Fig. 9From: Contribution to crustal strain accumulation of minor faults: a case study across the Niigata–Kobe Tectonic Zone, JapanPaired stereonets of slip data in the Inobuseyama area showing results of the multiple inverse method and k-means clustering. Upper plots show results obtained using the multiple inverse method (Yamaji 2000), and lower plots show results obtained using the k-means clustering (Otsubo et al. 2006). The circles and triangles in the stereo of lower side are cluster centersBack to article page