Hydrological and hydrogeochemical observations (piezometry, chemistry, electric properties, etc.) carried out in groundwaters in Italy in the past 40 years have been recovered and processed. Available data time series recorded by government agencies, scientific institutions and independent researchers in the field of groundwater and geochemical monitoring in 5480 different sites have been recovered, systematized and processed. Meteorological data useful for data evaluation have been recovered too. Some possible precursors have been identified but the relatively high amount of earthquakes not preceded by hydrologic or geochemical anomalies suggest the need to consider all together geophysical and geochemical parameters for future researches....
Seismic precursors are an as yet unattained frontier in earthquake studies. With the aim of making a...
Hydrological and hydrogeochemical changes caused by pre- and co-seismic processes have been reported...
A seismic swarm characterized by a Ml = 5.9 mainshock occurred in the Po Valley, northern Italy, in ...
Hydrological and hydrogeochemical observations (piezometry, chemistry, electric properties, etc.) ca...
Hydrological and hydrogeochemical observations (piezometry, chemistry, electric properties, etc.) ca...
Central Apennines are one of the highest seismic risk regions in Italy. A number of energetic events...
Central Apennines are one of the highest seismic risk regions in Italy. A number of energetic events...
Hydrological data relative to springs and water wells collected by the Hydrografic National Service ...
Central Apennines are one of the highest seismic risk regions in Italy. A number of energetic events...
International audienceSince late 2002, a continuous automatic monitoring network (CAMN) was designed...
The aim of this thesis is to illustrate the importance of establishing a method of investigation of ...
AbstractWe present the results of a hydrogeochemical survey of 111 springs and wells from Magra Vall...
This work explores three years of geochemical signals recorded by Pieschi station (Southern Italy). ...
The 23 July 1930 earthquake (MS=6.7) in the Southern Apennines (Italy) was a catastrophic event that...
A seismic swarm characterized by a Ml= 5.9 mainshock occurred in the Po Valley, northern Italy, in 2...
Seismic precursors are an as yet unattained frontier in earthquake studies. With the aim of making a...
Hydrological and hydrogeochemical changes caused by pre- and co-seismic processes have been reported...
A seismic swarm characterized by a Ml = 5.9 mainshock occurred in the Po Valley, northern Italy, in ...
Hydrological and hydrogeochemical observations (piezometry, chemistry, electric properties, etc.) ca...
Hydrological and hydrogeochemical observations (piezometry, chemistry, electric properties, etc.) ca...
Central Apennines are one of the highest seismic risk regions in Italy. A number of energetic events...
Central Apennines are one of the highest seismic risk regions in Italy. A number of energetic events...
Hydrological data relative to springs and water wells collected by the Hydrografic National Service ...
Central Apennines are one of the highest seismic risk regions in Italy. A number of energetic events...
International audienceSince late 2002, a continuous automatic monitoring network (CAMN) was designed...
The aim of this thesis is to illustrate the importance of establishing a method of investigation of ...
AbstractWe present the results of a hydrogeochemical survey of 111 springs and wells from Magra Vall...
This work explores three years of geochemical signals recorded by Pieschi station (Southern Italy). ...
The 23 July 1930 earthquake (MS=6.7) in the Southern Apennines (Italy) was a catastrophic event that...
A seismic swarm characterized by a Ml= 5.9 mainshock occurred in the Po Valley, northern Italy, in 2...
Seismic precursors are an as yet unattained frontier in earthquake studies. With the aim of making a...
Hydrological and hydrogeochemical changes caused by pre- and co-seismic processes have been reported...
A seismic swarm characterized by a Ml = 5.9 mainshock occurred in the Po Valley, northern Italy, in ...