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  • 1
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    In:  Geophys. J. Int., Luxembourg, EGS-Gauthier-Villars, vol. 159, no. 1, pp. 347-352, pp. 1689
    Publikationsdatum: 2004
    Schlagwort(e): Rheology ; Friction ; red ; silent ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Strain ; Seismology ; fault ; slip, ; gouge, ; rheology ; strain ; measurements ; GJI
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  • 2
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    In:  Bull. Seism. Soc. Am., Luxembourg, EGS-Gauthier-Villars, vol. 95, no. 2, pp. 390-400, pp. 2324
    Publikationsdatum: 2005
    Schlagwort(e): Seismology ; Moment tensor ; Data analysis / ~ processing ; Error analysis ; BSSA
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  • 3
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    In:  Rev. Geophys., Luxembourg, EGS-Gauthier-Villars, vol. 29, no. S, pp. 700-720, pp. 1310
    Publikationsdatum: 1991
    Schlagwort(e): Strong motions ; Review article ; Earthquake engineering, engineering seismology ; 7235 ; Seismology ; Strong ; motions ; and ; engineering ; seismology ; 7294 ; Instruments ; and ; techniques ; 7215 ; Earthquake ; parameters ; 7205 ; Body ; waves
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  • 4
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    In:  Bulletin of the Seismological Society of America, Luxembourg, EGS-Gauthier-Villars, vol. 89, no. 2, pp. 456-467, pp. 1310
    Publikationsdatum: 1999
    Schlagwort(e): Nuclear explosion ; Earthquake hazard ; Seismology ; BSSA
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  • 5
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    In:  Geophys. J. Int., Luxembourg, EGS-Gauthier-Villars, vol. 143, no. 2, pp. 279-294, pp. L23608
    Publikationsdatum: 2000
    Schlagwort(e): Seismology ; Elasticity ; Geothermics ; thermodynamics ; compression ; earth Core ; GJI
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  • 6
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    In:  Bull. Seism. Soc. Am., Washington D.C., Bundesanstalt für Geowissenschaften und Rohstoffe, vol. 93, no. 1, pp. 465-479, pp. 2122
    Publikationsdatum: 2003
    Beschreibung: To investigate the effect of the shallow, low-velocity sediments on the seismic wave field in the northern San Francisco Bay, we modeled tangential component displacement seismograms recorded during the 18 August 1999 MW 4.6 Bolinas, California, earthquake. The modeling indicates that the velocity structure of Pleistocene horizons in the San Francisco Bay is important for simulations of weak ground motions for Bay Area earthquakes. Models including the Pleistocene sediments generate the 1-sec-period surface waves observed at several stations. Modeling of Treasure and Yerba Buena Island records requires structures approximately an order of magnitude higher in spatial resolution than the current 3D velocity models for the region. This pair of sites, located only 2 km apart in the bay, records a sixfold difference in peak ground acceleration during the Bolinas earthquake. Three transects are forward modeled using 1D frequency-wavenumber integration and 2D finite-difference methods. Generally the ground motions are characterized by a direct shear wave (S0), a midcrustal reflection (S1), a near-receiver multiple (S2), and surface waves. The direct S0 arrival at all six stations requires a faster model than GIL7, the model routinely used to estimate earthquake source parameters using the Berkeley Digital Seismic Network. In addition, the timing of S1 indicates the possibility of a dipping midcrustal interface. S2 can be matched with a single strong impedance contrast at 3 km depth. A thin (200-m) surface layer of weathered rock and sediments simulates the surface waves that follow S2 at the Richmond Field Station site. However, the surface waves at Treasure Island and the Berkeley sites are longer in duration and higher amplitude than at Richmond and require 2D structure. A simple shallow uniform basin model for the San Francisco Bay consisting of stiff sediments (shear-wave velocity, Vs = 400 m/sec; thickness ~100 m) over weathered rock (Vs = 1.5 km/sec) of the Franciscan assemblage produces surface waves in the 0.02-2 Hz passband at Treasure Island and the Berkeley sites.
    Schlagwort(e): Seismology ; Earthquake ; Site amplification ; Wave propagation ; Wave form analysis ; USA ; Two-dimensional ; Finite difference method ; Modelling ; Velocity depth profile ; Shear waves ; Surface waves ; Seismic networks ; Reflectivity ; noksp ; BSSA
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  • 7
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    In:  Bull. Seism. Soc. Am., Washington D.C., Bundesanstalt für Geowissenschaften und Rohstoffe, vol. 92, no. 1, pp. 509-526, pp. L09611
    Publikationsdatum: 2002
    Schlagwort(e): Seismology ; Site amplification ; Earthquake risk ; Strong motions ; Turkey ; Izmit ; Earthquake ; Earthquake engineering, engineering seismology ; Review article ; Fault zone ; NAF ; Bakir ; Sucuoglu ; Yilmaz ; BSSA ; SPAROLAI
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  • 8
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    In:  Bull. Seism. Soc. Am., Washington D.C., Bundesanstalt für Geowissenschaften und Rohstoffe, vol. 69, no. 4, pp. 1027-1038, pp. L09611
    Publikationsdatum: 1979
    Schlagwort(e): Fore-shocks ; Earthquake ; Discrimination ; Earthquake precursor: prediction research ; Spectrum ; Corner frequency ; Seismology ; Body waves ; BSSA
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  • 9
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    In:  Proceedings of the Yorkshire Geological Society, Warszawa, Bundesanstalt für Geowissenschaften und Rohstoffe, vol. 45, no. 1 & 2, pp. 19-24, pp. 2121
    Publikationsdatum: 1984
    Schlagwort(e): Seismics (controlled source seismology) ; Seismology ; Velocity depth profile ; Guerbuez ; Gurbuz
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  • 10
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    In:  Bull. Seism. Soc. Am., Warszawa, Bundesanstalt für Geowissenschaften und Rohstoffe, vol. 80, no. 3, pp. 1999-2015, pp. 2121
    Publikationsdatum: 1990
    Schlagwort(e): Resolution ; Nuclear explosion ; Seismology ; Seismic arrays ; BSSA
    Standort Signatur Erwartet Verfügbarkeit
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