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In the Saxo-Thuringian there are intensely sheared banded gneisses after a coarse granite. This banded gneiss underwent partial melting to form some beautiful migmatites with neatly spaced shear bands filled with leucosomes. These photos are from the Kadanie dam. |
Face of block parallel to lineation and perpendicular to foliation. Leucosomes on axial plane of folds. |