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  • 04.07. Tectonophysics  (2)
  • 05.04. Instrumentation and techniques of general interest
  • Copernicus  (2)
  • Ras  (1)
  • American Geophysical Union
  • American Meteorological Society
  • Blackwell Publishing Ltd
  • Hindawi
  • Institute of Electrical and Electronics Engineers
  • Springer Nature
  • Springer Science + Business Media
  • 2020-2022  (3)
  • 1985-1989
  • 1980-1984
  • 1970-1974
  • 1960-1964
Collection
Publisher
Years
  • 2020-2022  (3)
  • 1985-1989
  • 1980-1984
  • 1970-1974
  • 1960-1964
Year
  • 1
    Publication Date: 2020-10-16
    Description: High strain rates and intense seismic activity characterize both the boundaries and the interior of the Aegean–Anatolian plate: the availability of geodetic and geophysical data makes this region ideal to make detailed models of continental deformation. Although the deformation occurring in the Aegean–Anatolian plate may be regarded as the primary effect of the Arabian indenter push, it has already been demonstrated that this mechanism cannot account for the observed extrusion/rotation of the whole plate. We investigate the present-day steady-state anelastic deformation of the Aegean–Anatolian plate by a thin plate thermomechanical finite element (FE) model that accounts for realistic rheological mechanisms and lateral variations of lithospheric properties. Studying the region with uniform models, where average values for thermal and geometric parameters are chosen, we find that two tectonic features, in addition to the Arabian plate push, are critical to reproduce a velocity field that gives a reasonable fit to the observations. The first is the E–W constraint of NW continental Greece, related to the collision between the Aegean–Anatolian plate and the Apulia–Adriatic platform, required in the model to attain the SW orientation of the velocity field along the Hellenic Arc. The second is the trench suction force (TSF) due to subduction of the African lithosphere, which is needed to fit the observed mean extrusion velocity of 30 mm yr−1 along the Hellenic Arc. Uniform models are useful to study the sensitivity to the interplay of rheological/thermal parameters in a simplified framework but, in all cases, predict a strong deformation localized along the Hellenic Arc, whereas geodetic and seismological data show that the highest strain rates are located in western Anatolia. Furthermore, uniform models are non-unique in the sense that since we model a vertically averaged thin plate, different thermal and rheological parameters can be combined to yield the same lithospheric strength. We account for internal sources of deformation with heterogeneous models, where the available constraints on lateral variations of crustal thickness and surface heat flow have been included. The heterogeneous distribution of lithospheric strength contributes to ameliorate the fit to geodetic and stress data, since the predicted velocity field is characterized by an acceleration from E to W, with a sharp increase in the proximity of the western margin of the Anatolian peninsula, where the highest rates of intraplate deformation are observed. In our model this partitioning of the deformation is due to the different rheology of the Aegean Sea, which, being slightly deformable, transmits the TSF to the western margin of Anatolia. Our results are consistent with the interpretation of the Aegean–Anatolian system as a single, rheologically heterogeneous plate.
    Description: Published
    Description: 760-780
    Description: 2T. Deformazione crostale attiva
    Description: JCR Journal
    Keywords: Rheology ; Tectonics ; 04.07. Tectonophysics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
    Publication Date: 2020-09-07
    Description: This study presents and discusses horizontal and vertical geodetic velocities for a low strain rate region of the south Alpine thrust front in northeastern Italy obtained by integrating GPS, interferometric synthetic aperture radar (InSAR) and leveling data. The area is characterized by the presence of subparallel, south-verging thrusts whose seismogenic potential is still poorly known. Horizontal GPS velocities show that this sector of the eastern Southern Alps is undergoing ∼1 mm a−1 of NW–SE shortening associated with the Adria–Eurasia plate convergence, but the horizontal GPS velocity gradient across the mountain front provides limited constraints on the geometry and slip rate of the several subparallel thrusts. In terms of vertical velocities, the three geodetic methods provide consistent results showing a positive velocity gradient, of ∼ 1.5 mm a−1, across the mountain front, which can hardly be explained solely by isostatic processes. We developed an interseismic dislocation model whose geometry is constrained by available subsurface geological reconstructions and instrumental seismicity. While a fraction of the measured uplift can be attributed to glacial and erosional isostatic processes, our results suggest that interseismic strain accumulation at the Montello and the Bassano–Valdobbiadene thrusts it significantly contributing to the measured uplift. The seismogenic potential of the Montello thrust turns out to be smaller than that of the Bassano–Valdobbiadene fault, whose estimated parameters (locking depth equals 9.1 km and slip rate equals 2.1 mm a−1) indicate a structure capable of potentially generating a Mw〉6.5 earthquake. These results demonstrate the importance of precise vertical ground velocity data for modeling interseismic strain accumulation in slowly deforming regions where seismological and geomorphological evidence of active tectonics is often scarce or not conclusive.
