Batova G.I.


Graduated from St. Petersburg Technological Institute (1973), specialization “chemical engineer-technologist”.
PhD of Geological and Mineralogical Sciences.
Senior Researcher of VNIIOkeangeologiya named after I.S. Gramberg.
Area of scientific interests: organic geochemistry of bottom sediments and rocks.
Author of more than 50 publications.
Geochemical research
Section editor – PhD in geology and mineralogy Bazhenova T.K.
Article # 23_2018 submitted on 04/27/2018 displayed on website on 07/05/2018
17 p.
pdf  Molecular geochemistry of organic matter and petroleum generation potential of the Upper Paleozoic rocks belonging to the Pre-Taimyr uplift zone
Studies of organic matter from the Upper Paleozoic sequences were carried out for the first time using complex of modern organic geochemistry (GC-MS) methods. Samples were obtained from outcrop in the junction zone with the Siberian Basin folded Taimyr. Bituminological analysis and distribution of hydrocarbon biomarkers allowed determining the composition, conditions of formation and the level of thermal maturity of organic mater. The impact of dynamocatagenesis on the activation of primary migration led to the appearance of epigenic hydrocarbons in the Permian sections. The source of which may be either the underlying rocks of the Lower Carboniferous other the adjacent Jurassic rocks of hydrocarbons the Mesozoic-Cenozoic megacomplex. The source rocks quality determined in samples collected only from outcrops is moderate but that does not exclude petroleum prospects in this areas as a whole.

Keywords: organic matter, Upper Paleozoic deposits, hydrocarbons biomarkers, petroleum potential, Pre-Taimyr uplift zone.
article citation Petrova V.I., Batova G.I., Kursheva A.V., Litvinenko I.V., Morgunova I.P., Rusinovich A.V. Molekulyarnaya geokhimiya organicheskogo veshchestva i neftegazogeneratsionnyy potentsial verkhnepaleozoyskikh porod Predtaymyrskoy zony podnyatiy [Molecular geochemistry of organic matter and petroleum generation potential of the Upper Paleozoic rocks belonging to the Pre-Taimyr uplift zone]. Neftegazovaya Geologiya. Teoriya I Praktika, 2018, vol. 13, no. 3, available at: http://www.ngtp.ru/rub/1/23_2018.pdf
DOI https://doi.org/10.17353/2070-5379/23_2018
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Geochemical research
Section editor – PhD in geology and mineralogy Bazhenova T.K.
Article # 35_2015 submitted on 08/18/2015 displayed on website on 09/21/2015
21 p.
pdf  Hydrocarbons in bottom sediments of the Shtokman area – distribution, genesis, temporal trends
The study of the composition, distribution and genesis of hydrocarbons in the components of the geological environment of water areas allows solving tasks of the forecast of oil and gas potential of mineral resources and at the same time provides a basis for future environmental monitoring in exploration and mining operations. The major geochemical parameters of dispersed organic matter are identified on the basis of long-term study of Late Quaternary sediments of the South-Barents depression. Studies have shown that the organic-geochemical background of Holocene Quaternary sediments of the Shtokmanarea formed due to the sedimentation flux of sedimentary material and possible endogenous influence, which determines the specificity of the local anomaly content and composition of dispersed organic matter. This results in high content of aromatic hydrocarbons and polyarenes and organic carbon, but in the absence of its correlation with particle size of bottom sediments. The composition of the hydrocarbon molecular markers indicates the enriched upper part of the sedimentary section by components of thermal mature dispersed organic matter that can be caused by emissions from point discharge of gas fluid of sedimentary rocks of the lower stratigraphic horizons and/or seeping migration.

Keywords: bottom sediments, hydrocarbons, biomarkers, polycyclic aromatic hydrocarbons, Barents Sea, Shtokman area.
article citation Petrova V.I., Batova G.I., Kursheva A.V., Litvinenko I.V., Morgunova I.P. Uglevodorody v donnykh osadkakh Shtokmanovskoy ploshchadi – raspredelenie, genezis, vremennye trendy [Hydrocarbons in bottom sediments of the Shtokman area – distribution, genesis, temporal trends]. Neftegazovaya Geologiya. Teoriya I Praktika, 2015, vol. 10, no. 3, available at: http://www.ngtp.ru/rub/1/35_2015.pdf
DOI https://doi.org/10.17353/2070-5379/35_2015
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