fault zone in the Kuusamo area, the gradient seems to
be associated with a zone of increased seismicity. In these areas, the crustal thickness gradients are
optimally oriented for reactivation. Because the spatial distribution of the registered earthquakes
exhibits little to no
correlation with the an existing ellipsoidal rebound model or Glacial Isostatic
Adjustment (GIA
/media/norsem/norsem_korja.pdf