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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Principais autores:	V. V. Shcherbakova, R. V. Veselovskiy, G. V. Zhidkov, N. A. Aphinogenova, A. V. Samsonov, A. V. Stepanova, M. A. Smirnov
Formato:	Artigo
Idioma:	Inglês
Publicado em:	Kazan Federal University 2024-01-01
coleção:	Учёные записки Казанского университета: Серия Естественные науки
Assuntos:	archean great dyke of the kola peninsula paleomagnetic pole paleointensity thellier–coe method
Acesso em linha:	https://uzakuesc.elpub.ru/jour/article/view/36
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