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Carbonates and Evaporites

, Volume 17, Issue 2, pp 154–158 | Cite as

Human-induced activation of gypsum karst in the southern Priangaria (East Siberia, Russia)

  • Yu. B. Trzhtsinsky
Article

Abstract

Over 25% of the area of the Siberian Platform is composed of carbonate, sulphate, and saline rock deposits that are marked by intensive karstification and leaching. Particularly intensive karst occurs under natural conditions within gypsiferous and saline rock formations in the southern part of the Irkutsk amphitheatre. Intensive economic development of the region, including creation of large industrial enterprises, man-made reservoirs, expansion of irrigation farming, and other activities, have stimulated substantial activation of karst processes, in some places with a more than a 10-fold acceleration.

Keywords

Dolomite Gypsum Lower Cambrian Shore Zone Aeration Zone 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

  1. ERASO, A. and TRZCINSKIJ, Y.B., 1993, Sinkhole collapses and gypsum karst in Cambrian platform of East Siberia. Proceedings of the XI. Intern. Congress on Speleology, Beijing, China, p. 171–173.Google Scholar
  2. GUIDE DES TERRAINS KARSTIQUES CHOISIS DE LA SIBERIE ORIENTALE ET DE I OURAL, 1996, Red. M. Pulina, J.B. Trzcinski. Sosnowiec, Universitete de Silesie, 126 p.Google Scholar
  3. FILIPPOV, V.M., 1981, The experimental study of the processes of dissolution of sulphate rocks in Pribaikalia. In: Some Questions of Geomorphology of East Siberia.- Irkutsk, p. 131–140 (in Russian).Google Scholar
  4. MAXIMOVICH, A.G., 1961, The compactness of karst holes and sustainability of karsted areas:Geologia i Razvedka, no. 7, p. 118–125 (in Russian).Google Scholar
  5. OVCHINNIKOV, G.I., PAVLOV, S.KH., and TRZHTSINSKY, YU.B., 1999, Changes of the geological environment within the area of influence of the Angara-Enisey man-made reservoirs. — Novosibirsk: Nauka, 254 p. (in Russian).Google Scholar
  6. PULINA, M. and TRZCINSKI, JU, 1994, Quelques changements dans le milieu Karstique en Sibirie Orientale dus aux activities de l’Homme (a l’ex du plateau d’Irkoutsk). — XIII Ecole de Speleologie. Sosnowiec. S. 10–12.Google Scholar
  7. THE PROBLEMS OF PROTECTION OF GEOLOGICAL ENVIRONMENT (ON THE EXAMPLE OF EAST SIBERIA), 1993, Novosibirsk: Nauka, 167 p. (in Russian).Google Scholar
  8. TRZCINSKY, JU.B., 1996, Gypsum karst in the south of the Siberian platform: Russia. Int. J. Speleol., v. 25, p. 3–4.Google Scholar
  9. TRZHTSINSKY, JU.B. and FILIPPOV, V.M., 1981, Technogenic Activization of Karst in Angara Water Reservoirs//Engineering-Geological Problems in Soluble Rocks. — Istanbul. p. 66–67.Google Scholar
  10. VOLOGODSKY, G.P., 1975, Karst of the Irkutsk amphitheatre. Moscow: Nauka, 123 p. (in Russian).Google Scholar
  11. WIKA, S., OVCHINNIKOV, G., TRZHTSINSKY, YU. TYC, A., and SZCZYPEK, T., 2000, Development of natural processes on the Bratsk reservoirs banks. — Irkutsk, 76 p. (in Russian).Google Scholar

Copyright information

© Springer 2002

Authors and Affiliations

  • Yu. B. Trzhtsinsky
    • 1
  1. 1.Institute of the Earth’s Crust, Siberian DepartmentRussian Academy of SciencesRussia

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