By Eduardo Leaubon, Viridien
Exploration activity along the Equatorial Atlantic Margins has intensified in recent years, driven by major oil discoveries in the Guyana-Suriname basins, where proven reserves now exceed 18 billion barrels. However, the Brazilian sector of this margin—particularly the Amapá Deep Water province within the Foz do Amazonas Basin—remains largely underexplored.
Fewer than a dozen offshore wells have been drilled in shallow waters of this area, with most relying on legacy seismic datasets acquired decades ago. Even so, industry interest remains strong, as seen in the latest bidding round where US and Chinese companies secured 19 new exploration blocks in the basin.
Several companies continue to invest in the Brazilian Equatorial Margin, recognizing its significant hydrocarbon potential.
Amapá Deep Water area seismic reimaging
New initiatives in seismic reimaging and acquisition have applied cutting-edge technologies and advanced imaging workflows. By upgrading legacy datasets and acquiring modern seismic data, previously unseen prospectivity has been revealed.
Three key surveys covering the Amapá Deep Water area combine reimaged legacy data (Phase 1) with new acquisition (Phase 2), along with a merged reimaging of three older surveys into a single enhanced dataset.
These surveys* have been imaged using the latest algorithms, including elastic full-waveform inversion (elastic FWI), which delivers ultrahigh-resolution velocity models. These models are vital for imaging subsurface geology in frontier regions with sparse well control, like the Foz do Amazonas Basin.
Mapping the Upper Cretaceous and beyond
The high-resolution seismic has enabled semi-regional interpretation with impressive accuracy, even across complex geological intervals and at greater depths. The main focus of exploration in this area is the Upper Cretaceous, which shares similarities with plays in Guyana and Suriname. Here, turbiditic reservoirs on the slope and basin floor are believed to have been charged by an exceptionally rich source rock deposited during the Albian–Cenomanian–Turonian oceanic anoxic event.
The improved imaging has made it possible to map depositional features such as channel levee systems, lobes and other turbiditic geometries in detail, reconstructing sediment transport systems and paleoenvironments with a higher degree of confidence.