Fig. 8From: Crustal structure of the eastern Piedmont and Atlantic coastal plain in North Carolina and Virginia, eastern North American marginS-wave velocity structure along the Line 1 seismic profile. The red line indicates the reflection boundaries used in the inversion. The red stars indicate the shotpoints (SP). As is evident in the seismic ray diagrams (Fig. 9), there is no seismic coverage beyond the white dash lines. The wide-angle reflections S1S, S2S, S3S, S4S, and PmP are generated from boundaries 1, 2, 3, 4, and Moho, respectivelyBack to article page