Geomorphological and paleoseismological evidence of capable faulting in the Northern Apennines (Italy): Insights into active tectonics and seismic hazard of the Lunigiana basin

Autor: Nirta G.[1], Vittori E.[1, Blumetti A.M.[2], Di Manna P.[2], Benvenuti M.[3], Montanari D.[1], Perini M.[4], Fiera F.[4], Moratti G.[1], Baglione M.[5], Piccardi L. [1]

Publikováno v: Geomorphology (Amst.) 374 (2021). doi:10.1016/j.geomorph.2020.107486
info:cnr-pdr/source/autori:Nirta G.[1], Vittori E.[1,2], Blumetti A.M.[2], Di Manna P.[2], Benvenuti M.[3], Montanari D.[1], Perini M.[4], Fiera F.[4], Moratti G.[1], Baglione M.[5], Piccardi L. [1]/titolo:Geomorphological and paleoseismological evidence of capable faulting in the Northern Apennines (Italy): Insights into active tectonics and seismic hazard of the Lunigiana basin/doi:10.1016%2Fj.geomorph.2020.107486/rivista:Geomorphology (Amst.)/anno:2021/pagina_da:/pagina_a:/intervallo_pagine:/volume:374

The Lunigiana basin is a NW trending tectonic depression located in the Northern Apennines of Italy. The basin is bounded by active normal faults, characterized by moderate to strong seismicity, with historical earthquakes reaching up to magnitude 6

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http://www.cnr.it/prodotto/i/443767