2020
DOI: 10.1016/j.jsames.2020.102867
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Neotectonic evolution of Northeastern Venezuela . Geomorphological and seismic analysis in the Monagas Fold and Thrust Belt

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“…This results in a high seismic activity in the region. The influence of tectonic processes is reflected in a variety of topographic forms, geological structures, and geomorphic settings of Venezuela, as discussed earlier [54][55][56][57]. The geodynamic heterogeneity of the upper mantle has resulted in a specific mountain geomorphology with notable features, such as the extent of the Tobago Trough, the Lara-Falcón Basin, and the crustal structure of the Cordillera de Mérida in southwestern Venezuela, which are important segments of the Andean orogeny [58].…”
Section: Study Areamentioning
confidence: 98%
“…This results in a high seismic activity in the region. The influence of tectonic processes is reflected in a variety of topographic forms, geological structures, and geomorphic settings of Venezuela, as discussed earlier [54][55][56][57]. The geodynamic heterogeneity of the upper mantle has resulted in a specific mountain geomorphology with notable features, such as the extent of the Tobago Trough, the Lara-Falcón Basin, and the crustal structure of the Cordillera de Mérida in southwestern Venezuela, which are important segments of the Andean orogeny [58].…”
Section: Study Areamentioning
confidence: 98%