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Matyushkin A. V., Balagansky V. V.
The first data on paleomagnetism of Palaeoproterozoic rocks of the Serpovidny structure (the Kola region, northeastern Baltic Shield)
DOI: 10.21443/1560-9278-2016-1/1-20-27
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
Keywords: palaeomagnetism, Palaeoproterozoic, the Kola region, the Baltic Shield
Printed reference: Matyushkin A. V., Balagansky V. V. The first data on paleomagnetism of Palaeoproterozoic rocks of the Serpovidny structure (the Kola region, northeastern Baltic Shield) // Vestnik of MSTU. 2016. V. 19, No 1. P. 20-27.
Electronic reference: Matyushkin A. V., Balagansky V. V. The first data on paleomagnetism of Palaeoproterozoic rocks of the Serpovidny structure (the Kola region, northeastern Baltic Shield) // Vestnik of MSTU. 2016. V. 19, No 1. P. 20-27. URL: http://vestnik.mstu.edu.ru/v19_1_1n64/3_Matyushkin_20_27.pdf.
