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  • Earthquake
  • 2015-2019  (19)
  • 1920-1924
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Years
Year
  • 1
    Unknown
    London : Bloomsbury Academic
    Keywords: Ecocriticism ; Earthquake ; Italy ; Literary Studies ; Literary Theory ; Comparative Literature ; European Literature
    Description / Table of Contents: Naples and the porous landscapes of ecomafia and volcanic eruptions; death in Venice as a literary trope and a petrochemical curse; earthquakes and political moves that shake territories, people, and ideas cross-country; the slow pace of wine, food and environmental violence in Piedmont: these are some of the texts that this book narrates and analyses. Here stories of justice, cultural visions, society and politics interlace with stories of land and life, ecosystems and body cells, pollution and redemption. Ecocriticism and Italy reads Italy as a text - a compound text made of matter and imagination - always keeping in mind the link between the horizon of this country and the world’s larger ecology of ideas and matter. Challenging stereotypes and ambivalent clichés, this book uses ecocriticism as a way to give voice to the forces, wounds, and messages of creativity dispersed on Italy’s body, arguing that a literature, an art, and a criticism that are able to transform these unexpressed voices into stories - into our stories - are not only ways to resist. They are a practice of liberation. | Table of Contents: Introduction, pp. 1–12 --- Chapter 1. Bodies of Naples : A Journey in the Landscapes of Porosity, pp. 13–46 --- Chapter 2. Cognitive Justice and the Truth of Biology : Death (and Life) in Venice, pp. 47–82 --- Chapter 3. Three Earthquakes : Wounds, Signs, and Resisting Arts in Belice, Irpinia, and L’Aquila, pp. 83–124 --- Chapter 4. Slow : Stories of Landscapes, Resistance, and Liberation, pp. 125–156
    Pages: Online-Ressource (VI, 184 Seiten)
    ISBN: 9781474219488
    Language: English
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  • 2
    Publication Date: 2021-05-12
    Description: Wastewater disposal systems are complex systems composed by several interconnected elements. In the aftermath of dramatic natural events, such as the earthquake, the failure of any of these elements can result in the deterioration of the environment as well as in the risk for the exposed population, due to leakage of untreated or un-properly treated wastewater on soil and/or its discharge into superficial waters. This paper presents a multi-disciplinary methodology for the evaluation of the seismic vulnerability of municipal or industrial wastewater treatment plants, based on damage observation of available earth- quake reports. Specific fragility curves and threshold values expressed in terms of Peak Ground Acceleration (PGA) are presented and compared with existing functions. The methodology fully comply requirements of most relevant and effective risk analysis tools or for land-use planning and can be adopted for the definition of structural priorities of plants.
    Description: Published
    Description: 51-57
    Description: 4T. Sismologia, geofisica e geologia per l'ingegneria sismica
    Description: JCR Journal
    Keywords: Wastewater treatment plant ; Earthquake ; NaTech ; Critical infrastructure ; Vulnerability ; Industrial risks
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 3
    Publication Date: 2021-01-27
    Description: The fault activation (fault on) interrupts the enduring fault locking (fault off) and marks the end of a seismic cycle in which the brittle-ductile transition (BDT) acts as a sort of switch. We suggest that the fluid flow rates differ during the different periods of the seismic cycle (interseismic, pre-seismic, coseismic and post-seismic) and in particular as a function of the tectonic style. Regional examples indicate that tectonic-related fluids anomalies depend on the stage of the tectonic cycle and the tectonic style. Although it is difficult to model an increasing permeability with depth and several BDT transitions plus independent acquicludes may occur in the crust, we devised the simplest numerical model of a fault constantly shearing in the ductile deeper crust while being locked in the brittle shallow layer, with variable homogeneous permeabilities. The results indicate different behaviors in the three main tectonic settings. In tensional tectonics, a stretched band antithetic to the normal fault forms above the BDT during the interseismic period. Fractures close and fluids are expelled during the coseismic stage. The mechanism reverses in compressional tectonics. During the interseismic stage, an over-compressed band forms above the BDT. The band dilates while rebounding in the coseismic stage and attracts fluids locally. At the tip lines along strike-slip faults, two couples of subvertical bands show different behavior, one in dilation/compression and one in compression/dilation. This deformation pattern inverts during the coseismic stage. Sometimes a pre-seismic stage in which fluids start moving may be observed and could potentially become a precursor.
