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Fig. 4 | Earth, Planets and Space

Fig. 4

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

Fig. 4

Dilatational co-seismic static offsets of the Ruisui earthquake on the central borehole dilatometer site predicted by source models from GPS and seismic data, respectively. a Source parameters inferred from GPS inversion. b Source parameters from seismology (209°, 59°, 50°). The reference is the location of the SSNB strainmeter. Strain field is estimated at a mean depth of 200 m. The right colorbar indicates the amplitude in n ε and positive value is an expansion. The dashed black line roughly denotes the surface projection of the fault

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