Multiple thermochronometers applied to the quantitative analysis of compressive systems: The southern sub-Andean fold and thrust belt of Bolivia. From source rock to trap

The evolution of fold and thrust belts requires time data restrictions to determine the rates related interaction surface subsurface processes quantify relationship between components petroleum system: reservoir, seal, source rock trap. sub-Andean fold-and-thrust belt in Bolivian territory general, regional transect that links structures Curuyuqui-Carohuaicho-Tatarenda-Borebigua-Charagua Mandeyapecua particular, constitutes a complex multi-variable system which definition time-Temperature (t-T) trajectories has led new suitable structural stratigraphic conclusions. integration multiple thermochronological-geochronological systems (Apatite Fission Track, Apatite (U-Th-Sm)/He UPb SHRIMP on zircon) existing geological constraints made it possible develop chrono-kinematic characterization fault-related anticlines, defining their formation chronology, growth rate link them study area. Furthermore, was also perform quantitative analysis subsidence-burial exhumation-erosion phenomena occurred from deposition Silurian-Devonian rocks present time, providing relevant determinations modeling Oil & Gas system.