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. Shaw, The balanced cross-section of Figure 14 shows that the Camisea FBS corresponds to a classic thin-skinned fold and thrust belt deforming the Paleozoic sedimentary wedge that pinches out to the east. The geometry and lithology of this preserved sedimentary wedge have exerted a strong control on the thrust propagation. Seismic data along the balanced cross-section do not reveal any basement thrust, The Camisea Subandean basin (Figure 13) is the most prolific hydrocarbon province of Peru and therefore the most studied, 1999.

, The Camisea anticlines are formed above north-verging thrust faults; from south to north, they correspond to the Timpia fault bend fold, the Armihuari and Cashiriari fault propagation folds, and the San Martin triangle zone that dies in the Paleogene infill of the Ucayali foreland (Figure 14a)

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, The geometric and kinematic analyses realized in this work from seismic and surface data shows the complex lateral evolution of the Subandean foreland basin system of Peru. Total horizontal Subandean shortening decreases from the Huallaga-Marañón FBS (70 km) to the Madre de Dios FBS (47 km). The northern part is characterized by the interference of thick and thin-skinned tectonics inherited from middle Permian thrust structures and a widespread Late Permian evaporites level

, In the Marañón-Huallaga FBS, a west-verging fossilized Middle Permian fold and thrust belts has been partly reactivated during Andean deformation and is still seismically active. It is related to the Gondwanide orogeny that we also identified in the Madre de Dios FBS (Madidi Arch). In the Ucayali FBS, Neocomian horizontal shortening has been evidenced in an intra-Paleozoic duplex sealed by the Cushabatay sandstones, Andean orogeny have been identified

, Thermochronologic ages (AFT) recorded the most recent periods of Subandean thrust exhumation from 23.2 Ma to 5.5 Ma. These ages are younger in the Madre de Dios FBS, where they could be related to an intense strong erosion due to the presence of a rainfall hotspot for several millions years

, Two older Subandean compressive deformation events have been evidenced in the stratigraphic record, and therefore led us confirm three Subandean stages of thrust propagation (Late Cretaceous, lower Eocene and Mio-Pliocene

, In the Huallaga Basin, the Chazuta overthrust preserves an unexplored large sub-thrust domain with Gondwanidian structures, Permian and Cretaceous petroleum systems, and salt cover. The Ucayali FBS contains pre-Cretaceous thin-skinned thrust structures developed in the preserved Paleozoic series that contains the prolongation of the Camisea petroleum system, Our synthesis confirms the structural traps attractiveness of the Peruvian Subandean FBS

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