THE GOTHENBURG MAGNETIC EXCURSION IN THE BLACK SEA SEDIMENTS

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dc.contributor.author Demidenko E.L.
dc.contributor.author Faustov S.S.
dc.contributor.author Nikolaev S.D.
dc.date.accessioned 2020-12-30T04:52:55Z
dc.date.available 2020-12-30T04:52:55Z
dc.date.issued 1998
dc.identifier https://elibrary.ru/item.asp?id=13279405
dc.identifier.citation Stratigraphy and Geological Correlation, 1998, , 2, 180-188
dc.identifier.issn 0869-5938
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/21774
dc.description.abstract The late Pleistocene-Holocene deposits are studied in 12 piston-core sections sampled at the continental slope and in the deep part of the Black Sea within the Adler-Tuapse test area. In four of these sections, the Neoeuxinian beds revealed paleomagnetic anomalies confined to the base of the hydrotroilite member1 and presumably induced by the Gothenburg excursion. Correlation with available data on the western region of the Black Sea, where the Gothenburg excursion was first identified, substantiate synchronism of hydrotroilite deposits in eastern and western areas of the sea and elucidate principal trends in the paleogeographic evolution of the Black Sea in the late Pleistocene-Holocene time.
dc.subject Pleistocene en
dc.subject Holocene en
dc.title THE GOTHENBURG MAGNETIC EXCURSION IN THE BLACK SEA SEDIMENTS
dc.type Статья
dc.subject.age Cenozoic::Quaternary::Pleistocene en
dc.subject.age Cenozoic::Quaternary::Holocene en
dc.subject.age Кайнозой::Четвертичная::Плейстоцен ru
dc.subject.age Кайнозой::Четвертичная::Голоцен ru


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