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vol.21 número4Evaluación de las condiciones físicas y análisis de la vulnerabilidad del barrio San José de las flores alto y medio (Mérida): Ejemplo de la importancia de la geomorfología en los estudios de microzonificación sísmicaModelado geofísico del basamento del área metropolitana de la ciudad de Mérida, Venezuela índice de autoresíndice de materiabúsqueda de artículos
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Revista de la Facultad de Ingeniería Universidad Central de Venezuela

versión impresa ISSN 0798-4065

Resumen

AUDEMARD, FRANCK et al. Ground penetrating radar as a tool for the recognition of active faults: application to the central sector of the boconó fault, Mérida state, Venezuela. Rev. Fac. Ing. UCV [online]. 2006, vol.21, n.4, pp.57-70. ISSN 0798-4065.

This paper presents the outcomes from a first calibration test on the application of the Ground-Penetrating Radar technique  (GPR) for the preliminary identification and characterization of active fault traces done in Venezuela. This test was performed on the central sector of the Boconó fault (between Apartaderos and Santo Domingo). By using an existing paleoseismological trench dug in Morro de Los Hoyos locality, we have calibrated the GPR, in order to correlate and corroborate the geo-radar profiles directly with the subsurface. Later, several profiles acquired at Mesa del Caballo allowed us to make an interpretatio  the structural style of the Boconó fault in this area, that in turn helped us to select a paleoseismic trench site. Finally, GPR was very useful in defining the active fault trace at different sites, where morphological expression of the fault is poor, subdued or concealed. In recent periglacial and interglacial alluvial sequences, GPR seems to reliably reveal the location of the active fault traces, as well as giving insights on the relative degree of recent activity.

Palabras clave : ground-penetrating radar; GPR; neotectonics; paleoseismology; Boconó fault; Mérida Andes; Venezuela.

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