A network of three absolute magnetometer stations and the geomagnetic Observatory of L'Aquila (42º 23N, 13º 19E) allow to monitor possible seismo- or tectonomagnetic effects in Central Italy, using L’Aquila observatory as a reference for differentiation. A system of two VLF search coil wide-band antennas, working in two different frequency bands, at the L’Aquila Observatory, allows to monitor possible electromagnetic effects related to seismic events occurring in Central Italy. Absolute magnetic field observations and VLF signals have been collected for several years. In particular the tectono-magnetic network started its operations in 1989. In this paper we report on the time variation of above mentioned data for the most recent y...
In February 2002 a digital OmniPAL receiver was put into operation at the Department of Physics of ...
It is well established that earthquakes and volcanic eruption can produce small variations in the lo...
Since 2007, a permanent magnetotelluric (MT) monitoring station has been working in the seismic area...
A network of three absolute magnetometer stations and the geomagnetic observatory of LAquila (42°23N...
Tectonomagnetic field observations from absolute magnetic field levels have been collected in Centra...
Tectonomagnetic field observations from absolute magnetic field level measurements were undertaken i...
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...
Tectonic events, as earthquakes and volcanic eruptions, may generate variations in the local geomagn...
Significant variations in the absolute value of the geomagnetic field intensity related to tectonic ...
A scientific collaboration between the Istituto Nazionale di Geofisica (Italy) and the Warsaw Academ...
During the last twenty years a time-synchronized network of magnetometers has operated in Central It...
Abstract. The Italian Istituto Nazionale di Geofisica e Vul-canologia (INGV) tectonomagnetic network...
Following the Mw 6.3 earthquake that hit the city of L'Aquila (Central Italy) on the 6th April 2009,...
In February 2002 a digital OmniPAL receiver was put into operation at the Department of Physics of ...
It is well established that earthquakes and volcanic eruption can produce small variations in the lo...
Since 2007, a permanent magnetotelluric (MT) monitoring station has been working in the seismic area...
A network of three absolute magnetometer stations and the geomagnetic observatory of LAquila (42°23N...
Tectonomagnetic field observations from absolute magnetic field levels have been collected in Centra...
Tectonomagnetic field observations from absolute magnetic field level measurements were undertaken i...
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...
Tectonic events, as earthquakes and volcanic eruptions, may generate variations in the local geomagn...
Significant variations in the absolute value of the geomagnetic field intensity related to tectonic ...
A scientific collaboration between the Istituto Nazionale di Geofisica (Italy) and the Warsaw Academ...
During the last twenty years a time-synchronized network of magnetometers has operated in Central It...
Abstract. The Italian Istituto Nazionale di Geofisica e Vul-canologia (INGV) tectonomagnetic network...
Following the Mw 6.3 earthquake that hit the city of L'Aquila (Central Italy) on the 6th April 2009,...
In February 2002 a digital OmniPAL receiver was put into operation at the Department of Physics of ...
It is well established that earthquakes and volcanic eruption can produce small variations in the lo...
Since 2007, a permanent magnetotelluric (MT) monitoring station has been working in the seismic area...