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  • ENDNOTE?  (5)
  • 04. Solid Earth::04.06. Seismology::04.06.07. Tomography and anisotropy  (4)
  • Fracture
  • European Seismological Commission  (5)
  • Agu  (3)
  • American Chemical Society
  • Institute of Physics
Collection
  • 1
    Publication Date: 2021-01-27
    Description: Does the application of seismic Born theory, as opposed to simpler ray theory, lead to an improvement in tomographic images of the Earth? In recent publications, Montelli et al. (2004a, 2004b) and van der Hilst and de Hoop (2005) among others have expressed opposite opinions. We propose a quantitative approach to the comparison of tomographic images, which we apply to the case of surface-wave phase velocity maps derived with Born vs. ray theory.
    Description: Published
    Description: L06302
    Description: JCR Journal
    Description: reserved
    Keywords: global seismic tomography ; 04. Solid Earth::04.06. Seismology::04.06.07. Tomography and anisotropy
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
    Publication Date: 2019-03-05
    Description: An edited version of this paper was published by AGU. Copyright (2010) American Geophysical Union.
    Description: Passive high‐resolution attenuation tomography is used here to image the geological structure in the first upper 4 km of the shallow crust beneath the Campi Flegrei caldera, southern Italy. The inverse Q was estimated for each source‐receiver path using the coda‐normalization method (S‐waves) and the slope decay method (P‐waves and S‐waves). Inversion was performed using a multi‐resolution method, which ensures a minimum cell‐size resolution of 500 m. The study of the resolution matrix as well as the synthetic tests guarantee an optimal reproduction of the input anomalies in the center of the caldera, between 0 and 3.5 km in depth. High attenuation vertical structures are connected at the surface with the main volcanological features (e.g., the Solfatara and Mofete fumarole fields), and depict vertical Q contrast imaging important geological structures, such as the La Starza fault. These high attenuation volumes extend between the surface and a depth of about 3 km, where a hard rock layer is imaged by the sharp contrast of the quality factors. The retrieved image of the Campi Flegrei has been jointly interpreted taking into account evidence from seismological, geological, volcanological and geochemical investigations. This analysis has allowed an unprecedented view of the feeding systems in this area, and in particular it recognizes the vertically extending, high attenuation structures that correspond to gas or fluid reservoirs beneath Pozzuoli‐Solfatara, Solfatara, Mofete‐Mt. Nuovo and Agnano. This high‐attenuation system is possibly connected with the magma sill revealed at about 7 km in depth by passive travel‐time tomography.
    Description: Published
    Description: B09312
    Description: 1.4. TTC - Sorveglianza sismologica delle aree vulcaniche attive
    Description: 3.1. Fisica dei terremoti
    Description: JCR Journal
    Description: reserved
    Keywords: Campi Flegrei ; gas ; 04. Solid Earth::04.06. Seismology::04.06.07. Tomography and anisotropy ; 04. Solid Earth::04.06. Seismology::04.06.08. Volcano seismology ; 04. Solid Earth::04.06. Seismology::04.06.09. Waves and wave analysis ; 05. General::05.01. Computational geophysics::05.01.03. Inverse methods
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 3
    Publication Date: 2017-04-04
    Description: Travel times of about 39,000 Pn arrivals recorded from regional earthquakes by the Italian Telemetered Seismic Network and by stations of nearby countries are inverted to image lateral variations of seismic velocity and anisotropy at subcrustal depth in Italy and surrounding regions. This method allows simultaneous imaging of variations of Pn velocity and anisotropy, as well as crustal thickness variations. The Po plain, the Adriatic Sea, and the Ionian Sea have normal to high Pn velocities. In contrast, lower velocities (7.9-8.0 km/s) are imaged in Italy beneath the western Alps, the northern Apennines, and eastern Sicily and nearby Calabria, as well as in northern Albania and beneath the Pannonian basin. Low Pn velocities beneath the northern Apennines correlate with present-day extension and may have resulted from thermal anomalies in the uppermost mantle due to delamination processes. Low velocities are consistent with the high-attenuation zone inferred in the uppermost mantle beneath the internal Apennine units and the Tyrrhenian margin of the peninsula by Mele et al. [1996, 1997]. On the contrary, low velocities beneath the western Alps may be an apparent effect due to the abrupt thickening of the crustal roots. Pn velocity is anisotropic in the study area with a maximum amplitude of ± 0.2 km/s. The largest anisotropic velocity anomalies are observed along the major arc structures of Italy, i.e., the northern Apennines and the Calabrian Arc, indicating that these features are controlled by uppermost mantle processes. The anisotropy anomaly along the Calabrian Arc extends as far as Albania but ends abruptly north of this area, suggesting that a lithospheric discontinuity is present along the northern Albanian border.
