Fig. 5From: Ductile to brittle fault zone evolution in Austroalpine units to the southeast of the Tauern Window (Eastern Alps)CPO and Quartz microstructures from the (a) Prijakt–Polinik Complex, the Main Mylonite Zone (b, c and d) and from the Strieden Complex (e).The red arrows in (e) document microcracks. The pole figures are lower hemisphere projections nad logarithmic gradiated. Schistosity (s) and lineation (l) are given in the top right corner of the pole figuresBack to article page