Nature and Age of Detrital Zircons from Rocks of the Shear Zone: The Problem of Occurrence of the Archean Basement in the Transangarian Yenisei Ridge


статья в журнале
Авторы: Likhanov I.I.     Kozlov P.S.     Reverdatto V.V.     Popov N.V.   (ИНГГ СО РАН)  
дата публикации: 2018
реферат:
Petrogeochemical and geochronological study of boudined quartzite sandstones and tonalites, as well as host amphibolites, in the shear zone showed that potential sources of detrital zircons were Neoarchean-Paleoproterozoic rocks of the Angara-Kan block and products of their metamorphism. Interpretation of the available data does not confirm the inferred presence of the Early Precambrian basement of the Siberian Craton in the Transangara region.
первоисточник: Doklady Earth Sciences
том: 1
страницы: 568-572
ISBN:
ISSN:
внешние ссылки:
WoS   WoS (цитирование)
DOI  
РИНЦ SPIN  
Scopus  

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полный текст статьи

des-2018-480-1-568