Fig. 9From: 3D crustal structure of the northwest Alborz region (Iran) from local earthquake tomographySimplified geological map of NW Iran modified from Solaymani Azad et al. (2011), overlain by the shallow depth local velocity anomalies corresponding to Fig. 8G. Labels 1a and 2 mark the well-resolved high- and low-velocity anomalies, respectively, while label 1b marks the fairly-well resolved high-velocity anomaly (see text)Back to article page