Sedimentology and alluvial architecture of the Bajo Barreal Formation (Upper Cretaceous) in the Golfo San Jorge Basin: Outcrop analogues of the richest oil-bearing fluvial succession in Argentina
文摘

A 450–650 m thick fluvial succession was analysed along a 4.5 km wide exposure.

A high-accommodation fluvial setting with multiple channel belts was identified.

A plural, equi-style fluvial system is interpreted.

Fluvial channels are narrow sheets of low sinuosity or braided that relocated by avulsion.

The temporo-spatial variability in the geometry of ∼300 fluvial channels is quantified.

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