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3.1 e. Slip systems in shear deformed wadsleyite (P. Cordier and D.J. Frost in collaboration with E. Thurel/Lille and S.I. Karato/Minneapolis)

The high pressure polymorphs of olivine, wadsleyite and ringwoodite are likely to control the rheology of the transition zone. It is thus important to determine their deformation mechanisms at high-pressure and high-temperature. Multianvil deformation experiments using simple shear geometry can achieve large strains (see Annual Reports 1998 and 1999) and produce strong fabrics. We present here a TEM characterisation of the slip systems activated in wadsleyite deformed in such conditions.

The wadsleyite samples were synthesised from San Carlos olivine powder annealed for 3 hours at 15 GPa and 1300°C. After the run, the specimen was recovered, sliced, and put in a shear assembly to induce plastic deformation. Two deformation experiments were run for 1 and 8 hrs at 14 GPa and 1300°C.

The same microstructures are observed in those two samples showing that steady deformation is maintained over long periods of time in such experiments (Fig. 3.1-5). The dislocations are in glide configuration. Three slip systems appear to be dominant: [100](010), [100](011) and 1/2[111](101).

Fig. 3.1-5: Sample deformed at 14 GPa, 1300°C during 8 hrs. [100] dislocations gliding in (010). Transmission electron micrograph. Weak beam dark field with g : 100.

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