Constraining Glacial Isostatic Adjustment with Horizontal GPS Velocities in Antarctica

Glacial isostatic adjustment is the viscoelastic response of the Earth to ice and ocean loads. In forward models of glacial isostatic adjustment, mantle viscosity is often assumed to be laterally homogeneous. However, a lateral transition in shear wave velocities suggests a sharp transition in visco...

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Bibliographic Details
Main Author: Hermans, Tim (author)
Other Authors: van der Wal, W. (mentor), Delft University of Technology (degree granting institution)
Format: Master Thesis
Language:English
Published: 2017
Subjects:
GPS
FEM
3D
Online Access:http://resolver.tudelft.nl/uuid:29f2aaca-239b-47c5-8323-4d1ed22fd11c