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  • Earthquake
  • Statistical investigations
  • 2005-2009  (433)
  • 1970-1974  (57)
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  • 1
    Publication Date: 2021-06-08
    Description: In the last few years, Robust Satellite data analysis Techniques (RST) have been proposed which significantly improved present capabilities to investigate possible relations between TIR signal fluctuations and earthquake occurrence. This paper, starting from a critical survey of results achieved by applying different RST-based algorithms to different satellite sensors to approximately ten earthquakes (two of them are discussed here for the first time) which occurred in three different continents, tries to offer a first assessment of main achievements, residual limits and perspectives of such studies. Even if it is still not possible to relate (or to exclude) observed anomalous TIR transients definitely to impending earthquakes, such studies demonstrate at least: a) the strong improvement of S/N ratio achievable moving from polar to geostationary satellites; b) the further S/N improvement achievable by using TIR sensors which also offer split-window possibilities; c) the crucial role played by a space-time persistence test to select TIR anomalies candidate to be associated to impending earthquakes; d) the possibility of identifying and correctly discarding TIR anomalies related to clouds and to image navigation errors; e) the scarce importance of spatial resolution of observations which encourages the use of passive MW sensors which are less affected by atmospheric conditions.
    Description: Published
    Description: 303 - 317
    Description: JCR Journal
    Description: open
    Keywords: RST ; Earthquake ; satellite thermal infrared ; Hector Mine ; Izmit ; GeoSTAR ; 04. Solid Earth::04.06. Seismology::04.06.06. Surveys, measurements, and monitoring
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
    Publication Date: 2017-04-04
    Description: This study presents the results of hydrogeochemical and seismological studies carried out at Mt. Vesuvius during the period June 1998 – December 2005. The data-set used for the seismological analysis was collected by: 1. The permanent seismic network of the INGV -Osservatorio Vesuviano, at the present composed of 11 short-period 1-Hz Mark L4C and Geotech S13 geophones and 2 broad band (40s) Guralp CMG40T seismometers; 2. Five digital stations (Lennartz PCM 5800) equipped with 3-component 1-Hz Lennartz LE-3Dlite sensors also operate in the area, in local recording mode. The monitered geochemical parameters (water temperature, pH, Eh, major ions, dissolved gases, 18O/16O ratios of groundwater) were detected at 10 private wells and 1 spring. Continuous soil temperature of the fumarolic fields was measured by a permanent device Gemini Tinytag Plus logger. Hydrogeochemical data show the occurrence of smooth long-term variations in the total dissolved salts (TDS) and bicarbonate contents of the groundwaters, accompanied by a general decline of water temperatures. These variations do not depend on changes in hydrologic regime, as suggested by the analysis of temporal distributions of air temperature and rainfall amount in the Vesuvius area. The changes in the geochemical pararameters are accompanied by a slight variations in both the seismicity rate and energy release. A further relationship between seismic activity and fluid discharge rate is highlighted by a particular episode occurred in August 2005, when a soil thermal anomaly was observed few weeks before the occurrence of a very shallow earthquake. Moment tensor analysis of this earthquake suggests that the most plausible source mechanism is a shear faulting combined with a tensile crack opening. This feature is often observed in volcanic areas and it is usually related to fluid-/gas-driven rock fracturing. The observed seismological, hydrological and geochemical temporal changes are interpreted not as changes of the volcanic system, but in terms of an external forcing, identified in the variation of the regional and local stress field acting on the volcano.
    Description: Published
    Description: Vienna (Austria)
    Description: open
    Keywords: Earthquake ; Fluid geochemistry ; Vesuvius ; 04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Abstract
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  • 3
    Publication Date: 2017-04-04
    Description: Seismicity is recognized to be a complex natural phenomenon either in space, time and energy domains: earthquakes occur as a sudden energy release after a strongly variable time period of stress accumulation, in locations not deterministically defined, with magnitude range spanning over several orders. But seismicity is certainly not a pure random process: spatial locations of events clearly display correlations with tectonic structures at all scales (from plates borders to small faults settings); on the other hand time evolution is clearly linked with strongest shocks occurrence and energy distribution displays hierarchical features. Although it is still not possible to propose deterministic models for earthquakes, well established statistical relations constrain seismicity under very specific and intriguing relations.
