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van den Berg & Yuen 1996
van den Berg, A.P. and Yuen, D.A. (1996). Is the lower-mantle rheology Newtonian today?. Geophysical Research Letters 23: doi: 10.1029/96GL02065. issn: 0094-8276.

The issue concerning the dominant creep mechanism in mantle convection has been studied numerically with a rheology incorporating both linear and non-linear elements. We have employed a rheology suggested by the recently obtained melting temperature of lower-mantle constituents. For an effective Rayleigh number between 105 and 106 this type of strongly temperature and pressure-dependent rheology induces a circulation in the Earth's mantle, which is characterized by a sluggish type of flow in the lower mantle with a prevailing Newtonian character, while in the upper mantle much more vigorous flows are developed in a predominantly non-Newtonian rheology. ¿ American Geophysical Union 1996

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Abstract

Keywords
Tectonophysics, Dynamics of lithosphere and mantle—general, Tectonophysics, Rheology—general
Journal
Geophysical Research Letters
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Publisher
American Geophysical Union
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