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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 132 (1990), S. 639-652 
    ISSN: 1420-9136
    Keywords: Seismic tomography ; local inhomogeneities ; probability ; maximum likelihood
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract A simple method to contour local inhomogeneities using seismic data is proposed. It formalizes an approximate inversion method which is based on the interpretation of local inhomogeneities as making the differences between an actual seismic data set and a previous reference model. It uses the optimal statistical criteria of parameter estimation and recognition and the ray representation of the waves spreading. Any combination of direct, reflected and/or other types of waves may be used as the database. Inhomogeneities, having a size two times above the wavelength of the seismic waves, can be resolved. Laboratory experiments, using ultrasonic waves and analysis of data from field experiments, confirmed the theoretical results. The method can be used to search for ore bodies, kimberlite cubes, oiltraps, etc.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1573-0840
    Keywords: Macroseismic data ; early seismographic records
    Source: Springer Online Journal Archives 1860-2000
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Geography , Geosciences
    Notes: Abstract The 19 November 1923 earthquake in the Aran Valley (Central Pyrenees), with observed maximum intensityI max = VIII (MSK), has been studied through the compiling and reviewing of macroseismic information and collecting and processing early seismograms. Analysis of macroseismic data gives a focal depth ofh = 5 km and an anelastic attenuation coefficientα ≤ 10−3 km−1. Analysis of early instrumental records allows the computation of estimate of magnitude (M L = 5.6) and seismic moment (M o = 1.1 × 1017 N × m) which are consistent with the values ofI o andh obtained from macroseismic data.
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 2014-10-04
    Description: On 26 January 1531, a strong-magnitude earthquake heavily impacted Lisbon downtown. Immediately after the earthquake, the eyewitnesses reported large waves in the Tagus estuary, mainly north of the city and along the northern bank of the river. Descriptions include large impacts on ships anchored in the estuary and even morphological changes in the riverbed. We present a synthesis of the available information concerning both the earthquake and the water disturbance as a basis for the discussion of the probable tectonic source and the magnitude of the associated river oscillations. We hypothesize that the initial disturbance of the water can be attributed to the coseismic deformation of the estuary riverbed, and we use a nonlinear shallow water model to simulate the tsunami propagation and inundation. We show that the Vila Franca de Xira fault is the most probable source of the 1531 event. The largest inundation effects of the model correlate well with the historical descriptions: the impact is relevant in the inner Tagus estuary, but inundation in downtown Lisbon is small.
    Print ISSN: 0037-1106
    Electronic ISSN: 1943-3573
    Topics: Geosciences , Physics
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  • 4
    Publication Date: 2017-04-04
    Description: The earthquake of 17th May 1916 at 12:50 hours (GMT) is the first event of a seismic sequence that struck the northeastern coast of Italy (in particular the towns of Rimini and Cattolica) and lasted until December of the same year. The Catalogue of Strong Italian Earthquakes (http://storing.ingv.it/cfti4med/) classifies 132 locations in regard to this earthquake which had a maximum and epicentral intensity equal to the VIII degree of MCS scale, with magnitude equivalent to 5.8. During the First World War, the ISS bulletin was unpublished and the available epicentral location was derived only from macroseismic analysis. In this work we col-lected the bulletins available from Euro-Mediterranean observatories and we performed the first instru-mental location for this event. This event is amongst the high priority earthquakes included in the Euro-seismos project (http://storing.ingv.it/es_web). In the database of the SISMOS Project – INGV (http://sismos.ingv.it) 50 recordings from 20 different Euro-Mediterranean observatories are available today for this earthquake. The analysis of all these data allowed us to obtain a reassessment of the main seismological parameters (MW, MS) and a re-location of the epicenter. Preliminary results suggest an east forward migration of previous location of the epicenter and a probable underestimation of the magnitude consigned into the catalogues. Special attention was devoted to determining the error margins of the obtained results. A comparison between these parameters and that extrapolated from macroseismic data will be discussed.
