Fig. 6From: Crustal structure of the eastern Piedmont and Atlantic coastal plain in North Carolina and Virginia, eastern North American margina The record section of SP1. Region A′ is the expansion of region A, showing that there is a strong reflection after the Pg phase. b The record section of SP3. Region B′ is the expansion of region B, indicating there is a reflection after Pg. It is close to Pg, so it is possibly generated by the very shallow structure. Region C shows a step of Pg, and region D shows that there is a shadow zone between 60 and 80 km, indicating a low-velocity zone (LVZ) in upper crust (Park et al. 2010). Note that this LVZ is not the LVZ above (Figs. 3a, 5); rather this LVZ is much shallower and smallerBack to article page