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Meso- and Microstructural Analysis of Coseismic Shear Zone of the 1999 M_W 7.6 Chi-Chi Earthquake, Taiwan

¹ Institute of Geosciences
Faculty of Science
Shizuoka University
Ohya 836, Shizuoka 422-8529, Japan
 (A.L., T.M.)

² Institute of Applied Geology
National Central University
Chung-Li 32001, Taiwan
 (C.-T.L.)

³ Institute of Applied Geophysics
Taiwan National Ocean University
Keelun 20224, Taiwan
 (A.C.)

The surface rupture of the 1999 M_w 7.6 Chi-Chi (Taiwan) earthquake was controlled primarily by the pre-existing Chelungpu fault zone, which is distributed in a wide zone of up to 60 m, although the main coseismic slip is localized in a narrow shear zone of <0.3 cm. The Chelungpu fault zone is composed of cataclasite, fault breccia, and gouge zones that are well observed in both the fault outcrops and the drill cores taken throughout the fault zone. The foliations developed in the cataclasite and fault breccia zones are oriented parallel to that of the fault gouge zone where the main coseismic slip occurred. The structural analyses of the shear zone and fault rocks show that the Chelungpu fault zone has slipped as a thrust fault with a significant left-lateral slip component since its formation in the Pleistocene. This oblique thrust motion is caused by the southeast–northwest oblique convergence between the Philippine Sea plate and the Eurasian plate.