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Stable Isotopes of Geological Interest
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Oxygen Isotopes
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Oxygen Isotope Variations
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Fractionation of Oxygen Isotopes
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Measurement of Oxygen Isotopes Analysis of oxygen isotopes in silicates and oxides usually involves the liberation of oxygen through fluorination with ClF 3 or BrF 5 followed by reduction of the oxygen gas to CO 2 at high- temperatures for measurement in a mass spectrometer. This method was first developed by Clayton and Mayeda (1963) using BrF 5 and modified by Borthwick and Harmon (1982) for use with ClF 3. This can be done using a conventional silicate line using Ni- reaction vessels, a laser line both of which need a fluorination agent or an ion-probe which doesn’t. Analysis is normally done on a dual-inlet gas source mass spectrometer.
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Mass Spectrometry
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Measurement of Oxygen Isotopes Low reaction yields can lead to fractionation of the oxygen isotopes and is a serious problem for analysis of refractory minerals such as olivine and garnet. In addition, conventional analysis on a silicate extraction line is not capable of analysing small samples in-situ and means that natural sample heterogeneity cannot be detected. These problems have to some extent been overcome with the development of laser-fluorination lines first described by Sharp (1990) More recently, the ion-probe has been used to determin oxygen isotope ratios at the sub-grain scale in zircons and other refractory minerals and has been pivotal in furthering our understanding of the development of the early Earth atmosphere.
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Measurement of Oxygen Isotopes
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Hydrogen Isotopes
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Hydrogen Isotope Variations
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Fractionation of Hydrogen Isotopes
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Measurement of Hydrogen Isotopes
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Carbon Isotopes
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Carbon Isotope Variation
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Carbon Isotope Fractionation
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Measurement of Carbon Isotopes
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Stable Isotope Standards
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Sulphur Isotopes
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Sulphur Isotope Variations
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Sulphur Isotope Fractionation
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Measurement of Sulphur Isotopes
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Nitrogen Isotopes
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Nitrogen Isotope Variations
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Nitrogen Isotope Fractionation
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Measurement of Nitrogen Isotopes
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