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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 ...
Liquefaction phenomena along the paleo-Reno River caused by the May 20,2012,Emilia (northern Italy) earthquake
Seismic hazard assessment Po Plain Morphogenic earthquakes
2015/8/26
On the May 20, 2012 (04:03:52 local time; 02:03:52 UTC), a moderate earthquake (Ml 5.9) [Scognamiglio et al. 2012, this volume] with a focal mechanism showing E-W-trending, S-dipping, reverse-faulting...
Slip rates on the Chelungpu and Chushiang thrust faults inferred from a deformed strath terrace along the Dungpuna river, west central Taiwan
Slip rates on the Chelungpu Chushiang thrust faults a deformed strath terrace along the Dungpuna river west central Taiwan
2014/4/15
The Chelungpu fault produced the September 1999Mw= 7.6 Chi-Chi earthquake,central Taiwan. The shortening rate accommodated by this structure, integrated over several seismic cycles, and its contributi...
Millennialsliprate of the Longitudinal Valley fault from river terraces: Implications for convergence across the active suture of eastern Taiwan
Millennials Pirate Longitudinal Valley fault river terraces Implications for convergence across the active suture eastern Taiwan
2014/4/15
The Longitudinal Valley fault is a key element in the active tectonics of Taiwan. It is the principal structure accommodating convergence across one of the two active sutures of the Taiwan orogeny. To...