Other
Scientific paper
Jul 1993
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993georl..20.1479v&link_type=abstract
Geophysical Research Letters (ISSN 0094-8276), vol. 20, no. 14, p. 1479-1482.
Other
51
Crystal Structure, Grain Size, Olivine, Recrystallization, Rock Mechanics, Deformation, Grain Boundaries, Temperature Dependence
Scientific paper
New microstructural data on experimentally deformed 'wet' and 'dry' natural olivine rocks (Anita Bay and Aheim dunite), together with the other reliable experimental data, indicate that the experimental stress - recrystallized grain size relationship in olivine rocks is largely independent of water content and temperature, and is only slightly dependent on the flow properties of the material. The experimental data cover a stress range of 30-300 MPa, water contents from less than 30 ppm to 300 ppm, and temperatures in the range 1100-1650 C. Local melt contents of up to 10 vol percent cannot be demonstrated to have a significant effect on the stress-grain size relationship.
Chopra Prame
Drury Martyn R.
Fitzgerald John D.
van der Wal Dirk
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