Quantification of major and trace elements in fluid inclusions and gas bubbles by laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) with no internal standard: a new method
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Published:2021-06-02
Issue:3
Volume:33
Page:305-314
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ISSN:1617-4011
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Container-title:European Journal of Mineralogy
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language:en
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Short-container-title:Eur. J. Mineral.
Author:
Borisova Anastassia Y.ORCID, Salvi Stefano, Velasquez German, Estrade Guillaume, Colin Aurelia, Gouy Sophie
Abstract
Abstract. Recent advances in laser ablation inductively coupled plasma mass
spectrometry (LA-ICP-MS) open new perspectives for quantification of trace
metals and metalloids in mineral-hosted fluid inclusions and glass-hosted
gas bubbles. This work is devoted to a new method applied to quantify
element concentrations (at parts-per-million and weight percent levels) in natural and synthetic
fluid inclusions and gas bubbles by using only an external calibrator in
cases where internal standardization is unavailable. For example, this
method can be applied to calculate element (metal and metalloid)
concentrations in carbonic (C–O–H) fluid inclusions and bubbles. The method
is devoted to measuring incompatible (with the host mineral and glass)
trace elements originally dissolved into the trapped fluid. The method
requires precise estimation of the fluid density, the inclusion/bubble
volume or average radius, and measurement of the laser ablation crater
radius by independent microanalytical techniques as well as accurate data
on the concentration of major/minor elements compatible with the host mineral
(or host glass). This method, applicable for analyses of hydrous
carbonic fluid inclusions and gas bubbles hosted in silicate minerals and
glasses, relies on the absence of a matrix effect between fluid, host
mineral and daughter phases (silicate, oxide or sulfide) and the external
calibrator (e.g., reference silicate glasses) during the LA-ICP-MS analysis,
an assumption validated by the use of femtosecond lasers.
Funder
Agence Nationale de la Recherche
Publisher
Copernicus GmbH
Reference34 articles.
1. Borisova, A. Y., Pichavant, M., Polvé, M., Wiedenbeck, M., Freydier, R., and
Candaudap, F.: Trace element geochemistry of the 1991 Mt. Pinatubo silicic
melts, Philippines: Implications for ore-forming potential of adakitic
magmatism, Geochim. Cosmochim. Ac., 70, 3702–3716, https://doi.org/10.1016/j.gca.2006.04.030, 2006. 2. Borisova, A. Y., Freydier, R., Polvé, M., Salvi, S., Candaudap, F., and
Aigouy, T.: In situ multi-elemental analysis of the Mount Pinatubo
quartz-hosted melt inclusions by NIR femtosecond laser ablation –
inductively coupled plasma – mass spectrometry, Geostand.
Geoanal. Res., 32, 209–229, https://doi.org/10.1111/j.1751-908X.2008.00882.x,
2008. 3. Borisova, A. Y., Thomas, R., Salvi, S., Candaudap, F., Lanzanova, A., and
Chmeleff, J.: Tin and associated metal and metaloid geochemistry by
femtosecond LA-ICP-MS microanalysis in pegmatite-leucogranite melt and fluid
inclusions: New evidence for melt-melt-fluid immiscibility, Mineral.
Mag., 76, 91–113, https://doi.org/10.1180/minmag.2012.076.1.91, 2012. 4. Borisova, A. Y., Toutain, J. P., Dubessy, J. Pallister J., Zwick, A., and Salvi, S.: H2O–CO2–S fluid triggering the 1991 Mount Pinatubo climactic
eruption (Philippines), Bull. Volcanol., 76, 800, https://doi.org/10.1007/s00445-014-0800-3, 2014. 5. Cauzid, J., Philippot, P., Somogyi, A., Ménez, B., Simionovici, A.,
and Bleuet, P.: Standardless quantification of single fluid inclusions using
synchrotron radiation induced X-ray fluorescence, Chem. Geol., 227,
165–183, https://doi.org/10.1016/j.chemgeo.2005.09.012, 2006.
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