Using a Three‐Component Distributed Array of Mixed, Horizontal, and Vertical Single‐Component Seismometers to Produce a Receiver Function from a Short Deployment

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 V_P/V_S ratio of the crust...