    Description: Published
    Description: 767–780
    Description: 2T. Tettonica attiva
    Description: N/A or not JCR
    Description: restricted
    Keywords: Fault activation ; Brittle-ductile transition ; Earthquake ; Fluids response ; 04. Solid Earth::04.06. Seismology::04.06.01. Earthquake faults: properties and evolution
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 4
    Publication Date: 2021-05-12
    Description: Earthquake early warning systems (EEWSs) are becoming a suitable instrument for seismic risk management in real time. In fact, they are implemented or are undergoing testing in many countries around the world because EEWSs represent an effective approach to mitigating seismic risk on a short timescale. EEWSs are based on the use of relationships between some parameters measured on the initial portion of seismic signal after the onsets. Here, we address the first approach to the implementation of EEWS in eastern Sicily, a region that has been hit by several destructive earthquakes. We estimated the peak displacement amplitude of the first portion of P and S waves Pd, the ground-motion period parameter τc, and the peak ground velocity (PGV) from earthquakes with ML ≥2:8 recorded by the broadband stations operated by the Istituto Nazionale di Geofisica e Vulcanologia. We found that the Pd is correlated with the size of the earthquake and may be used to compute the magnitude for an EEWS in this area.We also derived the relationships between τc and ML, and between Pd and PGV, which can be used to provide on-site warning in the area around a given station and to evaluate the potential damaging effects. These relationships may be deemed a useful guide for future implementation of the EEWS in the region.
    Description: Published
    Description: 1464-1477
    Description: 4T. Sismologia, geofisica e geologia per l'ingegneria sismica
    Description: JCR Journal
    Keywords: Earthquake ; early warning systems
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 5
    Publication Date: 2017-04-04
    Description: This version incorporates several updated sources and a few new sources based on the outcomes of the EC-funded projects SHARE and GeoMol, on the SIGMA project funded by EDF, Areva, CEA (France) and ENEL (Italy), on the "Progetto FIRB-Abruzzo" and "Progetto PON-MASSIMO" funded by the Italian Ministry for Education, University and Research (MIUR), and on activities funded in the framework of the INGV-DPC multiannual agreement.
    Description: Published
    Description: 2T. Tettonica attiva
    Description: 3T. Pericolosità sismica e contributo alla definizione del rischio
    Description: 4IT. Banche dati
    Description: open
    Keywords: Seismogenic source ; Active tectonics ; Earthquake ; Active faults ; Seismogenic faulting ; 04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismology ; 04. Solid Earth::04.04. Geology::04.04.09. Structural geology ; 04. Solid Earth::04.06. Seismology::04.06.01. Earthquake faults: properties and evolution ; 04. Solid Earth::04.06. Seismology::04.06.03. Earthquake source and dynamics ; 04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: web product
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  • 6
    Publication Date: 2017-04-04
    Description: We investigate magnetic effects in correspondence of the Mw6.1 L’Aquila earthquake. Magnetic and seismic records are analyzed. Rapid and distinct changes and an offset can be seen in magnetic field components after the main shock. We show that these effects result from electromagnetic induction due to the movement of the sensors through the Earth’s magnetic field and from a permanent displacement of the sensors from their original position caused by the passing seismic waves. A transient signal in total field data from an overhauser magnetometer apparently occurs in correspondence with the earthquake. Our analysis shows that the transient was not observed by other sensors that were operating in close proximity to the overhauser. Thus, the transient signal in the total magnetic field data, and the offset in the magnetic field components, cannot be associated with a hypothetical underground electric current generated by the earthquake, as suggested by Nenovski (2015).