    Description: Published
    Description: 259-279
    Description: reserved
    Keywords: Earthquake ; 04. Solid Earth::04.06. Seismology::04.06.02. Earthquake interactions and probability ; 05. General::05.01. Computational geophysics::05.01.04. Statistical analysis
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: book chapter
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  • 4
    Publication Date: 2017-04-04
    Description: Nei primi anni del Settecento il giornalismo italiano ed europeo raggiunge il suo pieno sviluppo. La grande diffusione delle gazzette a stampa (consolidatasi da un paio di decenni con particolare vivacità nell'Italia Centrale) il successo commerciale delle relazioni monografiche a stampa, l’ininterrotto flusso sotterraneo di informazioni riservate che alimenta la produzione di avvisi manoscritti sono alcuni degli aspetti di una realtà vivace e competitiva, che influenza profondamente l'intero sistema della circolazione delle informazioni in età moderna, in una costante interazione con la memorialistica e la diaristica privata e con la stessa documentazione amministrativa. L'analisi sistematica dei resoconti giornalistici sui terremoti del 1703, e in particolare la verifica del loro contenuto informativo, ci consente di evidenziarne il contributo originale rispetto a quello di altre tipologie di fonti e di verificarne l'influenza sul processo di costituzione della tradizione storiografica e sismologica relativa a questi eventi.
    Description: Unpublished
    Description: open
    Keywords: Earthquake ; 1703 ; 04. Solid Earth::04.06. Seismology::04.06.05. Historical seismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: manuscript
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  • 5
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    Earthquake Engineering Research Institute
    Publication Date: 2017-04-04
    Description: Two earthquakes (both having Mw 5.7) struck the eastern portion of Molise on October 31 and November 1, 2002. Both caused severe damage over a 2000 km2 region straddling Molise and Puglia. The two larger shocks and the rather unusual aftershock sequence surprised most Italian seismologists and tectonicists. Although Italy has a good record of historical and instrumental seismicity and its main seismogenic trends are quite established, the epicentral location, depth and kinematics of this earthquake sequence were largely unexpected. In fact, the 2002 Molise earthquakes shed light on a previously unsuspected style of seismogenic faulting in this region. From the seismotectonic perspective, much of the significance of the two quakes arises from the possibility that this style of faulting might be shared by several much larger quakes that took place on the Adriatic side of the southern Apennines. In the first part of this paper we briefly describe the main seismological characteristics of the sequence. These were largely derived from the analysis of data supplied by permanent networks and from a preliminary analysis of data recorded by a portable network deployed a few hours after the first shock. In the second part of the paper we discuss the seismotectonic characteristics of the sequence in the framework of Italian tectonics and the implications for future earthquakes in the same region.
    Description: Published
    Description: S23-S37
    Description: reserved
    Keywords: Earthquake ; Molise 2002 ; Seismology ; Tectonic ; 04. Solid Earth::04.06. Seismology::04.06.04. Ground motion ; 04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Format: 1422638 bytes
    Format: application/pdf
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  • 6
    Publication Date: 2017-04-04
    Description: To define more accurately the near field and the directivity effect, different methodologies of finite-fault modelling have been used to describe the behaviour of ground shaking based on deterministic, stochastic and hybrid stochastic-deterministic approaches as in the framework of the ongoing European project “LESSLOSS – Risk Mitigation for Earthquakes and Landslides”. In this study, we simulate and compare seismic scenarios obtained from the complex source characteristic of the 1980 Irpinia earthquake, M 6.9, Southern Italy, using models based on the source models hypothesized in Bernard and Zollo (1989) and in Valensise et al. (1990). Furthermore, two finite-fault numerical approaches are used: 1. The approach RSSIM [Carvalho et al., 2004] that is a non-stationary stochastic simulation method that synthesizes the ground motion due to an extended source; 2. The approach EXSIM [Motazedian and Atkinson, 2005] that is a new version of FINSIM [Beresnev and Atkinson, 1998] introducing a new variation based on a “dynamic corner frequency”. The shaking scenarios are computed in terms of Response Acceleration Spectra (PSA), time series, peak ground acceleration (PGA) at bedrock level. Source and path propagation parameters taken from other studies were tested and the computed shaking scenarios are compared to acceleration records to eight different stations. Preliminary results are here presented in terms of PGA maps for the Campania region (Southern Italy).
