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Geophysical characterization of areas prone to quick-clay landslides using radio-magnetotelluric and seismic methods
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文摘

High-resolution seismic and RMT data were acquired for studying quick-clay landslides.

Results suggest that both coarse-grained materials and bedrock play key roles.

Quick clays overlay coarse-grained materials that overlap bedrock.

Bedrock shows at places a full bowl-shaped structure implying minimum risk of a landslide.

Two possible scenarios triggering quick-clay landslides are presented.

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