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- W1979804930 abstract "Isotopic analysis of recent carbonate sediments from the Coorong area of South Australia show dolomite enriched in O18 and depleted in C13 relative to calcite by at least two permil. This isotopic behavior suggests that the two minerals were precipitated under different conditions, and that the dolomite is not formed from calcite by solid-state ion exchange." @default.
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- W1979804930 date "1968-09-01" @default.
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- W1979804930 title "Isotopic compositions of recent South Australian lagoonal carbonates" @default.
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- W1979804930 doi "https://doi.org/10.1016/0016-7037(68)90062-8" @default.
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