The Istituto Nazionale di Geofisica e Vulcanologia (INGV) has systematically undertaken the task of making measurements of the Earth's magnetic field in Italy. By tradition and because of the elongated geometric shape of our peninsula and islands, in Italy, a grid of more than 110 points, called the first order repeat stations, with an average spacing around 55-60 km, is in operation. Over this grid the measurements are repeated regularly, every 5 years. A survey of 131 repeat stations of the Italian Magnetic Network (including 2 observatories, 11 stations in Albania, 3 stations in Corsica and 1 in Malta) was carried out between 2009 and 2010 with the main purpose of updating our magnetic cartography. We describe the characteristics of m...
In 1985.0 the Istituto Nazionale di Geofisica and Istituto Geografico Militare Italiano have complet...
A shaded relief magnetic anomaly map of total intensity of the Earth’s magnetic field for Italy and ...
Tectonic events, as earthquakes and volcanic eruptions, may generate variations in the local geomagn...
<p>The Istituto Nazionale di Geofisica e Vulcanologia (INGV) has systematically undertaken the task ...
In Italy INGV (Istituto Nazionale di Geofisica e Vulcanologia) has systematically undertaken the tas...
In the frame of a collaboration between Istituto Nazionale di Geofisica e Vulcanologia (INGV) and Is...
In the frame of a long-time collaboration between INGV (Istituto Nazionale di Geofisica e Vulcanolog...
The 2010 survey started in September 2009 and was concluded in November 2010. In this period of tim...
Istituto Nazionale di Geofisica e Vulcanologia (INGV) is responsible for systematic magnetic obser...
Attached 4 geomagnetic mapsThe new national geomagnetic network of repeat stations for total field F...
The Italian Magnetic Network is composed of 114 repeat stations and its last complete measurement to...
attached an anomaly map for FA national network of 106 repeat stations for total field F, horizonta...
A survey of 116 repeat stations of the Italian Magnetic Network was carried out between 1989 and 199...
A new national geomagnetic network of repeat stations for total field F, horizontal component H, ver...
In the middle of 1989, the INGV (Italian Istituto Nazionale di Geofisica e Vulcanologia) installed i...
In 1985.0 the Istituto Nazionale di Geofisica and Istituto Geografico Militare Italiano have complet...
A shaded relief magnetic anomaly map of total intensity of the Earth’s magnetic field for Italy and ...
Tectonic events, as earthquakes and volcanic eruptions, may generate variations in the local geomagn...
<p>The Istituto Nazionale di Geofisica e Vulcanologia (INGV) has systematically undertaken the task ...
In Italy INGV (Istituto Nazionale di Geofisica e Vulcanologia) has systematically undertaken the tas...
In the frame of a collaboration between Istituto Nazionale di Geofisica e Vulcanologia (INGV) and Is...
In the frame of a long-time collaboration between INGV (Istituto Nazionale di Geofisica e Vulcanolog...
The 2010 survey started in September 2009 and was concluded in November 2010. In this period of tim...
Istituto Nazionale di Geofisica e Vulcanologia (INGV) is responsible for systematic magnetic obser...
Attached 4 geomagnetic mapsThe new national geomagnetic network of repeat stations for total field F...
The Italian Magnetic Network is composed of 114 repeat stations and its last complete measurement to...
attached an anomaly map for FA national network of 106 repeat stations for total field F, horizonta...
A survey of 116 repeat stations of the Italian Magnetic Network was carried out between 1989 and 199...
A new national geomagnetic network of repeat stations for total field F, horizontal component H, ver...
In the middle of 1989, the INGV (Italian Istituto Nazionale di Geofisica e Vulcanologia) installed i...
In 1985.0 the Istituto Nazionale di Geofisica and Istituto Geografico Militare Italiano have complet...
A shaded relief magnetic anomaly map of total intensity of the Earth’s magnetic field for Italy and ...
Tectonic events, as earthquakes and volcanic eruptions, may generate variations in the local geomagn...