Popov V.V.



Graduated from Leningrad State University, the Faculty of Physics (1988), specialization «geophysics».
Engineer of St. Petersburg State University, resource center "Geomodel".
Area of scientific interests: paleomagnetism (paleogeodynamics, magnetostratigraphy), rock magnetism, equipment for paleomagnetic research, programming.
Author of 67 publications.
Stratigraphy and lithology
Article # 39_2021 submitted on 11/18/2021 displayed on website on 12/03/2021
13 p.
pdf Paleomagnetic studies of the Middle-Upper Devonian section of the Voronezh anteclise (Pavlov quarry)
New paleomagnetic determinations are presented for a collection of rocks of the Middle-Upper Devonian (Givetian and Frasnian stages), sampled from an outcrop on the southwestern slope of the Pavlov granite quarry. Three characteristic components of natural remanent magnetization have been identified. The bipolar component C corresponds to the Late Paleozoic remagnetization in the Carboniferous and two components of Givetian - Frasnian age. The bipolar component of D2NR passes the geomagnetic field polarity reversal test. The obtained position of the paleomagnetic pole in terms of the bipolar component of the natural remanent magnetization is consistent with the available data on the Middle Devonian strata of the Main Devonian Field (Russian platform).

Keywords: paleomagnetic determinations, Middle-Upper Devonian, geomagnetic field, paleomagnetic pole, Main Devonian Field, Russian platform.
article citation Iosifidi A.G., Popov V.V. Paleomagnitnye issledovaniya sredne-verkhnedevonskikh otlozheniy Voronezhskoy anteklizy (Pavlovskiy kar'er) [Paleomagnetic studies of the Middle-Upper Devonian section of the Voronezh anteclise (Pavlov quarry)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2021, vol. 16, no. 4, available at: http://www.ngtp.ru/rub/2021/39_2021.html
DOI https://doi.org/10.17353/2070-5379/39_2021
References
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   Chadima M., Hrouda F. Remasoft 3.0 a user-friendly paleomagnetic data browser and analyzer. Travaux Géophysiques, 2006, XXVII, pp. 20-21.
   Chadima M., Jelinek V. Anisoft 42, 2009. - www.AGICO.com
   Dopolneniya k Stratigraficheskomu kodeksu Rossii [Additions to the Stratigraphic Code of Russia]. Editor A.I. Zhamoyda. St.Petersburg: VSEGEI, 2000, 112 p.
   Gurevich E.L., Khramov A.N., Rodionov V.P., Dekkers M., Fedorov P.V. Paleomagnetizm ordovikskikh i devonskikh osadochnykh porod severo-zapada Russkoy platformy: novye dannye o kinematike Baltiki v palezoe i o permo-triasovom peremagnichivanii [Paleomagnetism of Ordovician and Devonian sedimentary rocks in the northwestern part of the Russian Platform: new constraints on the Baltica kinematics in the Paleozoic and the remagnetization in the Permian-Triassic]. Fizika Zemli, 2005, no. 7, pp. 48-64.
   Iosifidi A.G., Popov V.V., Zhuravlev A.V. Verkhnedevonskie otlozheniya (franskiy yarus) severo-zapada Russkoy platformy: paleomagnitnye dannye [Upper Devonian (Frasnian stage) of the north-western part of the Russian Platform: paleomagnetic data]. Neftegazovaya Geologiya. Teoriya I Praktika, 2020, vol. 15, no. 4, available at: http://www.ngtp.ru/rub/2020/42_2020.html. DOI: https://doi.org/10.17353/2070-5379/42_2020
   Karpova E.V. Osobennosti sedimento- i litogeneza v zhivetskom-ranne franskom vekakh srednego-verkhnego devona na Pavlovskom mestorozhdenii (yugo-vostok Voronezhskoy anteklizy) [Peculiarities of sedimentary and lithogenesis in Givetian-Early Frasnian centuries of the Middle-Upper Devonian at the Pavlov field (southeast of the Voronezh anteclise)]. Vestnik Moskovskogo universiteta. Seriya 4. Geologiya, 2003, no.5, pp. 47-56.
