With the advent of the ambient noise cross-correlation technique (Campillo & Paul, 2003;Shapiro & Campillo, 2004), surface wave imaging was freed from its dependence on the occurrence of earthquakes; as a consequence, surface wave imaging has undergone substantial development in the past two decades (e.g., Shapiro et al., 2005;Yao et al., 2006). By calculating the cross-correlation function, body wave impulse responses (which are much weaker than surface waves) can also be retrieved from earthquake coda waves and continuous ambient noise data (e.g.,