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  • Textbook of geophysics  (9)
  • 04. Solid Earth::04.06. Seismology::04.06.08. Volcano seismology  (2)
  • Fluids  (2)
  • 03. Hydrosphere::03.04. Chemical and biological::03.04.06. Hydrothermal systems
  • 04. Solid Earth::04.04. Geology::04.04.08. Sediments: dating, processes, transport
  • 04. Solid Earth::04.04. Geology::04.04.10. Stratigraphy
  • Acoustics
  • Applied geophysics
  • Data analysis / ~ processing
  • Schussler
  • Elsevier  (6)
  • Cambridge Univ. Press  (3)
  • Cambridge U. Press  (2)
  • EGU - Copernicus  (1)
  • Soc. of Exploration Geophys.
  • W.H. Freeman
  • 2010-2014  (2)
  • 2000-2004  (10)
  • 1980-1984
  • 2013  (2)
  • 2001  (10)
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Keywords
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  • 2010-2014  (2)
  • 2000-2004  (10)
  • 1980-1984
Year
  • 1
    Publication Date: 2017-04-04
    Description: During his trip on the Beagle, Charles Darwin wrote about the eruptions associated with the Concepci´on earthquake of 1835. A later survey by Lorenzo Casertano, following the great 1960 Chilean earthquake, identified some unclear evidence of a link between eruptions and the seismic event, although some reservations were also raised. Using data available in 2006 in the Smithsonian Institution Catalogue of volcanic eruptions, Scalera revealed grounded evidence that South-American Wadati-Benioff zone earthquakes of magnitudes greater than 8.4 are associated with an increased rate of volcanic eruptions, but it was still impossible to determine a causal link between the two phenomena. An average return period of about 50 yr was deducible from the data for the time window 1800–1999. After 2006, the Smithsonian Institution’s effort to improve our knowledge of this region has greatly increased the completeness of the catalogue, adding the eruptions from the 2000– 2010 interval, together with 50% more new entries in the list of Andean volcanoes. The great Chilean Maule earthquake of 27 February 2010 (M = 8.8), occurring exactly five decades after the 1960 event, provided an occasion to reanalyse this updated database. The results suggest a preferential causal eruptions-earthquake relationship, but additional future volcano-seismic events should be studied to arrive at a definitive conclusion, within the perspective of using this phenomenon for Civil Protection. The possible correlation of South American volcano-seismic events with the Markowitz oscillation of the Polar Motion is another good reason for trying to establish an integrated geodynamic explanation.
    Description: Published
    Description: 89-103
    Description: 1.5. TTC - Sorveglianza dell'attività eruttiva dei vulcani
    Description: 3.3. Geodinamica e struttura dell'interno della Terra
    Description: 5.3. TTC - Banche dati vulcanologiche
    Description: JCR Journal
    Description: open
    Keywords: Volcano-seismic correlation ; Volcano-seismic risk ; Polar Motion and volcano-seismic events ; Expanding Earth ; 04. Solid Earth::04.01. Earth Interior::04.01.02. Geological and geophysical evidences of deep processes ; 04. Solid Earth::04.06. Seismology::04.06.08. Volcano seismology ; 04. Solid Earth::04.07. Tectonophysics::04.07.02. Geodynamics ; 04. Solid Earth::04.08. Volcanology::04.08.06. Volcano monitoring ; 05. General::05.02. Data dissemination::05.02.03. Volcanic eruptions ; 05. General::05.08. Risk::05.08.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
    Publication Date: 2017-04-04
    Description: Repeating volcano-tectonic (VT) earthquakes, taking place at Mt. Etna during 1999–2009,were detected and analyzed to investigate their behavior. We found 735 families amounting to 2479 VT earthquakes, representing ~38% of all the analyzed VT earthquakes. The number of VT earthquakes making up the families ranges from 2 to 23. Over 70% of the families comprise 2 or 3 VT earthquakes and only 20 families by more than 10 events. The occurrence lifetime is also highly variable ranging from some minutes to ten years. In particular, more than half of the families have a lifetime shorter than 0.5 day and only ~10% longer than 1 year. On the basis of these results, most of the detected families were considered “burst-type”, i.e., show swarm-like occurrence, and hence their origin cannot be explained by a temporally constant tectonic loading. Indeed, since the analyzed earthquakes take place in a volcanic area, the rocks are affected not only by tectonic stresses related to the fairly steady regional stress field but also by local stresses, caused by the volcano, such as magma batch intrusions/ movements and gravitational loading.We focused on the five groups of families characterized by the longest repeatability over time, namely high number of events and long lifetime, located in the north-eastern, eastern and southern flanks of the volcano. Unlike the first four groups, which similarly to most of the detected families show swarm-like VT occurrences, group “v”, located in the north-eastern sector, exhibits a more “tectonic” behavior with the events making up such a group spread over almost the entire analyzed period. It is clear how both occurrence and slip rates do not remain constant but vary over time, and such changes are time-related to the occurrence of the 2002–2003 eruption. Finally, by FPFIT algorithm a good agreement between directions identified by nodal planes and the earthquake epicentral distribution was generally found.
