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  • 1
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    In:  J. Geodynamics, L'wiw, 3-4, vol. 38, no. 2, pp. 147-159, pp. L24312, (ISSN: 1340-4202)
    Publication Date: 2004
    Keywords: Modelling ; cracks and fractures (.NE. fracturing) ; Volcanology ; Plate tectonics ; Boundary Element Method ; Fluids ; JGD ; Kuehn ; Kuhn
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  • 2
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    In:  Geophys. J. Int., Warszawa, Pergamon, vol. 130, no. 1, pp. 183-192, pp. L19306, (ISBN: 0-12-018847-3)
    Publication Date: 1997
    Keywords: Moment tensor ; Volcanology ; Seismicity ; GJI
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  • 3
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    In:  Geophys. J. Int., Warszawa, Pergamon, vol. 141, no. 3, pp. 623-638, pp. L19306, (ISBN: 0-12-018847-3)
    Publication Date: 2000
    Keywords: Boundary Element Method ; Modelling ; cracks and fractures (.NE. fracturing) ; Fluids ; Rock mechanics ; fracture ; growth ; propagation ; Volcanology
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  • 4
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    In:  Geophys. J. Int., Warszawa, Pergamon, vol. 142, no. 1, pp. 181-192, pp. L19306, (ISBN: 0-12-018847-3)
    Publication Date: 2000
    Keywords: cracks and fractures (.NE. fracturing) ; Fluids ; Gravimetry, Gravitation ; Fracture ; Rock mechanics ; Modelling ; Inelastic ; Rheology ; Volcanology ; dykes ; Two-dimensional ; Elasticity ; Boundary Element Method ; GJI
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  • 5
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    Forschungszentrum Jülich GmbH
    In:  Professional Paper, Volcanic Tremor and Magma Flow, Jülich, Forschungszentrum Jülich GmbH, vol. 4, no. 16, pp. 97-114, (ISBN 1-86239-165-3, vi + 330 pp.)
    Publication Date: 1991
    Keywords: Fluids ; Tectonics ; Seismicity ; Volcanology
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  • 6
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    In:  J. Volcanology Geothermal Res., Tokyo, Lawrence Livermore National Laboratory, vol. 144, no. 1-4, pp. 273-285, pp. L18610, (ISSN: 1340-4202)
    Publication Date: 2005
    Keywords: Volcanology ; Laboratory measurements ; Modelling ; cracks and fractures (.NE. fracturing) ; Plate tectonics ; JVGR ; Boettinger ; Bottinger ; analogue ; experiments ; layered ; media ; fluid-filled ; fractures ; dike ; propagation ; sill
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  • 7
    Publication Date: 2021-06-16
    Description: According to the U.S. Geological Survey’s Earthquake Hazards Program, a seismic swarm is “a localized surge of earth- quakes, with no one shock being conspicuously larger than all other shocks of the swarm. They might occur in a variety of geologic environments and are not known to be indicative of any change in the long- term seismic risk of the region in which they occur” (http://vulcan.wr.usgs.gov/Glossary/ Seismicitydescription_earthquakes.html). The definition reveals how little is actually known about seismic swarms. For example, could certain seismic settings be more prone to swarms? Could a fault zone prone to large energetic earthquakes release part of its stress through seismic swarms? Do swarms keep hazards in balance, or could their onset increase hazards? To gain insight into the nature of seismic swarms in nonvolcanic areas and to better understand their influence on seismic hazards, the Istituto Nazionale di Geofisica e Vulcanologia (INGV) and the German Research Centre for Geoscience (GFZ) began a combined research project within the framework of the Network of European Research Infrastructures for Earthquake Risk Assessment and Mitigation (NERA; see http:// www.nera-eu.org/). The project focused on monitoring swarm activity occurring in the Pollino range in Southern Apennines, Italy.
    Description: Published
    Description: 361-372
    Description: 1.1. TTC - Monitoraggio sismico del territorio nazionale
    Description: N/A or not JCR
    Description: restricted
    Keywords: Pollino ; Seismic Swarms ; Seismic Hazard ; Rapid Response Networks ; 04. Solid Earth::04.06. Seismology::04.06.06. Surveys, measurements, and monitoring
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 8
    Publication Date: 2017-04-04
    Description: The Institute for Geophysics at Hamburg University and the Research Center for Marine Geoscience (GEOMAR) of Kiel University have developed new, wideband ocean bottom seismic stations for long-term, deep sea deplyments of up to 1 year.
    Description: Published
    Description: 309-315
    Description: 1.4. TTC - Sorveglianza sismologica delle aree vulcaniche attive
    Description: open
    Keywords: Ocean Bottom Seismometer ; Tyrrhenian Sea ; 04. Solid Earth::04.06. Seismology::04.06.06. Surveys, measurements, and monitoring
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 9
    Publication Date: 2017-04-04
    Description: With the scientific purpose to monitor the micro-seismicity in the Central Apennines, we recently deployed in Eastern Tuscany (Casentino) a temporary 12 element seismic array, composed exclusively of 3-component seismometers. During the one month of registration we recorded an unexpected high rate of local micro-seismicity with up to 180 events per day.
    Description: Published
    Description: Rome
    Description: 1.1. TTC - Monitoraggio sismico del territorio nazionale
    Description: open
    Keywords: Tornillos ; seismicity ; Northern Apennines ; 04. Solid Earth::04.06. Seismology::04.06.06. Surveys, measurements, and monitoring
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Oral presentation
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  • 10
    Publication Date: 2017-04-04
    Description: We present results from the first crustal seismic tomography for the southern Tyrrhenian area, which includes ocean bottom seismometer (OBS) data and a bathymetry correction. This area comprises Mt. Etna, the Aeolian Islands, and many volcanic seamounts, including the Marsili Seamount. The seismicity distribution in the area depends on the complex interaction between tectonics and volcanism. The 3-D velocity model presented in this study is obtained by the inversion of P wave arrival times from crustal earthquakes. We integrate travel time data recorded by an OBS network (Tyrrhenian Deep Sea Experiment), the SN-1 seafloor observatory, and the land network. Our model shows a high correlation between the P wave anomaly distribution and seismic and volcanic structures. Two main low-velocity anomalies underlie the central Aeolian Islands and Mt. Etna. The two volumes, which are related to the well-known active volcanism, are separated and located at different depths. This finding, in agreement with structural, petrography, and GPS data from literature, confirms the independence of the two systems. The strongest negative anomaly is found below Mt. Etna at the base of the crust, and we associate it with the deep feeding system of the volcano. We infer that most of the seismicity is generated in brittle rock volumes that are affected by the action of hot fluids under high pressure due to the active volcanism in the area. Lateral changes of velocity are related to a transition from the western to the central Aeolian Islands and to the passage from continental crust to the Tyrrhenian oceanic uppermost mantle.
    Description: Published
    Description: 3703–3719
    Description: 1.4. TTC - Sorveglianza sismologica delle aree vulcaniche attive
    Description: 3.3. Geodinamica e struttura dell'interno della Terra
    Description: JCR Journal
    Description: open
    Keywords: ocean bottom seismometers ; southern Tyrrhenian Sea ; seismic tomography ; Aeolian Islands ; Etna ; oceanic continental crust ; 04. Solid Earth::04.06. Seismology::04.06.06. Surveys, measurements, and monitoring ; 04. Solid Earth::04.06. Seismology::04.06.07. Tomography and anisotropy ; 04. Solid Earth::04.07. Tectonophysics::04.07.04. Plate boundaries, motion, and tectonics ; 04. Solid Earth::04.07. Tectonophysics::04.07.06. Subduction related processes ; 04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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