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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

Crossref DOI link: https://doi.org/10.1134/S1028334X20050037

Published Online: 2020-07-07

Published Print: 2020-05

Update policy: https://doi.org/10.1007/springer_crossmark_policy

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