1887

Abstract

Visco-elastic landslides triggered by seismic phenomena along Adriatic slopes of the Apennine Ridge (Central Italy) are studied in the frame of L-Transfonn applications also accounting for oscillating aspects of their instabilitics (Bland 1960, Flügge 1967, Donnell 1976); starting from elementary one-dimensional model approaches towards two-dirnensional, various landslides representations are suggested and discussed.

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/content/papers/10.3997/2214-4609.201407178
1998-09-14
2020-11-24
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201407178
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