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granite mylonite (top) in contact with amphibolite (bottom) with EW-trending steep foliation. In the mylonite, isoclinal folds are refolded by open folds with NS steep axial planes.

granite mylonite (top) in contact with amphibolite (bottom) with EW-trending steep foliation. In the mylonite, isoclinal folds are refolded by open folds with NS steep axial planes.

Photograph: Cees Passchier