Add to ORKGIn this work we apply a probabilistic procedure to estimate the macroseismic intensity attenuation in the volcanic areas of Italy which allows to exploit additional information on historical earthquakes following the Bayesianapproach. The method starts from the intensity data points of the selected earthquakes and arrives at theassessment of the probability distribution for the intensity at a site given the epicentral intensity and thesite-epicenter distance. The CMTE local earthquake catalogue has been used for the Etna region while for theother Italian volcanic districts (Aeolian Islands, Ischia, Vesuvius and Albani Hills) the CPTI04 Italian seismic catalogue and the DBMI04 associated database have been considered. For the analysis, subse...
In the framework of the UPStrat-MAFA project, a seismic hazard assessment has been undertaken in the...
Seismic intensity is, by definition, an index for the classification of the severity of earthquake e...
The regional intensity attenuation and its variation as a function of the distance and earthquake si...
In Italian volcanic areas, we apply a probabilistic procedure for Macroseismic Intensity Attenuation...
In this work we apply a probabilistic procedure to estimate the macroseismic intensity attenuation i...
We present the probabilistic version of the analysis performed in Azzaro et al. (2006a) on the atten...
Results of probabilistic seismic hazard assessment (PSHA), in terms of macroseismic intensity applie...
Intensity attenuation and its variation as a function of the distance and earthquake size is still a...
This article has been originated by thoughts on previous analyses related to the probabilistic treat...
The analysis of the seismic attenuation is a prominent and problematic component of hazard assessmen...
Earthquakes are, by far, the most relevant source of hazard for the densely urbanised areas of Mt. E...
One of the most common practice to estimate the effects of a past earthquakes at given localities wh...
In this paper, we apply a probabilistic procedure to model the attenuation of the macroseismic inten...
A detailed analysis of the intensity attenuation in the Etna and other Italian volcanic districts, w...
We present a method that allows us to incorporate additional information from the historical earthqu...
In the framework of the UPStrat-MAFA project, a seismic hazard assessment has been undertaken in the...
Seismic intensity is, by definition, an index for the classification of the severity of earthquake e...
The regional intensity attenuation and its variation as a function of the distance and earthquake si...
In Italian volcanic areas, we apply a probabilistic procedure for Macroseismic Intensity Attenuation...
In this work we apply a probabilistic procedure to estimate the macroseismic intensity attenuation i...
We present the probabilistic version of the analysis performed in Azzaro et al. (2006a) on the atten...
Results of probabilistic seismic hazard assessment (PSHA), in terms of macroseismic intensity applie...
Intensity attenuation and its variation as a function of the distance and earthquake size is still a...
This article has been originated by thoughts on previous analyses related to the probabilistic treat...
The analysis of the seismic attenuation is a prominent and problematic component of hazard assessmen...
Earthquakes are, by far, the most relevant source of hazard for the densely urbanised areas of Mt. E...
One of the most common practice to estimate the effects of a past earthquakes at given localities wh...
In this paper, we apply a probabilistic procedure to model the attenuation of the macroseismic inten...
A detailed analysis of the intensity attenuation in the Etna and other Italian volcanic districts, w...
We present a method that allows us to incorporate additional information from the historical earthqu...
In the framework of the UPStrat-MAFA project, a seismic hazard assessment has been undertaken in the...
Seismic intensity is, by definition, an index for the classification of the severity of earthquake e...
The regional intensity attenuation and its variation as a function of the distance and earthquake si...