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fluorination

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Journal Article
Published: 01 February 1965
American Mineralogist (1965) 50 (1-2): 85–95.
...George Switzer; Roy S. Clarke, Jr.; John Sinkankas; Helen W. Worthing Abstract A chemical analysis of hambergite [Be 2 (OH, F)(BO 3 )] from the Little Three mine, near Ramona, San Diego County, California, disclosed that the mineral from this locality contains 6.0 per cent fluorine. Hambergite from...
Journal Article
Published: 01 February 1990
Clays and Clay Minerals (1990) 38 (1): 63–68.
Journal Article
Published: 01 February 1978
Clays and Clay Minerals (1978) 26 (1): 76–78.
Journal Article
Published: 01 October 1972
American Mineralogist (1972) 57 (9-10): 1386–1403.
...Georg Troll; M.C. Gilbert Abstract Experiments at 1 to 2 kbar total pressure, 600-850 °C aimed at exchanging fluorine and hydroxyl ions in tremolite under controlled conditions of HF and H 2 O fugacities have only been partially successful. The fluorine buffer technique of Munoz and Eugster...
Journal Article
Published: 01 October 1967
American Mineralogist (1967) 52 (9-10): 1503–1507.
Journal Article
Published: 01 June 1939
American Mineralogist (1939) 24 (6): 398–399.
...Frank C. Foley; Phillip W. West Abstract A method for the quantitative determination of fluorine in samples of ground water from North Dakota, which proved reliable for amounts of less than one part per million of fluorine, has also been used successfully for the qualitative determination...
Journal Article
Published: 01 November 2022
American Mineralogist (2022) 107 (11): 2008–2019.
... generated from volatile-rich mantle sources rich in fluorine and water. To clarify the mantle sources of lamproites, we present experimentally determined mineral/melt partition coefficients for fluorine and barium between phlogopite and lamproite melts. Both fluorine and barium are compatible in phlogopite...
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Journal Article
Published: 01 May 2022
American Mineralogist (2022) 107 (5): 815–825.
... by the Mineralogical Society of America 2022 Mineralogical Society of America Fluorine water thermal stability phlogopite mantle Experimental Halogens in Honor of Jim Webster Volatiles (e.g., hydrogen, nitrogen, carbon, and halogens) are not only present on the surface of the Earth, but also...
FIGURES
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Journal Article
Published: 01 November 2000
Russ. Geol. Geophys. (2000) 41 (11): 1520–1527.
...L. V. Zamana Anomalous fluorine contents in nitric hydrothermal waters are considered in the context of water-rock interaction. Study of this phenomenon involves processing and plotting of physicochemical data, correlation and factor analyses, and computation of the fluoride-calcium equilibrium...
FIGURES
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Journal Article
Published: 01 September 1993
South African Journal of Geology (1993) 96 (3): 149–159.
Journal Article
Published: 01 April 1989
American Mineralogist (1989) 74 (3-4): 333–338.
Journal Article
Published: 01 June 1982
American Mineralogist (1982) 67 (5-6): 538–544.
...E. U. Petersen; E. J. Essene; D. R. Peacor Abstract The near end-member minerals fluorphlogopite ( X F = 0.96) and fluortremolite ( X F = 0.82) have been found in Grenville marbles near Balmat, New York. These micas and amphiboles, like other fluorine-rich minerals reported in the literature...
Journal Article
Published: 01 October 1979
American Mineralogist (1979) 64 (9-10): 1027–1035.
Journal Article
Published: 01 February 1972
American Mineralogist (1972) 57 (1-2): 246–252.
...H.A. El-Attar; M.L. Jackson; V.V. Volk Abstract Fluorine loss from hectorite (2.3% F in the <2 μm fraction) upon heating for 24 hours at temperatures of 110° and 300° C was negligible, and at 540° C was less than 3%; however, upon ignition at 950°C for 6 hours, the fluorine loss was 100...
Journal Article
Published: 01 December 1956
American Mineralogist (1956) 41 (11-12): 929–932.
...Tokiti Noda; Rustum Roy Abstract Synthetic fluorine micas have assumed an important part in the literature of crystal chemistry, and the substances themselves are now commercial products. In the commercial operation the intergrowth of crystals and the bonding action of any residual melt make...
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Published: 19 May 2023
TABLE 3. SUMMARY OF BULK-ROCK AND QUARTZ OXYGEN-ISOTOPE VALUES BY LASER FLUORINATION AND SIMS SEPARATED BY SAMPLE AND LOCALITY
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Summary of oxygen isotope measurements by laser fluorination and secondary ion mass spectroscopy (SIMS) for the El Quemado Complex (EQC) and Chon Aike Formation (CA). All magmatic quartz values are elevated relative to the primitive mantle value of 5.5 ‰. SIMS measurements in quartz are separated by positioning on the crystal (core, mid, rim). Bulk rock samples of basement units are separated by location, but multiple samples from the same location are overlain on the same horizon; values per sample are indicated in Table 2. Ea.—Estancia; Ign/Rhy—ignimbrite/rhyolite; VSMOW—Vienna standard mean ocean water.
Published: 19 May 2023
Figure 11. Summary of oxygen isotope measurements by laser fluorination and secondary ion mass spectroscopy (SIMS) for the El Quemado Complex (EQC) and Chon Aike Formation (CA). All magmatic quartz values are elevated relative to the primitive mantle value of 5.5 ‰. SIMS measurements in quartz
Journal Article
Published: 01 February 2022
American Mineralogist (2022) 107 (2): 167–177.
...Don R. Baker; Sara Callegaro; Angelo De Min; Martin J. Whitehouse; Andrea Marzoli Abstract Concentrations of fluorine and chlorine were measured in glasses (quenched melts) and coexisting clinopyroxene, orthopyroxene, olivine, and plagioclase in run products of experiments previously used...
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Jurassic skarn garnet δ18O data. Symbols each mark one laser fluorination analysis. Sierra Nevada (southwestern United States) data suggest mixed magmatic- and metamorphic-derived fluids with a limited range of δ18O values. Mojave skarn garnet values show mixed fluid sources heavily influenced by surface-derived fluid. VSMOW—Vienna standard mean ocean water.
Published: 20 July 2021
Figure 3. Jurassic skarn garnet δ 18 O data. Symbols each mark one laser fluorination analysis. Sierra Nevada (southwestern United States) data suggest mixed magmatic- and metamorphic-derived fluids with a limited range of δ 18 O values. Mojave skarn garnet values show mixed fluid sources heavily
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Comparison of the data measured in bulk by laser fluorination GS-IRMS in this study versus the average values of the same samples measured by SIMS. The vertical error bar in each plot represents the total range of values measured by SIMS (e.g., length = δ′18Omax − δ′18Omin). Panel A shows oxygen isotope compositions of cherts measured by two different methods with the least-square regression line and 95% confidence intervals shown with dashed lines. The equation of the line is displayed in the upper left corner with standard errors shown in parentheses. The black solid line has slope of 1 and xy-intercept of 0. The oxygen isotope values versus average δ30Si is shown in Panel B. The vertical bars show the range of δ 30Si determined by SIMS. The symbols with black rims are plotted as δ′18O values determined in bulk analyses. The symbols without the black rim were plotted using the average δ′18O values determined by SIMS. The Δ′17O values plotted against δ30Si are shown in C. The horizontal error bars in C are analytical.
Published: 01 January 2021
Figure 8. Comparison of the data measured in bulk by laser fluorination GS-IRMS in this study versus the average values of the same samples measured by SIMS. The vertical error bar in each plot represents the total range of values measured by SIMS (e.g., length = δ′ 18 O max − δ′ 18 O min