Sribnian ring structure (Dnieper-Donets depression) — a possible testing ground for the development of the hydrogen potential of the Earth’s interior

Authors

DOI:

https://doi.org/10.15407/dopovidi2021.05.050

Keywords:

endogenic hydrogen, Earth degassing, ring structures

Abstract

Tectonic-volcanic ring structures correspond to the notion of tube-de-gassing most completely. Endogenic hydrogen is considered as the leading factor of their formation and lithogeodynamic evolution at the both stages “hot” (burning of endogenic hydrogen) and “cold” (ascending migration of “light gases”) phases. Hydrogen, helium, and hybride fields must be connected most of all wit such structures. Among them, megacalderas type with long-term “cold” degassing stage are of the priority of prospecting interest. Sribnian depression (within Dnieper-Donets depression serves as the example of such structures. It is genetically related to the explosion of a volcanic caldera and is characterized by ancient origin (Proterozoic) and long-term geologic evolution on the background of the ascending light gases migration. Intensive hydrogen degassing through the Sribnean ring structure is confirmed by micro- and nano-inclusions in the black-shale domanicoid rocks in the form of particles of native metals (including oxyphile elements — Al, Zn, W, and others) natural alloys and in termetallides — the tracers of ascending flows of deep reduced fluids. The paper deals with comparative cha racteristics of Uzon volcanic caldera (East Kamchatka) and Sribnian ancient volcanic-tectonic ring structure that had special significance in the geological history of the Dnieper-Donets aulacogen. There are all reasons to consider this structure as the exclusive prospecting object for endogenic hydrogen.

References

State and forecast of the World energetic consumer basket. Journal of the Petrotech Society “Energy Independence with global co-operation: Challenges & Solutions”, Petrotech 2009, № 12, Commorate Issue, December, 2008.

Larin, V. N. (2005). Our Earth (origin, composition, structure and development of the originally hydride Earth). Мoscow: Аgar (in Russian).

Gilat, A. L. & Vol, A. (2012). Degassing of primordial hydrogen and helium as the major energy source for internal terrestrial processes. Geosci. Front., 3, Iss. 6, pp. 911-921.

Shestopalov, V. M., Lukin, A. E., Zgonnik, V. А., Мakarenko, А. N., Larin, N. V. & Bohuslavsky, А. S. (2018). Essays on Earth degassing. Kyiv (in Russian).

Larin, N. V., Zgonnik, V., Rodina, S., Deville, E., Prinzhofer, A. & Larin, V. N. (2015). Natural molecular hydrogen seepage associated with surficial, rounded depressions on the European craton in Russia. Nat. Resour. Res., 24, pp. 369-383. https://doi.org/10.1007/s11053-014-9257-5

Prinzhofer, A., Tahara Cisse, C. S. & Diallo, A. B. (2018). Discovery of a large accumulation of natural hydrogen in Bourakebougou (Mali). Int. J. Hydrog. Energy, 43, pp. 19315-19326. https://doi.org/10.1016/j.ijhydene.2018.08.193

Borodzich, E. V., Korotkina, M. P., Lobanov, E. V. & Shmakov, A. P. (1990). About the origin of ring structures. Dokl. AN SSSR, 311, No. 5, pp. 1081-1085 (in Russian).

Portnov, A. M. (2005). Energy of volcanoes. Priroda i chelovek, No. 4, pp. 10-11 (in Russian).

Beskrovny, N. S. & Lеbedev, B. А. (1971).Oil show in the caldera of the Uzon volcano in Kamchatka. Dokl. AN SSSR, 201, No. 4, pp. 953-956 (in Russian).

Kamensky, I. L., Lobkov, V. А., Prasolov, E.M. et al. (1976). Components of the earth’s upper mantle in the gases of Kamchatka (by isotopes He, Ne, Ar, C). Geochemistry, No. 5, pp. 682-695 (in Russian).

Lukin, A. E. & Pikovsky, Y. I. (2004). New data on the isotopic composition of hydrothermal oil (Uzon caldera in Kamchatka). Dokl. АN, 398, No. 1, pp. 1-4 (in Russian).

Lukin, A. E. (2005). Depth hydrogeologic inversion as a global synergetic phenomenon: theoretical and applied aspects. Paper 2. Tectonic-geodynamics aspects of hydrogeologic inversion. Geol. J., No. 1, pp. 53-69 (in Russian).

Lukin, A. E., Dovzhok, E. I., Knishman, A. Sh., Goncharenko, V. I. & Dzyubenko, A. I. (2012). Helium anomaly in petroliferous Visean carbonate reservoirs of the Dnieper-Donets Depression. Dopov. Nac. akad. nauk Ukr., No. 7, pp 97-104 (in Russian).

Published

27.10.2021

How to Cite

Lukin О., & Shestopalov В. (2021). Sribnian ring structure (Dnieper-Donets depression) — a possible testing ground for the development of the hydrogen potential of the Earth’s interior. Reports of the National Academy of Sciences of Ukraine, (5), 50–60. https://doi.org/10.15407/dopovidi2021.05.050