Fig. 5From: Source and strong-motion characteristics of two M > 6 buried earthquakes in southwest TaiwanThe observed peak ground velocity distribution and slip models of the 2010 Jiashian (Lee et al. 2013) and 2016 Meinong (Lee et al. 2016) events, respectively. The gray rectangles show the SMGA models of the 2010 Jiashian (blue star) and 2016 Meinong (green star) events, respectively, with black dots representing the rupture starting points. The crosses and squares represent the locations of damaged structures and liquefactions investigated by the Central Geological Survey, respectively. The regular and inverted triangles indicate strong-motion stations affected by the dominant frequency band of energy bursts in low-frequency band (LF, ≤ 1.67 Hz) and high-frequency band (HF, > 1.67 Hz), respectivelyBack to article page