Isotopic compositions of recent South Australian lagoonal carbonates

Details Isotopic compositions of recent South Australian lagoonal carbonates Isotopic compositions of recent South Australian lagoonal carbonates

Sep 1968

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1968gecoa..32..983c&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 32, Issue 9, pp.983-988

Physics

6

Scientific paper

Isotopic analysis of recent carbonate sediments from the Coorong area of South Australia show dolomite enriched in O 18 and depleted in C 13 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.

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