Abstract
Being a country exposed to strong seismicity, the estimation of seismic hazard in Tajikistan is essential for urbanized areas, such as the rapidly growing capital city Dushanbe. To ensure people’s safety and adequate construction work, a detailed seismic microzonation is the key to proper hazard planning. Existing estimations of seismic hazard date back to 1978; they are based on engineering geological investigations and observed macroseismic data. Thereupon relies the Tajik Building Code, which considers seismic intensities according to the Medvedev–Sponheuer–Karnik Scale, MSK-64. However, this code does not accurately account for soil types, which vary considerably in Dushanbe—not only by their nature, but also due to increasing anthropogenic influences. In this study, we performed a series of analyses based on microtremor array measurements, seismic refraction tomography, and instrumental data recording from permanent stations for standard spectral ration and from mobile seismic stations for the horizontal to vertical spectral ratio in order to provide a comprehensive full-cover microzonation of Dushanbe accounting for soil types. Our results identify several critical areas where major damage is likely to occur during strong earthquakes.
Subject
General Earth and Planetary Sciences
Reference72 articles.
1. Seismic Conditions of the Territory of Tajikistan;Babaev,2005
2. Strong Motion Service of Tajikistan;Negmatullaev,1987
3. The Khait Earthquake of 1949 July 10: Effect on Regime of Dushanbe and Garm;Katok,1965
4. Neue seismische Skala Intensity Scale of Earthquakes, 7. Tagung der Europäischen Seismologischen Kommission vom 24. 9. bis 30. 9. 1962 in Jena, DDR;Medvedev,1964
5. Liquefaction-Induced Flow Slide in the Collapsible Loess Deposit in Soviet Tajik
Cited by
5 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献