We present the results of magneto-mineralogical and paleomagnetic studies of the Middle and Upper Devonian section of the Pavlovsky quarry located in the Central Devonian field of the East European Platform. The magneto-mineralogical composition of the studied deposits is complex, with up to 4-6 magnetic phases recorded in them. The section is subdivided into several zones by magnetic mineralogy and by the observed characteristic components of natural remanent magnetization, however, the boundaries of zones do not coincide with each other. Two interpretable characteristic components are distinguished in the section. The bipolar Devonian component DE+DW and the anomalous component S, which paleomagnetic poles are consistent with the poles of a number of sections of Devonian rocks of the East European Platform.
N.V. Salnaia (Wed,) studied this question.
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