Rodionov V.P.



Graduated from the Geophysical Faculty of the Moscow Institute of Petrochemical and Gas Industry (1960), specialization "geophysics".
PhD in Geological and Mineralogical Sciences, Senior Researcher.
Leading researcher of the laboratory of magnetostratigraphy and paleomagnetic reconstructions, VNIGRI.
Area of scientific interest: magnetism of rocks, paleomagnetic studies of the Paleozoic and Precambrian deposits of the Siberian platform and its framing.
Author of 72 publications.
Stratigraphy and lithology
Section editor – PhD in geology and mineralogy Kirichkova A.I.
Article # 43_2014 submitted on 10/08/2014 displayed on website on 10/18/2014
21 p.
pdf  Paleomagnetic research of the Paleozoic sections of Polar Urals (Paga River)
Paleomagnetic studying of Cambrian-Ordovician-Devonian collection of Paleozoic deposits of the Paga River valley has been carried out. The results of paleomagnetic research show a two-component structure of natural residual magnetization (NRM). The identified typical components are postfolded. The estimates of horizontal turns of structures are executed. The possible model of magnetic reversal of the studied deposits has been realized.

Keywords: paleomagnetic vectors, anisotropy of magnetic susceptibility, overthrust, Polar Urals.
article citation Sal'naya N.V., Popov V.V., Rodionov V.P., Yakubson A.M., Iosifidi A.G. Paleomagnitnye issledovaniya paleozoyskikh otlozheniy Pripolyarnogo Urala, reka Paga [Paleomagnetic research of the Paleozoic sections of Polar Urals (Paga River)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2014, vol. 9, no. 4, available at: http://www.ngtp.ru/rub/2/43_2014.pdf
DOI https://doi.org/10.17353/2070-5379/43_2014
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Stratigraphy and lithology
Section editor – PhD in geology and mineralogy Kirichkova A.I.
Article # 38_2010 submitted on 08/23/2010 displayed on website on 09/03/2010
17 p.
pdf  Key magneto-stratigraphic sequence of the Lower Ordovician deposits, north-western Siberian platform
Key magnetostratigraphic sequence of the Lower Ordovician is constructed, including Nya Tremadoc horizon, Ugorsky and Kimaisky horizons of the Arenigo. Sequence on the right bank of the Kulyumbe river (Iltyksk formation, represented by carbonate rocks) has been studied. The character of geomagnetic field variation in the Early Ordovician (notably Tremadoc and Areniga boundary) is traced. Stratigraphic level of the geomagnetic polarity change in the sequence-stratotype of the Lower Ordovician on the Kulyumbe river provides the broad prospects for the synchronization of this boundary according to paleomagnetic data not only within the territory of Siberian plate, but also within its framework.
Key words: polarity, magnetostratigraphy, Lower Ordovician, the Kulyumbe river, Siberian platform.
article citation Rodionov V.P., Gurevich E.L. Key magneto-stratigraphic sequence of the Lower Ordovician deposits, north-western Siberian platform // Neftegazovaya Geologiya. Teoriya I Praktika. – 2010. - V.5. - #3.- http://www.ngtp.ru/rub/2/38_2010.pdf