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The study investigates the thermal evolution of the eastern Serranía del Interior foreland fold and thrust belt in northeastern Venezuela using apatite fission-track analyses. It identifies two cooling paths and distinct populations of grain ages, suggesting a two-stage tectonic evolution involving piggyback folding and envelopment thrusting. The findings indicate that deformation in the region is related to the convergence of the North and South American plates, with significant tectonic activity occurring

Author

seserenable

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EN