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  • Greece  (2)
  • seismic survey
  • 2020-2022  (3)
  • 1
    Publication Date: 2020-11-09
    Description: A long-term gravity and elevation changes time series (2001-2006) at the restless caldera of Nisyros in Greece is here reported. After a period of intense seismic activity (1995-1998), associated with an increase of fumarolic activity and ground deformation of Nisyros volcano which no any eruption occurred, and then a gravity network was settled in June 2001 and re-occupied annually up to 2004 and in June 2006. Discrete gravity measurements have been carried out at located benchmarks surrounding Nisyros island in proximity to hydrotermal area within the caldera floor and taking into account the effect of the vertical ground movements in order to quantify gravity changes of the volcano. A general positive observed gravity change was determined at all stations of the network inside caldera rim. In the same time, a temporal and spatial evolution of the gravity changes was found between 2001 and 2004: it was observed a steady-rise in gravity variations between 2001-2003, obtaining maximum positive gravity variations up to +60 Gal confined in the caldera floor area at the base of the presently active crater, where the most fumarolic activity is concentrated; in contrast a spatial distribution of gravity changes is recorded during 2003-2004 and the maximum positive gravity variations are confined in the caldera rim near Nikia village. In this way residual gravity changes were obtained and applications of Gausss theorem to the study of the excess mass recorded during 2001-2006 is explored. During recent unrest period magma replenishment genereted a great quantity of steam hot hydrothermal fluids which is released towards the surface underneath the southeastern part of the caldera floor. The gravity changes might be attributed to the migration of fluids probably occurring through pre-existing faults.
    Description: Published
    Description: Perugia (Italy), 2-13 July 2007
    Description: 2V. Struttura e sistema di alimentazione dei vulcani
    Description: 6V. Pericolosità vulcanica e contributi alla stima del rischio
    Description: 6SR VULCANI – Servizi e ricerca per la società
    Keywords: Nisyros ; Greece ; gravity changes ; gravity monitoring ; volcanic hazards ; GPS
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Conference paper
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  • 2
    Publication Date: 2020-11-18
    Description: Negli ultimi anni l'incremento di fenomeni di sprofondamento nel territorio di Roma Capitale e nella sua area metropolitana costituisce un rischio sempre maggiore per la popolazione e per le infrastrutture. Il verificarsi di questi eventi è in gran parte dei casi connesso alla presenza di sistemi caveali di origine antropica e diversa età e funzione. Il presente studio ha permesso di perfezionare un protocollo speditivo di utilizzo integrato di alcuni metodi geofisici (microgravimetrico, georadar e sismico) funzionale all’individuazione di cavità nel sottosuolo, che permette di mappare dimensioni, distribuzione spaziale e profondità. Tale base informativa risulta imprescindibile per una gestione in sicurezza degli edifici scolastici esistenti e per la progettazione di nuovi interventi.
    Description: Published
    Description: 1 dicembre 2017, Sala Convegni del CNR, P. le Aldo Moro, Roma
    Description: 7A. Geofisica per il monitoraggio ambientale
    Description: 7SR AMBIENTE – Servizi e ricerca per la società
    Keywords: Rome ; microgravity survey ; gpr ; seismic survey
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Abstract
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  • 3
    Publication Date: 2020-11-09
    Description: The island of Nisyros is a stratovolcano at the eastern end of the Hellenic island arc. This arc of volcanoes is related to the northward subduction of the African plate beneath the Aegean microplate. The eastern sector of the arc, including the islands of Kos, Yiali and Nisyros seems to be geodynamically very active since it comprises the largest volumes of volcanic products and is at present a region of high tectonic unrest. The island of Nisyros is almost circular, with an average diameter of 8 km, and covers an area of approximately 42 km2. It lies above a basement of Mesozoic limestone and the volcanic edifice of Nisyros comprises a succession of calc-alkaline lavas and pyroclastic rocks, with a summit caldera of an average diameter of 4 km. In June 2001, a microgravity network was installed on the Nysyros island, with the aim to monitor gravity variations and report changes, if any, in elevation and/or density induced by geodynamic activity. Topographic monitoring of gravity benchmarks based on a differential-mode, dual-frequency GPS, started in 2002. The sites were selected in parts of the island experiencing different seismic-tectonic processes, in order to detect their relative movements. In June 2002, monitoring measurements by the microgravity network was repeated for the first time. The comparison of the resulting values with those recorded in 2001 showed a maximum variation of +0.034 mGal in the active volcanic area, with an increasing trend towards South. In 2003 and 2004, the monitoring measurements was repeated again. The resulting G variations were comparable to those observed in 2001-2002. However, with the installation of a new station in 2002, the G variations proved to be confined to the most active volcanic areas. The extent of the variations recorded between 2001 and 2004 largely exceeded the measuring errors, suggesting that such variations are to be ascribed to mass variations of the volcanic complex.
    Description: Published
    Description: Pucon-Chile, 14-19 novembre 2004
    Description: 5V. Processi eruttivi e post-eruttivi
    Description: 6V. Pericolosità vulcanica e contributi alla stima del rischio
    Description: 6SR VULCANI – Servizi e ricerca per la società
    Keywords: Nisiros ; Greece ; gravity monitoring ; deformation monitoring survey
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Extended abstract
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