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Spatiotemporal evolution of seismic and aseismic slip on the Longitudinal Valley Fault, Taiwan

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Academic year: 2021

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Figure 3. Plots of time series recorded at cGPS stations chen and s105 (http://gps.earth.sinica.edu.tw) and creepmeter measurements [Chang et al., 2009; Lee et al., 2005]
Figure 4. (a) Three-dimensional fault geometry (blue grid) determined from the surface fault trace (red line) and relo- relo-cated seismicity(black dots) for events of M w ≥ 2
Figure 5. Resolution test. (a) The input is theoretical displacements computed for a rectangular source (black box) with a uniform slip of 1 m
Table 1. Location of Axis and Angular Rotation Rates of Euler Poles Used to Describe the Relative Motions of the Philippine Sea Plate (Ph), Central Range Block (CeR), and Coastal Range Block (CoR)
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