Research Article
Heat Flow in the Campos Sedimentary Basin and Thermal History of the Continental Margin of Southeast Brazil
Table 1
Sedimentary formations in the Campos and Santos basins (modified after [
76]) and periods of main thermal activity.
| Basins | Age (Ma) | Tectonothermal activity | Campos | Santos | Group/formation | Member | Group/formation |
| | | Sepetiba | Tertiary | Depositional sequences controlled by thermal subsidence and occurrence of intrusions associated with hot-spot activity | Campos | Ubatuba | Marambaia | Emboré | | Iguape | Campos | Tamoios | Itajai-Açu, Santos | Cenomanian to Maastrichtian | Emborê | | Juréia | Santonian to Maastrichtian |
| Macaé | Outeiro | Itanhaém | Neo-Albian | Depositional sequences controlled by fault-bounded subsidence | Quissamã | Guarujá |
Eo-Albian |
Goytacas | Florianópolis | Albian | Lagoa Feia | Retiro | Ariri | Neo-Alagoas | | Guaratiba |
Aratu-EoAlagoas | Cabiunas | | Camboriú |
Eo-Cretaceous |
| Basement | | Basement | Pre-Cretaceous | Extensive magmatic activity associated with early rifting episodes |
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