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Post-glacial rebound of Iceland during the Holocene
2010
Journal of the Geological Society
The geodynamic context of Iceland provides the rare opportunity to analyse the combined effect of ridge and hot spot on the deformation processes. The ground deformation results from rifting, magmatic (hot spot and volcanism) and ice loading/unloading. We present in this study a quantitative synthesis of vertical crustal motions of Iceland during the Holocene time with a focus on the postglacial isostatic rebound around the whole island after the retreat of the Weichselian ice cap. Quantitative
doi:10.1144/0016-76492008-126
fatcat:7kmynfpo3bcpvlezkr64nrxrwa