   Legenda Voronezhskoy serii listov Gosudarstvennoy geologicheskoy karty Rossiyskoy Federatsii masshtaba 1:200 000 (izdanie vtoroe). Ob"yasnitel'naya zapiska [Legend of the Voronezh series of sheets of the State Geological Map of the Russian Federation at a scale of 1:200,000 (second edition). Explanatory letter]. T.E. Gorbatkina, Yu.I. Iosifova, R.V. Krasnenkov, Yu.T. Kuz'menko, M.Kh. Makhlina, A.G. Olfer'ev, B.M. Petrov, T.D. Rodionova, S.M. Shik. Moscow, 1999.
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   Milash A.V. Aktsessornye mineraly eyfel'skikh, zhivetskikh i nizhnefranskikh otlozheniy yugo-vostoka Voronezhskoy anteklizy [Accessory minerals of the Eifelian, Givetian, and Lower Frasnian of the southeastern Voronezh anteclise]. Vestnik Voronezhskogo gosudarstvennogo universiteta. Seriya Geologiya, 2017, no.1, pp. 31-42.
   Raskatova M.G. Miosporovaya zonal'nost' sredne-verkhnedevonskikh otlozheniy yugo-vostochnoy chasti Voronezhskoy anteklizy (Pavlovskiy kar'er) [Miospore zoning of the Middle-Upper Devonian strata of the southeastern part of the Voronezh anteclise (Pavlov quarry)]. Vestnik Voronezhskogo gosudarstvennogo universiteta. Seriya Geologiya, 2004, no. 2, pp. 89-98.
   Rodionov V.P., Khramov A.N., Gurevich E.L., Tomsha V.A. Paleomagnetizm devona severo-vostoka glavnogo devonskogo polya: klyuchevoy paleomagnitnyy polyus i magnitostratigrafiya verkhnego frana [Devonian paleomagnetism of the northeastern Main Devonian Field: key paleomagnetic pole and magnetostratigraphy of the Upper Frasnian]. Paleomagnetizm i magnetizm gornykh porod; teoriya, praktika, eksperiment: materialy mezhdunarodnoy shkoly-seminara. St.Petersburg: SOLO, 2010, pp. 121-126.
   Rusetskaya G.A., Tarasenko A.B., Verbitskiy V.R., Khramov A.N., Zhuravlev A.V., Evdokimova I.O., Iosifidi A.G., Tomsha V.A., Sokiran E.V. Stratopip buregskikh sloev (franskiy yarus, glavnoe devonskoe pole) [Stratotype of the Bureg Beds (Frasnian Stage, Main Devonian Field)]. Litosfera, 2013, no. 5, pp. 42-56.
   Savko A.D. Geologiya Voronezhskoy anteklizy [Geology of the Voronezh anteclise]. Trudy nauchno-issledovatel'skogo instituta geologii Voronezhskogo gosudarstvennogo universiteta. Voronezh: Izd-vo VGU, 2002, issue 12, 165 p.
   Tarling D.H., Hrounda F. The magnetic anisotropy of rocks. Chapman and Hall, New York. 1993, 217 p.
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   Zhuravlev A.V., Sokiran E.V., Evdokimova I.O., Dorofeeva L.A., Rusetskaya G.A., Malkowski K. Faunal and facies changes at the Early-Middle Frasnian boundary in the Northwestern East European Platform. Acta Palaeontologica Polonica, 2006, vol. 51 (4), pp. 747-758.
Stratigraphy and lithology
Section editor – PhD in geology and mineralogy Kirichkova A.I.
Article # 42_2020 submitted on 11/10/2020 displayed on website on 12/08/2020
16 p.
pdf Upper Devonian (Frasnian stage) of the north-western part of the Russian Platform: paleomagnetic data
Paleomagnetic determinations for the Devonian strata of the Main Devonian Field, available in the international paleomagnetic data base, do not make it possible to construct both detailed magnetostratigraphic scales and reliable trajectories of the apparent polar wander path of the paleomagnetic pole. This is primarily due to the insufficient amount of data that determine modern reliability criteria. Obtaining more complete series of reliable paleomagnetic determinations is one of the important tasks of paleomagnetic studies. The paper presents new paleomagnetic determinations from a collection of rocks of the Frasnian stage of the Upper Devonian (Ilmen and Bureg Beds of the Semiluky Formation), sampled on the southern shore of Lake Ilmen, east of the village. Korostyn in 2009. Magnetomineralogical studies were carried out to determine the magnetic minerals of carriers of natural remanent magnetization. Three characteristic components of natural remanent magnetization have been identified. Two components correspond to the Late Paleozoic magnetization reversal (in the Carboniferous and Permian times). The third, bipolar component of the Frasnian age passes the reverse polarity test of the geomagnetic field.. The obtained position of the paleomagnetic pole by the bipolar component of the natural remanent magnetization is consistent with the available data on the section of the Late Upper Devonian of the Main Devonian Field.