    Description: Published
    Description: 12,529-12,543
    Description: JCR Journal
    Description: reserved
    Keywords: Pn anisotropic tomography ; Italy ; 04. Solid Earth::04.06. Seismology::04.06.07. Tomography and anisotropy
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 4
    Publication Date: 2017-04-04
    Description: The many studies conducted on the Italian area led to several models to explain the present-day structural setting. Some of the most debated questions are the presence or not of continuous subduction and the presence or not of a slab detachment in the northern or in the central part of the Apenninic chain. The absence of a continuous, high velocity body beneath the Apennines has been interpreted by some researchers as an evidence of the detachment of the Apenninic slab. According to this view the Apenninic slab is expected to be inactive whether the Ionian lithosphere subducting underneath Calabria is considered to be on the verge of detaching or just detached. Other researchers however, suggest that a fairly continuous and fast slab exists beneath the Apennines and the Calabrian arc. Different geodynamical models have also been proposed for the Tyrrhenian area considering it as an active or as a passive margin. Our working group has conducted several seismic tomographies in the search of the geometry, size and extension with depth of the subduction under the Italian peninsula. While the images resulting from teleseismic data were clearly showing a subducting slab under the Calabrian arc, they were not conclusive for the rest of the Apennines since they were showing, only in the Northern sector, a likely subduction in the shallower part apparently detached from other high velocities body in the deeper zone. At that stage it was not possible to distinguish between thrust and subduction due to the poor horizontal resolution of the applied methodology. In order to analyze in more details this apparent discrepancy, a new seismic local tomography has been conducted with a very dense grid, the selection of a smaller area to be investigated (limited to the Apennines only) and the addition of new data: all these features contributed to partly improve the results, which cannot anyway extend beyond the maximum depth of seismic events. The main limitation in this kind of experiment is the lack of seismic events deeper than 60-70 km under the northern and central Apennines although, as many authors assume, is not itself an evidence against subduction. Analyzing different cross sections of the enhanced resolution tomography results, we do not see any slab in the northern-central Apennines in the first 80-100 km depth. The downgoing material (Adriatic plate) of this area has a rather low dip angle, as also partly shown by the distribution of the (few) deep seismic events. Along the central and also the northern part of the Apennines there are more overlapping than subducting geometries.
    Description: Published
    Description: Montpellier, France
    Description: 3.3. Geodinamica e struttura dell'interno della Terra
    Description: open
    Keywords: Tomography ; Apennines ; 04. Solid Earth::04.06. Seismology::04.06.07. Tomography and anisotropy
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Abstract
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  • 5
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    European Seismological Commission
    In:  Seismology in Europe. Papers presented at the XXV General Assembly of ESC, September 9-14, 1996 in Reykjavík, Iceland, Reykjavík, European Seismological Commission, vol. 37, pp. 199-204, (ISBN 0080419208)
    Publication Date: 1996
    Keywords: Structural geology ; Fault plane solution, focal mechanism ; Geol. aspects ; Tectonics ; Roegnvaldsson ; Rognvaldsson ; Gudmundsson ; Stefansson ; BIBTEX? ; ENDNOTE?
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  • 6
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    Institute of Physics
    In:  Professional Paper, Boundary Element Methods. Theory and Application, Bristol, Institute of Physics, vol. 9, no. 16, pp. 1-23, (ISBN 1-4020-1729-4)
    Publication Date: 1986
    Keywords: Stress ; Rock mechanics ; Stress intensity factor ; Boundary Element Method ; Fracture ; ENDNOTE?
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  • 7
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    European Seismological Commission
    In:  Professional Paper, Seismology in Europe. Papers presented at the XXV General Assembly of ESC, September 9-14, 1996 in Reykjavík, Iceland, Reykjavík, European Seismological Commission, vol. 65, no. 16, pp. 193-198, (ISBN: 3-540-23712-7)
    Publication Date: 1996
    Keywords: Stress ; Fault zone ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Geol. aspects ; Structural geology ; ENDNOTE?
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  • 8
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    European Seismological Commission
    In:  Bull., Open-File Rept., Seismology in Europe. Papers presented at the XXV General Assembly of ESC, September 9-14, 1996 in Reykjavík, Iceland, Reykjavík, European Seismological Commission, vol. 10, no. 16, pp. 461-466, (ISBN 0080419208)
    Publication Date: 1996
    Keywords: Seismicity ; Volcanology ; Plate tectonics ; Gudmundsson ; Augustsson ; Agustsson ; Stefansson ; Rognvaldsson ; ENDNOTE?
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  • 9
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    Institute of Physics
    In:  Bristol, Institute of Physics, vol. 8, no. Publ. No. 12, pp. 95-104, (ISBN 0-865-42078-5)
    Publication Date: 1986
    Keywords: Rock mechanics ; Fracture ; Boundary Element Method ; Elasticity ; Dynamic
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  • 10
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    European Seismological Commission
    In:  Bull., Open-File Rept., Seismology in Europe. Papers presented at the XXV General Assembly of ESC, September 9-14, 1996 in Reykjavík, Iceland, Reykjavík, European Seismological Commission, vol. 76, no. 16, pp. 491-497 Iceland, (ISBN 1-86239-165-3, vi + 330 pp.)
    Publication Date: 1996
    Keywords: Seismicity ; Seismic networks ; Gudmundsson ; Stefansson ; ENDNOTE?
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