Bounds on the subsolidus attenuation for four rock types at simultaneous high temperature and pressure

Author:

Goetze C.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference10 articles.

1. High-temperature rheology of Westerly Granite;Goetze;J. Geophys. Res.,1971

2. A brief summary of our present-day understanding of the effect of volatiles and partial melt on the mechanical properties of the upper mantle;Goetze,1977

3. Laboratory observations of high-temperature rheology of rocks;Goetze;Tectonophysics,1972

4. Physical mechanisms of seismic-wave attenuaion;Jackson;Rev. Geophys.,1970

5. Low stress high temperature creep in olivine single crystals;Kohlstedt;J. Geophys. Res.,1974

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1. The importance of grain size to mantle dynamics and seismological observations;Geochemistry, Geophysics, Geosystems;2017-08

2. Transient Creep and Strain Energy Dissipation: An Experimental Perspective;Annual Review of Earth and Planetary Sciences;2015-05-30

3. The Anelasticity of the Earth: How Much do We Know about Q?;Upper Mantle Heterogeneities from Active and Passive Seismology;1997

4. Progress in the Experimental Study of Seismic Wave Attenuation;Annual Review of Earth and Planetary Sciences;1993-05

5. Rheology of the lithosphere;Reviews of Geophysics;1983

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