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  • 1
    Publication Date: 2017-04-04
    Description: The Educational & Outreach Group (E&O Group) of the Istituto Nazionale di Geofisica e Vulcanologia (INGV) designed a portable museum to bring on the road educational activities focused on seismology, seismic hazard and Earth science. This project was developed for the first edition of the Science Festival organized in Genoa, Italy, in 2003. The museum has been mainly focused to school students of all ages and explains the main topics of geophysics through posters, movie and slide presentations, and exciting interactive experiments. This new INGV museum has been remarkably successful, being visited by more than 8,000 children and adults during the 10 days of the Science Festival. It is now installed at the INGV headquarters in Rome and represents the main attraction during the visits of the schools all year round.
    Description: Published
    Description: 15-18
    Description: reserved
    Keywords: Interactive museum ; earthquake ; seismic hazard ; educational ; 04. Solid Earth::04.01. Earth Interior::04.01.99. General or miscellaneous ; 04. Solid Earth::04.04. Geology::04.04.99. General or miscellaneous ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous ; 04. Solid Earth::04.07. Tectonophysics::04.07.99. General or miscellaneous ; 05. General::05.03. Educational, History of Science, Public Issues::05.03.99. General or miscellaneous ; 05. General::05.08. Risk::05.08.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Format: 4797947 bytes
    Format: application/pdf
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  • 2
    Publication Date: 2020-02-24
    Description: In October 2011 a strong earthquake hit the Van province, Eastern Turkey. Few days later (November 9th) an aftershock occurred few km southward. Finally in November 1976 another mainshock took place north of Van along the Caldiran fault. We have investigated the possible relations between 2011 mainshock and aftershock and the link with the 1976 earthquake. In order to complete the work SAR interferometryhasbeenappliedtomeasuresurface displacements, while the fault geometries of the mainshock have been retrieved by a novel Neural Network approach. Moreover the CFF has been calculated to evaluate the role of 1976 earthquake in promoting the 2011 mainshock and, later on, the role of this latter respect to the aftershock in November 9th, 2011
    Description: Unpublished
    Description: Napoli, IT
    Description: 4T. Fisica dei terremoti e scenari cosismici
    Description: open
    Keywords: DInSAR ; Van Earthquake ; Coseismic displacement field ; CFF ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Conference paper
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  • 3
    Publication Date: 2017-04-04
    Description: On March 11th, 2011 (at 05:46:23 UTC) a megaearthquake (M 9.0) occurred near the NE coast of Honshu island ( Japan), originated near the subduction plate boundary between the Pacific and the North America plates. The epicenter has been located at about 130 km East of Sendai city, at a depth of about 32 km. This seismic event has been followed by a devastating tsunami. The location, the geometric parameters, the focal mechanism, are in agreement with the occurrence of the earthquake along the subduction plate boundary. The initial seismological analysis indicated that a surface of about 300 km x 150 km over the fault moved upwards of 30-40 m. The Tohoku-Oki INGV Team has made available a wide and multisciplinary expertise to investigate the different scientific issues concerning the earthquake. Indeed from Seismology to Geomorphology, from Remote Sensing to GPS, from Tsunami to Source Modeling the INGV Team has completed a wide range of analysis, obtaining relevant outcomes that are summarized in this work.
    Description: Published
    Description: 1-27
    Description: 2T. Tettonica attiva
    Description: N/A or not JCR
    Description: open
    Keywords: Tohoku-Oki earthquake; DInSAR; change detection:Tsunami ; 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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  • 4
    Publication Date: 2019-03-14
    Description: The aim of this work is to provide an overview of the capabilities and limitations of Differential Interferometric SAR (DInSAR) technique to supply reliable information about earthquakes over a very wide range of magnitudes, from mega-earthquakes (of magnitude 8+) up to those reaching the lower limits of detection. The capability of DIn- SAR to detect surface movements over large areas has been successfully used in seismology, where traditionally the main topic of scientists is to determine the seismic source parameters, such as geometry and slip distribution. In recent years some scientific reviews have been focused on defining the thresholds of detection of a coseismic signal (i.e., surface deformation) and to investigate the tradeoff magnitude-depth. An additional variable to pro- vide reliable constraints concerning the role of “remote sensing” is the available satellite system. Today we may exploit the capabilities of VHR (very high resolution) SAR systems that are addressed to investigate moderate size earthquakes at high sampling density. Additionally, we may say to be in the middle between the past generation of SAR systems (from ERS to Envisat) and the forthcoming Sentinel-1 missions that are specifically addressed to the investigation of surface effects of major and medium size natural disasters. This work will describe which role remote sensing and, in particular, DInSAR had in the case of the March 11, 2011, Tohoku-Oki (Japan) earthquake (Mw 9.0), with particular emphasis on the retrieval of source parameters. On the other side, we will focus on the June 21, 2013, Lunigiana (Northern Italy) earthquake (Mw 5.3), which is only the last example of low magnitude events where, however, DInSAR results are able to provide information relevant to seismological analyses.
    Description: Published
    Description: Wien AUSTRIA
    Description: 4T. Fisica dei terremoti e scenari cosismici
    Description: open
    Keywords: Mega-earthquake ; Remote Sensing ; source parameters ; 04. Solid Earth::04.03. Geodesy::04.03.99. General or miscellaneous ; 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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  • 5
    Publication Date: 2019-12-05
    Description: This paper re-evaluates the origin of some peculiar patterns of ground deformation observed by space geodetic techniques during the two earthquakes of September 26th of the Colfiorito seismic sequence. The surface displacement field due to the fault dislocation, as modeled with the classic Okada elastic formulations, shows some areas with high residuals which cannot be attributed to unsimulated model complexities. The latter was investigated using geomorphological analysis, by recognising the geologic evidence of deep seated gravitational slope deformations (DSGSD) of the block-slide type. The shape and direction of the co-seismic ground displacement observed in these areas are correlated with the expected pattern of movement produced by the reactivation of the identified DSGSD. At least a few centimetres of negative Line of Sight ground displacement was determined for the Costa Picchio, Mt. Pennino, and Mt. Prefoglio areas. A considerable horizontal component of movement in the Costa Picchio DSGSD is evident from a qualitative analysis of ascending and descending interferograms. The timing of the geodetic data indicates that the ground movement occurred during the seismic shaking, and that it did not progress appreciably during the following months. In this work it has been verified the seismic triggering of DSGSD previously hypothesized by many authors. A further implication is that in the assessment of DSGSD hazard it is necessary to consider the seismic input as an important cause of acceleration of the deformation rates.
    Description: Unpublished
    Description: open
    Keywords: Umbria ; earthquakes ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: manuscript
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