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Journal ArticleDOI

Calculation of oxygen isotope fractionation in hydroxyl-bearing silicates

TLDR
In this article, the modified increment method has been applied to the calculation of oxygen isotope fractionation factors for hydroxyl-bearing silicate minerals, which can be used as a test of isotopic equilibrium or disequilibrium in natural mineral assemblages over all temperature ranges.
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This article is published in Earth and Planetary Science Letters.The article was published on 1993-12-01. It has received 672 citations till now. The article focuses on the topics: Silicate minerals & Silicate.

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Stable isotope geochemistry of ultrahigh pressure metamorphic rocks from the Dabie–Sulu orogen in China: implications for geodynamics and fluid regime

TL;DR: In this article, a fried ice cream model was proposed to explain the rapid processes of both plate subduction and exhumation, with a short residence time of the UHP slab at mantle depths.
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Oxygen Isotopes in Zircon

TL;DR: A large number of studies have shown that non-metamict zircons preserve their δ18O value from the time of crystallization; hence oxygen isotope ratio can be correlated with age (U-Pb) or trace element composition as discussed by the authors.
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Contrasting zircon Hf and O isotopes in the two episodes of Neoproterozoic granitoids in South China: Implications for growth and reworking of continental crust

TL;DR: In this article, a combined study of Hf and O isotopes in zircons from Neoproterozoic granitoids in South China provides evidence for growth and reworking of juvenile and ancient crusts with different styles of water-rock interactions along rift tectonic zones.
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Stable isotope geochemistry of clay minerals; The story of sloppy, sticky, lumpy and tough, Cairns-Smith (1971)

TL;DR: The equilibrium H- and O-isotope fractionation of clays can be approximated by the following equations which are based on experimental, empirical and/or theoretical data.
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Rift melting of juvenile arc-derived crust: Geochemical evidence from Neoproterozoic volcanic and granitic rocks in the Jiangnan Orogen, South China

TL;DR: In this article, a combined study of zircon U-Pb and Lu-Hf isotopes, mineral O isotope, whole-rock elements and Sr-Nd isotopes was carried out for Neoproterozoic volcanics and granites from the eastern part of the Jiangnan Orogen in South China.
References
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Journal ArticleDOI

Oxygen isotope fractionation in divalent metal carbonates

TL;DR: In this article, the fractionation factors for the distribution of 18O between alkaline-earth carbonates and water have been measured over the temperature range 0 −500°C.
Journal ArticleDOI

Calculation of Equilibrium Constants for Isotopic Exchange Reactions

TL;DR: In this article, it was pointed out that the possibility of chemical separation of isotopes is a quantum effect and that the difference in the free energies of two isotopic molecules can be directly calculated.
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Oxygen isotopic fractionation in the system quartz-albite-anorthite-water

TL;DR: Oxygen isotopic fractionations have been determined between quartz and water, albite and water and anorthite and water at temperatures from 300 to 825°C, and pressures from 15 to 25 kbar as mentioned in this paper.