Seismic Activation in the Eastern Part of the Southern Slope of the Great Caucasus in the Late XX to Early XXI Centuries

Author:

Yetirmishli G. J.,Mammadli T. Y.,Rogozhin E. A.,Sysolin A. I.

Publisher

Pleiades Publishing Ltd

Subject

Atmospheric Science,Oceanography

Reference36 articles.

1. Agamirzoev, R.A., Seismotektonika Azerbaidzhanskoi chasti Bol’shogo Kavkaza (Seismotectonics of the Azerbaijan Part of the Greater Caucasus), Baku: Elm, 1987.

2. Aref’ev, S.S., Pletnev, K.G., Tatevosyan, R.E., et al., The Racha earthquake of 1991: Results of field seismological observations, Fiz. Zemli, 1993, no. 3, pp. 12–23.

3. Aref’ev, S.S., Rogozhin, E.A., Bykova, V.V., and Dorbath, C., Deep structure of the Racha earthquake source zone from seismic tomography data, Izv.,Phys. Solid Earth, 2006, vol. 42, no. 1, pp. 27–40.

4. Babayan, T.O., Kuliev, F.T., Papalashvili, V.G., Shebalin, N.V., and Vandysheva, N.V., II. The Greater Caucasus (50–1974, M ≥ 4.0, I 0 ≥ 5), Novyi katalog sil’nykh zemletryasenii na territorii SSSR s drevneishikh vremen do 1975 g (New Catalog of Earthquakes in the USSR Territory from Ancient Times to 1975), Moscow: Nauka, 1977, pp. 69–170.

5. Balakina, L.M., Mechanism of the source of the Racha earthquake, Fiz. Zemli, 1993, no. 3, pp. 42–52.

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