Seismic activity has complexity and randomness, and its temporal and spatial distribution
has complexity, stage, level, and inheritance. The study of the temporal and spatial …

Fault barriers are key structures for studying seismic hazard in regions of intense brittle
deformation. The interaction between fault sets affects their seismogenic behavior, if some of …

The seismotectonically induced changes in groundwater radon (Rn) are considered to be
strong imputes for the surveillance of imminent major earthquakes. Groundwater facilitates …

The present study reports measurements of radon in groundwater conducted in China
between January and December 2013. During the measurement period, a great M s= 6.6 …

Here, we employ natural time analysis of seismicity together with non-extensive statistical
mechanics aiming at shortening the occurrence time window of the Kahramanmaraş …

The three aftershock sequences that occurred in Al Hoceima, Morocco, in May 1994 (Mw
6.0), February 2004 (Mw 6.4) and January 2016 (Mw 6.3) were stochastically modeled to …

We examined the spatio-temporal variation of correlation fractal dimension (DC) for M≥ 2. 5
earthquakes in southern and Baja California to ascertain the incidence of seismic precursors …

The Betic Cordillera was formed by the collision between the Alboran Domain and the South
Iberian paleomargin in the frame of the NW–SE convergent Eurasia–Nubia plate boundary …

We propose the use of entropy, H, as an indicator of the equilibrium state of a seismically
active region (seismic system). The relationship between an increase in H and the …

As a step toward probabilistic seismic hazard assessment in the Ibero–Maghreb region, this
study focuses on the estimation and the analysis of main seismic hazard parameters …