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  • 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
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2017-04-04
    Description: The ocean bottom seismometer with hydrophone deployed on the flat top of the Marsili submarine volcano (790 m deep) by the Gibilmanna OBS Lab (CNT–INGV) from 12th to 21st July, 2006, recorded more than 1000 transient seismic signals. Nineteen of these signals were associated with tectonic earthquakes: 1 teleseismic, 8 regional (located by INGV) and 10 small local seismic events (non located earthquakes). The regional events were used to determine sensor orientation. By comparing the signals recorded with typical volcanic seismic activity, we were able to group all the other signals into three categories: 817 volcano–tectonic type B (VT-B) events, 159 occurrences of high frequency tremor (HFT) and 32 short duration events (SDE). Smallmagnitude VT-B swarms, having a frequency band of 2–6 Hz and a mean length of about 30 s, were almost all recorded during the first 7 days. During the last 2 days, the OBS/H mainly recorded HFT events with frequencies of over 40 Hz and of a few minutes in length. Signals that have similar features in frequency and time domain are generally associated with hydrothermal activity. During the last two days a signal was recorded that had a frequency content similar to that of VT-B events was recorded. It will be referred to as continuous volcanic tremor (CVT). The SDE signals, characterized by a quasi-monochromatic waveform and having an exponential decaying envelope, may have been generated by oscillations of resonant bodies excited by magmatic or hydrothermal activity. By applying polarization and parametric spectral analyses, we inferred that the VT-B were probably multi P-phase events having shallow sources that were situated in narrow azimuthal windows in relation to the positions of the OBS/H. The parametric spectral analysis of the SDE signals allowed us to determine their dominant complex frequencies with high accuracy; these frequencies are distributed in two distinct clusters on the complex plane.
    Description: Published
    Description: 17-29
    Description: 2.5. Laboratorio per lo sviluppo di sistemi di rilevamento sottomarini
    Description: JCR Journal
    Description: reserved
    Keywords: Marsili Seamount OBS/H Transient volcano–seismic signals Continuous volcanic tremor Polarization analysis Spectral analysis ; 04. Solid Earth::04.08. Volcanology::04.08.07. Instruments and techniques
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
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