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Is blind faulting truly invisible?Tectonic-controlled drainage evolution in the epicentral area of the May 2012,Emilia-Romagna earthquake sequence (northern Italy)
Blind faulting Tectonic geomorphology Seismogenic source 2012 Emilia-Romagna earthquake sequence Po Plain
2015/8/26
For decades, alluvial plains have been the areas of the fastest population growth over most of the globe. Modern societies demand growing extensions of flat and easily accessible land to accommodate t...
Static stress transfer from the May 20,2012,M 6.1 Emilia-Romagna (northern Italy) earthquake using a co-seismic slip distribution model
Stress Transfer Slip distribution Italy
2015/8/26
We model the static stress transfer for the May 2012 northern Italy earthquakes, assuming that failure of the crust occurs by shear. This allows the mechanics of the process to be approximated by the ...
Technologies and new approaches used by the INGV EMERGEO Working Group for real-time data sourcing and processing during the Emilia Romagna (northern Italy) 2012 earthquake sequence
Earthquake geology and paleoseismology Coseismic effects Liquefaction GIS Po Plain
2015/8/26
On May 20, 2012, a Ml 5.9 seismic event hit the Emilia Po Plain, triggering intense earthquake activity along a broad area of the Po Plain across the provinces of Modena, Ferrara, Rovigo and Mantova (...
Geological evidence of pre-2012 seismic events, Emilia-Romagna,Italy
Morphogenic earthquakes Seismic hazard assessment
2015/8/26
In May 2012, two moderate (-to-strong) earthquakes that were associated with a noticeable aftershock sequence affected the eastern sector of the Po Plain, Italy, in correspondence with a buried portio...