Abstract
New results for the Carboniferous rocks (Moscovian, Bashkirian and Visean stages) from four sections of the Russian Platform are presented. Primary magnetite and secondary hematite are the main carriers of magnetization in the studied rocks. All isolated NRM components generally correspond to the geomagnetic field of reversed polarity. Only in the rocks of the Visean stage a small zone of normal polarity is found. Widespread late Paleozoic remagnetization of the Carboniferous rocks of the Russian Platform is detected.
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Acknowledgements
We are grateful to A. Yu. Kazansky for criticism and constructive comments, A. A. Kosterov for help in translating the text into English.
Scientific research was carried out at VNIGRI and the Research Park of St. Petersburg State University: Center for Geo-Environmental Research and Modeling (GEOMODEL); Center for Microscopy and Microanalysis; Center for X-ray Diffraction Studies.
The work was supported by the Russian Foundation for Basic Research under project no. 16-05-00603a.
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Iosifidi, A.G. et al. (2019). Carboniferous of the Russian Platform: Paleomagnetic Data. In: Nurgaliev, D., Shcherbakov, V., Kosterov, A., Spassov, S. (eds) Recent Advances in Rock Magnetism, Environmental Magnetism and Paleomagnetism. Springer Geophysics. Springer, Cham. https://doi.org/10.1007/978-3-319-90437-5_4
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