Secondary effects generated by earthquakes: liquefaction occurrences in and around Hungary

被引:7
作者
Gyori, Erzsebet [1 ]
Toth, Laszlo [1 ]
Monus, Peter [1 ]
机构
[1] MTA CSFK GGI Kovesligethy Rado Seismol Observ, H-1112 Budapest, Hungary
基金
匈牙利科学研究基金会;
关键词
Earthquake; Liquefaction; Acceleration; Subsoil; AVERAGE HORIZONTAL COMPONENT; GROUND-MOTION; RESPONSE SPECTRA; MAGNITUDE; DISTANCE; PERIODS; MODEL; PGV;
D O I
10.1007/s40328-014-0079-z
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Soil liquefaction have been observed and documented at least eight times during moderate to larger magnitude historical and recent earthquakes in Hungary. Surface manifestations of liquefaction were reported from Komarom (1763, 1783, 1822), Mor (1810), Ermellek (1829, 1834), Kecskemet (1911) and Dunaharaszti (1956) earthquakes. In the study, we give a brief description of these earthquakes and make available reports that demonstrate the occurrence of soil liquefaction. Where available, we describe local subsoil conditions and information regarding ground water level. Distribution of horizontal ground accelerations possibly caused by these historical earthquakes has been modelled by ShakeMap program. Simulations indicate horizontal PGA of 0.2-0.3 g in areas where liquefaction occurred.
引用
收藏
页码:79 / 95
页数:17
相关论文
共 39 条