The objective of our study is to supplement the regional P/S 3-D velocity model in the Reno basin with shear-wave velocity models derived from ambient noise interferometry (Aki 1957; Claerbout 1968; Shapiro et al. 2005; Sabra et al. 2005; Lin et al. 2008; Yang et al. 2008). We use a variety of seismic sensors in the Reno-Carson area (Figure 1).

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There is a gap for demonstrated extraction of Green's functions (GFs) from ambient noise between short and long interstation distances. The lateral resolution of existing tomographic models exceeds the...

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