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  • 1
    Publikationsdatum: 2017-04-04
    Beschreibung: Quaternary tectonics of the abruzzi Appennines (Italy) inferred from integrated geomorfological-stratigraphic data
    Beschreibung: Published
    Beschreibung: Rimini
    Beschreibung: 3.10. Sismologia storica e archeosismologia
    Beschreibung: open
    Schlagwort(e): quaternary tectonics Abruzzi apennines ; 02. Cryosphere::02.02. Glaciers::02.02.03. Geomorphology
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: Oral presentation
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Publikationsdatum: 2017-04-04
    Beschreibung: Setting new tools to quantify the tectonic and gravity contribution in seismogenic areas
    Beschreibung: Published
    Beschreibung: Rimini
    Beschreibung: 3.10. Sismologia storica e archeosismologia
    Beschreibung: open
    Schlagwort(e): seismogenic areas ; 02. Cryosphere::02.02. Glaciers::02.02.03. Geomorphology
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: Oral presentation
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Publikationsdatum: 2017-04-04
    Beschreibung: In the present work we analyse one of the active normal faults affecting the central Apennines, i.e. the Mt. Morrone normal fault system. This tectonic structure, which comprises two parallel, NW-SE trending fault segments, is considered as potentially responsible for earthquakes of magnitude C 6.5 and its last activation probably occurred during the second century AD. Structural observations performed along the fault planes have allowed to define the mainly normal kinematics of the tectonic structure, fitting an approximately N 20 trending extensional deformation. Geological and geomorphological investigations performed along the whole Mt. Morrone south-western slopes permitted us to identify the displacement of alluvial fans, attributed to Middle and Late Pleistocene by means of tephro-stratigraphic analyses and geomorphological correlations with dated lacustrine sequences, along the western fault branch. This allowed to evaluate in 0.4 ± 0.07 mm/year the slip rate of this segment. On the other hand, the lack of synchronous landforms and/or deposits that can be correlated across the eastern fault segment prevented the definition of the slip rate related to this fault branch. Nevertheless, basing on a critical review of the available literature dealing with normal fault systems evolution, we hypothesised a total slip rate of the fault system in the range of 0.4 ± 0.07 to 0.8 ± 0.09 mm/year. Moreover, basing on the length at surface of the Mt. Morrone fault system (i.e. 22–23 km) we estimated the maximum expected magnitude of an earthquake that might originate along this tectonic structure in the order of 6.6–6.7.
    Beschreibung: Dipartimento della Protezione Civile Nazionale
    Beschreibung: In press
    Beschreibung: 3.2. Tettonica attiva
    Beschreibung: JCR Journal
    Beschreibung: open
    Schlagwort(e): Active fault ; Slip rate ; Maximum expected magnitude ; Continental stratigraphy ; Sulmona basin ; Central Apennines ; 04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismology
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: article
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Publikationsdatum: 2017-04-04
    Beschreibung: Paleoseismological techniques have been applied to characterize the kinematic behavior of large-scale gravitational phenomena located in proximity of the seismogenic fault responsible for the Mw 7.0, 1915 Avezzano earthquake and to identify evidence of a possible coseismic reactivation. The above mentioned techniques were applied along the surface expression of the main sliding planes of the Mt. Serrone gravitational deformation - located in the southeastern border of the Fucino basin (central Italy) - allowing us to detect instantaneous events of deformation along the uphill-facing scarp. These events are testified by the presence of faulted deposits and by colluvial wedges. The identified and chronologically-constrained episodes of rapid displacement can be probably correlated with seismic events determined by the activation of the Fucino seismogenic fault, affecting the toe of the gravitationally unstable rock mass. Indeed this fault can produce strong, short-term dynamic stresses able to trigger the release of local gravitational stress accumulated by Mt. Serrone’s large-scale gravitational phenomena.
    Beschreibung: Published
    Beschreibung: 164-174
    Beschreibung: 3.2. Tettonica attiva
    Beschreibung: JCR Journal
    Beschreibung: restricted
    Schlagwort(e): Deep-seated gravitational slope deformations ; Active fault ; Paleoseismology ; Seismic triggering ; 04. Solid Earth::04.04. Geology::04.04.03. Geomorphology
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: article
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    Publikationsdatum: 2020-02-24
    Beschreibung: Active faulting is one of the main factors that induce deep-seated gravitational slope deformations (DGSDs). In this study, we investigate the relationships between the tectonic activity of the NW–SE normal fault system along Mt. Morrone, central Apennines, Italy, and the evolution of the associated sackung-type DGSD. The fault system is considered to be the source of M 6.5–7 earthquakes. Our investigations have revealed that the DGSD began to affect the Mt. Morrone SW slope after the Early Pleistocene. This was due to the progressive slope instability arising from the onset of the younger western fault, with the older eastern fault acting as the preferred sliding zone. Paleoseismological investigations based on the excavation of slope deposits across gravitational troughs revealed that the DGSD was also responsible for the displacement of Late Pleistocene–Holocene sediments accumulated in the sackung troughs. Moreover, we observed that the investigated DGSD can evolve into large-scale rock slides. Therefore, as well as active normal faulting, the DGSD should be considered as the source of a further geological hazard. Overall, our approach can be successfully applied to other contexts where active normal faults control the inception and evolution of a DGSD.
    Beschreibung: Published
    Beschreibung: 88-101
    Beschreibung: 2T. Tettonica attiva
    Beschreibung: JCR Journal
    Beschreibung: open
    Schlagwort(e): Large-scale slope instability; ; Active normal faulting ; Trenching technique ; Rock avalanche ; Sulmona basin ; Central Italy ; 02. Cryosphere::02.02. Glaciers::02.02.03. Geomorphology
    Repository-Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Materialart: article
    Standort Signatur Einschränkungen Verfügbarkeit
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