Barnhoorn, AukeBystricky, MKunze, KBurlini, LBurg, Jean-Pierre2015-12-132015-12-130012-821Xhttp://hdl.handle.net/1885/83432Deformation of synthetic calcite-anhydrite aggregates to large shear strains (up to γ=12.4 at 600 °C, 300 MPa confining pressure and a constant angular displacement rate corresponding to a shear strain rate of 10-3 s-1) resulted in the first experimentaKeywords: Deformation mechanism; Heterogeneous deformation; Shear strains; Calcite; Creep; Deformation; Grain boundaries; Microstructure; Porosity; Rocks; Strain rate; Torsional stress; Structural geology; anhydrite; calcite; deformation; strain analysis Deformation mechanism; Heterogeneous deformation; Large strain; Softening; Torsion200510.1016/j.epsl.2005.09.0142015-12-12