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- W2306239937 abstract "The Longitudinal Valley fault, a major reverse fault dipping eastward in eastern Taiwan, is commonly considered as the collision boundar y between the Eurasian plate and Philippine Sea plate. Some aseismic creep motions had been detected across the central and southern part of the Longitudinal Valley fault based on the GPS measurements and creep- meters. In order to discuss the spatio-temporal distribution of the aseismic creep motion in the central part of this fault, we established four precise leveling routes (the Yuli , Dongli , Fuli , and Chike-shan routes). At first, four precise leveling surveys along the Yuli route were repeatedly conducted in every August from 2008 to 2011. The overview of the deforma- tion detected in the Yuli route is as follows. An uplift rate of about 30 mm/year has been detected within 2 km in width across the fault. To the east of the fault, the uplift rate gradually reduce eastward with the distance, and down to 15 mm/ year at the east coast. Since there was no significant earthquake occurred in the fault during the 3-year observation peri- od, the detected deformation has been resulted from the aseismic creep motion. The creeping motion might occur at the same location of the fault with a constant rate in that the deformation denoted the same tendency and rate during all mea- surement periods. Furthermore, we conducted another three routes in the Dongli, Fuli, and Chike-shan areas to detect the spatial distribution of the aseismic creep motion in August 2010 and 2011. The results show vertical deformation rates of 25 mm/year and 10 mm/year were detected in the Fuli route and the Chike-shan route, respectively." @default.
- W2306239937 created "2016-06-24" @default.
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- W2306239937 date "2012-01-01" @default.
- W2306239937 modified "2023-09-26" @default.
- W2306239937 title "Large Aseismic Creep Detected by Precise Leveling Survey at the Central Part of the Longitudinal Valley Fault, Southeast Taiwan (2008-2011)" @default.
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