Abstract
The Cenozoic of the Santa Marı́a Valley is composed of four allostratigraphic units defined by regional discontinuities. The two lower units are related to arching upward and shallow extension of the upper crust composed of Precambrian–Cambrian crystalline rocks (Sierras Pampeanas); the two upper ones are subjected to compression due to thickening of the lithosphere and mountain uplift. Unit I reflects the pre-rift stage and consists of reddish, very fine sandstones and shales (locally conglomerates) older than 13Ma. Unit II was divided in two units. The lower one (Unit IIa or initial rift stage) is composed of fine paralic deposits related to the Paraná marine ingression. The upper one (Unit IIb or rift climax stage, 7–5.2Ma) is composed of several lacustrine (fresh to saline) episodes and medium- to coarse-grained fluvial sandstones. Unit III started (around 5.2Ma) with a change of tectonic style from extensive to compressive, reflected in the intra-Andalhuala unconformity. This unit is the initial compressive stage (5.2–2.9Ma) and involves a coarsening-up succession of conglomerates and sandstones. Progressive aridity is evident in the facies association and is related to the rise of eastern mountain barriers. Unit IV, the climax compressive stage (2.9Ma), is represented by local coarse conglomerates.
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