Oxygen isotopic fractionation in TiO2 polymorphs (rutile, anatase, brookite) estimated from “first principles”
- Authors: Krylov D.P.1, Kuznetsov A.B.1
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Affiliations:
- Institute of Precambrian Geology and Geochronology of the Russian Academy of Sciences
- Issue: Vol 489, No 1 (2019)
- Pages: 62-64
- Section: Geochemistry
- URL: https://journals.eco-vector.com/0869-5652/article/view/17884
- DOI: https://doi.org/10.31857/S0869-5652489162-64
- ID: 17884
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Abstract
Temperature relations of b-factors for 18O/16O substitutions in TiO2 polymorphs have been determined using the density functional theory (DFT):
1000lnbrt(18O/16O) = 6,93039x - 0,08158x2 + 0,00116x3 + 0,08305*P,
1000lnbant(18O/16O) = 7,34275x - 0,09906x2 + 0,00153x3 + 0,08027*P,
1000lnbbrk(18O/16O) = 7,19088x - 009157x2 + 0,00139x3 + 0,07601*P,
x = 106/T(K)2, P - pressure (GPa).
The relations can be applied for isotope thermometry if combined with β-factors of coexisting phases.
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About the authors
D. P. Krylov
Institute of Precambrian Geology and Geochronology of the Russian Academy of Sciences
Author for correspondence.
Email: dkrylov@dk1899.spb.edu
Russian Federation, 2, Makarova embankment, St.Petersburg, 199034
A. B. Kuznetsov
Institute of Precambrian Geology and Geochronology of the Russian Academy of Sciences
Email: dkrylov@dk1899.spb.edu
Corresponding Member of the Russian Academy of Sciences
Russian Federation, 2, Makarova embankment, St.Petersburg, 199034References
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