Skip to main content
Fig. 3 | Earth, Planets and Space

Fig. 3

From: Near-field strain observations of the October 2013 Ruisui, Taiwan, earthquake: source parameters and limits of very short-term strain detection

Fig. 3

High sample rate (100 Hz) dilatational strain signals of the Ruisui earthquake recorded by borehole dilatometer sites in central LV (see Fig. 1 and Table 1 for details). (Left) 10-min window depicting the co-seismic static offset. (Right) Zoom on the first 30 s of the rupture depicting the near field and the phasis of P- and S-waves. A positive sign denotes an expansion. The time-origin is the occurrence of the mainshock

Back to article page