Focal mechanism of the main shock provided by the solution of the Geological Survey of Japan (P-axis: 60/82. T-axis: 157/1). b. Stress pattern (ó3-NNW-SSE trending. ó1: vertical) in western Macedonia as derived by palaeostress analysis of neotectonic striated faults (Pavlides, 1985). c. Stress pattern in the meisoseismal area as derived by the analysis of seismic fault data. d. P and T axis of the main shock in the areas of ó1 and ó3 previously calculated from neotectonic data.
[from Mountrakis et al. (1998)].
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