3A. A gravimetric method to determine stress related glacial isostatic adjustment in Fennoscandia

The Earth’s gravity field is a basic geophysical parameter that reflects the Earth’s mass distribution and its changes with time. As the Earth is not a rigid body but is constantly changing under the influence of external and internal forces, the gravity field and its changes with time are of great significance for studying various … Läs mer

Författare: Mohammad Bagherbandi, Nureldin Gido and Goran Jedrejcic, Högskolan i Gävle/KTH
Datum: 29 mars 2017
Ursprung: Kartdagar 2017
3A. A gravimetric method to determine stress related glacial isostatic adjustment in Fennoscandia