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Paleomagnetism of the Great Dyke of the Kola Peninsula (2.68 Ga): New Evidence of Ultra-Low Paleointensity of the Earth’s Magnetic Field in the Late Archean

Giant mafic dykes are the key markers of the Earth’s evolution in the Precambrian and have been the subject of extensive research. This article presents the results of the paleomagnetic, rock-magnetic, and paleointensity Banc studies of the Great Dyke of the Kola Peninsula (2.68 Ga). The mean paleom...

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Bibliografische gegevens
Hoofdauteurs: V. V. Shcherbakova, R. V. Veselovskiy, G. V. Zhidkov, N. A. Aphinogenova, A. V. Samsonov, A. V. Stepanova, M. A. Smirnov
Formaat: Artigo
Taal:Inglês
Gepubliceerd in: Kazan Federal University 2024-01-01
Reeks:Учёные записки Казанского университета: Серия Естественные науки
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Online toegang:https://uzakuesc.elpub.ru/jour/article/view/36
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