ГЕОМОРФОЛОГИЯ И ПОЗДНЕКАЙНОЗОЙСКАЯ ПАЛЕОГЕОГРАФИЯ РАЙОНА ОЗ. ЭЛЬГЫГЫТГЫН (ЦЕНТРАЛЬНАЯ ЧУКОТКА)
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dc.contributor.author | Глушкова О.Ю. | |
dc.contributor.author | Смирнов В.Н. | |
dc.date.accessioned | 2024-03-09T07:07:15Z | |
dc.date.available | 2024-03-09T07:07:15Z | |
dc.date.issued | 2006 | |
dc.identifier | https://elibrary.ru/item.asp?id=9213550 | |
dc.identifier.citation | Геоморфология, 2006, , 1, 57-69 | |
dc.identifier.issn | 0435-4281 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/42924 | |
dc.description.abstract | Paleogeogaphic reconstructions of the area of meteorite crater Elgygytgyn were fulfilled for several epochs in the Late Cenozoic: 3.58 million years - the fall of the meteorite; the second half of the Pliocene - tectonic activation and uprise of the Anadyr Highland; the Middle Pleistocene - accumulation of sediments of the socle terrace 35-40 meters high, marking the maximum level of Lake Elgygytgyn; the Late Pleistocene - accumulation of sediments of 9-12 meters terrace; the Early Holocene - accumulation of sediments of 2-3 meters terrace; late 5000 years - decrease of the lake's level and formation of the contemporary coastline. | |
dc.title | ГЕОМОРФОЛОГИЯ И ПОЗДНЕКАЙНОЗОЙСКАЯ ПАЛЕОГЕОГРАФИЯ РАЙОНА ОЗ. ЭЛЬГЫГЫТГЫН (ЦЕНТРАЛЬНАЯ ЧУКОТКА) | |
dc.type | Статья | |
dc.subject.udc | 551.4(1/9)(571.651) | |
dc.subject.age | Кайнозой::Четвертичная::Голоцен | |
dc.subject.age | Кайнозой::Четвертичная::Плейстоцен | |
dc.subject.age | Кайнозой::Неоген::Плиоцен |
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