Fig. 2From: Source process of the 12 May 2008 Wenchuan, China, earthquake determined by waveform inversion of teleseismic body waves with a data covariance matrixTeleseismic station distribution (a) and comparison of observed and synthetic seismograms (b). In (a) the triangles indicate the global stations used in this study, and the yellow star indicates the epicenter. In (b) black and red lines indicate observed and synthetic velocity seismograms, respectively, band-passed between 0.001 and 4.5 Hz with a sampling rate of 10 Hz. The station code, maximum amplitude, azimuth, and distance from the epicenter are given above each waveform.Back to article page