Active compressional tectonics, Quaternary capable faults, and seismic landscape in the Po Plain (N. Italy)

Autor: Michetti, A.M. [1], Giardina, F. [1], Livio, F. [1], Mueller, K. [2], Serva, L. [3], Sileo, G. [1], Vittori, E. [3], Devoti, R. [4], Riguzzi, F. [4], Carcano, C. [5], Rogledi, S. [6], Bonadeo, L. [1], Brunamonte, F. [1], Fioraso, G. [7]

Publikováno v: Annals of geophysics (Online) 55 (2012): 969–1001. doi:10.4401/ag-5462
info:cnr-pdr/source/autori:Michetti, A.M. [1]; Giardina, F. [1]; Livio, F. [1]; Mueller, K. [2]; Serva, L. [3]; Sileo, G. [1]; Vittori, E. [3]; Devoti, R. [4]; Riguzzi, F. [4]; Carcano, C. [5]; Rogledi, S. [6]; Bonadeo, L. [1]; Brunamonte, F. [1]; Fioraso, G. [7]/titolo:Active compressional tectonics, Quaternary capable faults, and seismic landscape in the Po Plain (N. Italy)./doi:10.4401%2Fag-5462/rivista:Annals of geophysics (Online)/anno:2012/pagina_da:969/pagina_a:1001/intervallo_pagine:969–1001/volume:55

It is commonly believed that the Po Plain is an area of low seismic hazard. This conclusion is essentially a combination of two factors: (1) the historical record of earthquakes, which shows a relatively small number of events of moderate magnitude,

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https://publications.cnr.it/doc/208479