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  • Body waves  (2)
  • Kajima Corp., Kajima Inst. of Constr. Technol., Japan  (1)
  • Oxford University Press  (1)
  • American Chemical Society
  • American Institute of Physics (AIP)
  • Nature Publishing Group
  • Periodicals Archive Online (PAO)
  • 2020-2023  (1)
  • 1990-1994  (1)
  • 1975-1979
  • 1955-1959
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Publisher
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  • 2020-2023  (1)
  • 1990-1994  (1)
  • 1975-1979
  • 1955-1959
  • 2015-2019  (3)
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  • 1
    Publication Date: 2021-12-15
    Description: This article has been accepted for publication in Geophysical Journal International ©: The Authors 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.
    Description: To understand the seismotectonics and the seismic hazard of the study sector of the Northern Apennines (Italy), one of the most important earthquakes of magnitude Mw = 6.5 which struck the Lunigiana and Garfagnana areas (Tuscany) on 7 September 1920 should be studied. Given the early instrumental epoch of the event, neither geometric and kinematic information on the fault-source nor its fault-plane solution were available. Both areas were candidates for hosting the source fault and there was uncertainty between a normal fault with Apenninic direction or an anti-Apenninic strike-slip. We retrieved 11 focal parameters (including the fault-plane solution) of the 1920 earthquake. Only macroseismic intensity information (from 499 inhabited centres) through the KF-NGA inversion technique was used. This technique uses a Kinematic model of the earthquake source and speeds up the calculation by a Genetic Algorithm with Niching. The result is a pure dip-slip focal solution. The intrinsic ambiguities of the KF-NGA method (±180° on the rake angle; choice of the fault plane between the two nodal planes) were solved with field and seismotectonic evidence. The earthquake was generated by a normal fault (rake angle = 265° ± 8°) with an Apennine direction (114° ± 5°) and dipping 38° ± 6° towards SW. The likely candidate for hosting the source-fault in 1920 is the Compione-Comano fault that borders the NE edge of the Lunigiana graben. The KF-NGA algorithm proved to be invaluable for studying the kinematics of early instrumental earthquakes and allowed us to uniquely individuate, for the first time ever, the seismogenic source of the 1920 earthquake. Our findings have implications in hazard computation and seismotectonic contexts.
    Description: Published
    Description: 1465–1477
    Description: 4T. Sismicità dell'Italia
    Description: JCR Journal
    Keywords: Inverse theory ; Body waves ; Earthquake source observations ; Seismicity and tectonics ; Dynamics: seismotectonics ; Fractures, faults, and high strain deformation zones ; 04.06. Seismology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
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    Kajima Corp., Kajima Inst. of Constr. Technol., Japan
    In:  Nippon Jishin Kogaku Shinpojiumu Ronbunshu (Proceedings of the Japan Earthquake Engineering Symposium), vol. 9, Part 2, pp. 2281-2286, Washington, D. C., 220 pp., Kajima Corp., Kajima Inst. of Constr. Technol., Japan, vol. C 560, 183 pp., no. 70, pp. 263-267, (ISBN 3-933346-037)
    Publication Date: 1994
    Description: A newly developed real-time earthquake information system is presented. This system is composed of five earthquake detection stations, information center, and transmission devices for users. For data communication between the detection station and the information center, a network using packet-switched communication service has been installed. The system is simplified warning system which notifies users of the occurrence of an earthquake and its information such as location, magnitude and seismic intensity by announcement units and pocket pagers. The purpose of this study is to develop the early warning system for the practical use which provides information before a strong earthquake strikes. The results of this study will be possible to provide various applications for the future earthquake hazard mitigation depending on the users' objectives.
    Keywords: Early warning systems (earthquakes, volcanic eruptions, tsunamis etc.) ; Rapid damage assessment ; hypocenter ; Seismometer ; LAN ; information ; system ; service ; Detectors ; workstation ; disaster ; prevention ; countermeasure ; P-waves ; Intensity ; Attenuation ; regression ; analysis ; Earthquake engineering, engineering seismology ; wave ; source ; computer ; network ; communication ; network ; countermeasure ; Body waves ; Statistical investigations
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