Keywords: paleomagnetism, Frasnian stage of the Upper Devonian, Ilmen and Bureg Beds of the Semiluky Formation, geomagnetic field polarity, magnetostratigraphy, paleomagnetic pole.
article citation Iosifidi A.G., Popov V.V., Zhuravlev A.V. Verkhnedevonskie otlozheniya (franskiy yarus) severo-zapada Russkoy platformy: paleomagnitnye dannye [Upper Devonian (Frasnian stage) of the north-western part of the Russian Platform: paleomagnetic data]. Neftegazovaya Geologiya. Teoriya I Praktika, 2020, vol. 15, no. 4, available at: http://www.ngtp.ru/rub/2020/42_2020.html
DOI https://doi.org/10.17353/2070-5379/42_2020
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   Zhuravlev A.V., Sokiran E.V., Evdokimova I.O., Dorofeeva L.A., Rusetskaya G.A., Malkowski K. Faunal and facies changes at the Early-Middle Frasnian boundary in the Northwestern East European Platform. Acta Palaeontologica Polonica, 2006, issue 51, no.4, pp. 747-758.
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 # 11_2012 submitted on 01/23/2012 displayed on website on 02/06/2012
21 p.
pdf  Anisotropy of various magnetic parameters use for determining directions of material transfer in the study of turbidite currents
The carbonate clastic fans are considered as promising objects for oil and gas prospecting targets. Thus reconstruction of the fan morphology, sources and directions is an important practical task. The method for detecting the turbidite currents based on investigation of the anisotropy of susceptibility ellipsoids axes is described. The new model of main axes distribution is developed. Study of 13 objects allows us reconstructing directions of the turbidite currents of the Ural Foredeep for the two time-slices and draw maps demonstrating palaeogeographical position of the carbonate material sources.
Key words: anisotropy, magnetic susceptibility, turbidites, direction of material transfer, paleogeography, reconstruction, fan morphology, Ural Foredeep.
article citation Popov V.V., Zhuravlev A.V. Ispol'zovanie anizotropii razlichnykh magnitnykh parametrov dlya opredeleniya napravleniya snosa materiala pri izuchenii turbiditnykh potokov [Anisotropy of various magnetic parameters use for determining directions of material transfer in the study of turbidite currents]. Neftegazovaya Geologiya. Teoriya I Praktika, 2012, vol. 7, no. 1, available at: http://www.ngtp.ru/rub/2/11_2012.pdf
References
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Stratigraphy and lithology
Section editor – PhD in geology and mineralogy Kirichkova A.I.
Article # 6_2012 submitted on 10/26/2011 displayed on website on 01/25/2012
19 p.
pdf  Devonian and Carboniferous boundary strata in the Kamenka River section (Pechora-Kozhvin megaswell, Timan-Pechora province)
The article deals with the Devonian-Carboniferous boundary in the shallow-water strata (the Kamenka River section as example) on the basis of cyclostratigraphy (maximum of regression) controlled by biostratigraphical data (conodonts and foraminifera). Facial control on the foraminifer and conodont associations is considered. Dependence of the magnetic suscessibility of the rocks on the sea-level changes is detected. The dependence is probably caused by variations of the terrigenous content in the carbonate rocks. Keywords: conodonts, foraminifera, cyclostratigraphic method, magnetic susceptibility of rocks, Devonian-Carboniferous boundary strata, Timan-Pechora province.
