NEW DATA ON AGE AND NATURE OF CARBONIZATION WITHIN SOUTHERN FLANK OF THE BAIKAL LEDGE OF THE SIBERIAN CRATON BASEMENT
https://doi.org/10.5800/GT-2017-8-3-0257
Abstract
The Baikal ledge rock formations in the Siberian craton structure are included in the Akitkan mobile belt which is considered as the Late Paleoproterozoic independent island arc system moved up to the ancient basement during the terrains amalgamation 1.91–2.00 Ga ago (Fig. 1) [Rosen, 2003; Gladkochub et al., 2009; Didenko et al., 2013].
About the Authors
Yu. V. Danilova
Institute of the Earth's Crust, Siberian Branch of RAS
Russian Federation
Irkutsk
Russian Federation
Irkutsk
V. B. Savelyeva
Institute of the Earth's Crust, Siberian Branch of RAS
Russian Federation
Irkutsk
Russian Federation
Irkutsk
T. G. Shumilova
Institute of Geology, Komi Scientific Center, Ural Branch of RAS
Russian Federation
Syktyvkar
Russian Federation
Syktyvkar
A. V. Ivanov
Institute of the Earth's Crust, Siberian Branch of RAS
Russian Federation
Irkutsk
Russian Federation
Irkutsk
B. S. Danilov
Institute of the Earth's Crust, Siberian Branch of RAS
Russian Federation
Irkutsk
Russian Federation
Irkutsk
E. P. Bazarova
Institute of the Earth's Crust, Siberian Branch of RAS
Russian Federation
Irkutsk
Russian Federation
Irkutsk
References
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Review
For citations:
Danilova Yu.V., Savelyeva V.B., Shumilova T.G., Ivanov A.V., Danilov B.S., Bazarova E.P. NEW DATA ON AGE AND NATURE OF CARBONIZATION WITHIN SOUTHERN FLANK OF THE BAIKAL LEDGE OF THE SIBERIAN CRATON BASEMENT. Geodynamics & Tectonophysics. 2017;8(3):441-444. https://doi.org/10.5800/GT-2017-8-3-0257
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