Fig. 14From: Estimation of shallow S-wave velocity structure in the Puli basin, Taiwan, using array measurements of microtremors(a) Based on Fig. 10, the variations of the depths of the bedrock (V S = 2000 m/s) are between 300 m and 870 m in the Puli basin. (b) Map sketching the variations in depth of the bedrock obtained by the seismic reflection method in the Puli basin (Huang, 2008).Back to article page