Glacial isostatic adjustment in Fennoscandia—A review of data and modeling

Fennoscandia is the key area for glacial isostatic adjustment (GIA) research. Owing to its long settlement and excellent infrastructure, ongoing land uplift in the north as well as subsidence in the south have affected human life and already triggered scientific investigations starting in the late 1...

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Veröffentlicht in:	Journal of geodynamics 2011-10, Vol.52 (3), p.169-204
Hauptverfasser:	Steffen, Holger, Wu, Patrick
Format:	Artikel
Sprache:	eng
Schlagworte:	Absolute gravity BIFROST Fennoscandia Finite element modeling Glacial isostatic adjustment GRACE Lateral heterogeneity Lithospheric thickness Mantle viscosity Post-glacial earthquakes Post-glacial rebound Relative sea levels Rheology of the Earth
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