Zobrazeno 1 - 10
of 152
pro vyhledávání: '"P. Palangio"'
Publikováno v:
Annales Geophysicae, Vol 32, Pp 1153-1161 (2014)
An analysis of measurements performed at L'Aquila (Italy) during a deep minimum of solar and magnetospheric activity (2008–2010) allowed for the evaluation of possible contamination of the ultralow-frequency (ULF) spectrum (f ≈ 1–500 mH
Externí odkaz:
https://doaj.org/article/04739b26632e44e7875d3e9664215e94
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 11, Iss 4, Pp 1047-1055 (2011)
On 6 April 2009 at 01:32:39 UT a strong earthquake occurred west of L'Aquila at the very shallow depth of 9 km. The main shock local magnitude was Ml = 5.8 (Mw = 6.3). Several powerful aftershocks occurred the following days. The epicentre of the mai
Externí odkaz:
https://doaj.org/article/22cb7f9678704fadb7a73dfc465876d8
Autor:
U. Villante, M. De Lauretis, C. De Paulis, P. Francia, A. Piancatelli, E. Pietropaolo, M. Vellante, A. Meloni, P. Palangio, K. Schwingenschuh, G. Prattes, W. Magnes, P. Nenovski
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 10, Iss 2, Pp 203-214 (2010)
Several investigations reported the possible identification of anomalous geomagnetic field signals prior to earthquake occurrence. In the ULF frequency range, candidates for precursory signatures have been proposed in the increase in the noise backgr
Externí odkaz:
https://doaj.org/article/09ffa2f344f8415b91b7342d529bf377
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 9, Iss 5, Pp 1567-1572 (2009)
During the last twenty years a time-synchronized network of magnetometers has operated in Central Italy along the Apennine chain to monitor the magnetic field anomalies eventually related to the tectonic activity. At present time the network consists
Externí odkaz:
https://doaj.org/article/81844ba4c0bd40d18ffa824f1801ad3d
Publikováno v:
Annals of Geophysics, Vol 51, Iss 1, Pp 225-236 (2008)
The MEM Project (Magnetic and Electric fields Monitoring) was activated in the INGV Observatory of LAquila since 2004. The principal purpose of the project is to create in Central Italy a network of observatories to monitoring the electromagnetic sig
Externí odkaz:
https://doaj.org/article/61754740de9c4e119a724b5363458227
Publikováno v:
Annals of Geophysics, Vol 51, Iss 1, Pp 137-146 (2008)
Tectonic events, as earthquakes and volcanic eruptions, may generate variations in the local geomagnetic field intensity. To detect possible effects related to seismic activity in central Italy, the INGV (Istituto Nazionale di Geofisica e Vulcanologi
Externí odkaz:
https://doaj.org/article/7853df7b40414a94a62245f46b71e723
Publikováno v:
Advances in Geosciences, Vol 14, Pp 65-68 (2008)
The Italian Istituto Nazionale di Geofisica e Vulcanologia (INGV) tectonomagnetic network was installed in Central Italy since the middle of 1989 to investigate possible magnetic anomalies related to earthquakes. The network is part of the INGV L'Aqu
Externí odkaz:
https://doaj.org/article/3a0354d4ecf44d089169192e6f877ca0
Publikováno v:
Advances in Geosciences, Vol 14, Pp 69-73 (2008)
We are reporting the technological and scientific objectives of the MEM project. The MEM project has been activated in the INGV Observatory of L'Aquila to create in Central Italy a network of observatories in order to monitoring the electromagnetic s
Externí odkaz:
https://doaj.org/article/3e112887202b45d3a59f35fc95a5c29a
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 7, Iss 5, Pp 507-511 (2007)
The technological and the scientific objectives of the MEM (Magnetic and Electric fields Monitoring) project concerning to the study of the electromagnetic signals linked with the Earth's crustal activity are reported. The MEM project has been activa
Externí odkaz:
https://doaj.org/article/ca6d0ab9790b4770b2014b7b76fd587f
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 7, Iss 4, Pp 473-478 (2007)
In the middle of 1989, the INGV (Italian Istituto Nazionale di Geofisica e Vulcanologia) installed in Central Italy a network of magnetic stations in order to investigate possible relationship of the local magnetic field with earthquakes occurrences.
Externí odkaz:
https://doaj.org/article/1224185f5b574313ac4cf7dde46e8e2c