Viscosity of the upper mantle from laboratory creep and anelasticity measurements in peridotite at high pressure and temperature

Recent laboratory results on anelasticity and viscoelasticity of mantle rocks at high pressure and temperature show the homologous temperature dependence of seismic Q and creep rate, i.e., both depend on the mantle solidus. These laboratory results enable us to estimate viscosity of the mantle from...

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Bibliographic Details
Published in:Geophysical Journal International
Main Author: Sato, Hiroki
Format: Text
Language:English
Published: Oxford University Press 1991
Subjects:
Online Access:http://gji.oxfordjournals.org/cgi/content/short/105/3/587
https://doi.org/10.1111/j.1365-246X.1991.tb00798.x