Fig. 11
From: Frictional strength of North Anatolian fault in eastern Marmara region
Stress tensor inversion results using the focal mechanisms of the aftershocks in Yalova–Çınarcık area as derived by Pinar et al. (2010). For more explanation, see the caption of Fig. 8. For the region, the best fit was attained for R = 0.4 and for the azimuth and plunge pairs of (276°, 28°) for σ 1, (132°, 57°) for σ 2 and (15°, 16°) for σ 3, respectively