Key words: Devonian/Carboniferous boundary, Timan-Pechora Province, conodonts, foraminifers, cyclostratigraphy, biostratigraphy, palaeomagnitology.
article citation Vevel' Ya.A., Zhuravlev A.V., Popov V.V. Pogranichnye otlozheniya devonskoy i kamennougol'noy sistem v razreze na r. Kamenka (Pechoro-Kozhvinskiy megaval, Timano-Pechorskaya provintsiya) [Devonian and Carboniferous boundary strata in the Kamenka River section (Pechora-Kozhvin megaswell, Timan-Pechora province)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2012, vol. 7, no. 1, available at: http://www.ngtp.ru/rub/2/6_2012.pdf
References
   Barskov I.S., Kononova L.I., Migdisova A.V. Konodonty nizhneturneyskikh otlozheniy podmoskovnogo basseyna [Conodonts of the Lower Tournaisian deposits of the Pre-Moscow Basin]. Paleontologicheskaya kharakteristika stratotipicheskikh i opornykh razrezov karbona Moskovskoy sineklizy. Editor V.V. Menner. Moscow: Moskow State University, 1984, pp. 3-33.
   Eremenko N.M., Vevel' Ya.A., Zhuravlev A.V. Interfatsial'naya korrelyatsiya morskikh ranneturneyskikh otlozheniy severa Urala i vostoka Timano-Pechorskoy plity – litostratigraficheskiy podkhod [Inter-facial correlation of the Lower Tournaisian marine deposits, northern Urals and eastern Timan-Pechora plate - lithostratigraphic approach]. Proceedings of the International Scientific Conference “Litologicheskie i geokhimicheskie osnovy prognoza neftegazonosnosti” [Lithological and geochemical basis of oil and gas potential forecast]. Saint Petersburg: VNIGRI, 2008, pp. 600-605.
   Fauna i biostratigrafiya pogranichnykh otlozheniy devona i karbona Berchogura (Mugodzhary) [Fauna and biostratigraphy of the Devonian and Carboniferous deposits, Berchogur (Mugodzhary)]. Moscow: Nauka, 1987, 121 p.
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   Shishlov S.B. Strukturno-geneticheskiy analiz osadochnykh formatsiy [Structural and genetic analysis of sedimentary formations]. Saint Petersburg: Saint Petersburg State Mining University, 2010, 276 p.
   Sobolev D.B. Ostrakody i biostratigrafiya turneyskogo yarusa severa Urala [Ostracoda and biostratigraphy of the Tournaisian stage, north of the Urals]. Ekaterinburg: UrO RAN, 2005, 113 p.
   Vevel' Ya.A. Nakhodka foraminifer Tournayellina beata pseudobeata Reitlinger et Kulagina v nizhnem karbone Pechorskoy gryady [Discovery of foraminifera Tournayellina beata pseudobeata Reitlinger et Kulagina in the Lower Carboniferous Pechora ridge]. Neftegazovaya geologiya. Teoriya i praktika, 2009, vol. 4, no. 2, available at: http://www.ngtp.ru/rub/2/17_2009.pdf
   Zhuravlev A. Biogeography of the Early Carboniferous conodont genus Patrognathus. In: Wong, Th. E. (Ed.): Proceedings of the XVth International Congress on Carboniferous and Permian Stratigraphy. Utrecht, the Netherlands, 10–16 August 2003. Royal Netherlands Academy of Arts and Sciences, 2007, pp. 325-329.
   Zhuravlev A.V. Gistologiya i mikroskul'ptura pozdnepaleozoyskikh konodontovykh elementov [Histology and microsculpture the Late Paleozoic conodont elements]. Saint Petersburg: Geoservis Plyus, 2002, 94 p.
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   Zhuravlev A.V. Konodonty verkhnego devona – nizhnego karbona severo-vostoka Evropeyskoy Rossii [Conodonts of the Upper Devonian - Lower Carboniferous north-east of European Russia]. Saint Petersburg: VSEGEI, 2003, 85 p.
   Zhuravlev A.V., Kossovaya O.L., Sobolev D.B., Vevel Y.A. Biostratigraphy of the Lower Tournaisian (Lower Carboniferous) shallow-water deposits of the Eastern Part of the Timan-Pechora Province. Newsletter on Carboniferous Stratigraphy, 1999, no. 17, pp. 22-26.
   Zhuravlev A.V., Kossovaya O.L., Sobolev D.B., Vevel Y.A. Early Tournasian (Early Carconiferous) Shallow water Communities (Eastern part of the Timan-Pechora Province). Ichthyolith Issues special Publication 4, 1998, pp. 60-62.
