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An upper bound on lithosphere thickness from glacio-isostatic adjustment in Fennoscandia

Item

Title (Dublin Core)

en-US An upper bound on lithosphere thickness from glacio-isostatic adjustment in Fennoscandia

Description (Dublin Core)

en-US The three-layer Maxwell half-space model of the Earth and a disk-load approximation of the Weichselian deglaciation history of Fennoscandia are used to calculate glacio-isostatic adjustment for this region. The calculations include the effects of deglaciation-induced geoid perturbations and eustatic sea-level rise and regard (1) lithosphere thickness, (2) asthenosphere viscosity and (3) ice thickness as the free model parameters. Numerical values of parameters (1)-(3) are estimated by calculating the past land uplift and present land-uplift rate observed in central Sweden (glaciation centre) and the past land uplift and past land tilt observed in southern Finland (glaciation margin). The uniqueness of the estimates and their sensitivity to uncertainties in (4) subasthenosphere viscosity, (5) ice cross-section and (6) deglaciation time are also assessed. The principal result of the investigation is that it suggests an upper bound of 80 km on the thickness of the Fennoscandian lithosphere.
        ARK: https://n2t.net/ark:/88439/y082218
Permalink: https://geophysicsjournal.com/article/93
 

Creator (Dublin Core)

Wolf, D.

Subject (Dublin Core)

en-US Asthenosphere
en-US Fennoscandia
en-US Glacio-isostasy
en-US Lithosphere
en-US Maxwell continuum
en-US Weichselian ice-sheet
en-US Methods

Publisher (Dublin Core)

en-US Journal of Geophysics

Date (Dublin Core)

1987-04-23

Type (Dublin Core)

info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
en-US Peer-reviewed Article

Format (Dublin Core)

application/pdf

Identifier (Dublin Core)

https://journal.geophysicsjournal.com/JofG/article/view/93

Source (Dublin Core)

en-US Journal of Geophysics; Vol 61 No 1 (1987): Journal of Geophysics; 141-149
2643-2986
2643-9271

Language (Dublin Core)

eng

Relation (Dublin Core)

https://journal.geophysicsjournal.com/JofG/article/view/93/54