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  • 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous  (4)
  • GRL  (4)
  • 1
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    In:  Geophys. Res. Lett., Kunming, China, 4, vol. 21(24), no. 1, pp. 2617-2620, pp. 2353, (ISSN: 1340-4202)
    Publication Date: 1994
    Keywords: Surface waves ; Dispersion ; GRL
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  • 2
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    In:  Geophys. Res. Lett., Kunming, China, 4, vol. 19, no. 1, pp. 1963-1966, pp. 2353, (ISSN: 1340-4202)
    Publication Date: 1992
    Keywords: Seismology ; Broad-band ; Strong motions ; Earthquake ; Waves ; GRL
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  • 3
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    In:  Geophys. Res. Lett., Kunming, China, 4, vol. 32, no. 10, pp. 1963-1966, pp. L10314, (ISSN: 1340-4202)
    Publication Date: 2005
    Keywords: Seismology ; Source parameters ; Real time earthquake monitoring ; Earthquake ; Banda ; Aceh ; GRL
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  • 4
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    In:  Geophys. Res. Lett., Luxembourg, Conseil de l'Europe, vol. 31, no. 9, pp. 1-4, pp. L09602, (ISSN: 1340-4202)
    Publication Date: 2004
    Description: We show that relative earthquake location using double-difference methods requires an accurate knowledge of the velocity structure throughout the study region to prevent artifacts in the relative position of hypocenters. The velocity structure determines the ray paths between hypocenters and receivers. These ray paths, and the corresponding ray take-off angles at the hypocenters, determine the partial derivatives of travel time with respect to the hypocentral coordinates which form the inversion kernel that maps double-differences into hypocentral perturbations. Thus the large-scale velocity structure enters into the core of the double-difference technique. By employing a 1D layered model with sharp interfaces to perform double-difference inversion of synthetic data generated using a simple, 1D gradient model; we show that inappropriate choice of the velocity model, combined with unbalanced source-receiver distributions, can lead to significant distortion and bias in the relative hypocenter positions of closely spaced events.
    Keywords: Seismology ; Location ; Velocity depth profile ; Error analysis ; 7215 ; Seismology: ; Earthquake ; parameters ; 7230 ; Seismicity ; and ; seismotectonics ; 7260 ; Theory ; and ; modeling ; 8180 ; Tectonophysics: ; Tomography ; GRL
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  • 5
    Publication Date: 2021-07-14
    Description: An edited version of this paper was published by AGU. Copyright (2016) American Geophysical Union.
    Description: The accuracy of earthquake locations and their correspondence with subsurface geology depends strongly on the accuracy of the available seismic velocity model. Most modern methods to construct a velocity model for earthquake location are based on the inversion of passive source seismological data. Another approach is the integration of high-resolution geological and geophysical data to construct deterministic velocity models in which earthquake locations can be directly correlated to the geological structures. Such models have to be kinematically consistent with independent seismological data in order to provide precise hypocenter solutions. We present the Altotiberina (AT) seismic model, a three-dimensional velocity model for the Upper Tiber Valley region (Northern Apennines, Italy), constructed by combining 300 km of seismic reflection profiles, 6 deep boreholes (down to 5 km depth), detailed data from geological surveys and direct measurements of P- and S-wave velocities performed in situ and in laboratory. We assess the robustness of the AT seismic model by locating 11,713 earthquakes with a non-linear, global-search inversion method and comparing the probabilistic hypocenter solutions to those calculated in three previously published velocity models, constructed by inverting passive seismological data only. Our results demonstrate that the AT seismic model is able to provide higher-quality hypocenter locations than the previous velocity models. Earthquake locations are consistent with the subsurface geological structures and show a high degree of spatial correlation with specific lithostratigraphic units, suggesting a lithological control on the seismic activity evolution.
    Description: Published
    Description: 8113-8135
    Description: 4T. Sismicità dell'Italia
    Description: JCR Journal
    Keywords: deterministic velocity model ; earthquakes ; nonlinear hypocenter location ; lithological control on seismicity ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 6
    Publication Date: 2017-04-04
    Description: We show that relative earthquake location using double-difference methods requires an accurate knowledge of the velocity structure throughout the study region to prevent artifacts in the relative position of hypocenters. The velocity structure determines the ray paths between hypocenters and receivers. These ray paths, and the corresponding ray take-off angles at the hypocenters, determine the partial derivatives of travel time with respect to the hypocentral coordinates which form the inversion kernel that maps double-differences into hypocentral perturbations. Thus the large-scale velocity structure enters into the core of the double-difference technique. By employing a 1D layered model with sharp interfaces to perform double-difference inversion of synthetic data generated using a simple, 1D gradient model; we show that inappropriate choice of the velocity model, combined with unbalanced source-receiver distributions, can lead to significant distortion and bias in the relative hypocenter positions of closely spaced events.
    Description: Published
    Description: L09602
    Description: partially_open
    Keywords: earthquake location ; Theory and modeling; ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Format: 167702 bytes
    Format: application/pdf
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  • 7
    Publication Date: 2017-04-04
    Description: Effective tsunami early warning for coastlines near a tsunamigenic earthquake requires notification within 5-15 minutes. We have shown recently that tsunamigenic earthquakes have an apparent rupture duration, T0, greater than about 50 s. Here we show that T0 gives more information on tsunami importance than moment magnitude, Mw, and we introduce a procedure using seismograms recorded near an earthquake to rapidly determine if T0 is likely to exceed T=50 or 100 s. We show that this “duration-exceedance” procedure can be completed within 3-10 min after the earthquake occurs, depending on station density, and that it correctly identifies most recent earthquakes which produced large or devastating tsunamis. This identification forms a complement to initial estimates of the location, depth and magnitude of an earthquake to improve the reliability of tsunami early warning, and, in some cases, may make possible such warning.
    Description: DPC-S3 2007-2009
    Description: Published
    Description: L09306
    Description: 1.1. TTC - Monitoraggio sismico del territorio nazionale
    Description: JCR Journal
    Description: open
    Keywords: tsunami ; fault rupture ; early warning ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 8
    Publication Date: 2017-04-04
    Description: The 26 December 2004 M9 Sumatra–Andaman Islands earthquake caused a tsunami that devastated Indian Ocean coasts within three hours after the earthquake. Improved tsunami warning and emergency response for future great earthquakes require knowing an earthquake’s size within minutes after the event. Although the hypocenter of a distant earthquake is routinely determined from the fi rst seismic P waves within about 15 min, several hours may pass before a reliable size determination for very large earthquakes is available (e.g., for the 2004 Sumatra–Andaman earthquake see Menke and Levin [2005]).
    Description: Published
    Description: (202)
    Description: reserved
    Keywords: Hazard Warning ; Earthquake ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Format: 125376 bytes
    Format: application/pdf
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