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- W2344178570 abstract "The orientation of natural magnetization vector components in amphibolites and amphibole schists (magnetite up to 10 %) coincides with that of the modern magnetic field vector. Different orientations have been discovered only in quartzitic gneiss (magnetite ≤ 2 %) and regressively changed chlorite-amphibole schist. The palaeopole position determined for these rocks corresponds on the apparent pole wander path to ages of 1.95 Ga and ~1.80 Ga, respectively. Ключевые слова: палеомагнетизм, палеопротерозой, Кольский регион, Балтийский щит." @default.
- W2344178570 created "2016-06-24" @default.
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- W2344178570 date "2016-03-01" @default.
- W2344178570 modified "2023-09-27" @default.
- W2344178570 title "The first data on paleomagnetism of Palaeoproterozoic rocks of the Serpovidny structure (the Kola region, northeastern Baltic Shield)" @default.
- W2344178570 cites W229595922 @default.
- W2344178570 doi "https://doi.org/10.21443/1560-9278-2016-1/1-20-27" @default.
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