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The Occurrence of a Lower Viscosity Layer in the Crust of Old Cratons as a Cause of the Strongly Differentiated Character of Postglacial Uplift
Authors:Artyushkov  E V  Kol’ka  V V  Chekhovich  P A
Institution:1.Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, 123995, Moscow, Russia
;2.Geological Institute, Kola Science Center, Russian Academy of Sciences, 184209, Apatity, Russia
;3.Moscow State University, 119991, Moscow, Russia
;
Abstract:Doklady Earth Sciences - Rapid glacio-isostatic rebound in Fennoscandia and Canada that is nonuniform in time and space indicates that there is a layer with strongly decreased viscosity at shallow...
Keywords:
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