Evaluation of kinetic effects on clumped isotope fractionation (Δ47) during inorganic calcite precipitation
Considerable efforts have been made to calibrate the Δ47 paleothermometer, which derives from the quantity of 13C–18O bonds in carbon dioxide produced during acid digestion of carbonate minerals versus its expected stochastic abundance, in a range of materials. However the impacts of precipitation r...
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Veröffentlicht in: | Geochimica et cosmochimica acta 2014-06, Vol.134, p.120-136 |
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