Abstract
Results of retrospective analysis of in situ observations in the dam foundation and adjacent bank rocks of the Sayano-Shushenskaya hydroelectric power station (SSHPS) during the nucleation and energy release of the Altai earthquake of September 27, 2003, are presented. A group of most reliable precursors of this earthquake is identified in measured parameters monitoring the state of the facility and surrounding bedrock. The correlation is examined between the precursor occurrence time and the energy of the earthquakes recorded in the regional catalog in 1990–2005, in the period of the normal SSHPS operation.
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V. I. Bryzgalov, V. D. Baryshnikov, V. A. Bulatov, and L. N. Gakhova, “Monitoring the Stress-Strain State of the Sayano-Shushenskaya Hydroelectric Power Dam,” Gidrotekhn. Stroit., No. 10, 51–59 (2000).
A. I. Lutikov, G. Yu. Dontsova, and S. L. Yunga, “Seismological Analysis of the Gornyi Altai Earthquake of September 27, 2003,” in Geophysical Research (OIFZ RAN, Moscow, 2004), pp. 90–109 [in Russian].
A. N. Marchuk, “New Perspectives in the Experimental Studies in Geodynamics and Earthquake Prediction,” Fiz. Zemli, No. 12, 78–86 (1994).
A. N. Marchuk, “Prediction of Earthquakes in the Area of the Sayano-Shushenskaya Hydroelectric Power Using Dam Measuring Systems,” Gidrotekhn. Stroit., No. 8, 34–38 (1995).
A. I. Savich et al., “An Integrated Approach to Seismic Hazard Protection of Hydropower Works,” Gidrotekhn. Stroit., No. 11, 8–15 (2005).
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Original Russian Text © N.A. Marchuk, 2008, published in Fizika Zemli, 2008, No. 3, pp. 58–64.
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Marchuk, N.A. The Altai earthquake response of the measuring systems of the Sayano-Shushenskaya hydroelectric power station dam on the Yenisei River. Izv., Phys. Solid Earth 44, 226–231 (2008). https://doi.org/10.1134/S1069351308030051
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DOI: https://doi.org/10.1134/S1069351308030051