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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...
The 2010Mw8.8 Maule, Chile earthquake: Nucleation and rupture propagation controlled by a subducted topographic high
2010Mw8.8 Maule Chile earthquake Nucleation rupture propagation controlled a subducted topographic high
2014/4/9
Knowledge of seismic properties in an earthquake rupture zone is essential for understanding the factors controlling rupture dynamics. We use data from aftershocks following the Maule earthquake to de...
Hysteresis-controlled instability waves in a scale-free driven current sheet model
Hysteresis-controlled instability waves scale-free driven current sheet model
2009/11/11
Magnetospheric dynamics is a complex multiscale process whose statistical features can be successfully reproduced using high-dimensional numerical transport models exhibiting the phenomenon of self-or...
Evolution of CO2 in Lakes Monoun and Nyos, Cameroon, before and during controlled degassing
Lake Nyos Lake Monoun hazard mitigation CO2 evolution natural recharge
2017/8/10
Evolution of CO2 in Lakes Monoun and Nyos (Cameroon) before and during controlled degassing is described using results of regular monitoring obtained during the last 21 years. The CO2(aq) profiles soo...