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Index Geophysics

The relaxation of spherical and flat Maxwell Earth models and effects due to the presence of the lithosphere

Item

Title (Dublin Core)

en-US The relaxation of spherical and flat Maxwell Earth models and effects due to the presence of the lithosphere

Description (Dublin Core)

en-US The radial surface deflection of a spherical Earth model appropriate to time scales characteristic of glacial loading is compared with the associated half-space response. For that purpose the analytical solution for a Maxwell sphere surrounded by a thick elastic shell is derived under the assumption of incompressibility. The half-space approximation is deduced as a special case directly from the spherical solution. Comparison of the response spectra, for different thicknesses of the elastic shell, reveals only minor differences. In the spatial domain, the half-space approximation may, nevertheless, diverge significantly from the spherical solution. For a disk load radius R = 800 km (Fennoscandia), the half-space approximation is adequate, whereas it is usually inappropriate if R = 1600 km (Laurentia). The sensitivity of the response to the thickness of the elastic shell is also investigated. For R = 800 km, the surface deflection in the central region below the load is fairly diagnostic of the shell thickness. If R = 1600 km, the peripheral region is more sensitive to this parameter.
          ARK: https://n2t.net/ark:/88439/y005336
Permalink: https://geophysicsjournal.com/article/210
 

Creator (Dublin Core)

Wolf, D.

Subject (Dublin Core)

en-US lsostasy
en-US Lithosphere
en-US Maxwell continuum
en-US Methods

Publisher (Dublin Core)

en-US Journal of Geophysics

Date (Dublin Core)

1984-12-13

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/210

Source (Dublin Core)

en-US Journal of Geophysics; Vol 56 No 1 (1985): Journal of Geophysics; 24-33
2643-2986
2643-9271

Language (Dublin Core)

eng

Relation (Dublin Core)

https://journal.geophysicsjournal.com/JofG/article/view/210/170