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- W2260485514 abstract "There are at least 13 Tertiary oil shale deposits scattered along 900 km of coastal Queensland with an in situ shale oil resource totalling in excess of 25 billion barrels of shale oil. The paper compares aspects of the geochemistry for five of these deposits, which contain about two thirds of the demonstrated resource. The oil shales are moist, with a dominance of clay and silica minerals, a range of accessory minerals including siderite, feldspar and lesser amounts of gypsum, calcite, dolomite, pyrite and a number of phosphate minerals. Organic petrography and organic element analysis reveal that the source of the kerogen is algal (lamosites dominating) while other maceral forms dominate locally to form carbonaceous shale and humic coals." @default.
- W2260485514 created "2016-06-24" @default.
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- W2260485514 date "1983-08-01" @default.
- W2260485514 modified "2023-10-17" @default.
- W2260485514 title "Geology and Geochemistry of Some Queensland Tertiary Oil Shales" @default.
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- W2260485514 doi "https://doi.org/10.1021/bk-1983-0230.ch006" @default.
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