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  • 1
    In: Geophysical Journal International, Oxford University Press (OUP)
    Abstract: We investigate temporal and spatial variations of the spectral decay parameter kappa (κ) before and after the April 6, 2009, L'Aquila earthquake (Mw 6.1), in central Italy. We analyzed foreshocks ten days before and aftershocks occurring ten days and six months after this main event. We select earthquakes with magnitudes Mw ≥ 3.2 registered by the seismic network of central Italy within a radius of 20 km from the epicenter of the L'Aquila mainshock and having hypocenter distances of less than 170 km. We separate near-source, along-path and near-site contributions of κ for each group of events and we detected temporal variations of this S-wave attenuation parameter. We find that ten days before the mainshock κ along the path has the lowest values, probably due to high tectonic stress accumulated, in agreement with previous investigations performed with other techniques, then κ increases during the main event and remains constant during the first ten days of aftershocks. The aftershocks that occurred six months after show an increase in the regional attenuation probably due to the tectonic stress released during the main shock and the earlier aftershocks. From the spatial point of view, ten days before the principal event the foreshocks located to the south show an increase in the near-source attenuation towards the northeast, in the direction of the mainshock. These spatial variations of κ may be related to the presence of crustal fluids near the rupture area, as evidenced by other previous studies. The first ten days of aftershocks that concentrate around the main earthquake have high near-source κ, and those located north of the main rupture have lower values. These observations are consistent with previous investigations that show variations of elastic and anisotropic crustal properties during the L'Aquila earthquake sequence due to dilatancy and fluid diffusion processes within the nucleation zone. We conclude that temporal variations of the spectral decay parameter κ provide important clues for the earthquake cycle in central Italy.
    Type of Medium: Online Resource
    ISSN: 0956-540X , 1365-246X
    Language: English
    Publisher: Oxford University Press (OUP)
    Publication Date: 2024
    detail.hit.zdb_id: 3042-9
    detail.hit.zdb_id: 2006420-2
    detail.hit.zdb_id: 1002799-3
    SSG: 16,13
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  • 2
    Online Resource
    Online Resource
    Seismological Society of America (SSA) ; 2022
    In:  Bulletin of the Seismological Society of America Vol. 112, No. 6 ( 2022-12-01), p. 3037-3045
    In: Bulletin of the Seismological Society of America, Seismological Society of America (SSA), Vol. 112, No. 6 ( 2022-12-01), p. 3037-3045
    Abstract: We investigated the temporal variation of the spectral decay parameter κ before and after two main earthquakes that occurred in the central Italy region, namely the Amatrice (Mw 6.0) of 24 August 2016 and the Norcia (Mw 6.5) of 30 October 2016 earthquakes. For this analysis, we used seismograms from the central Italy dense seismic array stations, and earthquakes located at hypocenter distances r & lt; 80 km, having magnitudes Mw 3.4–6.5. The dataset consists of 393 events recorded at 92 stations. We estimated, for both earthquake sequences, average functions κ˜(r) that describe the distance dependence of κ along the S-wave source-station paths using acceleration spectra from foreshocks, mainshock, and aftershocks. We observed that there was a regional attenuation drop within approximately two months after the Amatrice earthquake. Then, κ˜(r) tends to return toward the attenuation values observed before the occurrence of the main event, namely to the values of κ˜(r) obtained from the foreshocks, when the earthquake cycle is probably completed. We also estimated the near-source kappa (κs) using aftershocks from 24 August 2016 to 3 September 2016. The results show that the values of κs are lower than those from aftershocks located to the north near the epicenter of the Amatrice earthquake, suggesting that the tectonic stress was probably high near the rupture zone, and that there may be a likely fluid flow of crustal fluids. κ˜(r) obtained from the foreshocks of the Norcia earthquake is like that calculated with the records of the Amatrice aftershocks. Then, κ˜(r) drops to lower attenuation values during the Norcia main event and tends to increase again during the aftershocks. From the analysis of these two earthquake sequences that occurred in a short-time interval in central Italy, we conclude that the temporal variation of κ˜(r) could be a valuable indicator to monitor the earthquake cycle.
