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...
Published in: | Geophysical Journal International |
---|---|
Main Author: | |
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 |