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The oil of Lapa Field is stored in microbialite sediments, organic build-ups of microscopic fauna formed in the Early Cretaceous Santos Basin
The northern edge of the basin is formed by the Cabo Frio High, extending southeastward from Cabo Frio at the coast.
The northern edge of the basin is formed by the Cabo Frio High, extending southeastward from Cabo Frio at the coast.
Itajaí (left) and Balneario Camboriú (right) at the southern edge of onshore Santos Basin
Itajaí (left) and Balneario Camboriú (right) at the southern edge of onshore Santos Basin
Outline of the Serra do Mar coastal forest ecoregion, bordering the Santos Basin
Outline of the Serra do Mar coastal forest ecoregion, bordering the Santos Basin
Sugarloaf Mountain and the other inselbergs of Rio de Janeiro are the onshore representatives of the basement of the Santos Basin.
Sugarloaf Mountain and the other inselbergs of Rio de Janeiro are the onshore representatives of the basement of the Santos Basin.