THE TUNAICHA FORMATION AND ITS AGE ANALOGUES, SOUTHERN SAKHALIN

dc.contributor.author	Zharov A.E.
dc.contributor.author	Gal'versen V.G.
dc.contributor.author	Serova M.Ya.
dc.contributor.author	Fot'yanova L.I.
dc.date.accessioned	2022-03-24T08:31:14Z
dc.date.available	2022-03-24T08:31:14Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13451171
dc.identifier.citation	Stratigraphy and Geological Correlation, 2004, 12, 4, 406-417
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/36648
dc.description.abstract	The terrigenous Tunaicha Formation overlying dislocated Mesozoic basement was recently established at the base of Cenozoic deposits in southeastern Sakhalin (the Aniva and Dolinsk districts). The formation stratotype is in the Cape Tunaicha area (Bay of Mordvinov). The formation is attributed to the terminal middle-upper Eocene based on benthic and associated sparse planktonic foraminifers and on coeval floral assemblage. The Tunaicha period corresponded to formation time of new sedimentary basins in southeastern Sakhalin and Hokkaido.
dc.title	THE TUNAICHA FORMATION AND ITS AGE ANALOGUES, SOUTHERN SAKHALIN
dc.type	Статья
dc.subject.age	Cenozoic::Paleogene::Eocene
dc.subject.age	Кайнозой::Палеоген::Эоцен	ru

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