Active fault recognition in northwestern Venezuela and its seismogenic characterization: Neotectonic and paleoseismic approach
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Resumen
Los tiempos de recurrencia obtenidos de trincheras en el NW de Venezuela son 1752 ± 133 años para la falla de Ancón y 4300±1000 años para la falla de Oca, con magnitudes de Ms 7.4-7.5. Las fallas menores en el norte del estado de Falcon pueden generar sismos de Ms 6.2 a 7.0 cada 1,500 años o más.
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