Caracterización de señales sísmicas del Volcán Cotopaxi utilizando estimadores espectrales clásicos y de máxima entropía

Abstract

A study of the detection and characterization of volcano-tectonic seismic type of events, using a long period of records of the Cotopaxi volcano, is presented. The sequential detection structure, proposed as part of this work, allows maximizing the likelihood of the presence of an event and minimizes the absence of this from a seismic record. The detection is performed in the near real time domain, maintaining a constant false alarm rate, enabling in a later stage a more detailed study of the spectral content of the events using classical spectral estimators such as the periodogram and the parametric maximum entropy method by Burg. The approach enabled to categorize phenomenon detected as volcano-tectonic from a long record of observations which even include activities of non-tectonic origin, such as the other two types of lightning.