    Description: Published
    Description: 6153–6161
    Description: 1A. Geomagnetismo e Paleomagnetismo
    Description: JCR Journal
    Description: restricted
    Keywords: Earthquake ; seismoelectric effect ; 04. Solid Earth::04.05. Geomagnetism::04.05.99. General or miscellaneous ; 04. Solid Earth::04.05. Geomagnetism::04.05.04. Magnetic anomalies ; 04. Solid Earth::04.05. Geomagnetism::04.05.08. Instruments and techniques
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 7
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    Unknown
    Seismological Society of America
    Publication Date: 2018-03-12
    Description: The paper has not any abstract
    Description: Published
    Description: 720-727
    Description: 2T. Sorgente Sismica
    Description: 1IT. Reti di monitoraggio
    Description: JCR Journal
    Keywords: Earthquake ; Monitoring ; 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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  • 8
    Publication Date: 2018-03-13
    Description: Abstract On August 24, 2016, at 03:36 (local time) a ML 6.0 earthquake (Mw 6.0) struck an extensive portion of the Central Apennines between the towns of Norcia and Amatrice. The epicenter was located near the town of Accumoli. The area was struck by several earthquakes in historical times (1627, 1639, 1672, 1703; http://emidius.mi.ingv.it/CPTI15-DBMI15/). The preliminary observations (seismological, geodetic and geological) collected in the area affected by the Amatrice earthquake sequence and the available scientific knowledge of the area allow to elaborate a first interpretative framework of the ongoing seismic sequence. The seismogenic structure is oriented NNW-SSE and extends about 25-30 km between the towns of Norcia and Amatrice with a width of about 10-12 km and a depth of 10-12 km. This seismogenic volume is characterized by a complex tectonic setting. The August 24, 2016 (ML 6.0) main shock likely ruptured a SW dipping, NNW-SSE trending fault segment. The coseismic rupture started near the town of Accumoli and appears to have spread bilaterally towards Amatrice to S-SE and toward Norcia to N-NW. Preliminary fault slip inversion suggests two patches of co-seismic deformation located NW and SE of the hypocenter. It is still unclear whether there is fault continuity between the two patches that generated the ML 6.0 main shock, namely whether rupture occurred on a single fault segment, or on two different segments separated by the Olevano-Antrodoco structural discontinuity. The seismicity of the seismic volume in the NW sector (i.e., between Accumoli and Norcia) is dispersed suggesting the activation of different fault segments after the main shock of August 24. In particular, the trend of the replicas shows the activation of the Monte Vector fault segment and of different structures antithetical dipping towards NE.
    Description: Istituto Nazionale di Geofisica e Vulcanologia
    Description: Published
    Description: 4T. Sismologia, geofisica e geologia per l'ingegneria sismica
    Keywords: Amatrice ; Earthquake ; PRIMO RAPPORTO DI SINTESI SUL TERREMOTO DI AMATRICE
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: report
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  • 9
    Publication Date: 2018-03-13
    Description: About four weeks have passed since the local magnitude Ml 6.0 (moment magnitude Mw 6.0) earthquake struck the central Apennines area, between the towns of Norcia an Amatrice, on August 24. The amount of data so far collected and the ongoing studies, allow for a more detailed knowledge of the processes behind the earthquake and its seismic sequence. In the following we will illustrate analyses and results that integrate the ones described in the “First Summary Report on the Amatrice Earthquake”.
    Description: Istituto Nazionale di Geofisica e Vulcanologia
    Description: Published
    Description: 4T. Sismologia, geofisica e geologia per l'ingegneria sismica
    Keywords: Amatrice ; Earthquake ; AMATRICE EARTHQUAKE
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: report
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  • 10
    Publication Date: 2018-03-13
    Description: The earthquake of October 30 th 2016 at 06:40:17 UTC, (07:40:17, Italian time) was the Italian strongest event after the 1980 M W 6.9 Irpinia earthquake. The hypocenter coordinates are: Latitude 42.84 North, Longitude 11.13 East, depth 9 km. The magnitude calculated in the INGV monitoring room is 6.1 M L e 6.5 M W . The earthquake affected the provinces of Perugia, Rieti and Macerata and was strongly felt in central Italy; the epicenter is located 5 km from Norcia, 7 from Castelsantangelo sul Nera and Preci, 10 from Visso. In case of an earthquake of magnitude 6.5 the fault has an area of several hundred square kilometers and therefore the entire area above and around the fault is affected by strong shaking. Up to this moment the earthquake of October 30 is the strongest event of the sequence which began with the earthquake of August 24 th of M W= 6.0 and also counts a quake of magnitude M W =5.9 of October 26 th .
    Description: Istituto Nazionale di geofisica e Vulcanologia
    Description: Published
    Description: 4T. Sismologia, geofisica e geologia per l'ingegneria sismica
    Keywords: Amatrice ; Earthquake ; Amatrice Earthquake
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: report
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