Stratigraphy and lithology
Section editor – PhD in geology and mineralogy Kirichkova A.I.
Article # 45_2009 submitted on 12/10/2009 displayed on website on 12/14/2009
20 p.
pdf Upper Devonian - Lower Carboniferous key sequence on the Talota river, Timan-Pechora province - results of lithologic, biostratigraphic and paleomagnetic researches
The results of complex studying the Upper Devonian - Lower Carboniferous key sequence on the Talota river (north of the Vashutkino-Talota zone of overthrusts, Timan-Pechora province) are presented. The tectonic twinning of the sequence on the zone of overthrusts is proved by biostratigraphy data. The parautochthonous and allochthonous parts of the sequence are dated by foraminifera and conodonts. The first part contains Early Famenian-Late Visean deposits, the second part - Late Famenian-Serpukhovsk deposits. Breaks in sedimentations are established in the Lower Tournaisian and Lower Visean. The presence of an ancient secondary prefolded component of magnetization, confined to the definite parts of the sequence and caused by tectonic and hypergene processes, is established. The direction of this magnetization allowed reconstructing the prefolded (Middle Paleozoic) position of the allochthone and parautochthone.
Key words: Upper Devonian, Lower Carboniferous, key sequence, Timan-Pechora province, stratigraphy, paleomagnetology, tectonics.

Sequence description by Eremenko N.M. and Zhuravlev A.V. is provided in the Annex 1.
article citation Eremenko N.M., Zhuravlev A.V., Iosifidi A.G., Popov V.V., Khramov A.N., Vevel Ya.A., Nickolaev A.I. Upper Devonian - Lower Carboniferous key sequence on the Talota river, Timan-Pechora province - results of lithologic, biostratigraphic and paleomagnetic researches // Neftegazovaya Geologiya. Teoriya I Praktika. - 2009. - V.4. - #4.- http://www.ngtp.ru/rub/2/45_2009.pdf
Eremenko N.M., Zhuravlev A.V., Iosifidi A.G., Popov V.V., Khramov A.N., Vevel Ya.A., Nickolaev A.I. Upper Devonian - Lower Carboniferous key sequence on the Talota river, Timan-Pechora province - results of lithologic, biostratigraphic and paleomagnetic researches // Neftegazovaya Geologiya. Teoriya I Praktika. - 2009. - V.4. - #4.- http://www.ngtp.ru/rub/2/45prilojenie_2009.pdf
References
New methods and technologies
Section editor – PhD in geology and mineralogy Prischepa O.M.
Article # 016 displayed on website on 04/16/2007
39 p.
pdf  New paleomagnetic method of borehole cores location determining
Geological study of large areas is based solely on the results of drilling. The relevance of such studies is obvious, as fields are very often found in closed areas. In such cases, the problem of sequence correlation of insufficiently faunistically characterized wells is common. Paleomagnetic (magnetostratigraphic) method is often the only method to enable such a correlation in these cases. However, it is necessary to find out the orientation of samples in the well in order to use paleomagnetic method. As for borehole cores, the orientation "top-bottom" is usually only known. The method that uses the direction of low-temperature (low-coercitive) modern viscous component of magnetization is applied in paleo-magnetism to orient the core samples to the cardinal. However, the possibilities of this method are limited for several reasons. We propose to use a new method that allows us to calculate the direction of the ancient magnetization components in those cases where conventional methods do not provide a satisfactory result. The new method was tested on the samples from two sequences of the Lower Vendian - Early Cambrian and one sequence of Cenozoic southeastern coastal of the White Sea area. The similarity of the results for natural outcrops and wells proves its high efficiency. The application of the new method has allowed us to calculate paleomagnetic poles for the Upper Vendian and Cenozoic Baltic as well as the age of reversal for the Late Vendian rocks. The alternative paleomagnetic poles for Vendian Baltic have been calculated through the results obtained and the reconstruction of paleogeographical position of the plate during the studied period of time has been made.
Key words: magnetostratigraphy, component composition of the rocks, Russian platform, correlation of geological sequences, core orientation.
article citation Popov V.V., Khramov A.N. New paleomagnetic method of borehole cores location determining // Neftegazovaya Geologiya. Teoriya I Praktika. – 2007. - V.2. - http://www.ngtp.ru/rub/12/016.pdf
References