izokh Abstract The Lukinda dunite–troctolite–gabbro massif in the SelengaStanovoy superterrane on the southeastern framing of the Siberian Platform was earlier considered Precambrian. The performed 40 Ar/ 39 Ar dating of the massif plagioclase...
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Journal Article
Published: 01 July 2017
Russ. Geol. Geophys. (2017) 58 (7): 822–835.
... ). The Aga–Shilka terrane has sedimentary (Late Paleozoic–Mesozoic) and sedimentary-metamorphic (Riphean–Paleozoic) layers up to 3–4 km (sometimes, 5–6 km) in thickness. The SelengaStanovoi superterrane is formed predominantly by Upper Archean–Lower Proterozoic granite-gneisses (upper 4–5 km thick layer...
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Journal Article
Published: 01 May 2009
Russ. Geol. Geophys. (2009) 50 (5): 485–499.
... production from concentrations of radioactive elements measured in situ for the upper crust; for the middle crust, we used mean U and Th abundances in high-grade Precambrian rocks exposed within the Aldan–Stanovoi and Sinian–Korean shields and in Precambrian terranes (microcontinents) of the Central Asian...
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Present tectonic framework of Uda–Vitim island arc system among Precambrian...
Published: 01 May 2010
Fig. 1. Present tectonic framework of Uda–Vitim island arc system among Precambrian and Paleozoic structures of Transbaikalia. 1 , Siberian craton; 2 , terranes: Archean and Early Proterozoic cratonic ( a ): West Baikal (WB), Sharyzhalgai (SZ), West Stanovoi (WS), Argun (Arg), Muya–Stanovoi (MS
Journal Article
Published: 01 October 2006
Russ. Geol. Geophys. (2006) 47 (10): 1045–1055.
.... [ 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, MO — Mongolian-Okhotsk belt...
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Journal Article
Published: 01 May 2007
Russ. Geol. Geophys. (2007) 48 (5): 442–455.
... anomalies ( Fig. 1 , b). Thus, the Western Stanovoy (Geological map…, 1986) (or the Selenga-Stanovoy ( Krasny et al., 1999 )) geoblock in northeastern Transbaikalia does not belong to the Stanovoy terrane. It is more reasonable to relate it to the Baikal-Vitim terrane ( Gusev and Khain, 1995 ), which...
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Journal Article
Published: 01 December 2011
Russ. Geol. Geophys. (2011) 52 (12): 1672–1679.
... Cretaceous coal-bearing continental sediments. It overlies the Paleozoic and older basement rocks with a sharp angular unconformity. The Strelka and Malaya Tynda sedimentary basins, which are shallower, are located inside the SelengaStanovoi orogenic belt, at its boundary with the Mongol–Okhotsk belt...
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