gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2017-8-3-0261gtcrust-402Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSGEOCHRONOLOGY AND SR-ND ISOTOPE GEOCHEMISTRY OF LATE PALEOZOIC COLLISIONAL GRANITOIDS OF UNDINSKY COMPLEX (EASTERN TRANSBAIKAL REGION)GEOCHRONOLOGY AND SR-ND ISOTOPE GEOCHEMISTRY OF LATE PALEOZOIC COLLISIONAL GRANITOIDS OF UNDINSKY COMPLEX (EASTERN TRANSBAIKAL REGION)DrilS. I.DrilS. I.

Irkutsk

Irkutsk

NoskovaYu. V.NoskovaYu. V.

Irkutsk

Irkutsk

WangK.-L.WangK.-L.

Taipei

Taipei

BelyaevV. A.BelyaevV. A.

Irkutsk;

Taipei

Irkutsk;

Taipei

SkuzovatovS. Yu.SkuzovatovS. Yu.

Irkutsk

Irkutsk

GrigorievD. A.GrigorievD. A.

Irkutsk

Irkutsk

BelkovD. A.BelkovD. A.

Irkutsk

Irkutsk

A.P. Vinogradov Institute of Geochemistry, Siberian Branch of RASРоссияA.P. Vinogradov Institute of Geochemistry, Siberian Branch of RASRussian FederationInstitute of Earth Sciences, Academia Sinica; Department of Geosciences, National Taiwan UniversityТайваньInstitute of Earth Sciences, Academia Sinica; Department of Geosciences, National Taiwan UniversityTaiwan, Province of ChinaA.P. Vinogradov Institute of Geochemistry, Siberian Branch of RAS; Institute of Earth Sciences, Academia SinicaРоссияA.P. Vinogradov Institute of Geochemistry, Siberian Branch of RAS; Institute of Earth Sciences, Academia SinicaRussian Federation20171110201783455459Copyright © Dril S.I., Noskova Y.V., Wang K., Belyaev V.A., Skuzovatov S.Y., Grigoriev D.A., Belkov D.A., 20172017Dril S.I., Noskova Y.V., Wang K., Belyaev V.A., Skuzovatov S.Y., Grigoriev D.A., Belkov D.A.Dril S.I., Noskova Y.V., Wang K., Belyaev V.A., Skuzovatov S.Y., Grigoriev D.A., Belkov D.A.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/402

There are several geodynamic models of the Central Asian Orogenic Belt (CAOB) development [Şengör et al., 1993, Zorin, 1999; Parfenov et al., 1999, 2003; Willem et al., 2012; and others]. The Mongol-Okhotsk Orogenic Belt (MOB) represents important part of CAOB. All geodymanic models of Late Riphean to Paleozoic structures of CAOB emphasize significance of subduction processes along Northern Asian craton margin at that time. Collage of CAOB terrains formed as a result of accretion of island arc, accretionary wedge, turbidite, and continental margin terrains to the Siberian paleocontinent.

There are several geodynamic models of the Central Asian Orogenic Belt (CAOB) development [Şengör et al., 1993, Zorin, 1999; Parfenov et al., 1999, 2003; Willem et al., 2012; and others]. The Mongol-Okhotsk Orogenic Belt (MOB) represents important part of CAOB. All geodymanic models of Late Riphean to Paleozoic structures of CAOB emphasize significance of subduction processes along Northern Asian craton margin at that time. Collage of CAOB terrains formed as a result of accretion of island arc, accretionary wedge, turbidite, and continental margin terrains to the Siberian paleocontinent.

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The authors declare that there are no conflicts of interest present.