Deep, Episodic Aseismic Slip Around an Active Suture Zone in Eastern Taiwan

Abstract:

An examination of repeating earthquakes in eastern Taiwan revealed previously unrecognized quasi-periodic repetition of aseismic creep along two reverse faults in an active suture zone. Using 202 M_L 2.0 to 4.6 repeating earthquake sequences (RES) during the period from 2000 to 2011, we studied where and how certain faults creep. The RES were found to be highly concentrated in the southern segment of the Longitudinal Valley fault (LVF) and in the northern segment of the Central Range fault (CRF). They are mainly located at a depth of 10 - 25 km, and show strong regional differences in creep behavior. Using the moment release rate of RES and geodetically derived long-term slip rate, we re-estimate the empirical relationship between deep creep and seismic moment for creeping sections in eastern Taiwan. For the 30 km long LVF, the creep rate increased dramatically from 1.5 cm/yr to 12.3 cm/yr under the influence of the M_L 6.4 Chengkung earthquake of 2003. For the 80 km long CRF, the high creep rate of 4.3 cm/yr appears to have been stable over time and is descriptive of a previously unrecognized deep structure underneath the eastern flank of the Central Range. The quasi-periodic pulsing of the deep slip rate has a predominant interval of one year for both segments. After the M_L 6.4 event, the predominant interval for the creeping LVF halved in duration. The time-dependent aseismic slip showed a strong correlation with the creepmeter data, suggesting that the positing of a common mechanism is needed to connect the surface and deep creep variation.