We present two examples of statistical analysis of seismicity conducted by integrating geological, geophysical and seismological data with the aim to characterize the active stress field and to define the spatio-temporal distribution of large earthquakes. Moreover, our data will help to improve the knowledge of the “seismogenic behavior” of the areas and to provide useful information for seismic hazard evaluation. The earthquakes are described by two non-parametric statistical procedures integrating also tectonic-physical parameters to study the spatio-temporal variability. The results show that the areas are characterized by: 1) a stress regime with mainly extensional kinematics; 2) tectonic structures mainly oriented with the active str...
We analyzed the distribution of seismic moment in Italy, computed from instrumental seismicity recor...
In this study, we compute the effect of stress change due to previous historical earthquakes on the ...
International audienceWe develop new approaches to calculating 30-year probabilities for occurrence ...
We present two examples of active stress field analysis conducted by integrating geological, geophys...
[1] The main goal of this work is to provide a probability map for the next moderate to large earthq...
A new non-parametric multivariate model is provided to characterize the spatio-temporal distribution...
A new non-parametric multivariate model is provided to characterize the spatio-temporal distribution...
A new non-parametric multivariate model is provided to characterize the spatio-temporal distribution...
A new non-parametric multivariate model is provided to characterize the spatio-temporal distribution...
The main goal of this work is to provide a probability map for the next moderate to large earthquake...
The main goal of this work is to provide a probability map for the next moderate to large earthquake...
The main goal of this work is to provide a probability map for the next moderate to large earthquake...
The investigation on the spatio-temporal distribution of large earthquakes is still a controversial ...
The investigation on the spatio-temporal distribution of large earthquakes is still a controversial ...
We analyzed the distribution of seismic moment in Italy, computed from instrumental seismicity recor...
We analyzed the distribution of seismic moment in Italy, computed from instrumental seismicity recor...
In this study, we compute the effect of stress change due to previous historical earthquakes on the ...
International audienceWe develop new approaches to calculating 30-year probabilities for occurrence ...
We present two examples of active stress field analysis conducted by integrating geological, geophys...
[1] The main goal of this work is to provide a probability map for the next moderate to large earthq...
A new non-parametric multivariate model is provided to characterize the spatio-temporal distribution...
A new non-parametric multivariate model is provided to characterize the spatio-temporal distribution...
A new non-parametric multivariate model is provided to characterize the spatio-temporal distribution...
A new non-parametric multivariate model is provided to characterize the spatio-temporal distribution...
The main goal of this work is to provide a probability map for the next moderate to large earthquake...
The main goal of this work is to provide a probability map for the next moderate to large earthquake...
The main goal of this work is to provide a probability map for the next moderate to large earthquake...
The investigation on the spatio-temporal distribution of large earthquakes is still a controversial ...
The investigation on the spatio-temporal distribution of large earthquakes is still a controversial ...
We analyzed the distribution of seismic moment in Italy, computed from instrumental seismicity recor...
We analyzed the distribution of seismic moment in Italy, computed from instrumental seismicity recor...
In this study, we compute the effect of stress change due to previous historical earthquakes on the ...
International audienceWe develop new approaches to calculating 30-year probabilities for occurrence ...