Ductile shear zone within the Roffna metarhyolite nucleated from brittle precursors.
Syn-kinematic metamorphic assemblage nucleated under HP-BT metamorphic conditions.
Quartz CPO reveals a switch from fracturation to SGR and dislocation creep.
Diffusion-accommodated grain boundary sliding is effective in the mature shear zone.
Fluid infiltration plays a key role in the development of ductile shear zone.