Opening and Closure of the Neuquén Basin in the Southern Andes

The Neuquén Basin:  Stratigraphy, subsidence controls and basin closure.- Heterogeneities and syn-rift evolution of Late Triassic-Early Jurassic Precuyano Cycle.- Structure of the Precuyo synrift in the Valenciana depocenter.- Structure of the Precuyo synrift in the Cara Cura-Sierra de Reyes depocenter.- Early Jurassic magmatism.- High-resolution sequence stratigraphy and main controls of the Middle Jurassic Cuyo Group.- Depositional environments and hyperpycnal shelfal sedimentation in the Late Jurassic Lotena Formation.- Environmental controls and facies architecture of a Late Jurassic (Oxfordian) carbonate episode (La Manga Formation).- The Cuyo and lower Mendoza cycles in the Aconcagua fold and thrust belt.- The extensional control of the Late Jurassic units.- Morphostructural configuration and sedimentary evolution of the Late Jurassic - Early Cretaceous Vaca Muerta -Quintuco system.- Magnetostratigraphy of the Early Jurassic - Early Cretaceous in the Neuquén Basin.- Orbital controls and high-resolution cyclostratigraphy of Late Jurassic - Early Cretaceous in the Neuquén Basin (Lower Callovian - Early Barremian).- Sedimentary evolution of the continental Late Cretaceous Neuquén Group.- The Cretaceous contractional stage and the first synorogenic basin in the Neuquén Basin.- The origin of the Malargüe Basin.- The Late Cretaceous-Paleocene extension.- The Paleocene to early Oligocene lull.- Causes and extent of the Oligocene extension.- The Late Cretaceous to Oligocene magmatism.- The Miocene orogenesis related to the subduction of the Payenia hot spot.- The Miocene magmatism in the Malargüe fold and thrust belt.- The structure of the Malargüe fold and thrust belt.- Thermochronological constraints on the exhumation of the Malargüe fold and thrust belt.- Structure and thermochronological constraints on the exhumation of the Chos Malal fold and thrust belt.- The structure and exhumation of the Agrio fold and thrust belt.- The Quaternary deformation in the Neuquén Basin and the impact of the Payenia hot spot.