地震学
地质学
液化
波速
土壤液化
响应分析
剪切(地质)
地震小区分带
清迈
强地震动
岩土工程
地震动
工程类
历史
结构工程
岩石学
民族学
作者
Lindung Zalbuin Mase,Suched Likitlersuang,Tetsuo Tobita
标识
DOI:10.4186/ej.2018.22.3.291
摘要
On 24 March 2011, the 6.8 Mw Tarlay Earthquake occurred at the border of Thailand and Myanmar.The earthquake not only resulted in structural building damage but also triggered liquefactions on sandy soils in Northern Thailand.Several site investigations including SPT and shear wave velocity measurements are conducted to study subsoils condition in this area.Ground motions at several seismic stations were recorded during the earthquake.In this study, four soil sites in Chiang Rai and Chiang Mai are selected, including a site at the border of Thailand and Myanmar.Next generation attenuation models are employed to generate the input ground motions for each site.Non-linear finite element analysis is employed to observe soil behaviour under the earthquake.The results showed that liquefaction could happen in the investigated area during an earthquake.The result is confirmed by the liquefaction evidence found in Chiang Rai during the 6.8 Mw Tarlay Earthquake.This research can help raise awareness of the impacts of earthquakes to this region.
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