THE MAJOR CYCLICITY OF MESOZOIC EPICONTINENTAL SEDIMENTATION AND GEODYNAMIC EVENTS IN THE ADJACENT ACTIVE OCEANIC REGION

dc.contributor.author	Markevich P.V.
dc.contributor.author	Khanchuk A.I.
dc.contributor.author	Kemkin I.V.
dc.contributor.author	Golozubov V.V.
dc.contributor.author	Zakharov Yu.D.
dc.date.accessioned	2024-11-02T11:07:49Z
dc.date.available	2024-11-02T11:07:49Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13522508
dc.identifier.citation	Doklady Earth Sciences, 2006, 407, 2, 184-187
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46352
dc.description.abstract	Mesozoic rocks of Sikhote Alin are well studied. However, they have been considered so far separately for the tectonically passive eastern margin of the Sino-Korean craton (hereafter, in the west) and for the active adjacent area of the Paleopacific, framing the craton from the east. Sedimentation in the west was not correlated with Mesozoic geodynamic events in the east. This statement is substantiated in the present paper.
dc.subject	Sikhote Alin
dc.title	THE MAJOR CYCLICITY OF MESOZOIC EPICONTINENTAL SEDIMENTATION AND GEODYNAMIC EVENTS IN THE ADJACENT ACTIVE OCEANIC REGION
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X0602005X

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