    Description: Published
    Description: 1681–1698
    Description: 2T. Deformazione crostale attiva
    Description: JCR Journal
    Keywords: Southern Alps ; Vertical Velocities ; GPS and InSAR integration ; Interseismic Deformation ; Dislocation Model ; Seismic Potential ; 04.03. Geodesy ; 04.07. Tectonophysics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 3
    Publication Date: 2021-06-07
    Description: The diagnosis of the conservation state of monumental structures from constraints to the spatial distribution of their physical properties on shallow and inner materials represents one of the key objectives in the application of non-invasive techniques. In situ, CRP and 3D ultrasonic tomography can provide an effective coverage of stone materials in space and time. The intrinsic characteristics of the materials that make up a monumental structure and affect the two properties (i.e., reflectivity, longitudinal velocity) through the above methods substantially differ. Consequently, the content of their information is mainly complementary rather than redundant. In this study we present the integrated application of different non-destructive techniques i.e., Close Range Photogrammetry (CRP), and low frequency (24 KHz) ultrasonic tomography complemented by petrographycal analysis based essentially on Optical Microscopy (OM). This integrated methodology has been applied to a Carrara marble column of the Basilica of San Saturnino, in Byzantine-Proto-Romanesque style, which is part of the Paleo Christian complex of the V-VI century. This complex also includes the adjacent Christian necropolis in the square of San Cosimo in the city of Cagliari, Sardinia, Italy. The column under study is made of bare material dating back probably to the first century A.D., it was subjected to various traumas due to disassembly and transport to the site, including damage caused by the close blast of a WWII fragmentation bomb. High resolution 3D modelling of the studied artifact was computed starting from the integration of proximal sensing techniques such as CRP based on Structure from Motion (SfM), with which information about the geometrical anomalies and reflectivity of the investigated marble column surface was obtained. On the other hand, the inner parts of the studied body were successfully inspected in a non-invasive way by computing the velocity pattern of the ultrasonic signal through the investigated materials using 3D ultrasonic tomography. This technique gives information on the elastic properties of the material related with mechanical properties and a number of factors, such as presence of fractures, voids, and flaws. Extracting information on such factors from the elastic wave velocity using 3D tomography provides a non-invasive approach to analyse the property changes of the inner material of the ancient column. The integrated application of in situ CRP and ultrasonic techniques provides a full 3D high resolution model of the investigated artifact. This model enhanced by the knowledge of the petrographic characteristics of the materials, improves the diagnostic process and affords reliable information on the state of conservation of the materials used in the construction processes of the studied monumental structure. The integrated use of the non-destructive techniques described above also provides suitable data for a possible restoration and future preservation.
    Description: Copernicus
    Description: Published
    Description: On line
    Description: 5T. Sismologia, geofisica e geologia per l'ingegneria sismica
    Keywords: Cultural Heritage ; Monumental Structures ; Non-Destructive Testing ; Close Range Photogrammetry ; 3D Ultrasonic Tomography ; High resolution 3D modelling ; Restoration ; Conservation ; 05.04. Instrumentation and techniques of general interest
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Abstract
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