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  • 2
    Publication Date: 2017-04-04
    Description: An edited version of this paper was published by AGU. Copyright (2009) American Geophysical Union.
    Description: We use InSAR and body-wave seismology to determine independent source parameters for the 6th April 2009 Mw 6.3 L’Aquila earthquake and confirm that the earthquake ruptured a SW-dipping normal fault with 0.6–0.8 m slip. The causative Paganica fault had been neglected relative to other nearby range-frontal faults, partly because it has a subdued geomorphological expression in comparison with these faults. The L’Aquila earthquake occurred in an area with a marked seismic deficit relative to geodetically determined strain accumulation. We use our source model to calculate stress changes on nearby faults produced by the L’Aquila earthquake and we find that several of these faults have been brought closer to failure.
    Description: Published
    Description: L17312
    Description: 3.2. Tettonica attiva
    Description: JCR Journal
    Description: reserved
    Keywords: L'Aquila earthquake ; InSAR ; 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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  • 3
    Publication Date: 2012-02-03
    Description: Strong earthquakes and tsunamis, like other natural disasters (storms, hurricanes, floods) are destructive events that strongly affect the standard of living of the populations they hit. Their impact on human societies varies according to the frequency with which they occur, the quality of the buildings, the demographic density and the economy of the areas involved. In areas with a precarious economic equilibrium, natural disasters have increate the speed of impoverishment in the short and medium term. The economic and social impact of seismic disasters over the medium and long term can be ossesse by analysing the quality of reconstruction work and the time taken to carry it out. Historical and recent records show that when reconstruction is slow and funds are largely or totally lacking, there is a negative effect even on later generations, increasing the vulnerability of the buildings and therefore increasing the hazard from other later destructive events. At times when reconstruction work is being carried out, now as in the past, local economic crises, emigration, famine, plague may also occur, leading to further losses. In so far as the increasing disparity in living standards across the world is affected by seismic disasters, the scenarios we find today tend to be new, since earthquakes and tsunamis of the same size can have effects of widely varying severity depending on the context. The poorest and most densely populated areas in the world (Near East, Asia, and along the coast of South America), are those most likely to suffer major disasters in the near future. This general trend does not exclude the possibility of economically strong regions being struck by natural disasters resulting in high death tolls and serious economic damage (see the case of New Orleans, in 2004). The technological systems on which urban life depends are in fact very vulnerable. But the difference lies in the resources available for recovery and the time required to effect it. We can therefore be sure, not only that very poor and highly populated areas will suffer the worst natural disasters, but also that the destructive effects of these disasters will tend to worsen pre-existing poverty levels. The authors present some cases that highlight this historical and current trend in Iran, Pakistan and Italy. For Italy, they present a historical case study of Calabria over the last three centuries. A sequence of destructive earthquakes has played a crucial role in the economy and the culture of that region, which is today one of the poorest in Italy. Historical research has shown that this kind of poverty results from the loss, not only of houses and other buildings needed for production purposes, but also of knowledge, skills and trade exchanges.
    Description: Published
    Description: 153-186
    Description: 3.10. Storia ed archeologia applicate alle Scienze della Terra
    Description: open
    Keywords: Calabria earthquakes ; poverty ; social impact ; seismic disaster ; 04. Solid Earth::04.06. Seismology::04.06.05. Historical seismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: book chapter
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  • 4
    Publication Date: 2017-04-04
    Description: In this paper we show that the processes that have shaped the Quaternary surface development of the Apennines in central Italy are all consequences of a single subcrustal process, the upwelling of the mantle. The relationship between gravity and topography shows that mantle convection is responsible for a long-wavelength (150–200 km) topographic bulge over the central Apennines, and stratigraphic evidence suggests this bulge developed in the Quaternary. Active normal faulting is localized at the crest of this bulge and produces internally-draining fault-bounded basins. These basins have been progressively captured by the aggressive headward erosion of major streams that cut down to the sea on the flanks of the regional bulge. The only surviving closed basins are those on the Apennine watershed most distant from the marine base level, where continued normal faulting is still able to provide local subsidence that defeats their capture by the regional drainage network. Understanding the competition between regional capture and local, fault-related subsidence of intermontane basins is crucial for recognizing potentially hazardous active faults in the landscape and also for interpreting the sediment supply to adjacent offshore regions. Central Italy provides a good modern analogue for processes that are probably common in the geological record, particularly on rifted margins and intracontinental rifts, but may not have been fully appreciated.
    Description: Published
    Description: 475-497
    Description: reserved
    Keywords: crustal deformation ; mantle upwelling ; Quaternary ; normal faulting ; 04. Solid Earth::04.07. Tectonophysics::04.07.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Format: 2062083 bytes
    Format: application/pdf
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  • 5
    Publication Date: 2019-11-04
    Description: JCR Journal
    Description: open
    Keywords: wavelength deformation ; continental litosphere ; 04. Solid Earth::04.07. Tectonophysics::04.07.01. Continents
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 6
    Publication Date: 2023-01-16
    Description: This article has been accepted for publication in Geophysical Journal International ©:The Author(s) 2022. Published by Oxford University Press on behalf of the Royal Astronomical Society. All rights reserved.Uploaded in accordance with the publisher's self-archiving policy. All rights reserved.
    Description: The western Balkans occupy a region influenced by two major active tectonic processes: the collision between the Adriatic Region and the Dinarides in the west, and the extension of the Aegean Region and its surroundings as they move towards the Hellenic Trench. An understanding of the kinematics and dynamics of the western Balkans has significance for our understanding of continental tectonics in general, and is the object of this paper. The region is rich in observational data, with many well-studied earthquakes, good geodetic coverage by GNSS (Global Navigation Satellite System) and abundant exposure of active faulting and its associated geomorphology, especially within the Mesozoic carbonates that cover large sectors of the extensional areas. We first use such observations to establish the regional kinematic patterns, by which we mean a clarification of how active faulting achieves the motions observed in the deforming velocity field obtained from GNSS measurements. We then use geomorphological observations on the evolution of drainage systems to establish how kinematic and faulting patterns have changed and migrated during the Late Neogene-Quaternary. The kinematics, and its evolution, can then be used to infer characteristics of the dynamics, by which we mean the origin and effect of the forces that control the overall deformation. The principal influences are: (i) the distribution and evolution of gravitational potential energy (GPE) contrasts arising from crustal thickness variations and elevation, in particular the growth of topography by shortening in the Albanides–Hellenides mountain ranges and the high elevation of mainland Greece relative to the Mediterranean seafloor and (ii) the ability of the boundaries of the region, along the Adriatic coast and in the Hellenic Trench, to support the forces arising from those GPE contrasts. The evolution in space and time indicates an interaction between the anisotropic strength fabric of the upper crust associated with faulting, and the more distributed and smoother patterns of flow that are likely to characterize the ductile deformation of the lower, aseismic part of the lithosphere—both of which influence the deformation on the scale of 100–200 km. The persistent argument about whether continental deformation is best described by a continuum or by rigid-block motions is largely a matter of scale and particular location: both are influential in establishing the patterns we see.
    Description: Published
    Description: 2102–2126
    Description: 2T. Deformazione crostale attiva
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 7
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Journal of the American Chemical Society 103 (1981), S. 4405-4410 
    ISSN: 1520-5126
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Macromolecules 1 (1968), S. 218-223 
    ISSN: 1520-5835
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Physics
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Macromolecules 2 (1969), S. 644-647 
    ISSN: 1520-5835
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Physics
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Macromolecules 27 (1994), S. 2426-2431 
    ISSN: 1520-5835
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Physics
    Type of Medium: Electronic Resource
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