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Relation between silicified faults and evolution of the Cabo Frio High
19th Congress of the Brazilian Geophysical Society - ProceedingsThe Cabo Frio High represents a structural and magmatic feature limiting Santos and Campos Basins. Several examples of faults and magmatic intrusions are pervasive on the continental border from Niterói, to Cabo Frio and Búzios municipalities. These structures present silicified faults that register information about the kinematic of the deformation,
Cleverson Guizan +4 more
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Modelling maximum chlorophyll in the Cabo Frio (Brazil) upwelling: a preliminary approach
Ecological Modelling, 1990Abstract The Cabo Frio area (Central-southern Brazilian littoral) is characterized by a coastal upwelling due to prevailing E-NE winds, mainly during the spring-summer season. This upwelling which has been studied for the last 15 years, is a local phenomenon with phytoplankton bloom of less than 1 day, and low intensity (max.
Jean Louis Valentin, Ricardo Coutinho
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The Cabo Frio Thrust: A folded suture zone, Ribeira belt, SE Brazil
Journal of Structural Geology, 2021Mónica Heilbron +2 more
exaly
Macroalgae of the Cabo Frio Upwelling Region, Brazil: Ordination of Communities
1992Y. Yoneshigue-Valentin, J.L. Valentin
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