Ayano-Shevlinsky pericratonic basin of the Siberian Platform, Far East of Russia
https://doi.org/10.52349/0869-7892_2022_91_31-44
Abstract
The Ayano-Shevlinsky pericratonic basin along the southeastern margin of the Aldan-Stanovy shield, the Siberian Platform, contains isolated outcrops of variegated Upper Riphean, Vendian, Cambrian, Ordovician, Silurian, Devonian and Carboniferous clastic-carbonate deposits, basalts, granitoids and gabbroids of similar formational type as the deposits of the Yudoma-Maya pericratonic basin located to the north. Stratigraphic hiatuses of varying durations are common throughout the section. Deposits are arranged in folds of different morphologies, from brachiform to isoclinal.
About the Author
V. Yu. Zabrodin
Institute of Tectonics and Geophysics FEB RAS (ITiG FEB RAS)
Russian Federation
Russian Federation
Zabrodin Vladimir Yur’evich – Doctor of Geological and Mineralogical Sciences, Leading Researcher
65 Ul. Kim Yu Chen, Khabarovsk, 680000
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For citations:
Zabrodin V.Yu. Ayano-Shevlinsky pericratonic basin of the Siberian Platform, Far East of Russia. Regional Geology and Metallogeny. 2022;(91):31-44. (In Russ.) https://doi.org/10.52349/0869-7892_2022_91_31-44
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