GEODYNAMIC FORMATION REGIME OF ROCKS OF THE UDOKAN COMPLEX

dc.contributor.author	Abramov B.N.
dc.date.accessioned	2022-07-25T04:36:25Z
dc.date.available	2022-07-25T04:36:25Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13461977
dc.identifier.citation	Doklady Earth Sciences, 2004, 398, 7, 922-924
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38390
dc.description.abstract	The similarity of the Early Proterozoic Udokan sedimentary basin to complexes of passive continental margins was established during analysis of the geodynamic environments of the southern framework of the Siberian Craton. The objective of this work is to show that the lower complex formed under conditions of an active continental margin that is of importance for paleogeodynamic reconstructions.
dc.title	GEODYNAMIC FORMATION REGIME OF ROCKS OF THE UDOKAN COMPLEX
dc.type	Статья

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