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Shishkhid Belt

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Journal Article
Published: 01 July 2011
Russ. Geol. Geophys. (2011) 52 (7): 685–700.
... continental margin and the Shishkhid island arc. Coeval analogs of the above structures are also reconstructed in the Yenisei Range and Baikal–Muya belt. This suggests that the Sarkhoi belt was initially localized along the margin of the Neoproterozoic Siberian continent. But the exotic origin...
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The Precambrian Tuva–Mongolian and Dzavhan massifs. Granitoids and young de...
Published: 01 July 2011
Fig. 1. The Precambrian Tuva–Mongolian and Dzavhan massifs. Granitoids and young deposits are not shown. 1 , Siberian Craton; 2 , Vendian–Cambrian carbonate cover of Precambrian massifs; 3 , Paleozoic belt; 4 , undivided Precambrian complexes; 5 – 8 , Neoproterozoic (<800 Ma) complexes
Journal Article
Published: 01 January 2013
Russ. Geol. Geophys. (2013) 54 (1): 34–43.
... . Kuzmichev , A.B. , 1991 . The geologic structure and stratigraphy of the Bilin subzone of the Shishkhid ophiolite belt (eastern Tuva and northern Mongolia) , in: The Late Precambrian and Early Paleozoic of Siberia. The Siberian Platform and Its Framing [in Russian] . IGiG SO AN SSSR , Novosibirsk...
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Journal Article
Published: 01 June 2003
Russ. Geol. Geophys. (2003) 44 (6): 531–541.
.... Khomentovsky , A.S. Gibsher , and G.A. Karlova , 104 – 123 , UIGGM , Novosibirsk , 1990 . 23. Kuzmichev , A.B. , and M.I. Buyakaite , Rb-Sr geochronology of volcanics of the Shishkhid ophiolite belt (Western Hovsgol region) , Dokl. RAN , 335 , 3 , 340 – 344 , 1994 . 24...
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Journal Article
Published: 01 January 2021
Russ. Geol. Geophys. (2021) 62 (1): 109–120.
... area is determined by its position among the structures of different ages in the eastern part of the Altai–Sayan region of the Central Asian fold belt and adjacent Precambrian structures of the Siberian craton ( Fig. 1 ). This tectonic scheme for the region presents a large number of terranes...
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Tectonic position and geologic structure of Late Vendian–Early Cambrian str...
Published: 01 May 2011
Fig. 1. Tectonic position and geologic structure of Late Vendian–Early Cambrian structure-lithologic complexes in the Tannu-Ola zone. A , Schematic structure of the Central Asian fold belt ( Yarmolyuk et al., 2003 ). Tectonic structures: 1 , Hercynian and Indosinian; 2 , zones of Vendian
Journal Article
Published: 01 January 2007
Journal of the Geological Society (2007) 164 (1): 31–47.
...-resolution ion microprobe (SHRIMP) U–Pb age of 800 ± 3 Ma. The Shishkhid ophiolite collided with the Tuva–Mongolian microcontinent at the end of the Neoproterozoic ( Kuzmichev et al . 2005 ). In the Baikal–Muya belt a plagiogranite in island arc volcanic rocks has a U–Pb zircon age of 812 ± 19 Ma ( Ritsk...
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Journal Article
Published: 01 September 2019
Russ. Geol. Geophys. (2019) 60 (9): 1008–1017.
... basins ( Fig. 1 ). Volcanic fields in the Central Asian orogenic belt are mainly localized within systems of rift basins along the Amur plate boundary. The volcanic fields among orogenic complexes consist of large (up to n ·1000 km 3 ) lava plateaus, cones, and flows. Cenozoic tectonic...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 December 2016
Lithosphere (2016) 8 (6): 729–750.
...Uyanga Bold; James L. Crowley; Emily F. Smith; Oyungerel Sambuu; Francis A. Macdonald Abstract The Zavkhan terrane is a Proterozoic cratonic fragment in southwestern Mongolia that forms the core of the Central Asian orogenic belt. We provide new geologic and U-Pb zircon geochronologic constraints...
Journal Article
Published: 01 May 2011
Russ. Geol. Geophys. (2011) 52 (5): 503–516.
...Fig. 1. Tectonic position and geologic structure of Late Vendian–Early Cambrian structure-lithologic complexes in the Tannu-Ola zone. A , Schematic structure of the Central Asian fold belt ( Yarmolyuk et al., 2003 ). Tectonic structures: 1 , Hercynian and Indosinian; 2 , zones of Vendian...
