Abstract
AbstractFluorine (F) and chlorine (Cl) are important volatiles in olivine and its high-pressure polymorphs, which would significantly affect olivine phase transition, melting temperature, and physical property of the mantle. F and Cl concentrations in olivine can be detected by electron probe microanalysis (EPMA). However, the analytical accuracy and precision can be impeded by severe peak overlaps, low peak intensities of traditional analytical crystals, and secondary fluorescence effects. In this study, we constructed an optimized analytical method with high accuracy and precision to analyze trace F and Cl in olivine. Key parameters of analytical crystals, beam conditions, peak overlaps, and secondary fluorescence effects were discussed. Variations in the levels of the analyzed trace elements fall within ± 10%. The detection limits (3σ) for F and Cl are lowered to 30 ppm and 5 ppm, respectively. This method can provide precise F and Cl analysis for natural olivine samples and help to provide significant information on its formation process.
Funder
National Key R&D Program of China
Key Research Program of Chinese Academy of Sciences
Experimental Technology Innovation Fund of the Institute of Geology and Geophysics, Chinese Academy of Sciences
Key Research Program of the Institute of Geology and Geophysics, Chinese Academy of Sciences
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Reference69 articles.
1. Almasi GS, Blair J, Ogilivie RE, Schwartz RJ (1965) A heat-flow problem in electron-beam microprobe analysis. J Appl Phys 36(6):1848–1854
2. Amli R, Griffin WL (1975) Microprobe analysis of REE minerals using empirical correction factors. Am Miner 60(7–8):599–606
3. Ancey M, Bastenaire F, Tixier R (1978) Applications of statistical methods in microanalysis. In: Maurice F (ed.), Proc. Summer School St. Martin-d'Herres. Les Editions de Physique, Orsay, France, pp 319–343
4. Antignano A, Manning CE (2008) Fluorapatite solubility in H2O and H2O–NaCl at 700 to 900 °C and 0.7 to 2.0 GPa. Chem Geol 251:112–119
5. Bartels A, Vetere F, Holtz F, Behrens H, Linnen RL (2011) Viscosity of flux-rich pegmatitic melts. Contrib Mineral Petrol 162:51–60
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