THE SEA OF OKHOTSK GEOTRAVERSE: TECTONOMAGMATIC EVOLUTION OF CENOZOIC EXTENSION STRUCTURES AND IMPLICATION FOR THEIR DEEP STRUCTURE

Filatova N.I.; Rodnikov A.G.

dc.contributor.author	Filatova N.I.
dc.contributor.author	Rodnikov A.G.
dc.date.accessioned	2024-11-02T11:07:52Z
dc.date.available	2024-11-02T11:07:52Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13522753
dc.identifier.citation	Doklady Earth Sciences, 2006, 411, 9, 1346-1350
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46362
dc.description.abstract	Issues of the origin of marginal seas and genesis of their igneous rocks remain controversial because of the insufficient amount of documentary information (small number of drilled holes, rare network of seismic profiles, and so on). Therefore, data on seismic profiles carried out within the framework of the Geotraverse International Project are of great significance. The geotraverse extends from the margin of Asia (Sikhote Alin) to the northwestern periphery of the Pacific plate and includes large Cenozoic extension structures, such as the Tatar continental rift and the South Kuril marginal basin.
dc.subject	sea of Okhotsk
dc.title	THE SEA OF OKHOTSK GEOTRAVERSE: TECTONOMAGMATIC EVOLUTION OF CENOZOIC EXTENSION STRUCTURES AND IMPLICATION FOR THEIR DEEP STRUCTURE
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06090030