Seismic Refraction/Wide-Angle Reflection Profiles
Seismic Refraction/Wide-Angle Reflection Profiles : Also referred to as Deep Seismic Sounding (DSS) profiles. Seismic velocity structures in the lithosphere derived from data recorded with long offsets (100- 300 km) between sources and receivers consisting of widelyspaced geophones (100-5,000 m). See Mooney et al. (2002)