The large volume multi-anvil press as a highP-T deformation apparatus |
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| Authors: | Gilles Y Bussod Tomoo Katsura David C Rubie |
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| Institution: | (1) Bayerisches Geoinstitut, Universität Bayreuth, D-95440 Bayreuth, Germany;(2) Present address: Los Alamos National Laboratory, EES-4, 87545 Los Alamos, NM, USA;(3) Present address: Institute for Study of the Earth's Interior, Okayama Univ., 682-01 Misasa, Tottori-ken, Japan |
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| Abstract: | The rheological properties of mantle materials are being investigated up to pressures of 16 GPa and temperatures of 1600°C for times up to 24 h, using a new sample assembly for the 6–8 multi-anvil apparatus. Al2O3 pistons, together with a liquid confining medium, are used to generate deviatoric stress in the specimen. Strain rates are estimated by monitoring the relative displacement of the guide blocks of the multi-anvil apparatus, scaled to the total axial strain of the sample. The applied stress on the sample is estimated using grain size piezometry. Strain rates and flow stresses of approximately 10–4 to 10–6 s–1 and 50 to 250 MPa respectively, are presently attainable.Preliminary results on San Carlos olivine single crystals, partially dynamically recrystallized to a grain size of 10 to 300  m, indicate that the effective viscosity of polycrystalline olivine is consistent with values obtained from olivine single crystal creep laws. Assuming a dislocation creep mechanism (n 3.5) with (010)001] as the dominant slip system, the data are best fit using a creep activation volume of 5 to 10×10–6 m3 mol–1. |
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| Keywords: | High pressure deformation olivine multi-anvil mantle rheology activation volume |
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