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Relation between silicified faults and evolution of the Cabo Frio High

19th Congress of the Brazilian Geophysical Society - Proceedings
The 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
openaire   +1 more source

Modelling maximum chlorophyll in the Cabo Frio (Brazil) upwelling: a preliminary approach

Ecological Modelling, 1990
Abstract 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
openaire   +1 more source

The Cabo Frio Thrust: A folded suture zone, Ribeira belt, SE Brazil

Journal of Structural Geology, 2021
Mónica Heilbron   +2 more
exaly  

Carbon, nitrogen, and phosphorus stoichiometry of plankton and the nutrient regime in Cabo Frio Bay, SE Brazil

Environmental Monitoring and Assessment, 2013
Emmanoel Silva-Filho   +2 more
exaly  

Reconstruction of southwestern Atlantic sea surface temperatures during the last Century: Cabo Frio continental shelf (Brazil)

Palaeogeography, Palaeoclimatology, Palaeoecology, 2014
Livia Cordeiro   +2 more
exaly  

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