Cited by 116High-pressure geophysics and materialsearthquake and tectonic studiesGeological and Geophysical Studies

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The Viscosity of the Mantle

MKenzie, D. P.·2010·Geophysical Journal of the Royal Astronomical Society

Abstract

Creep under low stresses is by diffusion and has a linear relation between stress and strain rate; it also obeys the Navier-Stokes equation. Therefore the viscosity of the mantle may be calculated from solid state theory and also from the slow deformations of the Earth. The viscosities derived by these methods are in reasonable agreement, and both show that the viscosity of the lower mantle is ∼ 105 greater than that of the upper. This high viscosity prevents polar wandering and lower mantle convection. Some suggested modifications of the viscosity depth calculations from post glacial uplift may improve their accuracy considerably.

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Crossref · 10.1111/j.1365-246x.1967.tb06246.x

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Research works printed but not linked: 25

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Metadata

Authors
MKenzie, D. P.
Affiliations
University of Cambridge (GB)
Corresponding author
MKenzie, D. P.
Venue
Geophysical Journal of the Royal Astronomical Society
Published
2010-01-26
Volume
14
Issue
1-4
Pages
297-305
ISSN
0016-8009 (ISSN-L)
OpenAlex
W2104321861
Cited by
116
References
0
Citations by year
2026: 1 · 2022: 2 · 2021: 1 · 2019: 1 · 2015: 3 · 2014: 1 · 2013: 3
FWCI
8.14
Type
journal article
Language
en
Open access
closed
Locations
Geophysical Journal of the Royal Astronomical Society (publishedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › earthquake and tectonic studies
  • Physical Sciences › Earth and Planetary Sciences › Geology › Geological and Geophysical Studies
Keywords
mantle viscosity, lower mantle, upper mantle, creep, diffusion, Navier-Stokes equations, polar wander, mantle convection, postglacial uplift, Earth deformation

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