Abstract
Summary The geological evolution of most sedimentary basins currently explored for hydrocarbon resources, involved more than one tectonic deformation phase. The earlier structures, concealed by the easily recognized latest deformation, often remain overlooked by interpreters. This might result in poor exploration decisions such as unnecessary exploratory wellbores or missed opportunities. The Maiella mountain outcrop, in the Southern Apennines of Italy, is an example where a Pliocene to Pleistocene aged compression anticline has folded carbonate sequences containing Cretaceous aged extension faults. The study of this outcrop provides insights for the deliberate search of exploration opportunities hidden within early structures in basins where multiple deformation phases are recorded.
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