seismicity map of the Nordland region
has been obtained and linkage to mapped and
hitherto non-mapped faults
has been done.
• Inversion methods have
been applied to estimate the regional stress field by integrating GPS,
DInSAR, seismic data (focal mechanisms) and in situ stress.
• The contribution of Pleistocene sediment redistribution
has been quantified using numerical
modeling with basis
/media/norsem/norsem_lindholm.pdf