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- W164622805 abstract "Baltic shield in the Devonian was the scene of large-scale alkaline magmatism which appears in the formation of alkaline-ultramafic massifs and dykes of different composition and structure. According to modern concepts the origin of the intraplate alkaline magmatism associated with mantle plume (plume-lithosphere interaction). The appearance of plumes are connected with deep mantle processes and may be an indication of the unstable state of the inner shells of the Earth, which may make some disturbance in the generation of the geomagnetic field. In addition it is assumed that the origination of mantle plumes is associated with the processes of amalgamation and destroying of the supercontinents. Therefore, the determination of the geodynamic pattern of Fennoscandia craton in Devonian is an important geological task." @default.
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- W164622805 date "2010-05-01" @default.
- W164622805 modified "2023-09-27" @default.
- W164622805 title "Results of paleomagnetic studies of Devonian dykes of the NE part of the Baltic Shield" @default.
- W164622805 hasPublicationYear "2010" @default.
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