Rotational motions induced by the M8.1 Tokachi‐oki earthquake, September 25, 2003

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Broad-band observations of earthquake-induced rotational ground motions (2007, methodology): “The rotation rates to be expected in seismology range from a few deg s−1 (e.g. Nigbor 1994) close to seismic sources to 10−11 rad s−1 observed for large earthquakes at teleseismic distances (e.g. Igel et al. 2005; Schreiber et al. 2005, 2006), thus spanning more than 10 orders of magnitude.”
First Comparison of Array-Derived Rotational Ground Motions with Direct Ring Laser Measurements (2006, methodology): “The Experiment After the successful observation of fully consistent rotational motions (Igel et al., 2005), a mobile seismic-array experiment with eight stations (S1–S8) was installed around the geodetic station Wettzell, Southeast Germany, the location of the ring laser.”
Introduction to the Special Issue on Rotational Seismology and Engineering Applications (2009, background): “The first review by Lee et al. is a progress report on observing rotational and translational ground motion from explosions and earthquakes in Taiwan, and it is based on the work by Lin et al., Liu et al., Wu et al., Langston et al. and Lin et al. Taiwan is at present the only country that has a pro”