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The 2014 Kefalonia Doublet (Mw6.1 and Mw6.0), Central Ionian Islands, Greece: Seismotectonic Implications along the Kefalonia Transform Fault Zone

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The 2014 Kefalonia earthquake sequence started on 26 January with the first main shock (Mw 6.1) and aftershock activity extending over 35 km, much longer than expected from the causative fault segment. The second main shock (Mw 6.0) occurred on 3 February on an adjacent fault segment, where the aftershock distribution was remarkably sparse, evidently encouraged by stress transfer of the first main shock. The aftershocks from the regional catalog were relocated using a 7-layer velocity model and station residuals, and their distribution evidenced two adjacent fault segments striking almost N-S and dipping to the east, in full agreement with the centroid moment tensor solutions, constituting segments of the Kefalonia Transform Fault (KTF). The KTF is bounded to the north by oblique parallel smaller fault segments, linking KTF with its northward continuation, the Lefkada Fault.
Czasopismo
Rocznik
Strony
1--16
Opis fizyczny
Bibliogr. 25 poz., rys., tab.
Twórcy
  • Geophysics Department, Aristotle University of Thessaloniki, Thessaloniki, Greece
  • Geophysics Department, Aristotle University of Thessaloniki, Thessaloniki, Greece
autor
  • Geophysics Department, Aristotle University of Thessaloniki, Thessaloniki, Greece
  • Geophysics Department, Aristotle University of Thessaloniki, Thessaloniki, Greece
  • Geophysics Department, Aristotle University of Thessaloniki, Thessaloniki, Greece
Bibliografia
  • [1] Beeler, N.M., R.W. Simpson, S.H. Hickman, and D.A. Lockner (2000), Pore fluid pressure, apparent friction, and Coulomb failure, J. Geophys. Res. 105, B11, 25533-25542, DOI: 10.1029/2000JB900119.
  • [2] Deng, J., and L.R. Sykes (1997), Evolution of the stress field in southern California and triggering of moderate-size earthquakes: A 200-year perspective, J. Geophys. Res. 102, B5, 9859-9886, DOI: 10.1029/96JB03897.
  • [3] Erickson, L. (1986), User’s manual for DIS3D: A three-dimensional dislocation program with applications to faulting in the Earth, M.Sc. Thesis, Geomechanics Applied Earth Science Dept., Stanford University, Stanford, USA, 167 pp.
  • [4] Harris, R.A. (1998), Introduction to special section: Stress triggers, stress shadows, and implications for seismic hazard, J. Geophys. Res. 103, B10, 24347-24358, DOI:10.1029/98JB01576.
  • [5] Haslinger, F., E. Kissling, J. Ansorge, D. Hatzfeld, E. Papadimitriou, V. Karakostas, K. Makropoulos, H.-G. Kahle, and Y. Peter (1999), 3D crustal structure from local earthquake tomography around the gulf of Arta (Ionian region, NW Greece), Tectonophysics 304, 3, 201-218, DOI: 10.1016/S0040-1951(98)00298-4.
  • [6] Karakostas, V. (2008), Relocation of aftershocks of the 2003 Lefkada sequence: Seismotectonic implications. In: Proc. 3rd Hellenic Conf. Earthquake Engineering and Engineering Seismology, 5-7 November 2008, Athens, Greece, CD ROM, 16 pp.
  • [7] Karakostas, V.G., and E.E. Papadimitriou (2010), Fault complexity associated with the 14 August 2003 Mw6.2, Lefkada, Greece, aftershock sequence, Acta Geophys. 58, 5, 838-854, DOI: 10.2478/s11600-010-0009-6.
  • [8] Karakostas, V.G., E.E. Papadimitriou, and C.B. Papazachos (2004), Properties of the 2003 Lefkada, Ionian Islands, Greece, earthquake seismic sequence and seismicity triggering, Bull. Seismol. Soc. Am. 94, 5, 1976-1981, DOI:10.1785/012003254.
  • [9] Karakostas, V.G., E.E. Papadimitriou, Ch.K. Karamanos, and D.A. Kementzetzidou (2010), Microseismicity and seismotectonic properties of the Lefkada–
  • [10] Kefalonia seismic zone, Bull. Geol. Soc. Greece 43, 2053-2063. Karakostas, V., E. Karagianni, and P. Paradisopoulou (2012), Space-time analysis, faulting and triggering of the 2010 earthquake doublet in western Corinth Gulf, Nat. Hazards 63, 2, 1181-1202, DOI:10.1007/s11069-012-0219-0.
