BIOFACIES OF UPPER JURASSIC AND LOWER CRETACEOUS SEDIMENTS OF CENTRAL WEST SIBERIA
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dc.contributor.author | Marinov V.A. | |
dc.contributor.author | Meledina S.V. | |
dc.contributor.author | Dzyuba O.S. | |
dc.contributor.author | Urman O.S. | |
dc.contributor.author | Yazikova O.V. | |
dc.contributor.author | Luchinina V.A. | |
dc.contributor.author | Zamirailova A.G. | |
dc.contributor.author | Fomin A.N. | |
dc.date.accessioned | 2024-07-20T12:14:01Z | |
dc.date.available | 2024-07-20T12:14:01Z | |
dc.date.issued | 2006 | |
dc.identifier | https://elibrary.ru/item.asp?id=13525899 | |
dc.identifier.citation | Stratigraphy and Geological Correlation, 2006, 14, 4, 418-432 | |
dc.identifier.issn | 0869-5938 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/44491 | |
dc.description.abstract | Paleontological study of Upper Jurassic and Lower Cretaceous sediments recovered by boreholes in the Agan-Vakh and Nadym-Vengapur interfluves clarified environments of their deposition. As is shown, influx of siliciclastic material to central areas of the West Siberian sea basin varied through time. Taxonomic composition and ecological structure of nektonic and benthic fossil assemblages are analyzed and considered in terms of environmental factors such as hydrodynamics, aeration, temperature, and salinity of seawater. © MAIK "Nauka/Interperiodica" 2006. | |
dc.subject | BIOFACIES ANALYSIS | |
dc.subject | LOWER CRETACEOUS | |
dc.subject | UPPER JURASSIC | |
dc.subject | WEST SIBERIA | |
dc.title | BIOFACIES OF UPPER JURASSIC AND LOWER CRETACEOUS SEDIMENTS OF CENTRAL WEST SIBERIA | |
dc.type | Статья | |
dc.identifier.doi | 10.1134/S0869593806040058 | |
dc.subject.age | Мезозой::Меловая | |
dc.subject.age | Мезозой::Юрская | |
dc.subject.age | Mesozoic::Cretaceous | |
dc.subject.age | Mesozoic::Jurassic |
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