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Cabo Frio

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Series: GCSSEPM
Published: 01 December 2012
DOI: 10.5724/gcs.12.32.0347
EISBN: 978-0-9836097-8-0
... pressure oil kitchen (external rift) and beyond the most prolific oil carrier bed of the Campos basin–the Cabo Frio fault system (Papa Terra, Maromba, Polvo and Peregrino oil fields and all of the discoveries made by OGX); (2) the Late Cretaceous and mainly early Tertiary magmatic events that contributed...
FIGURES | View All (7)
Journal Article
Journal: Geology
Published: 01 October 2012
Geology (2012) 40 (10): 879-882.
... the depositional conditions of Cabo Frio, the degree of reactive iron pyritization was limited by both dissolved sulfide availability and pyrite oxidation events. Textural analyses of pyrite framboids provide evidence of re-oxidation processes, reflecting dynamic redox conditions in the sediments. The isotope...
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Series: AAPG Memoir
Published: 01 January 1995
DOI: 10.1306/M65604C13
EISBN: 9781629810867
... Abstract The Cabo Frio region, offshore Rio de Janeiro, lies between two of the most prolific Brazilian oil provinces, the Campos and Santos basins. Major geologic features have been identified using a multidisciplinary approach integrating seismic, gravity, petrographic, and borehole data...
Series: Geological Society, London, Special Publications
Published: 01 January 2013
DOI: 10.1144/SP369.21
EISBN: 9781862396173
...–0.5 Gough Island Hot spot 12–1.5 Fernando de Noronha 14–11 St Helena island Hot spot ? 18–5 Tristão da Cunha Ocean ridge 60–45 Abrolhos Plume ? 85–55 East–west Poços de Caldas–Cabo Frio alkaline lineament, NW-trend along Paranaíba Arch Plume 52–0.0 Cameroon Line Parallel...
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Cross sections of the <b>Cabo</b> <b>Frio</b> Terrain. location of A-A′ and B-B′ in Figur...
Published: 15 October 2014
Figure 3. Cross sections of the Cabo Frio Terrain. location of A-A′ and B-B′ in Figure  2 . Modified from Schmitt et al. (2004) .
Image
Location of Campos Basin, offshore Brazil, demarcated by the <b>Cabo</b> <b>Frio</b> High...
in > Geophysics
Published: 07 November 2011
Figure 1. Location of Campos Basin, offshore Brazil, demarcated by the Cabo Frio High to the south and the Vitoria High to the north. Expanded right panel shows outline of reprocessed poststack 3D data used in this study. Transects A-A′, B-B′, C-C′, D-D′, and E-E′ reference seismic lines used
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Geoseismic section CC&#x27; across transfer zone, <b>Cabo</b> <b>Frio</b> area (modified from ...
Published: 01 November 2001
Figure 9 Geoseismic section CC' across transfer zone, Cabo Frio area (modified from Mohriak et al., 1995 ). See Figure 1 for location.
Series: Geological Society, London, Special Publications
Published: 01 January 2012
DOI: 10.1144/SP363.9
EISBN: 9781862396111
... circular features, segmented faults at the slope break and crestal collapse above salt ridges in the distal deepwater domain (b). Fig. 4. A regional seismic section (in depth) displays the extensive and compressive halokinetic domains separated by the Cabo Frio Fault and an adjacent, also...
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Journal Article
Published: 01 August 2010
Petroleum Geoscience (2010) 16 (3): 231-245.
...W. U. Mohriak; M. Nóbrega; M. E. Odegard; B. S. Gomes; W. G. Dickson Abstract ABSTRACT This paper discusses the geological and geophysical interpretation of rift structures in the region extending from the Rio Grande Rise, in the Southeastern Brazilian margin, towards the Cabo Frio High, which...
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Series: Geological Society, London, Special Publications
Published: 01 January 2008
DOI: 10.1144/SP294.15
EISBN: 9781862395428
... information. Emphasis is placed on the sequence of deformation of the Cambrian tectonic events recorded in the Ribeira Belt, together with a review of related published data. The Cabo Frio tectonic domain (CFTD) crops out in the southeastern part of the Neoproterozoic–Palaeozoic NE–SW-trending Ribeira Belt...