    Type of Medium: Online Resource
    ISSN: 0037-1106 , 1943-3573
    Language: English
    Publisher: Seismological Society of America (SSA)
    Publication Date: 2022
    detail.hit.zdb_id: 2065447-9
    SSG: 16,13
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  • 3
    Online Resource
    Online Resource
    Springer Science and Business Media LLC ; 2023
    In:  Bulletin of Earthquake Engineering Vol. 21, No. 9 ( 2023-07), p. 4111-4137
    In: Bulletin of Earthquake Engineering, Springer Science and Business Media LLC, Vol. 21, No. 9 ( 2023-07), p. 4111-4137
    Abstract: We propose a new fully nonergodic ground motion model for Central Italy, which is one of the most sampled areas in the world after the occurrence of the last seismic sequences of 2009 and 2016–2017. The model predicts 69 ordinates of the Fourier Amplitude Spectrum in the magnitude range 3.2–6.5 and is constrained on a dense set of seismological and geophysical parameters (i.e. stress-drop $$\Delta \sigma$$ Δ σ , shear-wave velocity in the uppermost 30 m, V S,30 and high-frequency attenuation parameter at source $${\kappa }_{source}$$ κ source and site $${\kappa }_{0}$$ κ 0 ) made available from a non-parametric generalized inversion technique (GIT). The aim of this work is to capture the underlying physics of ground motion related to different source energy levels, as well as to the crustal and geological structure of the region, thus providing less uncertain predictions. Calibration is performed using a stepwise regression approach which has the advantage of taking a more complex functional form ( advanced model) when all physical parameters are known while returning a simpler form ( base model) when physical data are missing. As a result, the advanced model reproduces the reference rock motion of the region in case the site additional proxies are set to their average values ( V S,30  = 1100 m/s, $${\kappa }_{0}$$ κ 0 =15 ms). We show that the inclusion of the set of physically-based explanatory variables in the regression has a beneficial effect in constraining the uncertainty, leading to a reduction of the high-frequency variability of about 70% on the between-event and 35% on the site-to-site. This reduction can be viewed as the result of the combination of a more effective physical description through the incorporation of the additional proxies and a calibration embedded in a completely nonergodic framework.
    Type of Medium: Online Resource
    ISSN: 1570-761X , 1573-1456
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2023
    detail.hit.zdb_id: 2098452-2
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  • 4
    In: Acta Geodaetica et Geophysica, Springer Science and Business Media LLC, Vol. 53, No. 3 ( 2018-9), p. 439-461
    Type of Medium: Online Resource
    ISSN: 2213-5812 , 2213-5820
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2018
    detail.hit.zdb_id: 2705307-6
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  • 5
    Online Resource
    Online Resource
    Springer Science and Business Media LLC ; 2022
    In:  Acta Geodaetica et Geophysica Vol. 57, No. 4 ( 2022-12), p. 529-562
    In: Acta Geodaetica et Geophysica, Springer Science and Business Media LLC, Vol. 57, No. 4 ( 2022-12), p. 529-562
    Abstract: We develop a new inversion approach to construct a 3-D structural and shear-wave velocity model of the crust based on teleseismic P-to-S converted waves. The proposed approach does not require local earthquakes such as body wave tomography, nor a large aperture seismic network such as ambient noise tomography, but a three-component station network with spacing similar to the expected crustal thickness. The main features of the new method are: (1) a novel model parametrization with 3-D mesh nodes that are fixed in the horizontal directions but can flexibly vary vertically; (2) the implementation of both sharp velocity changes across discontinuities and smooth gradients; (3) an accurate ray propagator that respects Snell’s law in 3-D at any interface geometry. Model parameters are inverted using a stochastic method composed of simulated annealing followed by a pattern search algorithm. The first application is carried out over the Central Alps, where long-standing permanent and the temporary AlpArray Seismic Network stations provide an ideal coverage. For this study we invert 4 independent parameters, which are the Moho discontinuity depth, the Conrad discontinuity depth, the P-velocity change at the Conrad and the average Vp/Vs of the crust. The 3-D inversion results clearly image the roots of the Alpine orogen, including the Ivrea Geophysical Body. The lower crust's thickness appears fairly constant. Average crustal Vp/Vs ratios are relatively higher beneath the orogen, and a low-Vp/Vs area in the northern foreland seems to correlate with lower crustal earthquakes, which can be related to mechanical differences in rock properties, probably inherited. Our results are in agreement with those found by 3-D ambient noise tomography, though our method inherently performs better at localizing discontinuities. Future developments of this technique can incorporate joint inversions, as well as more efficient parameter space exploration.
