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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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commodities
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upper Paleozoic
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Primary terms
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Atlantic Ocean
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Australasia
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Australia
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bitumens
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asphalt (1)
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Canada
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Ontario
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Western Canada
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carbon
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Cenozoic
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Holocene
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upper Holocene
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Paleogene
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upper Paleocene (1)
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chemical analysis (9)
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coal deposits
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construction materials (1)
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crystal structure (1)
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dams (1)
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data processing (2)
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Deep Sea Drilling Project
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IPOD
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Leg 86
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DSDP Site 577 (1)
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Leg 32
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DSDP Site 305 (1)
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diagenesis (1)
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Europe
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Iberian Peninsula
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faults (1)
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metal ores
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metals
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Ocean Drilling Program
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Leg 199
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ODP Site 1221 (1)
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upper Paleozoic
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paragenesis (1)
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petroleum
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sediments
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soils
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Chernozems (1)
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South America
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Brazil
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spectroscopy (2)
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thermal analysis (1)
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United States
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Colorado
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Pueblo County Colorado
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Illinois Basin (1)
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Montana
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Texas
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waste disposal (4)
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weathering (6)
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X-ray analysis (1)
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sedimentary rocks
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sedimentary rocks
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bauxite (1)
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carbonate rocks
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limestone
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chemically precipitated rocks
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duricrust (1)
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weathering crust (1)
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clastic rocks
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alum shale (1)
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shale (1)
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coal
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bituminous coal (1)
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sediments
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sediments
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clastic sediments
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clay (2)
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mud (1)
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silt (1)
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marine sediments (2)
-
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soils
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soils
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Chernozems (1)
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sequential extraction
Enrichment and fractionation of rare earth elements (REEs) in ion-adsorption-type REE deposits: Constraints of an iron (hydr)oxide-clay mineral composite
Hexavalent chromium mobility in a high amorphous phase Chromite Ore Processing Residue (COPR) in the perspective of a chromium remediation treatment
Evaluation of forensic soil traces from a crime scene: robbery of a safety deposit box in Brazil
Abstract Soil traces can be used as evidence in criminal investigations due their transferability, great variability and persistence. The soil samples originated from a crime scene that occurred in the Curitiba Metropolitan Region, Brazil. Physical, chemical and mineralogical analyses were carried out on the soil samples. All results were statistically analysed using multivariate analysis (PCA) to verify the relative positioning of soil traces which had been recovered from a stolen safety deposit box (SDB) from a vehicle suspected of being used in the SDB transportation, and from the site allegedly used in the opening of the SDB. The methods employed were effective in discriminating between the sampling sites. The soil from the site used in the opening of the SDB could be excluded as being the location where the soil transferred to the SDB had originated as it was different in many characteristics.
Formation of bitumen in the Elgin–Franklin complex, Central Graben, North Sea: implications for hydrocarbon charging
Abstract The Elgin–Franklin complex contains gas condensates in Upper Jurassic reservoirs in the North Sea Central Graben. Upper parts of the reservoirs contain bitumens, which previous studies have suggested were formed by the thermal cracking of oil as the reservoirs experienced temperatures of >150°C during rapid Plio-Pleistocene subsidence. Bitumen-stained cores contaminated by oil-based drilling muds have been analysed by hydropyrolysis. Asphaltene-bound aliphatic hydrocarbon fractions were dominated by n -hexadecane and n -octadecane originating from fatty acid additives in the muds. Uncontaminated asphaltene-bound aromatic hydrocarbon fractions, however, contained a PAH distribution very similar to normal North Sea oils, suggesting that the bitumens may not have been derived from oil cracking. 1D basin models of well 29/5b-6 and a pseudo-well east of the Elgin–Franklin complex utilize a thermal history derived from the basin's rifting and subsidence histories, combined with the conservation of energy currently not contained in the thermal histories. Vitrinite reflectance values predicted by the conventional kinetic models do not match the measured data. Using the pressure-dependent PresRo ® model, however, a good match was achieved between observed and measured data. The predicted petroleum generation is combined with published diagenetic cement data from the Elgin and Franklin fields to produce a composite model for petroleum generation, diagenetic cement and bitumen formation.