The Metamorphic Fabrics in the Taroko High-strain zone of Taiwan Mountain Belt: A Regional-scale, Left-lateral Shear Zone that Accommodated Highly Oblique Plate Convergence in the Plio-Pleistocene

Gong-Ruei Ho1, Jian-Cheng Lee1, Timothy B Byrne2 and Yuli Exhumation Study Team (YES Team), (1)Academia Sinica, Institute of Earth Sciences, Taipei, Taiwan, (2)University of Connecticut, Department of Geosciences, Storrs, United States
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