Fig. 7From: Tectonic exhumation of a metamorphic core in an arc-continent collision during oblique convergence, TaiwanOutcrop photograph of S–C phyllonite in the Chulai Fm along the north bank of the eastern Chingsuei River. This location is west of Fig. 6 and may represent a transition from the Chulai Fm to the Yuli Belt. See text for discussion. Sense of shear inferred from the S–C mylonite fabric shown with two opposing arrows. B S–C relations with curved arrows showing sense of rotation. C S1 and S–C planes, undifferentiatedBack to article page