“…By using a quasi-real time waveform, information related to the seismic event (e.g., seismic moment— and moment magnitude— ) and its effect on the ground where stations are positioned (e.g., the peak ground acceleration, velocity, and displacement (PGA, PGV, and PGD, respectively), Housner intensity ( ), Arias intensity ( ), and spectral acceleration (SA) at different times, commonly at , , and ) can be retrieved [ 18 ]. Combinations of this information help scientists and engineers to determine the possible damage to structures and infrastructures and the possibility of triggering other natural phenomena (e.g., landslide, soil liquefaction) [ 2 , 4 , 18 , 19 ].…”