A scientific collaboration between the Istituto Nazionale di Geofisica (Italy) and the Warsaw Academy of Science (Poland) gave rise to the installation of a few stations for the long-term measurement of magnetotelluric fields in Central Italy. The investigation sites were determined following the individual seismic interest of each location. For this project, the magnetic observatory in L'Aquila was also equipped with electric lines, for simultaneous measurements of the telluric field. After a few years of experience some of the installed stations had to be removed for their high noise level that made this study almost impossible. A first time interval was considered from January 1992 to February 1993 and showed the existence of significant...
This paper reports the analyses of ULF (Ultra-Low-Frequency) geomagnetic field observations coming f...
Following the Mw 6.3 earthquake that hit the city of L'Aquila (Central Italy) on the 6th April 2009,...
There has recently been much discussion of large-scale interactions of fault zones and the influence...
A scientific collaboration between the Istituto Nazionale di Geofisica (Italy) and the Warsaw Academ...
A scientific collaboration between the Warsaw Academy of Science, (Poland) and the National Institut...
It has been reported that earthquakes and volcanic eruptions produce significant variations in the g...
Magnetotelluric data were collected at Collemeluccio (41.72°N, 14.37°E) in Central Italy from summer...
Tectonomagnetic field observations from absolute magnetic field levels have been collected in Centra...
Significant variations in the absolute value of the geomagnetic field intensity related to tectonic ...
Tectonic events, as earthquakes and volcanic eruptions, may generate variations in the local geomagn...
A network of three absolute magnetometer stations and the geomagnetic Observatory of L'Aquila (42º ...
A network of three absolute magnetometer stations and the geomagnetic observatory of LAquila (42°23N...
Since 2007, a permanent magnetotelluric (MT) monitoring station has been working in the seismic area...
Tectonomagnetic field observations from absolute magnetic field level measurements were undertaken i...
During the last twenty years a time-synchronized network of magnetometers has operated in Central It...
This paper reports the analyses of ULF (Ultra-Low-Frequency) geomagnetic field observations coming f...
Following the Mw 6.3 earthquake that hit the city of L'Aquila (Central Italy) on the 6th April 2009,...
There has recently been much discussion of large-scale interactions of fault zones and the influence...
A scientific collaboration between the Istituto Nazionale di Geofisica (Italy) and the Warsaw Academ...
A scientific collaboration between the Warsaw Academy of Science, (Poland) and the National Institut...
It has been reported that earthquakes and volcanic eruptions produce significant variations in the g...
Magnetotelluric data were collected at Collemeluccio (41.72°N, 14.37°E) in Central Italy from summer...
Tectonomagnetic field observations from absolute magnetic field levels have been collected in Centra...
Significant variations in the absolute value of the geomagnetic field intensity related to tectonic ...
Tectonic events, as earthquakes and volcanic eruptions, may generate variations in the local geomagn...
A network of three absolute magnetometer stations and the geomagnetic Observatory of L'Aquila (42º ...
A network of three absolute magnetometer stations and the geomagnetic observatory of LAquila (42°23N...
Since 2007, a permanent magnetotelluric (MT) monitoring station has been working in the seismic area...
Tectonomagnetic field observations from absolute magnetic field level measurements were undertaken i...
During the last twenty years a time-synchronized network of magnetometers has operated in Central It...
This paper reports the analyses of ULF (Ultra-Low-Frequency) geomagnetic field observations coming f...
Following the Mw 6.3 earthquake that hit the city of L'Aquila (Central Italy) on the 6th April 2009,...
There has recently been much discussion of large-scale interactions of fault zones and the influence...