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Swiss Journal of Geosciences
Fig. 4 | Swiss Journal of Geosciences

Fig. 4

From: Major fault zones in the Austroalpine units of the Kreuzeck Mountains south of the Tauern Window (Eastern Alps, Austria)

Fig. 4

Equal area, lower hemisphere stereoplots: a Dip of schistosity planes and the stretching lineation (red) from the Polinik Complex. b Orientation of two well developed joint systems from the Polinik Complex. Rocks are preferably fractured along the NNW-SSE striking joint system. c Dip of schistosity planes and the stretching lineation (red) from the Strieden Complex. Rocks are intensely folded by steeply SSW dipping folding axes

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