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Coseismic displacements and slip distribution from GPS and leveling observations for the 2006 Peinan earthquake (Mw 6 1) in southeastern Taiwan

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Figure

Fig. 1. (a) Tectonic framework of the Taiwan area. The Longitudinal Valley Fault (LVF) represents the plate suture between the Eurasian and PhilippineSea plates
Fig. 2. Single epoch solution in 1 Hz sampling rate at station PEIN, which is a CGPS site close to the main shock
Fig. 3.The time series of daily solutions from the six CGPS sites in the study area. Four different slip behaviors, including co- and postseismicdisplacements, can be observed among the six CGPS stations
Fig. 3. (continued).
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