Articles | Volume 6, issue 2
https://doi.org/10.5194/esurf-6-525-2018
https://doi.org/10.5194/esurf-6-525-2018
Research article
 | 
27 Jun 2018
Research article |  | 27 Jun 2018

Characterizing the complexity of microseismic signals at slow-moving clay-rich debris slides: the Super-Sauze (southeastern France) and Pechgraben (Upper Austria) case studies

Naomi Vouillamoz, Sabrina Rothmund, and Manfred Joswig

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Naomi Vouillamoz on behalf of the Authors (05 Feb 2018)  Author's response   Manuscript 
ED: Reconsider after major revisions (14 Feb 2018) by Fabian Walter
AR by Naomi Vouillamoz on behalf of the Authors (18 Mar 2018)
ED: Referee Nomination & Report Request started (05 Apr 2018) by Fabian Walter
RR by Andreas Köhler (17 Apr 2018)
RR by Emma Surinach (23 Apr 2018)
ED: Publish subject to minor revisions (review by editor) (01 May 2018) by Fabian Walter
AR by Naomi Vouillamoz on behalf of the Authors (10 May 2018)  Author's response   Manuscript 
ED: Publish as is (04 Jun 2018) by Fabian Walter
ED: Publish as is (05 Jun 2018) by Tom Coulthard (Editor)
AR by Naomi Vouillamoz on behalf of the Authors (07 Jun 2018)
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Short summary
Seismic monitoring of active landslides enables the detection of microseismic signals generated by slope activity. We propose a classification of microseismic signals observed at two active clay-rich debris slides and a simple method to constrain their source origin and their size based on their signal amplitudes. A better understanding of landslide-induced microseismicity is crucial for the development of early warning systems based on landslide-induced microseismic signal precursors.