Geophysical investigation of a large landslide in glaciolacustrine clays in the Trièves area (French Alps) (original) (raw)
2009, Engineering Geology
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Geophysical investigation of a large landslide in glaciolacustrine clays in the Trièves
2000
article i nfo Slope movements in clay deposits are spread all over the world and result from complex deformation processes, including internal strains in the landslide body and slipping along rupture surfaces. Such mass movements are likely to generate changes in the geophysical parameters characterizing the ground, which can be used to map the landslide body. In the last decade,
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