Fig. 9From: Stress state along the Anninghe-Zemuhe fault zone, southwestern China, estimated from an array of stress orientation measurements with a new methodMap of SHmax orientations. The length of the white bar is proportional to the value of the flattening parameter of the ellipse which expresses the degree of borehole deformation. The data from the other study of Cui et al. (2006) (open circles) and in Huang et al. (2009) (closed circles) are also shown. The dotted line at each site denotes a theoretical stress orientation caused by the gravitational effect of landscape topography.Back to article page