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Journal Article
Published: 01 March 2004
Russ. Geol. Geophys. (2004) 45 (3): 295–309.
... , ibid. , 169 – 171 . 78. Kuz’michev , A.B. , Geological structure and stratigraphy of the Bilinskaya subzone of the Shishkhid ophiolite belt, eastern Tuva and northern Mongolia , in The Late Precambrian and Early Paleozoic of Siberia. Siberian Platform and its framing [in Russian], 130...
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Journal Article
Published: 01 October 2006
Russ. Geol. Geophys. (2006) 47 (10): 1045–1055.
... is valid. Different authors outline the Barguzin microcontinent in different ways. According to Zonenshain et al. [ 2 ], it is composed of the Olokit structure, Baikal-Muya belt, and the southern Barguzin zone ( Fig. 1 ). Belichenko et al. [ 3 ] extend the microcontinent southward, to Kyakhta, where...
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Journal Article
Published: 01 November 2022
Russ. Geol. Geophys. (2022) 63 (11): 1300–1312.
..., Novosibirsk State University 2022 Novosibirsk State University gold metallogeny deposits ore gold dating Tuva The territory of Tyva occupies the southeastern part of the Altai–Sayan folded area, which is part of the Central Asian Orogenic Belt (CAOB). It borders the West Sayan structures...
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Journal Article
Published: 01 January 2016
Russ. Geol. Geophys. (2016) 57 (1): 127–140.
... suprasubduction ophiolites of the Flin Flon greenstone belt in the Trans-Hudson Orogon (Canadian Shield) and within the Payson ophiolites in Central Arizona ( Dann, 1991 ). Neoarchean boninites (2.7–2.8 Ga) are known from the Fennoscandian and Canadian Shields ( Shchipansky, 2008 ). Namely, they occur...
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Journal Article
Published: 01 August 2022
Russ. Geol. Geophys. (2022) 63 (8): 901–914.
..., it is assumed that the carbonate rocks of the Tunka ridge are part of the Vendian–Cambrian sedimentary cover of the Tuva–Mongolian massif ( Belichenko et al., 1986 , 2003 ; Boos, 1991 ) located west of the Tunka ridge and being a large tectonic segment in the Caledonides of the Central Asian Orogenic Belt...
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Journal Article
Journal: GSA Bulletin
Published: 24 March 2022
GSA Bulletin (2022) 134 (11-12): 3099–3112.
... Orogenic Belt, this integrated study focuses on Cambrian tholeiitic to calc-alkaline plutons in the Barleik-Mayile-Saleinuohai area of West Junggar, NW China. Zircon U-Pb results of felsic plutons reveal a wide range (511–488 Ma) of ages with older ages up to 514–511 Ma. The felsic rocks exhibit variable...
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Journal Article
Published: 01 January 2016
Russ. Geol. Geophys. (2016) 57 (1): 69–81.
... of the Central Asian Orogenic Belt, including eastern Altai–Sayan, Transbaikalia, and Northern Mongolia. Comparison of the igneous complexes of modern and ancient ensimatic and ensialic island arcs in the subduction zone forms a basis for possible geodynamic scenarios of the subduction zone magmatism...
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Journal Article
Published: 01 October 2013
Russ. Geol. Geophys. (2013) 54 (10): 1135–1149.
...- and trace-element compositions were inferred from chemical and isotope data for Late Precambrian sediments in the Anamakit–Muya zone of the Baikal–Muya belt southeast of the craton (Ust‘-Kelyana and Tuluya sequences), including preliminary U–Pb LA-ICP-MS ages of detrital zircons and Sm–Nd data...
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Journal Article
Published: 01 February 2019
Russ. Geol. Geophys. (2019) 60 (2): 133–149.
...-adjacent part of the Central Asian mobile belt ( Betekhtin, 1946 ; Belichenko, 1969 ; Osokin et al., 1989 ; Koneva et al., 1998 ; etc.). All ore occurrences tend to distribute within thick volcanosedimentary sequences of the terranes (Khamardaban, Olkhon, and Ikat), whose degree of metamorphic change...
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Journal Article
Journal: Economic Geology
Published: 01 August 2005
Economic Geology (2005) 100 (5): 1055–1066.
...) at 25 °C as a function of pH— Lara Duro, Fatima El Aamrani, Miquel Rovira, Javier Giménez, Ignasi Casas, Joan de Pablo, and Jordi Bruno 1284 Acid mine drainage in the Iberian Pyrite Belt (Odiel river watershed, Huelva, SW Spain): Geochemistry, mineralogy and environmental implications— Javier...