Archeoseismological investigation of the Kurmenty medieval settlement site, northeastern Issyk-Kul region, Kyrgyzstan
А. М. КорженковSchmidt Institute of Physics of the Earth, Russian Academy of Sciences, ul. Bol’shaya Gruzinskaya 10, str. 1, Moscow, 123885, RussiaValerii A. KolchenkoInstitute of History and Cultural Heritage, National Academy of Sciences of Kyrgyz Republic, prosp. Chui 265a, Bishkek, 720000, KyrgyzstanD. V. LuzhanskiyYeltsin Kyrgyz-Russian Slavic University, prosp. Chui 36, str. 60, Bishkek, 720000, KyrgyzstanЕ. А. РогожинSchmidt Institute of Physics of the Earth, Russian Academy of Sciences, ul. Bol’shaya Gruzinskaya 10, str. 1, Moscow, 123885, RussiaMiklós KázmérEötvös University, Pázmány Péter sétány 1/C, Budapest, H-1117, HungaryJonas MažeikaState Research Institute Center of Natural Studies, Akademijos st. 2, Vilnius, LT-08412, LithuaniaE. V. DeevNovosibirsk State University, Novosibirsk, RussiaA. B. FortunaInstitute of Seismology, National Academy of Sciences of Kyrgys Republic, mkrn Asanbai 21, str. 1, Bishkek, 720060, KyrgyzstanJun ShenInstitute of Disaster Prevention, Beijing, ChinaA. S. YudakhinYeltsin Kyrgyz-Russian Slavic University, prosp. Chui 36, str. 60, Bishkek, 720000, KyrgyzstanS. V. AbdievaYeltsin Kyrgyz-Russian Slavic University, prosp. Chui 36, str. 60, Bishkek, 720000, KyrgyzstanS. N. RodinaSchmidt Institute of Physics of the Earth, Russian Academy of Sciences, ul. Bol’shaya Gruzinskaya 10, str. 1, Moscow, 123885, Russia
2016en
ABI
Аннотация
Archeoseismological studies of the Kurmenty settlement have proved the seismogenic origin of the deformation in the walls at this site. The radiocarbon age of the first seismic event damaged the walls of the settlement is 7th century AD. The second seismic event occurred a few centuries later, probably in the late Middle Ages. The strongest seismic events of North Tien Shan occurred in the late 19th–early 20th century as the Chilik (1889, M = 8.4) and Kebin (1911, M = 7.9) also damaged the walls of the Kurmenty settlement. The local shaking intensity during these seismic events was I ≥ VII on MSK-64 scale.
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