Fig. 5From: Surface wave group velocity in the Osaka sedimentary basin, Japan, estimated using ambient noise cross-correlation functionsComparison of the causal and acausal parts of the obtained inter-station cross-correlation functions for two station pairs (UEMC06–UEMC09 and UEMC05–UEMC13). Black and blue traces represent the causal and acausal parts, respectively. The R–R and T–T components in five different frequency ranges are presentedBack to article page