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In Situ Analysis of Trace Elements in Quartz Using Laser Ablation Inductively Coupled Plasma Mass Spectrometry

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Quartz: Deposits, Mineralogy and Analytics

Part of the book series: Springer Geology ((SPRINGERGEOL))

Abstract

In situ micro analysis of ultra trace element composition of quartz using laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) allows rapid screening of lattice bound impurities of potential high-purity quartz resources and samples for petrological research without the need to remove solid and liquid inclusions by expensive dressing techniques prior to chemical analysis. Information of the analysed trace element content can not only be used to determine the economic quality of quartz but also the conditions of quartz crystallisation and the origin of the quartz-forming fluids and melts. The main purpose of this paper is to describe an efficient and precise analytical method for estimating the concentrations of lattice-bound trace elements in quartz. The best choice of instrument is considered to be a double focusing sector field inductively coupled plasma mass spectrometry ICP-MS that provides high sensitivity and a mass resolution high enough to separate K from its interferences. The ICP-MS should be coupled to a 193 nm excimer laser, a femto second laser or a similar ablation system. The following elements are included in the standard analytical protocol applied at the Geological Survey of Norway (NGU): Al, B, Be, Ca, Cr, Fe, Ga, Ge, K, Li, Mg, Mn, Na, P, Rb, Sb, Sr, Ti and Zn. Any element with isotopes that can be ionised in an Ar plasma can easily be included if suitable reference materials are available. External calibration was done using the international reference materials NIST SRM 610, 612, 614, 616 and 1830 from the National Institute of Standards and Technology (NIST), BCS 313/1 from the Bureau of Analysed Samples (BAS) and the certified reference material “pure substance No. 1” silicon dioxide SiO2 from the Federal Institute for Material Research and Testing, Berlin, Germany (BAM). To improve the lower limit of quantification and analytical uncertainty at low concentrations, it is important to have calibration curves with well defined intercepts. This can be achieved by the use of certified standards, with trace element concentrations lower than the quantification limit. Even better is to use a standard where the analyte is not present, however in laserablation matrixmatcing is usually important and a standard blank is usually not avilable. In this work, BAM no. 1 SiO2 is the reference material used whith the lowest consentration of the analytes. Because of the absence of a SiO2 blank, the BAM no. 1 SiO2 is used for the estimation of detection limits. Detection limits for most of the elements are between 1 and 0.02 μg g−1. Analysis time and laser spot size are adjusted to the size of the quartz crystal and the thickness (~300 μm) of the polished thick section. The size of the ablation raster is commonly 100 × 350 μm with a depth of 10–20 μm applying the analysis time of less than 1 min.

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References

  • Beurlen H, Müller A, Silva D, Da Silva MRR (2011) Petrogenetic significance of trace-element data analysed with LA-ICP-MS in quartz from the borborema pegmatite province, Northeastern brazil. Mineral Mag 75(5):2703–2719

    Article  Google Scholar 

  • Breiter K, Müller A (2009) Evolution of rare-metal granitic magmas documented by quartz chemistry. Eur J Mineral 21:335–346

    Article  Google Scholar 

  • Fanderlik I (1991) Silica glass and its application. Elsevier, Amsterdam

    Google Scholar 

  • Feldmann I, Tittes W, Jakubowski N, Stuewer D, Giessmann U (1994) Performance characteristics of inductively coupled plasma mass spectrometry with high mass resolution. J Anal At Spectrom 9:1007–1014

    Article  Google Scholar 

  • Fernandes B, Claverie F, Pecheyran C, Donard OFX (2007) Direct analysis of solid samples by fs-LA-ICP-MS. Trends Anal Chem 26(10):951–966

    Article  Google Scholar 

  • Flem B, Larsen RB, Grimstvedt A, Mansfeld J (2002) In situ analysis of trace elements in quartz by using laser ablation inductively coupled plasma mass spectrometry. Chem Geol 182:237–247

    Article  Google Scholar 

  • Gießmann U, Greb U (1994) High resolution ICP-MS a new concept for elemental mass spectrometry. Fresenius’ J Anal Chem 350:186–193

    Article  Google Scholar 

  • Gonzalez J, Liu C, Mao X, Russo RE (2004) UV-femtosecond laser ablation-ICP-MS for analysis of alloy samples. J Anal At Spectrom 19:1165–1168

    Article  Google Scholar 

  • Götze J, Plötze M, Habermann D (2001) Origin, spectral characteristics and practical applications of the cathodoluminescence (CL) of quartz—a review. Mineral Petrol 71:225–250

    Article  Google Scholar 

  • Günther D, Heinrich CA (1999) Enhanced sensitivity in laser ablation-ICP mass spectrometry using helium–argon mixtures as aerosol carrier. J Anal At Spectrom 14:1363–1368

    Article  Google Scholar 

  • Günther D, Frischknecht R, Heinrich CA, Kahlert HJ (1997) Capabilities of an argon fluoride 193 nm excimer laser for laser ablation inductively coupled plasma mass spectrometry microanalysis of geological materials. J Anal At Spectrom 12:939–944

    Article  Google Scholar 

  • Harben PW (2002) The industrial mineral handybook—a guide to markets, specifications and prices, 4th edn. Industrial Mineral Information.Worcester Park, United Kingdom, p 412

