In the present paper, we analyse ground tilt and seismicity at Campi Flegrei caldera and Ischia Island, two volcanic areas located in the south of Italy. These areas have been well studied for many years from a petrological, volcanological and geophysical view point. Moreover, due to the high seismic and volcanic risk for the populations living there, they are continuously monitored by networks of geophysical and geochemical sensors. We summarize the most important results that we obtained so far, concerning the observations of relationships between seismic activity and ground tilt anomalies, focusing on the time interval 2015–2018. First, we present a detailed description of the tiltmeter and seismic networks in both the investigate...
The present study analysed volcano tectonic earthquakes that occurred in the caldera of Campi Flegre...
In 2004, the DINEV project started in the Campi Flegrei - Vesuvius volcanic areas (Scarpa et al., 20...
We report, for the first time, evidence of seismically induced soft-sediment deformations in the cen...
In the present paper, we analyse ground tilt and seismicity at Campi Flegrei caldera and Ischia Isl...
In the present paper, we analyse ground tilt and seismicity at Campi Flegrei caldera and Ischia Isl...
The study of the ground deformation in active calderas provides valuable indications of the ongoing...
Since 2004 a research project has been developed to monitor subsurface deformation of Italian volcan...
Volcanoes are complex systems whose dynamics is the result of the interplay between endogenous and e...
We analyse tiltmetric time series recorded at borehole instruments recently installed at Campi Flegr...
The Campi Flegrei is an active volcanic area characterized by many different eruptive episodes. A pe...
We report, for the first time, evidence of seismically induced soft‐sediment deformations in the cen...
A network of tiltmeters has been operational on Vulcano Island for numerous years. At present, the n...
This paper analyses data regarding the seismicity and ground deformations of the island of Ischia. T...
The tiltmetric dataset of Phlegrean Fields area showed a discrete correlation with the volcanic dyna...
The knowledge of the dynamic of the Campi Flegrei calderic system is a primary goal to mitigate the ...
The present study analysed volcano tectonic earthquakes that occurred in the caldera of Campi Flegre...
In 2004, the DINEV project started in the Campi Flegrei - Vesuvius volcanic areas (Scarpa et al., 20...
We report, for the first time, evidence of seismically induced soft-sediment deformations in the cen...
In the present paper, we analyse ground tilt and seismicity at Campi Flegrei caldera and Ischia Isl...
In the present paper, we analyse ground tilt and seismicity at Campi Flegrei caldera and Ischia Isl...
The study of the ground deformation in active calderas provides valuable indications of the ongoing...
Since 2004 a research project has been developed to monitor subsurface deformation of Italian volcan...
Volcanoes are complex systems whose dynamics is the result of the interplay between endogenous and e...
We analyse tiltmetric time series recorded at borehole instruments recently installed at Campi Flegr...
The Campi Flegrei is an active volcanic area characterized by many different eruptive episodes. A pe...
We report, for the first time, evidence of seismically induced soft‐sediment deformations in the cen...
A network of tiltmeters has been operational on Vulcano Island for numerous years. At present, the n...
This paper analyses data regarding the seismicity and ground deformations of the island of Ischia. T...
The tiltmetric dataset of Phlegrean Fields area showed a discrete correlation with the volcanic dyna...
The knowledge of the dynamic of the Campi Flegrei calderic system is a primary goal to mitigate the ...
The present study analysed volcano tectonic earthquakes that occurred in the caldera of Campi Flegre...
In 2004, the DINEV project started in the Campi Flegrei - Vesuvius volcanic areas (Scarpa et al., 20...
We report, for the first time, evidence of seismically induced soft-sediment deformations in the cen...