  • [11] Karakostas, V., E. Papadimitriou, and D. Gospodinov (2014), Modelling the 2013 North Aegean (Greece) seismic sequence: geometrical and frictional constraints, and aftershock probabilities, Geophys. J. Int. 197, 1, 525-541, DOI:10.1093/gji/ggt523.
  • [12] Kiratzi, A.A., and C.A. Langston (1991), Moment tensor inversion of the 1983 January 17, Kefallinia event of Ionian islands (Greece), Geophys. J. Int. 105, 2, 529-535, DOI: 10.1111/j.1365-246X.1991.tb06731.x.
  • [13] Klein, F.W. (2000), User’s guide to HYPOINVERSE-2000, a Fortran program to solve earthquake locations and magnitudes, Open File Rep. 02-171, Ver. 1.0, U.S. Geological Survey, Menlo Park, USA.
  • [14] Kokinou, E., E. Papadimitriou, V. Karakostas, E. Kamberis, and F. Vallianatos (2006), The Kefalonia Transform Zone (offshore Western Greece) with special emphasis to its prolongation towards the Ionian Abyssal Plain, Mar. Geophys. Res. 27, 4, 241-252, DOI: 10.1007/s11001-006-9005-2.
  • [15] Louvari, E., A.A. Kiratzi, and B.C. Papazachos (1999), The Cephalonia Transform Fault and its extension to western Lefkada Island (Greece), Tectonophysics 308, 1-2, 223-236, DOI:10.1016/S0040-1951(99)00078-5.
  • [16] Paige, C.C., and M.A. Saunders (1982), Algorithm 583: LSQR – sparse linear equations and least squares problems, ACM Trans. Math. Software 8, 2, 195-209, DOI:10.1145/355993.356000.
  • [17] Papadimitriou, E.E. (1993), Focal mechanism along the convex side of the Hellenic Arc, Boll. Geof. Teor. Appl. 35, 140, 401-426.
  • [18] Papadimitriou, E.E. (2002), Mode of strong earthquake recurrence in the central Ionian Islands (Greece): Possible triggering due to Coulomb stress changes generated by the occurrence of previous strong shocks, Bull. Seismol. Soc. Am. 92, 8, 3293-3308, DOI:10.1785/0120000290.
  • [19] Papadimitriou, E.E., and B.C. Papazachos (1985), Evidence for precursory seismicity patterns in the Ionian Islands (Greece), Earthq. Predict. Res. 3, 95-103.
  • [20] Papazachos, B.C., and C.C. Papazachou (2003), The Earthquakes of Greece, Ziti Publ., Thessaloniki, 304 pp.
  • [21] Rice, J.R., and M.P. Cleary (1976), Some basic stress diffusion solutions for fluidsaturated elastic porous media with compressible constituents, Rev. Geophys. 14, 2, 227-241, DOI: 10.1029/RG014i002p00227.
  • [22] Scordilis, E.M., G.F. Karakaisis, B.G. Karakostas, D.G. Panagiotopoulos, P.E. Comninakis, and B.C. Papazachos (1985), Evidence for transform faulting in the Ionian Sea: The Cephalonia Island earthquake sequence of 1983, Pure Appl. Geophys. 123, 3, 388-397, DOI: 10.1007/BF00880738.
  • [23] Waldhauser, F. (2001), HypoDD – A program to compute double-difference hypocenter locations, Open File Rep. 01-113, U.S. Geological Survey, Menlo Park, USA.
  • [24] Waldhauser, F., and W.L. Ellsworth (2000), A double-difference earthquake location algorithm: Method and application to the Northern Hayward Fault, California, Bull. Seismol. Soc. Am. 90, 6, 1353-1368, DOI: 10.1785/0120000006.
  • [25] Wessel, P., and W.H.F. Smith (1998), New, improved version of Generic Mapping Tools released, EOS Trans. Am. Geophys. Union 79, 47, 579, DOI:10.1029/98EO00426.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-78fb7a44-4d6b-4d07-8f93-a99b09182b28
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