    Description: Published
    Description: 1223 – 1236
    Description: 1.4. TTC - Sorveglianza sismologica delle aree vulcaniche attive
    Description: JCR Journal
    Description: restricted
    Keywords: repeating earthquakes ; Etna ; 04. Solid Earth::04.06. Seismology::04.06.08. Volcano seismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 3
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    Cambridge Univ. Press
    In:  New York (306 pp.), Cambridge Univ. Press, vol. 4, no. 3, pp. 2-203, (ISBN 0-521-80604-6, ISBN 0-521-01472-7 paper)
    Publication Date: 2001
    Keywords: Textbook of geophysics ; hot ; spots ; Plate tectonics ; ConvolutionE ; Geol. aspects
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  • 4
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    Cambridge U. Press
    In:  New York (573 pp.), Cambridge U. Press, vol. 10, no. 2, pp. 125-169, (ISBN 0-521-00098-X)
    Publication Date: 2001
    Keywords: Geomagnetics ; Physical properties of rocks ; Textbook of geophysics ; Oezdemir ; Ozdemir
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  • 5
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    Elsevier
    In:  Amsterdam, 300 pp., Elsevier, vol. 34, no. 22, pp. 65-70, (ISBN 3-7643-0253-4)
    Publication Date: 2001
    Keywords: Fluids ; Textbook of geophysics ; Geochemistry
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  • 6
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    Cambridge Univ. Press
    In:  New York (343 pp.), Cambridge Univ. Press, vol. 1, no. Publ. No. 12, pp. 127, (ISBN 0-521-66034-3, ISBN 0-521-66948-0 paper)
    Publication Date: 2001
    Keywords: Textbook of geophysics ; Textbook of geology ; optics ; LASER ; RADAR
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  • 7
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    Elsevier
    In:  Amsterdam, 298 pp., Elsevier, vol. 70, no. Publ. No. 12, pp. 1039-1054, (ISBN 0-444-50971-2)
    Publication Date: 2001
    Keywords: Subduction zone ; Review article ; Hypocentral depth ; Fault plane solution, focal mechanism ; Seismicity ; Mineralogy ; Hilst ; triggering ; Stress ; Rheology ; Geochemistry ; Strength ; Fluids ; ConvolutionE
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  • 8
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    Elsevier
    In:  Amsterdam, Elsevier, vol. 10, no. ALEX(01)-FR-77-01, AFTAC Contract F08606-76-C-0025, pp. 329, (ISBN: 0-08-043649-8)
    Publication Date: 2001
    Description: Following the breakthrough in the last decade in identifying the key parameters for time and depth imaging in anisotropic media and developing practical methodologies for estimating them from seismic data, this title primarily focuses on the far reaching exploration benefits of anisotropic processing. This volume provides the first comprehensive description of reflection seismic signatures and processing methods in anisotropic media. It identifies the key parameters for time and depth imaging in transversely isotropic media and describes practical methodologies for estimating them from seismic data. Also, it contains a thorough discussion of the important issues of uniqueness and stability of seismic velocity analysis in the presence of anisotropy. The book contains a complete description of anisotropic imaging methods, from the theoretical background to algorithms to implementation issues. Numerous applications to synthetic and field data illustrate the improvements achieved by the anisotropic processing and the possibility of using the estimated anisotropic parameters in lithology discrimination.
    Keywords: Textbook of geophysics ; Seismics (controlled source seismology) ; Reflection seismics ; Anisotropy
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  • 9
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    Cambridge Univ. Press
    In:  New York, Cambridge Univ. Press, vol. 10, no. 1, pp. 1-40, (ISBN 0-521-62272-7, ISBN 0-521-00600-7 paper)
    Publication Date: 2001
    Keywords: Textbook of geophysics ; Gravimetry, Gravitation ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Tectonics ; density
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  • 10
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    Elsevier
    In:  Amsterdam, 680 pp., Elsevier, vol. 33, no. 2, pp. 125-169, (ISBN: 3-540-42642-6, Approx. 620 p. 30 illus., Hardcover)
    Publication Date: 2001
    Keywords: Borehole geophys. ; Textbook of geophysics ; Electromagnetic methods/phenomena
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  • 11
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    Cambridge U. Press
    In:  New York (370 pp.), Cambridge U. Press, vol. 13, no. XVI:, pp. 227-235, (ISBN 0-521-80945-2, ISBN 0-521-00663-5 paper)
    Publication Date: 2001
    Keywords: Waves ; Wave propagation ; Textbook of geophysics ; observations ; (part ; 1), ; theory ; (part ; 2) ; Ray seismics ; Anisotropy ; Attenuation ; Elasticity
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  • 12
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    Elsevier
    In:  Amsterdam, 356 pp., Elsevier, vol. 2, no. XVI:, pp. 1-14, (ISBN: 0-387-30752-4)
    Publication Date: 2001
    Keywords: Textbook of engineering ; Textbook of geophysics ; Statistical investigations
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