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Fig. 2 | Journal of Palaeogeography

Fig. 2

From: Computerized geochemical modeling of burial diagenesis of the Eocene turbidite reservoir elements: Urucutuca Formation, Espírito Santo Basin, southeastern Brazil passive margin

Fig. 2

The simplified and schematic tectonostratigraphic succession of the Espírito Santo Basin (after Françaet al., 2007). The lithostratigraphic units shown here have the most basinal distribution. The localized and minor units are not shown. Note that the Urucutuca Formation discussed in this article covers all the mud-dominated deep-marine sedimentary interval of the basin spanning between Upper Cretaceous and almost the entire Cenozoic. The studied Eocene interval is shown with a white rectangle

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