The ratio between corner frequencies of source spectra of P- and S-waves—a new discriminant between earthquakes and quarry blasts

• Published in: Journal of seismology 2017, Vol.21 (1), p.209-220
• Main Authors: Ataeva, G., Gitterman, Y., Shapira, A.
• Format: Article
• Language: English
• Subjects: Blasts; Corners; Displacement; Earth and Environmental Science; Earth Sciences; Earthquakes; Explosions; Geophysics/Geodesy; Geotechnical Engineering & Applied Earth Sciences; Hydrogeology; Original Article; Quarries; Spectra; Stations; Structural Geology
• ISSN: 1383-4649; 1573-157X
• DOI: 10.1007/s10950-016-9598-0

This study analyzes and compares the P - and S -wave displacement spectra from local earthquakes and explosions of similar magnitudes. We propose a new approach to discrimination between low-magnitude shallow earthquakes and explosions by using ratios of P- to S -wave corner frequencies as a criterion. We have explored 2430 digital records of the Israeli Seismic Network (ISN) from 456 local events (226 earthquakes, 230 quarry blasts, and a few underwater explosions) of magnitudes Md  = 1.4–3.4, which occurred at distances up to 250 km during 2001–2013 years. P -wave and S -wave displacement spectra were computed for all events following Brune’s source model of earthquakes (1970, 1971) and applying the distance correction coefficients (Shapira and Hofstetter, Teconophysics 217:217–226, 1993; Ataeva G, Shapira A, Hofstetter A, J Seismol 19:389-401, 2015), The corner frequencies and moment magnitudes were determined using multiple stations for each event, and then the comparative analysis was performed. The analysis showed that both P -wave and especially S -wave displacement spectra of quarry blasts demonstrate the corner frequencies lower than those obtained from earthquakes of similar magnitudes. A clear separation between earthquake and explosion populations was obtained for ratios of P- to S -wave corner frequency f 0 ( P )/ f 0 ( S ). The ratios were computed for each event with corner frequencies f 0 of P- and S -wave, which were obtained from the measured f 0 I at individual stations, then corrected for distance and finally averaged. We obtained empirically the average estimation of f 0 ( P )/ f 0 ( S ) = 1.23 for all used earthquakes, and 1.86 for all explosions. We found that the difference in the ratios can be an effective discrimination parameter which does not depend on estimated moment magnitude M w . The new multi-station Corner Frequency Discriminant ( CFD ) for earthquakes and explosions in Israel was developed based on ratios P - to S -wave corner frequencies f 0 ( P )/ f 0 ( S ), with the empirical threshold value of the ratio for Israel as 1.48.