gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2017-8-3-0272gtcrust-413Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSEARLY NEOPROTEROZOIC CRUST FORMATON IN THE DZABKHAN MICROCONTINENT, CENTRAL ASIAN OROGENIC BELTEARLY NEOPROTEROZOIC CRUST FORMATON IN THE DZABKHAN MICROCONTINENT, CENTRAL ASIAN OROGENIC BELTKovachV. P.KovachV. P.

St. Petersburg

St. Petersburg

KozakovI. K.KozakovI. K.

St. Petersburg

St. Petersburg

KrönerA.KrönerA.

Beijing 1000373;

55099 Mainz

Beijing 100037;

55099 Mainz

SalnikovaE. B.SalnikovaE. B.

St. Petersburg

St. Petersburg

WangK.-L.WangK.-L.

Taipei 11529;

Department of Geosciences, Taipei 106

Taipei 11529;

Department of Geosciences, Taipei 106

LeeH.-Y.LeeH.-Y.

Taipei 11529

Taipei 11529

ChungS.-L.ChungS.-L.

Taipei 11529;

Department of Geosciences, Taipei 106

Taipei 11529;

Department of Geosciences, Taipei 106

Institute of Precambrian Geology and Geochronology of RASРоссияInstitute of Precambrian Geology and Geochronology of RASRussian FederationBeijing SHRIMP Centre, Institute of Geology, Chinese Academy of Geological Sciences; Institute of Geosciences, University of MainzКитайBeijing SHRIMP Centre, Institute of Geology, Chinese Academy of Geological Sciences; Institute of Geosciences, University of MainzChinaInstitute of Earth Sciences, Academia Sinica; National Taiwan UniversityКитайInstitute of Earth Sciences, Academia Sinica; National Taiwan UniversityChinaInstitute of Earth Sciences, Academia SinicaКитайInstitute of Earth Sciences, Academia SinicaChina20171210201783499501Copyright © Kovach V.P., Kozakov I.K., Kröner A., Salnikova E.B., Wang K., Lee H., Chung S., 20172017Kovach V.P., Kozakov I.K., Kröner A., Salnikova E.B., Wang K., Lee H., Chung S.Kovach V.P., Kozakov I.K., Kröner A., Salnikova E.B., Wang K., Lee H., Chung S.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/413

The Dzabkhan microcontinent was defined by [Mossakovsky et al., 1994] as a cratonic terrane with an early Precambrian basement that combines highgrade metamorphic complexes of the Songino, Dzabkhan, Otgon, Baidarik, Ider and Jargalant Blocks. However, early Precambrian ages have so far only been recognized in the Baidarik and Ider blocks [Kozakov et al., 2007, 2011; Kröner et al., 2015].

The Dzabkhan microcontinent was defined by [Mossakovsky et al., 1994] as a cratonic terrane with an early Precambrian basement that combines highgrade metamorphic complexes of the Songino, Dzabkhan, Otgon, Baidarik, Ider and Jargalant Blocks. However, early Precambrian ages have so far only been recognized in the Baidarik and Ider blocks [Kozakov et al., 2007, 2011; Kröner et al., 2015].

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