An earthquake is a phenomenon, which begins at its source with fault ruture and is completed after the propagation of generated seimic waves through the Earth and the excitation of seismic ground motions and deformations at a site (Fig. 1). This laboratory works for these seismic waves, ground motions, and ground deformations based on the research theme:
Fig. 1. Seismic waves and seismic ground motions.
Jul. 03, 2004
Jul. 07, 2009
Feb. 20, 2011
May 12, 2017