Deformation experiment at P - T conditions of the mantle transition zone using D-DIA apparatus

Details Deformation experiment at P - T conditions of the mantle transition zone using D-DIA apparatus Deformation experiment at P - T conditions of the mantle transition zone using D-DIA apparatus

Nov 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010pepi..183..190k&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 183, Issue 1-2, p. 190-195.

Physics

Scientific paper

Technical developments in high-pressure and high-temperature generation have been made, adopting a recently devised multi-anvil 6-6 (MA 6-6) assembly with tungsten carbide (WC) anvils. As a result, the pressure and temperature conditions available in a cubic-anvil DIA type apparatus have been extended to 20 GPa and 2000 K. Using this assembly operated in a deformation-DIA (D-DIA) apparatus, a deformation experiment to a strain of 15% on a mixture of wadsleyite and ringwoodite was successfully conducted at 16 GPa and 1700 K and at a strain rate of 6 × 10 -5 s -1 , demonstrating potential of the present MA 6-6 assembly as an important tool to investigate rheological properties of high-pressure phases under the conditions of the mantle transition zone.

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