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- W4235091431 abstract "Abstract. Soil and debris slides are prone to rapid and dramatic reactivation. Deformation within the instability is accommodated by sliding, whereby weak seismic energies are released through material deformation. Thus, passive microseismic monitoring provides information that relate to the slope dynamics. In this study, passive seismic data acquired at Super-Sauze (Southeastern France) and Pechgraben (Upper Austria) slow-moving clay-rich debris slides (“clayey landslides”) are investigated. Observations are benchmarked to previous similar case studies to provide a comprehensive and homogenized typology of seismic signals at clayey landslides. A well knowledge of the various seismic signals potentially triggered by the slope deformation is crucial for the future development of automatic detection systems to be implemented in early-warning systems. Detected seismic events range from short duration (" @default.
- W4235091431 created "2022-05-12" @default.
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- W4235091431 date "2017-11-23" @default.
- W4235091431 modified "2023-10-14" @default.
- W4235091431 title "Characterizing the complexity of seismic signals at slow-moving clay-rich debris slides: The Super-Sauze (Southeastern France) and Pechgraben (Upper Austria) case studies" @default.
- W4235091431 doi "https://doi.org/10.5194/esurf-2017-65" @default.
- W4235091431 hasPublicationYear "2017" @default.
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