Abstract

In this work, a method for localization, recognition, and classification of a superficial seismic source in a real geological medium is presented. Localization is based on the DOA (Direction of Arrival) and on RSSR (Received Signal Strength Ratio) algorithms applied after Love and Rayleigh superficial wave separation. Recognition and classification methods make use of PCA (Principal Component Analysis) and K-means algorithm. The efficiency of this method is illustrated with experimental results.

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