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  • Articles  (3)
  • 04.07. Tectonophysics  (3)
  • American Geophysical Union (AGU)  (1)
  • Consiglio Nazionale degli Ingegneri  (1)
  • Copernicus  (1)
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  • Articles  (3)
Years
  • 1
    Publication Date: 2020-09-07
    Description: This study presents and discusses horizontal and vertical geodetic velocities for a low strain rate region of the south Alpine thrust front in northeastern Italy obtained by integrating GPS, interferometric synthetic aperture radar (InSAR) and leveling data. The area is characterized by the presence of subparallel, south-verging thrusts whose seismogenic potential is still poorly known. Horizontal GPS velocities show that this sector of the eastern Southern Alps is undergoing ∼1 mm a−1 of NW–SE shortening associated with the Adria–Eurasia plate convergence, but the horizontal GPS velocity gradient across the mountain front provides limited constraints on the geometry and slip rate of the several subparallel thrusts. In terms of vertical velocities, the three geodetic methods provide consistent results showing a positive velocity gradient, of ∼ 1.5 mm a−1, across the mountain front, which can hardly be explained solely by isostatic processes. We developed an interseismic dislocation model whose geometry is constrained by available subsurface geological reconstructions and instrumental seismicity. While a fraction of the measured uplift can be attributed to glacial and erosional isostatic processes, our results suggest that interseismic strain accumulation at the Montello and the Bassano–Valdobbiadene thrusts it significantly contributing to the measured uplift. The seismogenic potential of the Montello thrust turns out to be smaller than that of the Bassano–Valdobbiadene fault, whose estimated parameters (locking depth equals 9.1 km and slip rate equals 2.1 mm a−1) indicate a structure capable of potentially generating a Mw〉6.5 earthquake. These results demonstrate the importance of precise vertical ground velocity data for modeling interseismic strain accumulation in slowly deforming regions where seismological and geomorphological evidence of active tectonics is often scarce or not conclusive.
    Description: Published
    Description: 1681–1698
    Description: 2T. Deformazione crostale attiva
    Description: JCR Journal
    Keywords: Southern Alps ; Vertical Velocities ; GPS and InSAR integration ; Interseismic Deformation ; Dislocation Model ; Seismic Potential ; 04.03. Geodesy ; 04.07. Tectonophysics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
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    Consiglio Nazionale degli Ingegneri
    Publication Date: 2023-07-10
    Description: È tracciato qui un sintetico percorso per descrivere la sismotettonica dell’Italia centrale e settentrionale, attraverso l’analisi delle deformazioni e delle dislocazioni oggi in atto nella litosfera, la porzione più esterna e fredda del pianeta. Usualmente non siamo non grado di renderci conto delle deformazioni crostali attualmente in corso - oggetto di studio della cosiddetta tettonica attiva - ma sappiamo che sono sempre presenti e che da queste si originano i terremoti. Descriveremo pertanto i principali sistemi di faglie ritenuti in grado di generare forti terremoti nell’Italia centrale e settentrionale. La completa parametrizzazione della geometria e della cinematica di una faglia attiva e in grado di generare terremoti viene definita sorgente sismogenetica; ci concentreremo sulle sorgenti ritenute responsabili dei terremoti più forti, in particolare dei terremoti di magnitudo superiore a 5.5. Precisiamo che la magnitudo di 5.5 è ritenuta discriminante per due principali motivi: 1. è usualmente considerata il valore “di soglia” oltre il quale la faglia assume dimensioni tali da poter – in taluni casi – essere identificata attraverso le metodologie geologiche; 2. in Italia, per via delle tipologie costruttive prevalenti, lo scuotimento generato da terremoti crostali con magnitudo superiore a 5.5 può creare danni significativi alle opere antropiche
    Description: Published
    Description: 17-22
    Description: 4T. Sismicità dell'Italia
    Keywords: 04.07. Tectonophysics ; 04.06. Seismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: book chapter
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  • 3
    Publication Date: 2024-03-13
    Description: In mid-September 2021 there was a rapid increase in geophysical and geochemical parameters on the island of Vulcano, Italy, reaching alarming values. This phase of unrest aroused serious concern among Civil Protection, local authorities and the scientific community due to the risk of phreatomagmatic activity, with potentially serious repercussions on the inhabitants of the island and on visiting tourists. The beginning of the unrest was marked by a high occurrence rate of local micro-seismicity related to fluid dynamics within the shallower hydrothermal system (mainly Long Period and Very Long Period events); Volcano-Tectonic (VT) earthquakes increased in late October after most of the monitored parameters reached their climax. Afterwards, major episodes of VT activity were also recorded from March to April and at the end of the year 2022, when an earthquake of ML 4.6 occurred on December 4, SW of the island of Vulcano. Here, we analyze the VT earthquakes from January 2020 to December 2022, in terms of space-time distribution, energy release and focal mechanisms in the framework of the regional geodynamic context and in the light of the main characteristics of the seismic activity recorded in the Vulcano area over the past 36 years.
    Description: Published
    Description: San Francisco, California, USA
    Description: OST3 Vicino alla faglia
    Keywords: earthquakes ; monitoring ; volcano unrest ; Vulcano ; 04.06. Seismology ; 04.07. Tectonophysics ; 04.08. Volcanology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Oral presentation
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