gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2017-8-3-0280gtcrust-421Research ArticleПАЛЕОГЕОДИНАМИКАPALEOGEODYNAMICSDETRITAL ZIRCON AGES AND SOURCES OF MATERIAL FOR THE LOWER CAMBRIAN DEPOSITS OF THE MEL'GIN TROUGH OF THE BUREYA CONTINENTAL MASSIFDETRITAL ZIRCON AGES AND SOURCES OF MATERIAL FOR THE LOWER CAMBRIAN DEPOSITS OF THE MEL'GIN TROUGH OF THE BUREYA CONTINENTAL MASSIFOvchinnikovR. O.OvchinnikovR. O.

Blagoveshchensk

Blagoveshchensk

SorokinA. A.SorokinA. A.

Blagoveshchensk

Blagoveshchensk

Institute of Geology and Nature Management, Far East Branch of RASРоссияInstitute of Geology and Nature Management, Far East Branch of RASRussian Federation20171210201783525527Copyright © Ovchinnikov R.O., Sorokin A.A., 20172017Ovchinnikov R.O., Sorokin A.A.Ovchinnikov R.O., Sorokin A.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/421

Bureya continental massif is one of the largest continental massifs in the eastern part of the Central Asian orogenic belt (CAOB) (Fig. 1), and knowledge of its geological structure is of fundamental importance in understanding the history of its formation.

Bureya continental massif is one of the largest continental massifs in the eastern part of the Central Asian orogenic belt (CAOB) (Fig. 1), and knowledge of its geological structure is of fundamental importance in understanding the history of its formation.

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