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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Arctic Ocean
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Barents Sea (2)
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Asia
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Arabian Peninsula
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elements, isotopes
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carbon
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hydrogen
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Primary terms
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isotopes
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C-13/C-12 (8)
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Mesozoic
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Middle Jurassic
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Triassic
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metals
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oil and gas fields (6)
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Paleozoic
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Cambrian
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Carboniferous (3)
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Devonian
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Lisburne Group (1)
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palynomorphs
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petroleum
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sediments
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triaromatic dinosteroids
Chemostratigraphic reconstruction of biofacies: Molecular evidence linking cyst-forming dinoflagellates with pre-Triassic ancestors
Representative saturate and aromatic fraction fragmentograms of Carbonifero...
Scatter plots of biomarker parameters used to justify oil groupings. Each o...
Uzon volcano caldera (Kamchatka): A unique natural laboratory of the present-day naphthide genesis
Organic geochemistry of oil and source rock strata of the Ordos Basin, north-central China
Charging of Carboniferous volcanic reservoirs in the eastern Chepaizi uplift, Junggar Basin (northwestern China) constrained by oil geochemistry and fluid inclusion
Recognition of an Infracambrian Source Rock Based on Biomarkers in the Baghewala-1 Oil, India
Molecular Organic Geochemistry of the Tarim Basin, Northwest China
Oil families and their inferred source rocks in the Barents Sea and northern Timan-Pechora Basin, Russia
Controls of oil family distribution and composition in nonmarine petroleum systems: A case study from the Turpan-Hami basin, northwestern China
Oil families and mixed oil of the North–Central West Siberian basin, Russia
Geochemical characteristics and correlation of oil and nonmarine source rocks from Mongolia
Cracking, mixing, and geochemical correlation of crude oils, North Slope, Alaska
Eve of biomineralization: Controls on skeletal mineralogy
Depositional environment and age determination of oils and condensates from the Barents Sea
Abstract The continental margin basins of Brazil and west Africa share very similar tectonostratigraphic units because of their proximity in Late Jurassic–Early Cretaceous time. As a result of the paleogeographic ties between the South American and the African plates, the oil habitat of the marginal basins of both continents can often be correlated. To better understand the petroleum systems along the South Atlantic margins, geochemical results obtained from the analysis of 290 oils from the major Brazilian and west African coastal basins were statistically evaluated to establish genetic relationships, distinguish source paleoenvironments and age, and identify different petroleum systems. A number of general oil families composed of genetically related oils were identified, several of which contain oils from both sides of the margin. Areas where oils of mixed provenance occur are also identified. Presalt (Neocomian–Aptian) lacustrine oils can be separated into at least three distinct families and are present in the Congo, Lower Congo, and Benguela Basins of west Africa and the Recôncavo, Campos, Potiguar, Ceará, and Bahia Sul Basins of Brazil. Genetically related oils may be present in the Campos Basin and offshore central Angola and in the Recôncavo Basin and central Gabon and northern Angola. Postsalt (Upper Cretaceous–Tertiary) marine oils are present in the Ivory Coast and the northern Gabon, Lower Congo, Kwanza, and Benguela Basins of west Africa and the Santos, Espírito Santo, and Sergipe–Alagoas Basins of Brazil. Oil mixing may have occurred in the Ivory Coast, Lower Congo, and Kwanza. Genetically related oils may occur in the Sergipe–Alagoas Basin and from northern Gabon. Oils from Nigeria, Benin, Equatorial Guinea, Cameroon, offshore northern Angola, and the Foz do Amazonas Basin of northern Brazil originated from Tertiary source rocks primarily composed of terrigenous organic matter deposited in fluvial deltaic or nearshore marine environments.