Oxygen isotope fractionation factors involving cassiterite (SnO 2): I. calculation of reduced partition function ratios from heat capacity and X-ray resonant studies
Oxygen isotope equilibrium fractionation constants (β 18O-factors) of cassiterite were evaluated on the basis of heat capacity and X-ray resonant (Mössbauer spectroscopy and X-ray inelastic scattering) data. The low-temperature heat capacity of cassiterite was measured in the range from 13 to 340 K...
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Veröffentlicht in: | Geochimica et cosmochimica acta 2005-03, Vol.69 (5), p.1287-1300 |
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Sprache: | eng |
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