2nd Croatian Conference on Earthquake Engineering 2CroCEE

ABSTRACT

The introductory part of this work gives a brief description of the recent earthquakes that have occurred in recent years in the Republic of Kazakhstan.
The following is more detailed information about the consequences of an earthquake: the scale of destruction, the procedure for dealing with the consequences of an earthquake, methods of strengthening buildings.

Annotation

The territory of the south and south-east of Kazakhstan is one of the most seismic of the Central Asian seismically active east of the Kazakhst. Over the past three, 120 strong earthquakes have occurred here: Vernenskoye – 7.3 with a magnitude of 1887, Chilikskoye – with a magnitude of 8.3 since 1889, and Keminskoye – with a magnitude of 8.2 since 1911, and the weaker number (5-7 points) is estimated in dozens.
Seismic regions of Kazakhstan occupy about 43% of the total area of the territory of the republic. More than 6 million live here. a person or about 40% of the total Kazakh population of the city. At the same time, the population of the city, in 9 living-2.0 million, is a ball zone. a person (V. G.) in the core. Almaty – 1.85 million people); in the 8-ball zone-1.1 million people; in the 7-ball zone – 2.0 million and 6-ball zone – 1.2 million people.
The earthquake of May 12, 2003 at 01:23 a.m. occurred Destructive local time (on May 12 at 18: 22 GMT) Of the Republic of Kazakhstan in the part west of the territory of the southern (350 km) city of Almaty, east (100 km) of the city. Taraz, point coordinates VS: 42o 52' s.sh., 72o 53' v.d. at the epicenter station of Lugovoye village. According to the data of the engineering seismometric station "Almaty" to the Lugovsky magnet, the earthquakes are M = 5.4 on the Richter scale, the focal depth (different estimates) is from 4 to 8 kom. According to the intensity of the MSK scale of the earthquake at the epicenter of 7-8, the score is 64. For almost 3 to 3 repeated Aftershocks with a ball intensity every day for months.
With the intensity of non-residential earthquakes in the house, the Lugovskoye earthquake depends on the manifestation, engineering-soil geological characteristics, space-planning structural and solutions, as well as the quality of construction work, damage to the severity of various combat tasks.
By earthquake manifestation, settlements and districts of intensity. T.Ryskulova the following are grouped into groups: 7-8 points (Lugovaya station), 7 points (village Enbekshi, Kokaryk, Kzylsharva), 6-7 points (village polovoy, Akbul, Karakyst, Zhalpaksaz, Bayteli), 6 points (village Kazakh, Tashol, Zhaksylyk), 5-6 points (village karasi, Kokdone, Zhanaturmys).