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Elements of regional organic geochemistry and separate prediction of oil and gas content of regions

T.K. Bazhenova

Original article

DOI https://doi.org/10.18599/grs.2021.2.3

35-43
rus.

open access

Under a Creative Commons license
The article considers the elements of organic geochemistry in the regional aspect, which aims to separate quantitative prediction of oil and gas content of regions. The principles and results of balance calculations of generation and emission of liquid and gaseous hydrocarbons for different facies-genetic types of organic matter and methods for calculating the scale of hydrocarbon emission are considered. Finally, a list of the main regularities of organic geochemistry is given.
 

organic geochemistry, organic matter, oil-gas formation, oil-gas accumulation, facial-genetic type of organic matter, catagenesis, balance calculations, separate forecast of oil and gas content

 

  • Bazhenova O.K., Bazhenova T.K. (2003). Ontological and epistemological aspects of geochemistry (organic geochemistry at different levels of organization of matter and in the system of knowledge). Geology geochemistry of fossil fuels. Moscow: GEOS, pp. 44–52. (In Russ.)
  • Bazhenova T.K. (2020). Fundamentals of Regional Organic Geochemistry. Moscow: GEOS, 120 p. (In Russ.)
  • Bazhenova T.K., Sukhanov A.A. (2007). Divergence of OM catagenetic transformation and genesis of non-graphite forms of carbon. The fundamental basis of new technologies in the oil and gas industry. Moscow: GEOS, pp.  26–27. (In Russ.)
  • Generation of hydrocarbons in the process of sediment lithogenesis (1976). Ed. A.A. Trofimuk; S.G. Neruchev. Novosibirsk: Nauka, 198 p. (In Russ.)
  • Martirosyan O.V. (2014). Factors and mechanisms of the structural evolution of mineraloids. Abstract Dr. sci. diss. Syktyvkar, 38 p. (In Russ.)
  • Neruchev S.G., Rogozina E.A. (2010). Geochemical foundations of forecasting oil and gas content. St.Petersburg: VNIGRI, 280 p. (In Russ.)
  • Parparova G.M., Neruchev S.G. (1977). Fundamentals of the genetic classification of dispersed organic matter in rocks. Russian Geology and Geophysics, 5, pp. 45–52. (In Russ.)
  • Parparova G.M., Zhukova A.V. (1990). Coal petrographic methods in the study of sedimentary rocks and minerals. Leningrad: Nedra, 308 p. (In Russ.)
  • Petrology of Organic Substances in the Geology of Fossil Fuels (1987). I.I. Ammosov, V.I. Gorshkov, N.P. Grechishnikov, I.V. Eremin, V.K, Pryanishnikov, Yu.V. Stepanov. Moscow: Nauka, pp. 333 p. (In Russ.)
  • Sukhanov A.A. (2003). Investigation of the regularities of distribution of natural fullerenes in shungites of the Lower Proterozoic of Karelia. Abstract Cand. sci. diss. St.Petersburg, 24 p. (In Russ.)
  • Sukhanov A.A., Bazhenova T.K., Kotelnikova E.N. (2011). Structural Characteristics of a Carbonic Matter of Sapropelite Kerogen: Dependence on the Biocoenotic Type of Organic Matter and Degree of Its Catagenesis. Geochemistry International, 9, pp. 904. https://doi.org/10.1134/S001670291107010X
  • Taxonomy and classification of sedimentary rocks and their analogues (1998). Ed. V.N. Shvanov, St.Petersburg: Nedra, 351 p. (In Russ.)
  • Tissot B., Welte D. (1984). Petroleum Formation and Occurrence. Springer, Berlin, Heidelberg, 702 p. https://doi.org/10.1007/978-3-642-87813-8
  • Uspenskii V.A. (1954). The experience of the material balance of the processes occurring during the metamorphism of coal seams. Izv. AN SSSR, ser. geol., 6, pp. 94–101. (In Russ.)
  • Vassoevich N.B., Neruchev S.G., Lopatin N.V. (1976). On the scale of catagenesis in connection with oil formation. Fossil fuels: problems of geology and geochemistry of naphthides and bituminous rocks. Moscow: Nauka, pp. 47–62. (In Russ.)
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Tatiana K. Bazhenova
Geologorazvedka LLC
20, Fayansovaya str, St. Petersburg, Russian Federation

 

For citation:

 Bazhenova T.K. (2021). Elements of regional organic geochemistry and separate prediction of oil and gas content of regions. Georesursy = Georesources, 23(2), pp. 35–43. DOI: https://doi.org/10.18599/grs.2021.2.3