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The crystallographic preferred orientations of quartz in gneiss taken from different spots of arecumbent fold structure in the Erzgebirge Mts. (southern GDR) are studied by means of neutrontime-of-flight diffraction. A single component texture has been found for all specimens, with quartz c -axes parallel to the tectonic  a -direction. The variations in texture sharpness are related to differentdeformation conditions of the samples. A fabric rotation of 30° has been found from the limb to thecrest of the fold on the basis of (   10   1  ¯   0   ) and (   11   2  ¯   0   ) pole figures. The basal pole figures of quartz derivedfrom an ODF analysis compared well with optical U-stage measurements. The determined fabrics arediscussed taking into account model calculations of experimentally deformed quartzites and geologicalinformations.

The Structural Evolution of an Orthogneiss-fold Within the Reitzenhainer Rotgneisstruktur (Erzgebirge Mts., GDR)