“…According to various authors, deep-seated tectonic processes led to leaching of feldspar from acidic rocks, karst formation in carbonate rocks, the development of caverns and fractures, and the leaching of minerals from basic lavas (basalts), resulting in the formation of porous and fractured reservoirs [21,34,35]. Traps in such rocks are typically located in structural highs of the basement (with more developed weathering crust), in areas of Triassic rock exposure on basement uplifts [7], and near fault disruptions that create collectors and tectonic-screened traps [36].…”