“…Taking into account the seismogram variability over time, time-variant features have been used to extract information, such as, linear frequency cepstral coefficients (LFCC) (Benítez et al, 2007), mel-frequency cepstral coefficients (MFCC) , instantaneous bandwidth, instantaneous frequency, seismic envelope, the centroid time , and the half octave band (HOB) . Throughout this study, instead of a longterm parameter set extracted from the seismogram, the volcano state events are detected by using short-time features, where each seismogram frame is quantified by a single vector.…”