We investigate the influence of the glacial isostatic adjustment (GIA) on the deformation at the surface and at seismogenic depths in Fennoscandia. The surface strain rate field, derived from geodetic data, is controlled by GIA which causes NW–SE extension of up to 4 × 10−9 yr−1 in most of mainland Fennoscandia, surrounded by regions of radial shortening towards the centre of upl…

Tahun Terbit

1997

ISBN/ISSN

0 582 23796 3

Deskripsi Fisik

xvii, 298p.;ill.:21 cm

No. Panggil

363.7 MIT r

Tahun Terbit

1997

ISBN/ISSN

0 582-23796 3

Deskripsi Fisik

xvii, 298p.;ill : 21 cm

No. Panggil

Ps 363.7 MIT r