NEW DATA ON THE GEOLOGY OF ITURUP ISLAND (KURIL ISLAND ARC)

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dc.contributor.author Vitukhin D.I.
dc.contributor.author Oreshkina T.V.
dc.contributor.author Pushcharovskii Yu.M.
dc.contributor.author Tsukanov N.V.
dc.date.accessioned 2020-11-30T07:42:19Z
dc.date.available 2020-11-30T07:42:19Z
dc.date.issued 1996
dc.identifier https://elibrary.ru/item.asp?id=13237752
dc.identifier.citation Stratigraphy and Geological Correlation, 1996, , 6, 580-593
dc.identifier.issn 0869-5938
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/19955
dc.description.abstract The geology of Iturup Island, which is the largest one in the Kuril island arc, has not yet been considered in any special publications. The island is marked by the occurrence of typical island-arc deposits of the middle Miocene-Pliocene age that show complicated facial variability. Based on the analysis of siliceous plankton assemblages (diatoms, radiolarians), the age of several formations distinguished in both the Iturup and Kunashir islands has been determined more accurately. Paleontologically dated levels of transgressive events correlative with similar levels in the Neogene section of the Karaginskii Island (eastern Kamchatka), the reference one in the Far East, have been defined.
dc.subject Neogene en
dc.subject Miocene en
dc.subject Pliocene en
dc.title NEW DATA ON THE GEOLOGY OF ITURUP ISLAND (KURIL ISLAND ARC)
dc.type Статья
dc.subject.age Кайнозой::Неоген ru
dc.subject.age Cenozoic::Neogene::Miocene en
dc.subject.age Cenozoic::Neogene::Pliocene en
dc.subject.age Cenozoic::Neogene en
dc.subject.age Кайнозой::Неоген::Миоцен ru
dc.subject.age Кайнозой::Неоген::Плиоцен ru


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