Titlebook: Experimental and Natural Rock Deformation / Experimentelle und natürliche Gesteinsverformung; Proceedings of the I Peter Paulitsch Conferen

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Garnet Orientation in Different Metamorphic faciesby the preferred orientation of omphacite, quartz and calcite, too..The results partly agree with Kamb’s (1959) calculation for cubic minerals: [100] or [ 111 ] parallel to the main compression direction.

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https://doi.org/10.1057/9781137412591e quartz-diagrams show a distinctive preferred orientation of poles of prism-planes a (1120) and m (lOlO), namely, am-girdle. At the part of the highest metamorphic grade the diagrams show almost nearly single one-crystal-fabrics through the positions of sub-planes of quartz. The mechanism of quartz-orientation was also discussed.

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Global Business Value Innovationsmade by simply combining the appropriate anisotropy coefficients with area-corrected pole density data obtained from the contour values of [hk?]. distributions, and standard calculated intensities for the given material. Calculated and observed diffraction patterns for apatite in tibia of . and for calcite in Yule marble are in good agreement.

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R?ntgenographische Gefügeanalyse [mit dem Z?hlrohr-Texturgoniometer] von Quarzschiefern aus Zentral-e quartz-diagrams show a distinctive preferred orientation of poles of prism-planes a (1120) and m (lOlO), namely, am-girdle. At the part of the highest metamorphic grade the diagrams show almost nearly single one-crystal-fabrics through the positions of sub-planes of quartz. The mechanism of quartz-orientation was also discussed.