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oxygen isotope fractionation |
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oxygen isotope fractionation [′äk·sə·jən ′īs·ə‚tōp ‚frak·shə′nā·shən]
(geochemistry) The use of temperature-dependent variations of the oxygen-18/oxygen-16 ratio in the carbonate shells of marine organisms, to measure water temperature at the time of deposition. Want to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit the webmaster's page for free fun content. |
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