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Series: AAPG Studies in Geology
Published: 01 January 1977
DOI: 10.1306/St4393C24
EISBN: 9781629812076
... Abstract Changes in the oceanographic and sedimentologic regime off southern Brazil are reflected in the carbonate enrichment and foraminiferal assemblages of the shelf sediments. North of Cabo Frio, carbonate-rich sands and gravels are characterized by Halimeda , bryozoans, and coralline...
Series: Geological Society, London, Special Publications
Published: 01 January 2008
DOI: 10.1144/SP294.11
EISBN: 9781862395428
... followed, such as those in the Borborema–Trans-Saharan province ( c. 0.62–0.60 Ga); in the Ribeira–Araçuaí belt ( c. 0.58 Ga); along the Araguaia and Paraguay belts (collision of Amazonia, c. 0.54–0.52 Ga); and the accretion of Cabo Frio terrane in the Ribeira Belt ( c. 0.53–0.50 Ga...
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Series: Geological Society, London, Special Publications
Published: 01 January 2008
DOI: 10.1144/SP294.12
EISBN: 9781862395428
... (c) The third collisional event is related to the docking of the Oriental terrane, which contains the Neoproterozoic Rio Negro arc, against the São Francisco palaeo-continent at c . 580–550 Ma. (d) Finally, collision of the Cabo Frio terrane took place during the Cambrian, at c . 530–510 Ma...
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Journal Article
Published: 01 April 2001
Journal of Foraminiferal Research (2001) 31 (2): 152-163.
... time in the laguno-estuarine complex of Cananéia-Iguape in 1995. It had never been reported before, probably because it was confused with juveniles of Ammonia. Its distribution has been studied in Brazilian coastal and paralic environments from Cabo Frio (Rio de Janeiro state) near latitude 22°50′S...
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Series: GCSSEPM
Published: 01 December 1993
DOI: 10.5724/gcs.95.16.0177
EISBN: 978-1-944966-30-0
... associated with early salt mobilization are often masked by the phenomenal Late Tertiary to Quaternary clastic progradation and by the presence of salt tongues near the surface ( Wu et al. 1990 ). Although possible analogs are much less developed than in the Cabo Frio region, there is evidence for Mid...
Journal Article
Journal: GSA Bulletin
Published: 01 January 1977
GSA Bulletin (1977) 88 (1): 101-112.
.... A hot-spot–South America relative motion approximately 1.4 ± 0.5 cm/yr in a northwest-southeast direction is suggested for this time. The littoral belt of alkalic rocks developed from São Sebastião to Cabo Frio starting about 82 m.y. ago and lasting until about 59 m.y. ago. This was about the same...
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A traverse line through the Santos (left) and Campos (right) Basins survey....
Published: 21 October 2014
Figure 6. A traverse line through the Santos (left) and Campos (right) Basins survey. The blue line indicates the positioning of the Cabo Frio high. There is an increase in high-amplitude volcanics above the TOS near the Cabo Frio high.
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Restorations modified from  Rowan and Ratliff (2012)  illustrating two end-...
Published: 01 November 2015
Figure 5. Restorations modified from Rowan and Ratliff (2012) illustrating two end-member hypotheses for the origin of the Albian Gap. (A) Sequential restoration assuming an origin as a landward-dipping fault (CFF—Cabo Frio fault). (B) Sequential restoration of an expulsion rollover
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REE diagrams of the main complexes in the Serra do Mar Province. Data from:...
Published: 16 May 2019
, 2007 (syenites and phonolites of Morro Redondo and Morro de Sao João); Bennio et al . 2002 (nepheline syenites and phonolites of Cabo Frio); and Traversa et al . 1994 (Lages nepheline syenites). The Monte de Trigo eudialytes are from Enrich et al . (2016) . Reference titanite compositions
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(A) Regional map showing the main basement-involved structures and salt-rel...
Published: 01 November 2015
) . The approximate locations of four of the boreholes used to constrain the seismic interpretation are projected onto this line (723C and 532A). CFF—Cabo Frio fault. UTM 24 South. Datum—WGS84.