Abstract

The most important Cenozoic marine transgression in Patagonia occurred during the late Oligocene-early Miocene when marine waters of Pacific and Atlantic origin flooded most of southern South America including the present Patagonian Andes between similar to 41 degrees and 47 degrees S. The age, correlation, and tectonic setting of the different marine formations deposited during this period are debated. However, recent studies based principally on U-Pb geochronology and Sr isotope stratigraphy, indicate that all of these units had accumulated during the late Oligocene-early Miocene. The marine transgression flooded a vast part of southern South America and, according to paleontological data, probably allowed for the first time in the history of this area a transient connection between the Pacific and Atlantic oceans. Marine deposition started in the late Oligocene-earliest Miocene (similar to 26-23 Ma) and was probably caused by a regional event of extension related to major plate reorganization in the Southeast Pacific. Progressive extension and crustal thinning allowed a generalized marine flooding of Patagonia that reached its maximum extension at similar to 20 Ma. It was followed by a phase of compressive tectonics that started around 19-16 Ma and led to the growth of the Patagonian Andes. The youngest (similar to 19-15 Ma) marine deposits that accumulated in the eastern Andean Cordillera and the extra-Andean regions are coeval with fluvial synorogenic deposits and probably had accumulated under a compressive regime.