THE LOWER PALEOCENE OF THE KRONOTSKII PENINSULA, EASTERN KAMCHATKA

dc.contributor.authorSerova M.Ya.
dc.date.accessioned2022-03-24T08:31:14Z
dc.date.available2022-03-24T08:31:14Z
dc.date.issued2004
dc.description.abstractUpper Cretaceous and Lower Paleocene deposits of the Kronotskii Peninsula and their foraminiferal and radiolarian faunas are considered. As is shown, marine sedimentation during the Late Cretaceous - Early Paleocene was continuous in the Kronotskii and other peninsulas of the eastern and western Kamchatka, in the Koryak Upland, and Sakhalin Island.
dc.identifierhttps://www.elibrary.ru/item.asp?id=13451506
dc.identifier.citationStratigraphy and Geological Correlation, 2004, 12, 5, 514-522
dc.identifier.issn0869-5938
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/36649
dc.subjectPaleocene
dc.subject.ageCenozoic::Paleogene::Paleocene
dc.subject.ageКайнозой::Палеоген::Палеоценru
dc.titleTHE LOWER PALEOCENE OF THE KRONOTSKII PENINSULA, EASTERN KAMCHATKA
dc.typeСтатья

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