Receiver function (RF) imaging is an important tool in the investigation of the crust (e.g., Burdick and Langston, 1977; Langston, 1979; Owens et al., 1984; Owens and Crosson, 1988; Zhang and Langston, 1995) and upper mantle (Vinnik, 1977; Gurrola et al., 1994). The P‐to‐S conversion (Ps) from the Moho is typically one of the most prominent phases on P‐wave RFs. Estimates of the depth and thickness of the Moho (e.g., Grad and Tiira, 2012) and VP/VS ratio of the crust...
You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
