Shallow upper mantle rheology and secular ice sheets fluctuations

On time scales from decades to centuries, continental cryospheric forcing in response to climate change constitutes a major source of isostatic disequilibrium that may influence future regional sea level variations. Current vertical displacements and gravity field variations are often estimated negl...

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Bibliographic Details
Published in:Tectonophysics
Main Authors: SPADA, GIORGIO, COLLEONI F, RUGGIERI G.
Format: Article in Journal/Newspaper
Language:English
Published: 2011
Subjects:
Online Access:http://hdl.handle.net/11585/771807
https://doi.org/10.1016/j.tecto.2009.12.020
http://www.sciencedirect.com/science/article/pii/S0040195109007082