Fig. 3From: Source process of the 12 May 2008 Wenchuan, China, earthquake determined by waveform inversion of teleseismic body waves with a data covariance matrixThe total slip distribution inverted by the present study (a) and obtained by Nishimura and Yagi (2008) (b). The star shows the hypocenter and the arrows are the slip vectors at each spatial knot.Back to article page