Structure and mineralogical composition of the tuff horizon of Petrikov potash deposit

Authors

  • Vladimir P. Samodurov Belarusian State University, 4 Niezaliežnasci Avenue, Minsk 220030, Belarus
  • Anatoly I. Druk Belgorkhimprom JSC, 17 Mašeraŭ Avenue, Minsk 220029, Belarus
  • Konstantin Yu. Balashov Belgorkhimprom JSC, 17 Mašeraŭ Avenue, Minsk 220029, Belarus
  • Yuriy N. Yalenski Belgorkhimprom JSC, 17 Mašeraŭ Avenue, Minsk 220029, Belarus

Keywords:

volcanic tuff, volcanic activity, illite 1M, lithological marker

Abstract

Integrated data of the structure and mineralogical composition of the marking tuff horizon in the Upper-Devonian bed of the North-Shestovich synclinal zone are presented in this paper. Dependence of the tuff bed structure on the volcanic activity stage is revealed. Find out that the prevailing mineral of tuff is the structure-ordered illite 1M. Marked tuff horizon is situated inside the Upper-Devonian salt bed within Petrikov synclinal zone and comes up into the overlaying clay-marl formation of the surrounding geological beds.

Author Biographies

  • Vladimir P. Samodurov, Belarusian State University, 4 Niezaliežnasci Avenue, Minsk 220030, Belarus

    PhD (geology and mineralogy), docent; associate professor at the department of regional geology, faculty of geography and geoinformatics

  • Anatoly I. Druk, Belgorkhimprom JSC, 17 Mašeraŭ Avenue, Minsk 220029, Belarus

    head of the laboratory of geological investigation

  • Konstantin Yu. Balashov, Belgorkhimprom JSC, 17 Mašeraŭ Avenue, Minsk 220029, Belarus

    head of the laboratory of hydrogeological investigation and ecology

  • Yuriy N. Yalenski, Belgorkhimprom JSC, 17 Mašeraŭ Avenue, Minsk 220029, Belarus

    leading engineer at the laboratory of geological investigation

References

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Published

2019-06-10

How to Cite

[1]
Samodurov, V.P. et al. 2019. Structure and mineralogical composition of the tuff horizon of Petrikov potash deposit. Journal of the Belarusian State University. Geography and Geology. 1 (Jun. 2019), 119–127. DOI:https://doi.org/10.33581/2521-6740-2019-1-119-127.