Structural framework, stratigraphy, and evolution of Brazilian marginal basins

The structural framework of the Brazilian continental margin is basically composed of eight structural types: antithetic tilted step-fault blocks, synthetic untilted step-fault blocks, structural inversion axes, hinges with compensation grabens, homoclinal structures, growth faults with rollovers, diapirs, and igneous structures. The antithetic tilted and synthetic untilted step-fault blocks are considered as synchronous, complementary structural systems, separated by an inversion axis. They originated during the rift phase of the South American and African plates; genesis of the hinge and the homocline is related to the divergent migration of those plates. Two evaporitic cycles (Paripueira and Ibura) were differentiated in the Sergipe-Aiagoas type basin and tentatively correlated to the evaporitic section of other Brazilian marginal basins. It is assumed that the Paripueira evaporites could have been continuous with their African correlatives, but the Ibura evaporites are marginal deposits and were never continuous with their west African equivalents. Four phases are considered in the evolution of the Brazilian marginal basins: pre-rift, rift, transitional, and drift. During the pre-rift phase (Late Jurassic-Early Cretaceous), continental sediments were deposited in peripheral intracratonic basins. In the rift phase (Early Cretaceous), the breakup of the continental crust of the Gondwana continent gave rise to a central graben and rift valleys where lacustrine sediments were deposited. The transitional phase (Aptian) developed under relative tectonic stability, when evaporitic and clastic lacustrine sequences were being deposited. In the drift phase (Albian to Holocene), a regional homoclinal structure developed, consisting of two distinct sedimentary sequences, a lower clastic-carbonate and an upper clastic. From the Albian to the Holocene Epoch, structures associated to plastic displacement of salt or shale developed in many Brazilian marginal basins. The diapirism deformed mainly Upper Cretaceous strata in proximal areas, and younger strata in distal areas lying, in some places, on the ocean floor. Two phases of major igneous activity occurred: one in the Early Cretaceous associated with the rift phase of the Gondwana continent, and the other in the Tertiary (Oligocene-Miocene) during the migration phase of the South American and African plates.