Email this article Relationship between magmatic, metamorphic and hydrothermal processes within the Baikal-Muya terrane (Eastern Siberia): constraints from a high-precision geochronological study of the Kedrovsky granitoid massif
- Authors: Chugaev A.V.1, Chernyshev I.V.1, Rytsk E.Y.2, Salnikova E.B.2, Nosova A.A.1, Travin A.V.3,4, Kotov A.B.2, Fedoseenko A.M.2, Anisimova I.V.2
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Affiliations:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry of the Russian Academy of Sciences
- Institute of Precambrian Geology and Geochronology of the Russian Academy of Sciences
- Novosibirsk State University
- Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences
- Issue: Vol 489, No 3 (2019)
- Pages: 292-297
- Section: Geochemistry
- URL: https://journals.eco-vector.com/0869-5652/article/view/18597
- DOI: https://doi.org/10.31857/S0869-56524893292-297
- ID: 18597
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Abstract
High-precision dating of granitoids is significant for identification the ages of the main stages of crust formation in various blocks of the continental crust. In this work, we dating the Kedrovskiy diorite-granodiorite massif localized within the South Muya block of the Baikal-Muya accretion terrane (BMT) (Eastern Siberia) among the Neoproterozoic gabbroids of the Kedrovskiy complex and metasedimentary rocks of the Kedrovskaya Formation. The results of U-Pb (ID TIMS) and 39Ar-40Ar geochronological studies of the Kedrovskiy massif are discussed. The formation of the massif (781 ± 3 Ma) occurred at an early stage formation of the Proterozoic continental crust of BMT during accretion of Baikalids with the Siberian craton. A later thermal event (626 ± 11 Ma) of the Ediacaran stage evolution BMT is reflected in the formation of of biotite-quartz-feldspar veins that cut through the granitoids of the Kedrovka massif. The obtained geochronological data show that the gold mineralization of the Kedrovskiy deposit (273 ± 4 Ma) was not generated by the Kedrovskiy massif granitoids.
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About the authors
A. V. Chugaev
Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry of the Russian Academy of Sciences
Author for correspondence.
Email: vassachav@mail.ru
Russian Federation, 35, Staromonetny, Moscow, 119017
I. V. Chernyshev
Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry of the Russian Academy of Sciences
Email: vassachav@mail.ru
Academician of the Russian Academy of Sciences
Russian Federation, 35, Staromonetny, Moscow, 119017E. Y. Rytsk
Institute of Precambrian Geology and Geochronology of the Russian Academy of Sciences
Email: vassachav@mail.ru
Russian Federation, 2, Makarova embankment, St.Petersburg, 199034
E. B. Salnikova
Institute of Precambrian Geology and Geochronology of the Russian Academy of Sciences
Email: vassachav@mail.ru
Russian Federation, 2, Makarova embankment, St.Petersburg, 199034
A. A. Nosova
Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry of the Russian Academy of Sciences
Email: vassachav@mail.ru
Russian Federation, 35, Staromonetny, Moscow, 119017
A. V. Travin
Novosibirsk State University; Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences
Email: vassachav@mail.ru
Russian Federation, 1, Pirogova street, Novosibirsk, 630090; 3, Koptyug prospect, Novosibirsk, 630090
A. B. Kotov
Institute of Precambrian Geology and Geochronology of the Russian Academy of Sciences
Email: vassachav@mail.ru
Russian Federation, 2, Makarova embankment, St.Petersburg, 199034
A. M. Fedoseenko
Institute of Precambrian Geology and Geochronology of the Russian Academy of Sciences
Email: vassachav@mail.ru
Russian Federation, 2, Makarova embankment, St.Petersburg, 199034
I. V. Anisimova
Institute of Precambrian Geology and Geochronology of the Russian Academy of Sciences
Email: vassachav@mail.ru
Russian Federation, 2, Makarova embankment, St.Petersburg, 199034
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