    Type of Medium: Online Resource
    ISSN: 2213-5812 , 2213-5820
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 2022
    detail.hit.zdb_id: 2705307-6
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  • 6
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 2022
    In:  Journal of Geophysical Research: Solid Earth Vol. 127, No. 6 ( 2022-06)
    In: Journal of Geophysical Research: Solid Earth, American Geophysical Union (AGU), Vol. 127, No. 6 ( 2022-06)
    Abstract: Statistical procedure to detect directivity effects in small‐to‐moderate earthquakes analyzing the aleatory residuals of the ground motion The directive events are the 36% of the data set and the distribution of rupture direction is aligned with the strikes of the faults system The observed directivity is a frequency‐dependent band‐limited phenomenon, which can occur up to five times the value of corner frequency
    Type of Medium: Online Resource
    ISSN: 2169-9313 , 2169-9356
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 2022
    detail.hit.zdb_id: 2016813-5
    detail.hit.zdb_id: 161666-3
    detail.hit.zdb_id: 3094197-0
    SSG: 16,13
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  • 7
    Online Resource
    Online Resource
    Seismological Society of America (SSA) ; 2022
    In:  Seismological Research Letters Vol. 93, No. 4 ( 2022-07-01), p. 2299-2310
    In: Seismological Research Letters, Seismological Society of America (SSA), Vol. 93, No. 4 ( 2022-07-01), p. 2299-2310
    Abstract: We study the spectral decay parameter κ using S-wave recordings from the central Italy dense regional array. The data set used consists of 266 earthquakes, 353 stations, and 13,952 observations of κ with a mean value of 0.0412 ± 0.0177 within the distance range of 7.1–168.8 km. We model the variation of κ with hypocenter distance r as κ(r)=κ0+κs+κ˜(r), in which κ0 and κs represent the near-site and the near-source decay parameters, respectively, and κ˜(r) the average κ along the S-wave source-station paths. We first determine κ˜(r) with a nonparametric inversion approach and then we solved for κ0 and κs with a second inversion. We found that κ˜(r) increases with distance within the whole distance range analyzed (9.2–80.6 km). The near-source decay parameter takes values in the range 0.0 & lt;κs≤0.026 with a mean value of 0.003 ± 0.006, which represents 7.52% of the mean value of the observed κ. The values of the near-site decay parameter vary in the range 0.0035≤κ0≤0.0823 with a mean value of 0.0298 ± 0.0133, that is, 72.28% of the mean value of the κ observed. We conclude that most of the high-frequency attenuation takes place near the site, because κ˜(r) contributes with only 20.2% of the spectral decay. We also investigate the spatial variability of κ by determining κ˜(r) within four quadrants that divide the studied region taking as a reference axis the Apennines chain orientation. We found higher values of κ˜(r) in the southern quadrants, where seismicity and faulting are more active, and less attenuation in the more stable northeast quadrant.
    Type of Medium: Online Resource
    ISSN: 0895-0695 , 1938-2057
    Language: English
    Publisher: Seismological Society of America (SSA)
    Publication Date: 2022
    detail.hit.zdb_id: 2403376-5
    SSG: 16,13
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