Abstract
Three strong earthquakes that occurred since the end of 8th century have been identified by archeoseismic data in the southwestern part of the Tere Khol’ Depression. The dates for these events are the 9th, 12th, and first two-thirds of 19th century, and the average recurrence interval is 500 years. The relative seismic passivity of the Tere Khol’ Depression at present may be related to the relatively recent discharge of stress in seismogenerating sources.
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References
S. G. Arzhannikov, Geol. i Geofiz. 41(11), 1499 (2000).
S. I. Vainshtein, Sov. Etnografiya, No. 6, 103 (1964).
E. P. Vasil’ev, V. G. Belichenko, and L. Z. Reznitskii, Dokl. Akad. Nauk 353(6), 789 (1997).
D. A. Klements, Archeological Diary on Travel to Middle Mongolia in 1891 (St. Petersburg, 1895) [in Russian].
A. V. Klyuchevskii, V. M. Dem’yanovich, and G. Bayar, Geol. i Geofiz. 46(7), 746–762 (2005).
A. V. Koshurnikov, Yu. D. Zykov, A. V. Panin, et al., Inzhenernye Izyskaniya, No. 6, 28 (2008).
A. A. Nikonov, Voprosy inzhenernoi seismologii, issue 31, pp. 137–142.
The New Catalogue of Strong Earthquakes within the Territory of Soviet Union since Ancient Times until 1975 (Nauka, Moscow, 1977) [in Russian].
O. P. Polyanskii and N. L. Dobretsov, Dokl. Akad. Nauk 380(3), 368–373 (2001).
V. I. Ulomov, Vulkanologiya i Seismologiya, No. 4/5, 6 (1999).
G. A. Chernov, Seismic Geology of the Eastern Part of the Altai-Sayan Mountain Region (Nauka, Novosibirsk, 1978) [in Russian].
Ramsey C. Bronk, Oxford Radiocarbon Accelerator Unit, http://c14.arch.ox.ac.uk/oxcal.php.
F. Galadini, K.-G. Hinzen, and S. Stiros, J. Seismol. 10, 395 (2006).
P. J. Reimer, M. G. L. Baillie, E. Bard, et al., Radiocarbon 46, 1029 (2004).
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Original Russian Text © A.V. Panin, 2011, published in Doklady Akademii Nauk, 2011, Vol. 438, No. 1, pp. 76–81.
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Panin, A.V. New data on the late holocene seismicity of the southwestern edge of the Baikal Rift Zone. Dokl. Earth Sc. 438, 563–568 (2011). https://doi.org/10.1134/S1028334X11050060
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DOI: https://doi.org/10.1134/S1028334X11050060