Matches in SemOpenAlex for { <https://semopenalex.org/work/W4361289792> ?p ?o ?g. }
- W4361289792 endingPage "106239" @default.
- W4361289792 startingPage "106239" @default.
- W4361289792 abstract "A multibeam survey carried out in November 2019 reveals a lineament of seafloor protrusions on the Santos Basin (SW Atlantic) continental slope. Shallow seismic data and seafloor composition suggest the lineament comprises a 35 km long arrangement of Cold-Water Coral (CWC) carbonate mounds, here named the Tupana Carbonate Ridge (TCR), defined in this contribution for the first time. Insights into genetic controlling factors of the TCR led to the analysis of single-channel seismic profiles that cross the lineament. Interpretation of deep seismic reflection data suggests a stratigraphic control provided by the lateral arrangement of coastal deposits formed during the protracted progradation that characterized a significant portion of Santos Basin's depositional history. Coastal sandstones encased in low-angle shelf-margin progradational wedges constitute a potential hydrocarbon reservoir supplied by the flow of fluids toward the surface through vertical structures. The ultimate source of fluids seems to be provided by halokinetic movements on a region depleted of salts known as the Albian Gap domain. This work questions the role of seafloor hydrodynamics in shaping the TCR morphology by eroding the carbonate mounds and forming elongated contourite systems." @default.
- W4361289792 created "2023-03-31" @default.
- W4361289792 creator A5009223025 @default.
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- W4361289792 creator A5091419259 @default.
- W4361289792 date "2023-06-01" @default.
- W4361289792 modified "2023-09-27" @default.
- W4361289792 title "What could form a 35-km lineament of carbonate mounds on the ocean floor?" @default.
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