Deformation of Olivine Single Crystals in a Hydrous Environment: Insight into the Rheological Behavior of the Lithospheric Mantle of Terrestrial Planets

Details Deformation of Olivine Single Crystals in a Hydrous Environment: Insight into the Rheological Behavior of the Lithospheric Mantle of Terrestrial Planets Deformation of Olivine Single Crystals in a Hydrous Environment: Insight into the Rheological Behavior of the Lithospheric Mantle of Terrestrial Planets

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.2273t&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.2273

Physics

Scientific paper

Deformation of olivine demonstrates that viscosity decreases with
increasing water fugacity and decreasing silica activity, consistent
with point defect models in which water is incorporated into olivine as
defect associates involving Si or Me vacancies with H ions.

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