Fig. 12From: Frictional strength of North Anatolian fault in eastern Marmara regionFrequency distributions of the P- and T-axis azimuths of the events in Yalova–Çınarcık region are shown. The negative values in the horizontal axis of the right panel correspond to NNW–SSE directions of the T-axis azimuths portrayed in Fig. 11cBack to article page