    Description: ESC, IUGG
    Description: Published
    Description: Hersonissos, Crete island, Greece
    Description: 3.1. Fisica dei terremoti
    Description: open
    Keywords: Historical seismograms ; 1916 Rimini eartquake ; Seismic parameters ; 04. Solid Earth::04.06. Seismology::04.06.09. Waves and wave analysis
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Oral presentation
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  • 5
    Publication Date: 2017-04-04
    Description: In the frame of the NA-4 module of the European project NERIES, a specific task is devoted to the determination of earthquakes parameters from macroseismic data. On this regard, a new methodology, implemented in the program MEEP, has been developed by Musson et al. (see relevant presentation in this session). Here we present and discuss some tests performed by using the MEEP program in order to contribute to the setting up of the code and to validate the methodology itself. To this purpose, a set of earthquakes occurred in different regions of Europe and with different ranges of magnitude have been selected. In particular, the main aspects investigated here are: •reliability of estimates of epicentre location, magnitude and hypocentral depth compared with instrumental determinations; •comparison with epicentral parameters derived by using other methods based on macroseismic data; •sensitivity of the methodology to number and geographic distribution of available intensity data points (IDPs); •sensitivity to the calibration parameters requested by the program. Results of this analysis suggested some modifications of the program
    Description: Published
    Description: Hersonissos, Creta island, Greece
    Description: 5.1. TTC - Banche dati e metodi macrosismici
    Description: open
    Keywords: earthquake parameters ; macroseismic ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Abstract
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  • 6
    Publication Date: 2017-04-04
    Description: The seismotectonics of the Upper Tiber Valley are dominated by the Altotiberina Fault (ATF), an NE-dipping low-angle normal fault system, and its antithetic W-dipping high-angle normal faults. A lthough the southern part of the ATF was demonstrated to creep, its capability to generate strong or moderate earthquakes is still under debate. On April 26, 1917 at 9:35:59 (GMT) a strong earthquake struck the northernmost portion of the Upper Tiber Valley (Tuscany) producing severe damages and about 20 fatalities. The Catalogue of Strong Italian Earthquakes reports this event as the so-c alled Monterchi earthquake, relating to 134 macroseismic observations, mainly distributed on the western side of the Tiber Valley. The maximum and epicentral intensity was determined as Io=IX- X (MCS), corresponding to an equivalent magnitude of Me=6, that defines this event as the most important of the area. A total of 49 historical seismograms from 19 different Euro-Mediterranean observatories are available in the database of the SISMOS Project - INGV. The BAAS bulletin of 1917 reports a list of 21 seismological observatories that record ed the P and S-phases for this earthquake. We included additional arrival-times deriving from further seismic bulletins - and from digitalizing original historical seismograms. We obtain a new, robust and consistent hypocentral solution, coherent with the macroseismic data, in particular by using S-P travel time differences for recordings where the absolute timing is uncertain. An accurate research on the technical characteristics of the recording historical seismometers (period, dampin g, gain etc.), allowed to deconvolve the original digitalized seismic traces (i) to determine the main seismic parameters (Mo, Mw, Circular Fault Radius), (ii) to constrain the possible source mechanism, by a combination of first motion analysis and modelling of synthetic seismograms, and (iii) to implement the solution in the framework of the regional tectonic setting.
    Description: Published
    Description: Pasadena, California, USA
    Description: 2T. Tettonica attiva
    Description: open
    Keywords: Historical earthquake ; Seismic analysis ; 04. Solid Earth::04.06. Seismology::04.06.03. Earthquake source and dynamics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Poster session
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  • 7
    Publication Date: 2021-12-15
    Description: Within the European Project NERIES, sponsored by the European Commission in the frame of the Specific Programme "Structuring the European Research Area", the NA4 module is devoted to establish a distributed archive of historical earthquake. NA4 objectives are to establish the required tools leading to the compilation of a comprehensive, digital macroseismic intensity database for the largest European earthquakes (with magnitude 〉=5.8 at least) and a validated and homogeneous European parametric earthquake catalogue for M〉=5, to serve as an authoritative reference for users involved in the assessment of seismic hazard and risk. The main focus is devoted to the time-window before 1900. Some highlights about the whole NA4 project, actual state of the initiatives undertaken in the Iberian Peninsula to contribute to it and future developments are presented.
