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Published November 2019 | Version v1
Journal article

Isotope Fractionation in TiO2 Polymorphs (Rutile, Anatase, Brookite) Estimated from "First Principles"

  • 1. Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences (Russian Federation)

Description

Temperature relations of β-factors for 18O/16O fractionations in TiO2 polymorphs have been determined using the density functional theory:1000 ln βrt(18O/16O) = 6.93039x – 0.08158x2 + 0.00116x3 + 0.08305*P1000 ln βant(18O/16O) = 7.34275x – 0.09906x2 + 0.00153x3 + 0.08027*P1000 ln βbrk(18O/16O) = 7.19088x – 0.09157x2 + 0.00139x3 + 0.07601*P,x = 106/T(K)2, P is pressure (GPa). The deduced relations can be applied for isotope thermometry if combined with β-factors of coexisting phases.

Additional details

Identifiers

Publishing Information

Journal Title
Doklady Earth Sciences
Journal Volume
489
Journal Issue
1
Journal Page Range
p. 1294-1296
ISSN
1028-334X

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Copyright
Copyright (c) 2019 © Pleiades Publishing, Ltd. 2019