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Slope Seismic Response Monitoring on the Aftershocks of the Wenchuan Earthquake in the Mianzhu Section
by
WANG Yunsheng LUO Yonghong WANG Fuhai WANG Dong MA Xiao LI Shun DENG Xi
in
Earth and Environmental Science
/ Earth Sciences
/ Earthquakes
/ Ecology
/ Environment
/ Geography
/ Geological surveys
/ Overburden
/ Quaternary
/ Seismic activity
/ Seismic response
/ Seismology
/ Slope stability
/ 中国地质调查局
/ 地震余震
/ 地震反应
/ 地震响应
/ 汶川
/ 监测断面
/ 绵竹市
/ 边坡
2012
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Slope Seismic Response Monitoring on the Aftershocks of the Wenchuan Earthquake in the Mianzhu Section
by
WANG Yunsheng LUO Yonghong WANG Fuhai WANG Dong MA Xiao LI Shun DENG Xi
in
Earth and Environmental Science
/ Earth Sciences
/ Earthquakes
/ Ecology
/ Environment
/ Geography
/ Geological surveys
/ Overburden
/ Quaternary
/ Seismic activity
/ Seismic response
/ Seismology
/ Slope stability
/ 中国地质调查局
/ 地震余震
/ 地震反应
/ 地震响应
/ 汶川
/ 监测断面
/ 绵竹市
/ 边坡
2012
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Slope Seismic Response Monitoring on the Aftershocks of the Wenchuan Earthquake in the Mianzhu Section
by
WANG Yunsheng LUO Yonghong WANG Fuhai WANG Dong MA Xiao LI Shun DENG Xi
in
Earth and Environmental Science
/ Earth Sciences
/ Earthquakes
/ Ecology
/ Environment
/ Geography
/ Geological surveys
/ Overburden
/ Quaternary
/ Seismic activity
/ Seismic response
/ Seismology
/ Slope stability
/ 中国地质调查局
/ 地震余震
/ 地震反应
/ 地震响应
/ 汶川
/ 监测断面
/ 绵竹市
/ 边坡
2012
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Slope Seismic Response Monitoring on the Aftershocks of the Wenchuan Earthquake in the Mianzhu Section
Journal Article
Slope Seismic Response Monitoring on the Aftershocks of the Wenchuan Earthquake in the Mianzhu Section
2012
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Overview
Previous investigations have shown that the seismic response of slopes during the Wenchuan earthquake was highly variable. The present study tries to give an answer to the question: Which are the main factors affecting the seismic response degree of slopes? With the support of the China Geological Survey Bureau, we set 3 monitoring sections in Jiulong slope, Mianzhu city, China with the aim to record the site response of the slope during the affershoeks of the Wenehuan earthquake. After the Wenchuan earthquake, which happened on 12 May 2008, 30 aftershocks have been recorded in these monitoring points. We analyzed 11 records, with magnitudes ranging from ML = 4.6 to ML = 3.1. The amplification factors of the horizontal compound PGA and 3D compound PGA have been determined for the 3 points at different elevations on the slope. Results showed that the dynamic response of the slope on the earthquake was controlled by factors such as topography and the thickness of the Quaternary overburden.
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