NEW PALEOMAGNETIC AND ISOTOPIC DATA ON THE MESOPROTEROZOIC IGNEOUS COMPLEX ON THE NORTHERN SLOPE OF THE ANABAR UPLIFT

Show simple item record

dc.contributor.author Veselovskiy R.V.
dc.contributor.author Pavlov V.E.
dc.contributor.author Petrov P.Yu.
dc.contributor.author Karpenko S.F.
dc.contributor.author Kostitsyn Yu.A.
dc.date.accessioned 2024-10-27T02:28:37Z
dc.date.available 2024-10-27T02:28:37Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=13514680
dc.identifier.citation Doklady Earth Sciences, 2006, 411, 8, 1190-1194
dc.identifier.issn 1028-334X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/46220
dc.description.abstract The existence of the Paleoproterozoic (2.1–1.5 Ga ago) supercontinent Columbia is one of the most debatable geological problems in the Late Precambrian geology. The subsequent evolution of the Siberian Craton and other ancient blocks within the supercontinent remains unclear as well. According to, the breakup of Columbia produced two supercratons. Arctica included Laurentia, Siberia, Baltica, North Australia, and North China. Atlantica was composed of Amazonia, Congo, West Africa, North Africa, and Rio de la Plata. The supercratons were subsequently integrated into the Neoproterozoic supercontinent Rodinia.
dc.subject Anabar uplift
dc.subject Mesoproterozoic
dc.title NEW PALEOMAGNETIC AND ISOTOPIC DATA ON THE MESOPROTEROZOIC IGNEOUS COMPLEX ON THE NORTHERN SLOPE OF THE ANABAR UPLIFT
dc.type Статья
dc.identifier.doi 10.1134/S1028334X06080058
dc.subject.age Precambrian::Proterozoic::Mesoproterozoic
dc.subject.age Докембрий::Протерозой::Мезопротерозойская


Files in this item

This item appears in the following Collection(s)

  • ELibrary
    Метаданные публикаций с сайта https://www.elibrary.ru

Show simple item record