“…Ambient noise tomography has mainly been applied to surface waves, has extended analysis to shorter periods (<20 s) than from traditional earthquake tomography, and has provided higher resolution constraints on the structures of the crust and uppermost mantle. Currently, ambient noise tomography has been applied around the world to study crustal and uppermost structures; for example, Shapiro et al (2005), Moschetti et al (2007), Bensen et al (2008), Liang and Langston (2009) in US; Kang and Shin (2006), Cho et al (2007), Fang et al (2010), Li et al (2009), Yang et al (2010, Yao et al (2006Yao et al ( , 2008 in Asia; and Villaseñor et al (2007) in Europe; Arroucau et al (2010), Behr et al (2010), Lin et al (2007), Saygin and Kennett (2010) in New Zealand and Australia, and so on.…”