This shows a kidney-shaped zone of subsidence reaching 30 cm flanked by an uplift zone reaching 5 cm. We reproduce this field using dislocations in an elastic half-space and our observations of the fault system. Our preliminary model includes significant NE-dipping scissors faulting at the eastern end of the rupture, clearly seen in the interferograms. Active faulting in the Kozani-Grevena area mapped with panchromatic SPOT imagery and fieldwork. 1995 earthquake epicenter, fault plane solution and aftershocks from Hatzfield et al.
Right inset shows tectonic framework.
Note the semi-elliptical shape of the hangingwall basin outlined by the 500 m elevation contour. Lower-case letters indicate location of photographs in Fig. 2. Note the southeastward tilt of the footwall surface, which is capped with pre-extensional sediments. Each fring represents 28 mm displacement. The two patches with 0.4 m have variable slip, see text.