“…Correspondingly, three sets of giant thick sedimentary sequences were developed, namely the continental giant sequences of the Guaratiba Group in the rift period, the evaporative salt giant sequences of the Ariri Formation in the transition period, and the marine giant sequences of the passive continental margin carbonates, deep-sea mudstones, and deep-sea turbidite sandstones in the drift period (Figure ). ,, From the bottom to the top, the basin mainly develops four sets of reservoirs: the lacustrine limestone of the Cretaceous Guaratiba Group, the shallow-sea sandstone, carbonate of the Florianopolis Group, the turbidite sandstones of Santos Group, and the turbidite sandstones of the Paleogene–Neogene Marambala Group. − , Oil and gas are mainly enriched in the limestone reservoir of the subsalt Guaratiba Group. Two sets of source rocks are mainly developed in the basin, one is the lacustrine source rocks of the Lower Cretaceous Barremian–Aptian Stage Guaratiba Group in the subsalt rift period, and the other is the marine source rocks of the Upper Cretaceous Cenomanian–Turonian Stage Itajai-Acu Formation in the postsalt drift period. ,, In recent years, the discoveries of a large amount of oil and gas have confirmed that the lacustrine mudstones of the Guaratiba Group deposited in the subsalt rift period are the main source rock of the basin. ,,, The lacustrine source rocks of the Guaratiba Group consist of the Picarras Formation and the Itapema Formation source rocks.…”