STRUCTURE OF ALDAN-MAYA SEDIMENTARY BASIN

E.P. Razvozzhaeva

Аннотация


The boundaries and inner structure of the Aldan-Maya sedimentary basin located in the east of the North Asian craton are specified on basis of seismographic and geological evidence synthesis.


Ключевые слова


seismic reflection section; riphean; Kyllakh zone; Yudoma-Maya semigraben.

Литература


Berzin A.G., Obolkin A.P., Sevostyanov S.Yu., Egoshin A.A., Dyakonova V.A. New Geological Data on the Aldan Mayan Depression. Otechestvennaya geologiya, 2011, no. 6, pp. 21–26. (In Russ.).

Varnavsky V.G., Kuznetsov V.E.The Riphean-Vendian-Cambrian Sedimentogenesis Zone at the Southeastern Margin of the North Asian Craton: the Geostructural Setting and Regionalization. Tikhookeanskaya geologiya, 2011, vol. 31, no. 5, pp. 67–79. (In Russ.).

Goroschko M.V., Malyshev Yu.Ph., Kirillov V.E. Metallogeniya urana Dal’nego Vostoka Rossii (Uranium Metallogeny of the Russian Far East). Moscow: Nauka Publ., 2006. 372 p. (In Russ.).

Razvozzhaeva E.P. Seismostratigraphic Model of the Aladan-Maya Sedimentary Basin, Southeastern Siberian Platform. Tikhookeanskaya geologiya, 2020, vol. 39, no. 6, pp. 25–47. (In Russ.).


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