Fig. 2From: Geophysical imaging of subsurface structures in volcanic area by seismic attenuation profilingPost-stack time migrated section of KR101. Stratified continuous layers can be seen in the shallowest part of the line. Beneath the stratified layers, only a chain of intermittently continuous reflectors with strong amplitude is recognized in about 2.5–3.0 s of two-way traveltime at shot point (SP) 1300–1500, which are marked by dotted circles Back to article page