CAMPANIAN-MAASTRICHTIAN DEPOSITS IN THE FRONTAL PART OF THE OLYUTOR ZONE (SOUTHERN KORYAK UPLAND)
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dc.contributor.author | Soloviev A.V. | |
dc.contributor.author | Palechek T.N. | |
dc.contributor.author | Ledneva G.V. | |
dc.date.accessioned | 2021-01-28T11:13:03Z | |
dc.date.available | 2021-01-28T11:13:03Z | |
dc.date.issued | 2000 | |
dc.identifier | https://elibrary.ru/item.asp?id=13344429 | |
dc.identifier.citation | Stratigraphy and Geological Correlation, 2000, 8, 2, 187-194 | |
dc.identifier.issn | 0869-5938 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/23879 | |
dc.description.abstract | New dating of volcanogenic-siliceous oceanic (marginal-sea) deposits of the frontal Olyutor zone correlative with rocks of the Vatyna Group indicates that, in addition to Albian-Campanian, they include the younger Campanian-Maastrichtian horizons. The data allow us to contend that the oceanic and/or marginal-sea (Vatyna) and island-arc (Achaivayam) deposits, also dating back to the Campanian-Maastrichtian, were in lateral connections at that time. On the other hand, the analysis of new and published data shows the Campanian-Maastrichtian island-arc deposits could probably overlap the pre-Campanian oceanic and/or marginal-sea sediments without any apparent disconformity. | |
dc.subject | Campanian | en |
dc.subject | Maastrichtian | en |
dc.title | CAMPANIAN-MAASTRICHTIAN DEPOSITS IN THE FRONTAL PART OF THE OLYUTOR ZONE (SOUTHERN KORYAK UPLAND) | |
dc.type | Статья | |
dc.subject.age | Mesozoic::Cretaceous::Upper::Maastrichtian | en |
dc.subject.age | Mesozoic::Cretaceous::Upper::Campanian | en |
dc.subject.age | Мезозой::Меловая::Верхний::Маастрихтский | ru |
dc.subject.age | Мезозой::Меловая::Верхний::Кампанский | ru |
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