Preliminary Estimation of Kappa Parameter in Croatia

World Multidisciplinary Earth Sciences Symposium 2017

Stanko, Davor^1 ; Markui, Snjeana^2 ; Ivani, Ines^2 ; Mario, Gazdek^1 ; Gülerce, Zeynep^3

Faculty of Geotechnical Engineering, University of Zagreb, Varadin, Croatia^1

Department of Geophysics, Faculty of Science, University of Zagreb, Zagreb, Croatia^2

Middle East Technical University, Civil Engineering Department, Ankara, Turkey^3

关键词: Acceleration amplitude;    Azimuthal distributions;    Earthquake parameters;    Geophysical measurements;    Local site condition;    Seismic hazard maps;    Shear wave velocity;    Vertical accelerations;   

Others  :  https://iopscience.iop.org/article/10.1088/1755-1315/95/3/032014/pdf
DOI  :  10.1088/1755-1315/95/3/032014

来源: IOP

【 摘 要 】

Spectral parameter kappa κ is used to describe spectral amplitude decay "crash syndrome" at high frequencies. The purpose of this research is to estimate spectral parameter kappa for the first time in Croatia based on small and moderate earthquakes. Recordings of local earthquakes with magnitudes higher than 3, epicentre distances less than 150 km, and focal depths less than 30 km from seismological stations in Croatia are used. The value of kappa was estimated from the acceleration amplitude spectrum of shear waves from the slope of the high-frequency part where the spectrum starts to decay rapidly to a noise floor. Kappa models as a function of a site and distance were derived from a standard linear regression of kappa-distance dependence. Site kappa was determined from the extrapolation of the regression line to a zero distance. The preliminary results of site kappa across Croatia are promising. In this research, these results are compared with local site condition parameters for each station, e.g. shear wave velocity in the upper 30 m from geophysical measurements and with existing global shear wave velocity - site kappa values. Spatial distribution of individual kappa's is compared with the azimuthal distribution of earthquake epicentres. These results are significant for a couple of reasons: to extend the knowledge of the attenuation of near-surface crust layers of the Dinarides and to provide additional information on the local earthquake parameters for updating seismic hazard maps of studied area. Site kappa can be used in the re-creation, and re-calibration of attenuation of peak horizontal and/or vertical acceleration in the Dinarides area since information on the local site conditions were not included in the previous studies.