    Description: Unpublished
    Description: Geneva, Switzerland
    Description: open
    Keywords: Earthquake ; Ground motion ; 04. Solid Earth::04.06. Seismology::04.06.04. Ground motion
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Poster session
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  • 7
    Publication Date: 2017-04-04
    Description: Acceleration time series recorded by the Italian Strong Motion Network (RAN) during the October 31, 2002 (Mw=5.8), Molise earthquake, are employed in order to investigate source effects on the ground motion in the epicentral area. We consider two different seismogenic sources: a fault model inferred from inversion of teleseismic, regional and local seismic signals [Vallée and Di Luccio, 2005], and a fault model based on seismotectonic data [Basili and Vannoli, 2005]. Both source studies suggest a deep location of the earthquake fault plane (ranging from 6.0 to 20.1 km and from 12.0 to 19.9 km, respectively), however, with considerably different fault lengths (5.2 and 10.5 km, respectively), and widths (14.2 and 8 km, respectively). Due to these differences, only the second model allows for effective horizontal unilateral rupture propagation. Finite fault effects are modelled by the Deterministic-Stochastic-Method (DSM) [Pacor et al., 2005], and the Hybrid Integral-Composite source model (HIC) [Gallovic and Brokesova, 2006]. In both methods k-square slip distributions on the faults are considered. We simulate the October 31, 2002 earthquake considering: 1) Vallée and Di Luccio [2005] faultwith a bilateral rupture propagation, and 2) Basili and Vannoli [2005] fault with unilateral directions of the rupture propagation. The spectral attenuation is modelled using a regional estimate of the quality factor [Castro et al., 2004] and k values estimated from acceleration records. Comparison between synthetic and recorded data at nearby stations (hypocentral distances 〈 60 km) performed in terms of frequency content and peak ground motion, favours the model with unilateral propagation of the rupture. Assuming the source model with unilateral rupture propagation, we utilize both asymptotic and full wave field methods in order to simulate ground shaking scenarios for an area extending up to 150 km epicentral distance. These results are then subjected to comparison with peak ground accelerations recorded in the far field.
    Description: Unpublished
    Description: Geneva, Switzerland
    Description: open
    Keywords: Earthquake ; Ground motion ; 04. Solid Earth::04.06. Seismology::04.06.04. Ground motion
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Conference paper
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  • 8
    Publication Date: 2017-04-04
    Description: We show that the low-pass filtered, peak amplitudes of initial P- and S-wave seismic signals recorded in the vicinity of an occurring earthquake source correlates with the earthquake magnitude and may be used for real-time estimation of the event size in seismic early warning applications. The earthquake size can be therefore estimated using only a couple of seconds of signal from the P- or S-wave onsets, i.e. while the rupture itself is still propagating and rupture dimension is far from complete. We argue that dynamic stress release and/or slip duration on the fault in the very early stage of seismic fracture, scales both with the observed peak amplitude and with the elastic energy available for fracture propagation. The probability that a fracture grows to a larger size should scale with the energy initially available.
    Description: Published
    Description: L23312
    Description: JCR Journal
    Description: partially_open
    Keywords: Earthquake ; 04. Solid Earth::04.06. Seismology::04.06.03. Earthquake source and dynamics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 9
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    Publication Date: 2017-04-03
    Description: Il documento consente di farsi un'idea immediata di cosa sia un terremoto attraverso i cinque concetti chiave: energia accumulata, tettonica delle placche, onde sismiche, ipocentro e faglie.
    Description: Un documento che sintetizza in una pagina web cos'è un terremoto messo in rete a fini divulgativi in occasione del primo sito web dell'allora Istituto Nazionale di Geofisica (ING).
    Description: Unpublished
    Description: 5.8. TTC - Formazione e informazione
    Description: open
    Keywords: Earthquake ; web ; 05. General::05.03. Educational, History of Science, Public Issues::05.03.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: web product
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  • 10
    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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