Fig. 4From: The Wechsel Gneiss Complex of Eastern Alps: an Ediacaran to Cambrian continental arc and its Early Proterozoic hinterlandRepresentative photographs of a typical porphyroblast-bearing Wechsel Gneiss. The rock is cut parallel to the stretching lineation and perpendicular to the foliation. The short axis of the image is ca. 4 cm. Chl: chlorite, Pl: plagioclase, Qz: quartz, Pl-PB: albite porphyroblastBack to article page