The Santos Basin is an approximately 352,000 square kilometres (136,000 sq mi) large mostly offshore sedimentary basin. It is located in the south Atlantic Ocean, some 300 kilometres (190 mi) southeast of Santos, Brazil. The basin is one of the Brazilian basins to have resulted from the break-up of Gondwana since the Early Cretaceous, where a sequence of rift basins formed on both sides of the South Atlantic; the Pelotas, Santos, Campos and Espírito Santo Basins in Brazil, and the Namibia, Kwanza and Congo Basins in southwestern Africa.
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
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.
The Campos Basin is one of 12 coastal sedimentary basins of Brazil. It spans both onshore and offshore parts of the South Atlantic with the onshore part located near Rio de Janeiro. The basin originated in Neocomian stage of the Cretaceous period 145–130 million years ago during the breakup of Gondwana. It has a total area of about 115,000 square kilometres (44,000 sq mi), with the onshore portion small at only 500 square kilometres (190 sq mi).
View of an oil platform in Campos oil field, Brazil