Article # 11_2015 | submitted on 01/26/2015 displayed on website on 03/23/2015 |
20 p. | Margulis L.S., Kovnir B.D., Serezhenkov S.V., Nafikov I.F. |
Structure of southeastern pericratonal plunging of Siberian Platform | |
The structural-stratigraphic complexes, the main structural elements and the main stages in the formation of the sedimentary cover of southeastern pericratonal plunging of the Siberian Platform are analyzed. The overwhelming part of the cover is complicated with Riphean and Vendian-Cambrian deposits. The main orogeny era, especially the final Late Cimmerian, led to the consolidation of sediments on the overwhelming eastern part of the pericratonal, formation of Sette-Daban folded zone and Aldan-May "residual" pericratonal depression at its extreme west.
Keywords: Riphean deposits, pericratonal plunging, Sette-Daban area, Aldan-May depression, Siberian Platform. |
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article citation | Margulis L.S., Kovnir B.D., Serezhenkov S.V., Nafikov I.F. Stroenie yugo-vostochnogo perikratonnogo pogruzheniya Sibirskoy platformy [Structure of southeastern pericratonal plunging of Siberian Platform]. Neftegazovaya Geologiya. Teoriya I Praktika, 2015, vol. 10, no. 1, available at: http://www.ngtp.ru/rub/4/11_2015.pdf |
DOI | https://doi.org/10.17353/2070-5379/11_2015 |
Berzin A.G., Obolkin A.P., Sevast'yanov S.Yu., Egoshin A.A., D'yakonova V.A. Novye dannye po geologii Aldano-Mayskogo progiba [New data on the geology of the Aldan-Maya depression]. Otechestvennaya geologiya, 2011, no. 6, p. 21-26. |