Инд. авторы: Likhanov I.I., Kozlov P.S., Reverdatto V.V., Popov N.V.
Заглавие: 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
Библ. ссылка: Likhanov I.I., Kozlov P.S., Reverdatto V.V., Popov N.V. 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 // Doklady Earth Sciences. - 2018. - Vol.480. - Iss. 1. - P.568-572. - ISSN 1028-334X. - EISSN 1531-8354.
Внешние системы: DOI: 10.1134/S1028334X18050161; РИНЦ: 35735606; SCOPUS: 2-s2.0-85048491712; WoS: 000435361200006;
Реферат: eng: 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. © 2018, Pleiades Publishing, Ltd.
Ключевые слова: Archean; Detrital zircon; Neoarchean; Potential sources; Precambrian basement; Shear zone; Buildings; Paleoproterozoic; Geochronology;
Издано: 2018
Физ. характеристика: с.568-572
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