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Se presenta resumen del uso de las medidas de ruido ambiental para determinar el período fundamental de las diferentes terrazas de la ciudad de La Serena, Chile. Se utiliza el método de Nakamura que establece la razón entre el espectro horizontal y el espectro vertical (H/V) de ruido ambiental para determinar el periodo fundamental del sitio en estudio. Por medio de este método se confeccionan mapas preliminares de isoperiodos y microzonificación sísmica de La Serena.
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