Fig. 2From: Near-field strain observations of the October 2013 Ruisui, Taiwan, earthquake: source parameters and limits of very short-term strain detectionCo-seismic GPS displacements and coseismic slip during the 2013 M w 6.2 Ruisui earthquake. The black and red arrows denote the observed and predicted displacements respectively (a horizontal components, b vertical component). The mean slip inferred from the best fit of GPS displacements is about 0.096 mBack to article page