Liquefaction, ground fissures and coastline change during the Egio earthquake (15 June 1995; Central‐Western Greece)
Liquefaction, ground fissures and coastline change during the Egio earthquake (15 June 1995; Central‐Western Greece)
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DOI：
10.1111/j.1365-3121.1996.tb00793.x
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发表时间：
1996-11
期刊：
影响因子：
2.4
通讯作者：
E. Lekkas;S. Lozios;E. Skourtsos;H. Kranis
中科院分区：
文献类型：
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作者：
E. Lekkas;S. Lozios;E. Skourtsos;H. Kranis
破坏性地震（Ms = 6.1 R）袭击了埃吉奥镇和北方伯罗奔尼撒半岛（希腊）周边地区，产生了广泛的液化，地面裂缝和海岸线的变化。历史数据表明，同一地区曾经历过间歇性地震破坏，一些孕震现象在同一地点再次发生。最后，它被证实，这是一个高地震风险区，适当的建筑设计和规划，可以减少潜在的危险，如果地球动力学设置是适当考虑。
The destructive earthquake (Ms = 6.1 R) that hit the town of Egio and the surrounding area of the Northern Peloponnessos (Greece) generated extensive liquefaction, ground fissuring and coastline changes. Historical data indicate that the same region has experienced episodic earthquake damage, with some seismogenic phenomena having reoccurred at the same locations. In conclusion, it is confirmed that this is a high seismic risk region, where proper building design and planning can reduce the potential danger if the geodynamic setting is properly taken into account.