Coseismic and postseismic deformation associated with the 2003 Chengkung, Taiwan, earthquake

• Published in: Geophysical journal international Vol. 176; no. 2; pp. 420 - 430
• Main Authors: Hsu, Ya-Ju, Yu, Shui-Beih, Chen, Horng-Yue
• Format: Journal Article
• Language: English
• Published: Oxford, UK Blackwell Publishing Ltd 01.02.2009
• Subjects: Earthquake source observations; Inverse theory; Kinematics of crustal and mantle deformation; Rheology and friction of fault zones; Seismic cycle; Space geodetic surveys
• ISSN: 0956-540X; 1365-246X
• DOI: 10.1111/j.1365-246X.2008.04009.x

We use GPS-derived coseismic and postseismic displacements of the 2003 Mw 6.8 Chengkung, Taiwan, earthquake to examine seismogenic behaviour of the southern Longitudinal Valley. We invert for fault slip on the Chihshang fault, a segment of the Longitudinal Valley fault, based on a simplified layered earth model and a listric-shape fault geometry. Our model infers that maximum coseismic slip of about 0.72 m occurred at a depth of 15 km. Conversely, postseismic slip of about 0.1 m over a 157 d period mainly occurred at depths less than 10 km. We find an anticorrelation between coseismic and postseismic slip distributions. However, the depth profiles of seismicity before and after the main shock are very similar and both show the peak seismicity at 15–25 km depth, consistent with the depth range of large coseismic slip. The potency distribution at depth reveals a coseismic slip deficit at shallow depths, which is compensated by postseismic and interseismic creep associated with the Lichi Mélange. Aseismic slip is an important component of the slip budget on the Chihshang fault. According to the historic earthquake records, interseismic slip rate and coseismic slip on the Chihshang fault, the recurrence interval of this type of event is between 12 and 36 yr. We use a rate-dependent friction model of afterslip to infer the frictional parameter, dτss/dlnV = 0.03–0.5 MPa, at shallow depths on the Chihshang fault. Assuming effective normal stress of 100 MPa at 5 km depth, the rheological parameter, , is about 3 × 10−4–5 × 10−3, which is in good agreement with laboratory experiments.