Intermediate-depth seismicity of the lesser Antilles subduction slab, close to the Paria peninsula, Venezuela

Authors

  • Franck A. Audemard
  • Leonardo Alvarado
  • Mariano Arnaiz
  • Gloria Romero
  • Carlos E. Reinoza-Gómez
  • Alejandra I. Martínez-González
  • Ana Karina Sánchez-Gamboa
  • Jean Frédéric Lebrun
  • Luz María Rodríguez
  • José Antonio Rodríguez
  • Mélody Philippon
  • André Singer
  • Jorge González
  • Mariana Lotuffo

Keywords:

Lithospheric tear, Seismic attenuation, Seismic energy radiation, Channeling, Seismic intensity, Seismic hazard

Abstract

From a macroseismic investigation of earthquakes ranging between 45 and 150 km in depth and magnitudes Mw ≥ 5.0 since year 2000, related to the South American-Atlantic (SAA) subduction in the region of the southeastern Caribbean STEP, we have determined that the cities of Ciudad Guayana and Ciudad Bolívar, sitting at the northernmost edge of competent rock outcrops of the Precambrian craton of Guyana, show seismic intensities which do not comply with a normal attenuation pattern of decreasing intensities with increasing distance. This necessarily leads to the revision of the current Venezuelan seismic-resistant code (COVENIN 1756-1:2019), since the seismic hazard estimations for this southern region of Venezuela appear to be clearly underestimated.

Published

2026-08-04

How to Cite

Audemard, F. A., Alvarado, L., Arnaiz, M., Romero, G., Reinoza-Gómez, C. E., Martínez-González, A. I., … Lotuffo, M. (2026). Intermediate-depth seismicity of the lesser Antilles subduction slab, close to the Paria peninsula, Venezuela . Boletín De La Academia De Ingeniería Y Habitad, (71), 455–456. https://n2t.net/ark:/42414/banih/712026/133

Issue

Section

Resúmenes de Trabajos Presentados en Eventos Externos o Revistas por Académicos y Comisionados

ARK