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The study objective was to derive a susceptibility model for shallow landslides that could include process-related non-stationary variables, to be adaptable to climate changes. We selected the territory of the Mont-Emilius and Mont-Cervin Mountain Co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0780672d3fe2a6c6d9a8d4aa4322f749
http://hdl.handle.net/11588/868937
http://hdl.handle.net/11588/868937
