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  • 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous  (2)
  • 04. Solid Earth::04.06. Seismology::04.06.04. Ground motion  (1)
  • Astronomy
  • E31
  • E52
  • J24
  • Geophysical Research Abstracts, Vol. 9, 06583, 2007  (1)
  • IUSS Press Pavia  (1)
  • Taylor and Francis  (1)
Collection
Keywords
Years
  • 1
    Publication Date: 2017-04-04
    Description: In July 2006, INGV (Istituto Nazionale di Geofisica e Vulcanologia) successfully deployed on the flat top of the submarine Marsili volcano, the first Italian OBS/H (Ocean Bottom Seismometer with Hydrophone), entirely developed at the Gibilmanna Geophysical Observatory within a project funded by an agreement between Italian National Civil Protection Department (DPC) and INGV. In this short deployment the OBS/H was equipped with a Nanometrics Trillium 40s seismometer and an OAS E- 2PD Hydrophone. A 21 bits four channel digitizer (SEND MLS) recorded data at 200 sps to exploit, as well as possible, the wide flat response of the hydrophone (0-5 KHz). For long-term deployments, the instrument will be provided with Cox-Webb 500s-2 Hz differential pressure gauge and Nanometrics Trillium 120s or Guralp CMG40TOBS and will record data at 50 sps, for as long as one or two years respectively, depending on the seismic sensor. Most of the recorded events (about 800) seem to be associated with the active nearby Marsili volcano. The instrument, during the 9 days of the test at a depth of 790 m, recorded 835 volcano-tectonic events, classifiable in 6 different categories: 1 teleseismic event (Java 2006/07/17, Mw=7.2), 8 located regional tectonic events, 9 not located local tectonic events, 705 low frequency volcanic events, 84 high frequency volcanic events, 26 “Tornillo” and 2 probable rockfall events. Spectral analysis shows, in the first 7 days of the deployment, an evident sequence of low energy events superimposed on the continuous background volcanic tremor, with dominant frequencies between 2 and 6 Hz, known in literature as VT-B (Volcanic-Tectonic event, type B) and related to shallow hypocenters (above 1-2 km). In the last two days of operation, the hydrophone recorded high frequency events, with dominant frequencies between 40 and 90 Hz; this kind of event could be associated with hydrothermal activity. In March 2007, three INGV OBS/H will be deployed in the southern Ionian sea, at different distances from the Malta escarpment, within the European project NERIES (Network of Research Information Infrastructures for European Seismology). At present, we are planning a further improvement of the instrument, equipping it with a 24 bits digitizer and a communication system based on an acoustic modem and a low power consumption PC with ARM processor. In this way, it would be possible to pick up events traces from the OBS on the sea bottom, without recovering it. Furthermore, the acoustic link with a buoy, in its turn satellite linked with an on shore control centre, in association with triggering algorithms, could be employed to insert the INGV OBS/H in a tsunami warning system.
    Description: Published
    Description: Vienna
    Description: 2.5. Laboratorio per lo sviluppo di sistemi di rilevamento sottomarini
    Description: open
    Keywords: OBS ; OBS/H ; Marsili ; Ocean Bottom Seismometer ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Oral presentation
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  • 2
    Publication Date: 2012-02-03
    Description: N/A
    Description: Published
    Description: 23-34
    Description: 4.2. TTC - Modelli per la stima della pericolosità sismica a scala nazionale
    Description: 5.1. TTC - Banche dati e metodi macrosismici
    Description: N/A or not JCR
    Description: reserved
    Keywords: Sismicità storica ; Pericolosità sismica ; Abruzzo ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 3
    Publication Date: 2017-04-04
    Description: The aim of this article is to investigate the ground motion attenuation of the most industrialized and populated regions of Italy, evaluating the capability of different approaches to estimate site dependent models. The 5.2 magnitude earthquake on November 24, 2004 shocked the areas of Northern Italy producing damage of about 215 million euros. The data set, including 243 earthquakes of local magnitude up to 5.2, has been collected in the period December 2002–October 2005 by 30 threecomponent seismic stations managed by Istituto Nazionale di Geofisica e Vulcanologia, Sezione of Milano (INGV-MI). Empirical attenuation relationships have been estimated for horizontal peak ground velocity (PGHV), acceleration (PGHA), displacement (PGHD), and for response spectral acceleration (SA) for periods between 0.1 and 1.5 s. To estimate suitable attenuation models, in particular for sites characterized by thick sedimentary geological formations, a soil discrimination based on EU8 code can lead to wrong evaluations. On the contrary, a classification based on H/V spectral ratios of seismic ambient noise (NHV) allows the models to fit better real and predicted data and to reduce the uncertainties of the process. For each receiver, NHV have been strengthened by additional H/V spectral ratio of earthquake data (EHV), calculated considering different portions of the analysed signals. In order to validate the PGHA attenuation relationship for greater magnitudes, accelerometric records, relative to Central-Northern Italy strong motions occurring in the last 30 years, have been collected and superimposed to our attenuation curves.
    Description: Published
    Description: 943-967
    Description: 4.1. Metodologie sismologiche per l'ingegneria sismica
    Description: JCR Journal
    Description: open
    Keywords: site effects ; 04. Solid Earth::04.06. Seismology::04.06.04. Ground motion
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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