    Description: Published
    Description: Tomar, Portugal
    Description: 5.1. TTC - Banche dati e metodi macrosismici
    Description: open
    Keywords: earthquake parameters ; macroseismic ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Poster session
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  • 8
    Publication Date: 2022-09-08
    Description: In the frame of the European Commission project “Seismic Hazard Harmonization in Europe” (SHARE), aiming at harmonizing seismic hazard at a European scale, the compilation of a homogeneous, European parametric earthquake catalogue was planned. The goal was to be achieved by considering the most updated historical dataset and assessing homogenous magnitudes, with support from several institutions. This paper describes the SHARE European Earthquake Catalogue (SHEEC), which covers the time-window 1000-1899. It strongly relies on the experience of the European Commission project “Network of Research Infrastructures for European Seismology” (NERIES), a module of which was dedicated to create the European “Archive of Historical Earthquake Data” (AHEAD) and to establish methodologies to homogenously derive earthquake parameters from macroseismic data. AHEAD has supplied the final earthquake list, obtained after sorting duplications out and eliminating many fake events, and the most updated historical dataset. Macroseismic data points (MDPs) provided by AHEAD have been processed with updated, repeatable procedures, regionally calibrated against a set of recent, instrumental earthquakes, to obtain earthquake parameters. From the same data, a set of epicentral intensity-to-magnitude relations has been derived, with the aim of providing another set of homogeneous Mw estimates. Then, a strategy focussed on maximizing the homogeneity of the final epicentral location and Mw, has been adopted. Special care has been devoted also to supply location and Mw uncertainty. The paper focuses on the procedure adopted for the compilation of SHEEC and briefly comments on the achieved results.
    Description: EC-Research Framework programme FP7, Seismic Hazard Harmonization in Europe, Grant Agreement No. 226769
    Description: Published
    Description: 523-544
    Description: 5.1. TTC - Banche dati e metodi macrosismici
    Description: JCR Journal
    Description: open
    Keywords: earthquake catalogue ; Europe ; earthquake parameters ; magnitude ; parameters uncertainty ; 04. Solid Earth::04.06. Seismology::04.06.11. Seismic risk
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 9
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    In:  Seismological Research Letters
    Publication Date: 2020-02-12
    Description: Additional keywords: figures of historical instruments, parameter listing of all historical seismographs operated in Spain, conclusions, Nutzung historischer Seismogramme fuer moderne Forschungen, Bestimmung von Polen und Nullstellen aus katalogisierten Parametern historischer Seismographen, Abbildungen historischer Seismographen in Spanien, Auflistung von Parametern aller in Spanien betriebenen historischen Seismographen, Schlussfolgerungen
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/article
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  • 10
    Publication Date: 2020-02-13
    Description: On 26 April 1917, an earthquake Mw 6.0 (known as the Monterchi earthquake) struck the upper Tiber basin, central Italy. This Quaternary basin is situated on the hanging wall of a segmented low‐angle normal fault (LANF) named the Alto Tiberina fault (ATF), whose capability to act with stick‐slip behavior is debated. We reanalyzed instrumental historical data and performed a relocation of the hypocenter along with a reassessment of the scalar moment and magnitudes (⁠Mw and Ms⁠); we calculate the fault radius and stress drop and propose a focal solution based on first‐arrival polarities. The methodologies that we applied strongly take into account the intrinsic uncertainties present in the historical data to obtain solutions that provide well‐defined error estimates. The hypocentral solution is consistent with the known macroseismic scenario and is plausible in terms of root mean square (rms) and error ellipse. The calculated focal depth at ≈8  km⁠, even considering the depth uncertainty of ±4  km⁠, locates the earthquake source inside the ATF footwall. The Mw distribution (median Mw 5.8) suggests an overestimate of the macroseismic Mw probably due to seismic amplification caused by site effects. A preferred focal solution (strike 60/dip 84/ rake −162) defines an antiapenninic‐oriented fault, with predominantly right‐lateral slip. Our results strongly suggest that the 1917 Monterchi earthquake did not nucleate on one of the splays of the low‐angle ATF but rather was generated by a deeper seismic source, which could be referred to as a structural transfer zone responsible for the Quaternary LANF segmentation.
    Language: English
    Type: info:eu-repo/semantics/article
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