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  • 1
    Publication Date: 2019-05-24
    Description: We adopted a multidisciplinary approach to investigate the seismotectonic scenario of the 30 October 2016, Mw 6.5, Norcia earthquake, the largest shock of the 2016-2017 central Italy earthquake sequence. First, we used seismological and geodetic data to infer the dip of the main slip patch of the seismogenic fault, that turned out to be rather low-angle (37°). To evaluate whether this is an acceptable dip for the main seismogenic source, we modeled earthquake deformation using single- and multiple-fault models deduced from aftershock pattern analyses. These models show that the coseismic deformation generated by the Norcia earthquake is coherent with slip along a rather shallow-dipping plane. To understand the geological significance of this solution we reconstructed the sub-surface architecture of the epicentral area. As the available data are not robust enough to converge on a single fault model, we built three different models encompassing all major geological evidence and the associated uncertainties, including the tectonic style and the location of major decollement levels. In all models the structures derived from the contractional phase play a significant role: from controlling segmentation to partially reusing inherited faults, to fully reactivating in extension a regional thrust, geometrically compatible with the source of the Norcia earthquake. Based on our conclusions, some additional seismogenic sources falling in the eastern, external portions of the Apennines may coincide with inherited structures. A circumstance that may be a common occurrence in this region of the chain, where the inception of extension is as recent as Middle-Upper Pleistocene.
    Description: This work was supported by INGV R.U. 0865.050, P.I. U. Fracassi, of Project MIUR-FISR 2016 “Centro di studio e monitoraggio dei rischi naturali dell'Italia centrale”, and by “Finanziamenti di Ateneo per Progetti Scientifici” - FRA 2015, P.I. L. Bonini. Petroleum Expert Ltd is acknowledged for making available the Move software to the to the University of Trieste.
    Description: Published
    Description: 990-1017
    Description: 2T. Deformazione crostale attiva
    Description: JCR Journal
    Keywords: 2016 central Italy earthquake sequence ; geodetic inversion ; geological modeling ; 04.07. Tectonophysics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
    Publication Date: 2018-03-16
    Description: This article has been accepted for publication in Geophysical Journal Internationa ©: 2016 Published by Oxford University Press on behalf of the Royal Astronomical Society. All rights reserved.
    Description: We propose a procedure for uncertainty quantification in Probabilistic Tsunami Hazard Analysis (PTHA), with a special emphasis on the uncertainty related to statistical modelling of the earthquake source in Seismic PTHA (SPTHA), and on the separate treatment of subduction and crustal earthquakes (treated as background seismicity). An event tree approach and ensemble modelling are used in spite of more classical approaches, such as the hazard integral and the logic tree. This procedure consists of four steps: (1) exploration of aleatory uncertainty through an event tree, with alternative implementations for exploring epistemic uncertainty; (2) numerical computation of tsunami generation and propagation up to a given offshore isobath; (3) (optional) site-specific quantification of inundation; (4) simultaneous quantification of aleatory and epistemic uncertainty through ensemble modelling. The proposed procedure is general and independent of the kind of tsunami source considered; however, we implement step 1, the event tree, specifically for SPTHA, focusing on seismic source uncertainty. To exemplify the procedure, we develop a case study considering seismic sources in the Ionian Sea (central-eastern Mediterranean Sea), using the coasts of Southern Italy as a target zone. The results show that an efficient and complete quantification of all the uncertainties is feasible even when treating a large number of potential sources and a large set of alternative model formulations. We also find that (i) treating separately subduction and background (crustal) earthquakes allows for optimal use of available information and for avoiding significant biases; (ii) both subduction interface and crustal faults contribute to the SPTHA, with different proportions that depend on source-target position and tsunami intensity; (iii) the proposed framework allows sensitivity and deaggregation analyses, demonstrating the applicability of the method for operational assessments.
    Description: Italian Flagship Project RITMARE, EC FP7 ASTARTE (Grant agreement 603839) and STREST(Grant agreement 603389) projects, Italian FIRB-‘Futuro in Ricerca’ project ‘ByMuR’ (Ref. RBFR0880SR), INGV-DPC Agreement, Annex B2
    Description: Published
    Description: 1780–1803
    Description: 5T. Modelli di pericolosità sismica e da maremoto
    Description: JCR Journal
    Keywords: Probabilistic forecasting ; Tsunamis ; Earthquake interaction ; Europe ; 04.07. Tectonophysics ; 05.06. Methods ; 05.08. Risk ; 05.01. Computational geophysics ; 04.06. Seismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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