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- W1966421906 abstract "Abstract Mississippi Valley-type mineralization occurs within Middle Devonian carbonates at the Pine Point lead-zinc mining property. Northwest Territories, Canada. A highly diverse suite of natural bitumens, ranging from liquid heavy oils to solid bitumens, is found in proximity to and distant from the ore bodies on the property. In this study, the bitumens are divided into different types based on qualitative observations in reflected white and fluorescent light. Five texturally distinct bitumens are distinguished; one homogeneous and four heterogeneous forms. Geochemical analyses (elemental analysis, solvent extraction and fractionation, gas chromatography, gas chromatography-mass spectrometry, and pyrolysis-gas chromatography) indicate that one of these bitumen types has a contribution from a source other than the ‘’ fades, which previously had been considered to be the source of all the Pine Point bitumens. Other factors besides source that have caused the variations in the properties of Pine Point b..." @default.
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- W1966421906 date "1993-04-01" @default.
- W1966421906 modified "2023-09-27" @default.
- W1966421906 title "Optical and Geochemical Classification of Pine Point Bitumens and Evidence for Their Origin from Two Separate Source Rocks" @default.
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- W1966421906 doi "https://doi.org/10.1080/00908319308909029" @default.
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