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An inventory of river anomalies in the Po Plain, Northern Italy:evidence for active blind thrust faulting
tectonic geomorphology drainage anomaly blind thrust Po Plain 1802 Oglio Valley earthquake
2015/9/16
The Po Plain is a low-relief area characterised by active shortening accommodated by blind thrust faulting. In this almost flat region depositional rates are similar to tectonic rates and deformation ...
Active compressional tectonics, Quaternary capable faults, and the seismic landscape of the Po Plain (northern Italy)
Active compressional tectonics paleoseismology seismic hazard Po Plain foredeep seismic landscape
2015/8/26
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 relativ...
Rapid response to the earthquake emergency of May 2012 in the Po Plain, northern Italy
Emilia 2012 sequence Rapid-response Temporary Seismic Network Sismiko Waveform data
2015/8/26
Rapid-response seismic networks are an important element in the response to seismic crises. They temporarily improve the detection performance of permanent monitoring systems during seismic sequences....
Seismic hazard in the Po Plain and the 2012 Emilia earthquakes
2012 Emilia earthquakes Seismic hazard Ground-motion recordings Design code spectra
2015/8/26
The Emilia earthquakes of May 20, 2012 (Ml 5.9, INGV; Mw 6.11, http://www.bo.ingv.it/RCMT/) and May 29, 2012 (Ml 5.8, INGV; Mw 5.96, http://www.bo.ingv.it/RCMT/) struck an area that in the national re...
Ground effects induced by the 2012 seismic sequence in Emilia:implications for seismic hazard assessment in the Po Plain
ESI 2007scale Coseismic effects Macroseismic intensity Seismic hazard Liquefaction-type phenomena
2015/8/26
Since May 16, 2012, a seismic sequence has affected a wide portion of the Emilia Region (northern Italy), chiefly for the Modena and Ferrara Provinces. The first mainshock (Ml 5.9; focal depth, ca. 6 ...
The INGVterremoti blog:a new communication tool to improve earthquake information during the Po Plain seismic sequence
Seismology Educational Public issues Earthquakes Seismic awareness Seismic hazard
2015/8/26
During a seismic sequence, it is extremely important that the population shaken by the earthquakes has continuous and timely information about the ongoing seismic activity. For this reason, a few days...
The July 17,2011,ML 4.7,Po Plain (northern Italy) earthquake: strong-motion observations from the RAIS network
17th July 2011 earthquake RAIS strong-motion network Po Plain Site effects Ground motion prediction equations Italian seismic code
2015/8/24
On July 17, 2011, at 18:30:23 UTC, a ML 4.7 earthquake occurred on the east side of the Po Plain (northern Italy), between the towns of Ferrara and Rovigo. The epicentral coordinates provided by the N...