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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Other Authors: | , |
Format: | Master Thesis |
Language: | English |
Published: |
2017
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Online Access: | http://resolver.tudelft.nl/uuid:29f2aaca-239b-47c5-8323-4d1ed22fd11c |