Comparative molecular, elemental, and U-Pb isotopic composition of stratiform and dispersed-globular matter in the paleoproterozoic uraniferous metasediments, Elliot Lake, Canada

Journal Article · · Energy Sources; (United States)

DOI:https://doi.org/10.1080/00908319308909032· OSTI ID:6424529

Mossman, D J ^[1]; Nagy, B ^[2]; Davis, D W ^[3]

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1. Mount Allison Univ., Sackville, New Brunswick (Canada)
2. Univ. of Arizona, Tucson (United States)
3. Royal Ontario Museum, Toronto (Canada)

Uraninite and other uranium minerals at the Elliot Lake-Blind River uranium ore deposits are held mainly within syngenetic kerogen. Bitumen was generated from kerogen by hydrothermal solutions, through a process similar to hydrous pyrolysis. Liquid bitumen migrated away from its parent kerogen, but transported virtually no U and Th. However, bitumen has a large excess of [sup 206]Pb, which indicates that the liquid bitumen must have acted as a sink for mobile intermediate decay products of [sup 238]U, probably the noble gas, [sup 222]Rn. Bitumen was then converted by heat into a solid, consisting of highly condensed aromatic hydrocarbons, preventing Pb mobility. The upper intersection of U-Pb isotopic data is within error of the Nipissing diabase event, which suggests that this was responsible for almost totally resetting the U-Pb systems in the uraninite. The tectonic and thermal anomaly associated with emplacement of the Nipissing diabase may have also been responsible for formation and migration of bitumen into pores and fissures and for outgassing of [sup 222]Rn into the same openings, leading to the [sup 206]Pb anomaly. Uraniferous kerogen occurs mainly in stratiform layers. The kerogen has Ro[sub max] = 2.63 to 7.31%; it is highly aromatic in molecular composition, contains large clusters of aromatic hydrocarbon moieties, and its H/C atomic ratios range from 0.41 to 0.60. Bitumen, derived from the syngenetic kerogen, occurs as solid pore and fracture fillings, has Ro[sub max] = 0.72 to 1.32%, H/C atomic ratios of 0.71-0.81, and contains more alkyl substitutions on aromatic molecular components than the kerogen. A functional relationship between these two groups of organic matter is supported by their molecular compositions and [delta][sup 13]C signatures.

• OSTI ID: 6424529
• Journal Information: Energy Sources; (United States), Vol. 15:2; ISSN 0090-8312
• Country of Publication: United States
• Language: English

Related Subjects

04 OIL SHALES AND TAR SANDS
11 NUCLEAR FUEL CYCLE AND FUEL MATERIALS
BITUMENS
GEOCHEMISTRY
GEOLOGIC FORMATIONS
ONTARIO
URANIUM DEPOSITS
AGE ESTIMATION
AROMATICS
CARBON 13
CHEMICAL COMPOSITION
DISTRIBUTION
ELLIOT LAKE
ENVIRONMENTAL TRANSPORT
EXPERIMENTAL DATA
GEOLOGIC HISTORY
HYDROTHERMAL ALTERATION
ISOTOPE RATIO
KEROGEN
LEAD 206
ORGANIC MATTER
RADON 222
RARE EARTHS
REFLECTIVITY
TECTONICS
URANIUM 238
ACTINIDE ISOTOPES
ACTINIDE NUCLEI
ALPHA DECAY RADIOISOTOPES
BITUMINOUS MATERIALS
CANADA
CARBON ISOTOPES
CARBONACEOUS MATERIALS
CHEMISTRY
DATA
DAYS LIVING RADIOISOTOPES
DEVELOPED COUNTRIES
ELEMENTS
EVEN-EVEN NUCLEI
EVEN-ODD NUCLEI
GEOLOGIC DEPOSITS
HEAVY NUCLEI
INFORMATION
ISOTOPES
LEAD ISOTOPES
LIGHT NUCLEI
MASS TRANSFER
MATERIALS
MATTER
METALS
MINERAL RESOURCES
NORTH AMERICA
NUCLEI
NUMERICAL DATA
OPTICAL PROPERTIES
ORGANIC COMPOUNDS
OTHER ORGANIC COMPOUNDS
PHYSICAL PROPERTIES
RADIOISOTOPES
RADON ISOTOPES
RESOURCES
SPONTANEOUS FISSION RADIOISOTOPES
STABLE ISOTOPES
SURFACE PROPERTIES
TAR
URANIUM ISOTOPES
YEARS LIVING RADIOISOTOPES
040200* - Oil Shales & Tar Sands- Reserves
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040500 - Oil Shales & Tar Sands- Properties & Composition
050100 - Nuclear Fuels- Reserves
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