Fig. 5
From: Offshore seismicity in the western Marmara Sea, Turkey, revealed by ocean bottom observation
Correlation coefficients (CCs) among pairs of cluster-A events recorded. a UD component, b horizontal component. CCs of events 3 to 5 at site 7 could not calculate due to the lack of P-wave arrival data. c Normalized waveforms of events 6 (black) and 7 (red). A 4–20 Hz band-pass filter was applied. d Normalized waveforms of events 1, 2, 8–13. A 4–20 Hz band-pass filter was applied