Fig. 19From: Tectonic exhumation of a metamorphic core in an arc-continent collision during oblique convergence, TaiwanOrientation data from the Yuli Belt along the north bank of the Mugua River (Fig. 18): A Late-stage foliation and associated stretching lineation and B quartz veins. Based on correlations with fabrics observed in the western Chingsuei River, the late fabrics are interpreted to be D4 structuresBack to article page