Archeoseismological investigation of the Kurmenty medieval settlement site, northeastern Issyk-Kul region, Kyrgyzstan

被引：0

作者：

A. M. Korzhenkov

V. A. Kol’chenko

D. V. Luzhanskiy

E. A. Rogozhin

M. Kazmer

J. V. Mazeika

E. V. Deev

A. B. Fortuna

J. Shen

A. S. Yudakhin

S. V. Abdieva

S. N. Rodina

机构：

[1] Russian Academy of Sciences,Schmidt Institute of Physics of the Earth

[2] National Academy of Sciences of Kyrgyz Republic,Institute of History and Cultural Heritage

[3] Yeltsin Kyrgyz-Russian Slavic University,Trofimuk Institute of Oil and Gas Geology and Geophysics

[4] Eötvös University,Institute of Seismology

[5] State Research Institute Center of Natural Studies,undefined

[6] Siberian Branch of the Russian Academy of Sciences,undefined

[7] Novosibirsk State University,undefined

[8] National Academy of Sciences of Kyrgys Republic,undefined

[9] Institute of Disaster Prevention,undefined

来源：

Seismic Instruments | 2016年 / 52卷 / 2期

关键词：

archeoseismology; Kurmenty settlement; Silk Road; Turkic peoples; Middle Ages; seismic deformations; radiocarbon age; Issyk-Kul depression; Tien Shan; Kyrgyzstan;

D O I：

10.3103/S0747923916020055

中图分类号：

学科分类号：

摘要：

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.

引用

页码：154 / 163

页数：9

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Peshkov Yu.(undefined)undefined undefined undefined undefined-undefined

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Savelieva T.(undefined)undefined undefined undefined undefined-undefined

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Korjenkov A.M.(undefined)undefined undefined undefined undefined-undefined

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