IJG  Vol.2 No.2 , May 2011
Seismic-Geodynamic Monitoring of Main Electric Power-Stations in East Europe and North Asia
ABSTRACT
In east Europe and north Asia the majority of nuclear power-stations (NPS) as well as large hydro-electric (HES) and thermal electric stations (TES) are located within the north Eurasian lithosphere plate, which is characterized by the low seismicity and weak modern tectonic activity besides the different exogenetic processes. Some operating and projected NPS are relatively near to zones of the moderate seismicity in the Kaliningrad Region of northwest Russia and in south Ukraine. HES and TES in Baltic, Byelorussia and Ukraine are in the same position. Zones of more intensive seismicity and existence of active faults include NPS, HEP and TEP in the Urals, the Kola Peninsula, south Siberia, Transbaikal and Far East regions of Russia. Some of these stations are situated within crust blocks in transit zones, which separate main lithosphere plates and are characterized by increased tectonic mobility. The electric power-stations are most danger in the transit zones between north Eurasian, Arabian and Indian lithosphere plates, where collision processes have yet not stopped. This concerns electric stations in central Asia and Caucasus including NPS in Armenia. Seven schemes of the seismic energy distribution are composed for different parts of east Europe and north Asia. The location of nuclear and main other electric power-stations on them makes it possible to form a correct estimate of negative consequences connected with the up-to-date inner-continental tectonic activity.

Cite this paper
nullY. Gatinsky, D. Rundquist, G. Vladova and T. Prokhorova, "Seismic-Geodynamic Monitoring of Main Electric Power-Stations in East Europe and North Asia," International Journal of Geosciences, Vol. 2 No. 2, 2011, pp. 75-83. doi: 10.4236/ijg.2011.22008.
References
[1]   V. G. Trifonov, O. V. Soboleva, R. V. Trifonov and G. A. Vostrikov, “Recent Geodynamics of the Alpine-Himala- yan Collision Belt,” Transactions of the Geological Institute RAS, In Russian, Vol. 541, 2002, pp. 1-224.

[2]   D. V. Rundkvist, Yu. G. Gatinsky, W. A. Bush and V. G. Kossobokov, “The Area of Russia in the Present-Day Structure of Eurasia: Geodynamics and Seismicity,” In: D. K. Chowdhury, Ed., Computational Seismology and Geo- dynamics, American Geophysics Union, Washington, 2005, pp. 224-233.

[3]   Yu. G. Gatinsky, D. V. Rundquist and Yu. S. Tyupkin, “Block Structures and Kinematics of Eastern and Central Asia from GPS Data,” Geotectonics, Vol. 39, No. 5, 2005, pp. 333-348.

[4]   Yu. G. Gatinsky, D. V. Rundquist and Yu. S. Tyupkin, “Block Structure and Kinematics of Western Eurasia According to GPS Data,” Geotectonics, Vol. 41, No. 1, 2007, pp. 26-37. doi:10.1134/S0016852107010049

[5]   Yu. G. Gatinsky, D. V. Rundquist, G. Vladova and T. Prokhorova, “Up-to-Date Geodynamics and Seismicity of Central Asia,” International Journal of Geosciences, Vol. 2, No. 1, 2011, pp. 1-12. doi:10.4236/ijg.2011.21001

[6]   Yu. G. Gatinsky, V. I. Zakharov, G. L. Vladova, T. V. Prokhorova and Yu. N. Sirota, “Applying of the Remote Sensing for Choosing an Area of the Nuclear Power-Station Construction,” Proceedings of IKI Conference Modern Problems of the Earth Remote Sensing from Cosmos, Moscow, 15-19 November 2010, pp. 262-263.

[7]   K. G. Levi, S. I. Sherman and V. A. San’kov, “Modern Geodynamics of Asia,” In: K. G. Levi and S. I. Sherman, Eds., Actual Problems of Modern Geodynamics of Central Asia, In Russian, Siberian Branch of RAS, Novosibirsk, 2005, pp. 253-267.

[8]   L.V. Podgornyi, “Heat Flow Map of Polar Territories in 1:30000000 Scale,” In Russian, Nedra, Moscow, 1997.

[9]   Yu. G. Gatinsky, T. V. Prokhorova, D. V. Rundquist and G. L. Vladova, “Zones of Catastrophic Earthquakes of Central Asia: Geodynamics and Seismic Energy,” 2009. http://dx.doi.org/10.2205/2009ES000326

 
 
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