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Titlebook: Seismic Hazard and Building Vulnerability in Post-Soviet Central Asian Republics; Stephanie A. King,Vitaly I. Khalturin,Brian E. Tuc Book

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41#
發(fā)表于 2025-3-28 14:38:21 | 只看該作者
Book 1999clusion is that the risk to residents of thesecities is extremely high. There is a roughly 40% probability that anearthquake will occur near one of the Central Asian republic‘scapitals within the next 20 years. Such an event will produce groundshaking in the affected city equal to the maximum ground
42#
發(fā)表于 2025-3-28 21:33:06 | 只看該作者
43#
發(fā)表于 2025-3-29 00:33:25 | 只看該作者
44#
發(fā)表于 2025-3-29 06:03:30 | 只看該作者
Seismic Hazard of the Central Asia Region, Tajikistan, and Turkmenistan. It is a very complicated region in its geological-tectonic aspect, and it is at present one of the most highly seismic geostructural areas in the world. Much research work in various scientific fields has been directed towards studying the nature of earthquakes, the as
45#
發(fā)表于 2025-3-29 09:36:33 | 只看該作者
Earthquake Resistance of Multi-Story Residential Buildings in Central Asian Capital Cities,strict centralized system for developing and approving building type design and construction codes. Because of this, residential buildings of the same type in these cities are in general of identical design and construction.
46#
發(fā)表于 2025-3-29 12:24:24 | 只看該作者
Seismic Hazard and Building Vulnerability in Kazakhstan,phic coordinates of the central part of the city are 40°14.5′ north latitude and 76°56.9′ east longitude. The elevation of the city is 700 to 900 meters. The founding date of Kazakhstan is considered to be 1868, the year when the fortress Verny, which was located here, became the city of Verny.
47#
發(fā)表于 2025-3-29 17:09:03 | 只看該作者
48#
發(fā)表于 2025-3-29 22:17:13 | 只看該作者
49#
發(fā)表于 2025-3-30 03:29:24 | 只看該作者
50#
發(fā)表于 2025-3-30 07:54:29 | 只看該作者
Destruction of Standard Residential Buildings in the 1988 Spitak, Armenia Earthquake,es of the main causes and characteristics of damage to buildings of different designs, types, and heights, as well as the features of the earthquake shaking on various geological conditions. This chapter has been prepared on the basis of results of inspections of residential and public buildings in
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