    Google Scholar 

  • Hirata T, Nesbitt RW (1995) U-Pb isotope geochronology of zircon: evaluation of the laser probe-inductively coupled plasma mass spectrometry technique. Geochim Cosmochim Acta 59:2491–2500

    Article  Google Scholar 

  • Jacamon F, Larsen RB (2009) Trace element evolution of quartz in the charnockitic Kleivan granite, SW Norway: the Ge/Ti ratio of quartz as an index of igneous differentiation. Lithos 107:281–291

    Article  Google Scholar 

  • Jacob DE (2006) High sensitivity analysis of trace element-poor geological reference glasses by laser ablation-inductively coupled plasma mass spectrometry (LA-ICP-MS). Geostand Geoanal Res 30:221–235

    Article  Google Scholar 

  • Jeffries T, Jackson SE, Longerich HP (1998) Application of a frequency quintupled Nd: YAG source (λ = 213 nm) for laser ablation inductively coupled plasma mass spectrometric analysis of minerals. J Anal At Spectrom 13:935–940

    Article  Google Scholar 

  • Jochum KP, Dingwell DB, Rocholl A, Stoll B, Hofmann AW et al (2000) The preparation and preliminary characterisation of eight geological MPI-DING reference glasses for in situ microanalysis. Geostand Newsl 24:87–133

    Article  Google Scholar 

  • Jourdan A-L, Vennemann TW, Mullis J, Ramseyer K (2009) Oxygen isotope sector zoning in natural hydrothermal quartz. Mineral Mag 73:615–632

    Article  Google Scholar 

  • Jung L (1992) High-purity natural quartz. Part 1: high-purity natural quartz for industrial use. Library of Congress-in-Publication Data, New Jersey, p 538

    Google Scholar 

  • Larsen RB, Polvé M, Juve G (2000a) Granite pegmatite quartz from Evje-Iveland: trace element chemistry and implications for high-purity quartz formation. Bull Geol Surv Norw 436:57–65

    Google Scholar 

  • Larsen RB, Flem B, Dundas S, Lahaye Y, Mansfeld J (2000b) LA-HR-ICP-MS analysis of quartz and principles governing the distribution and speciation of structural impurities in igneous quartz. Report Geological Survey of Norway, 081

    Google Scholar 

  • Müller A, Welch MD (eds.) (2009) Frontiers in quartz research. Mineral Mag themat issue 73(4)

    Google Scholar 

  • Müller A, Wiedenbeck M, van den Kerkhof AM, Kronz A, Simon K (2003) Trace elements in quartz—a combined electron microprobe, secondary ion mass spectrometry, laser-ablation ICP-MS, and cathodoluminescence study. Eur J Mineral 15:747–763

    Article  Google Scholar 

  • Müller A, Wiedenbeck M, Flem B, Schiellerup H (2008) Refinement of phosphorus determination in quartz by LA-ICP-MS through defining new reference material values. Geostand Geoanalytical Res 32:361–376

    Article  Google Scholar 

  • Müller A, Herrington R, Armstrong R, Seltmann R, Kirwin G, Stenina N, Kronz A (2010) Trace elements and cathodoluminescence of quartz in stockwork veins of Mongolian porphyry-style deposits. Miner Deposita 45:707–727

    Article  Google Scholar 

  • Ødegård M, Dundas SH, Flem B, Grimstvedt A (1998) Application of a double-focusing magnetic sector inductively coupled plasma mass spectrometer with laser ablation for the bulk analysis of rare earth elements in rocks fused with Li2B4O7. Fresenius’ J Anal Chem 362:477–482

    Article  Google Scholar 

  • Perny B, Eberhardt P, Ramseyer K, Mullis J, Pankrath R (1992) Microdistribution of Al, Li and Na in alpha -quartz: possible causes and correlation with short-lived cathodoluminescence. Am Mineral 77:534–544

    Google Scholar 

  • Reimann C, Filzmoser P, Garrett RG, Dutter R (2008) Statistical data analysis explained applies enviromental statistics. Wiley,Chichester

    Book  Google Scholar 

  • Rodushkin I, Nordlund P, Engström E, Baxter D (2005) Improved multi-elemental analyses by inductively coupled plasma-sector field mass spectrometry through methane addition to the plasma. J Anal At Spectrom 20:1250–1255

    Article  Google Scholar 

  • Rusk B, Koenig A, Lowers H (2011) Visualizing trace element distribution in quartz using cathodoluminescence, electron microprobe, and laser ablation inductively coupled mass spectrometry. Am Mineral 96:703–708

    Article  Google Scholar 

  • Russo RE, Mao XL, Borisov OV, Liu H (2000) Influence of wavelength on fractionation in laser ablation ICP-MS. J Anal At Spectrom 15:1115–1120

    Article  Google Scholar 

  • Staudte RG, Sheather SJ (1990) Robust estimation and testing. Wiley, New York, p 350

    Book  Google Scholar 

  • Thermo Scientific (2011) <http://www.thermo.com/eThermo/CMA/PDFs/Various/File_265.pdf>. Accessed 30 May 2011

  • Wark DA, Watson EB (2006) TitaniQ: a titanium-in-quartz geothermometer. Contrib Mineral Petrol 152:743–754

    Article  Google Scholar 

  • Weil JA (1993) A review of the EPR spectroscopy of point defects in α-quartz: the decade 1982–1992. In: Helms CR, Deal BE (eds.) Physics and chemistry of SiO2 and the Si–SiO2 interface. Plenum Press, New York, pp 131–144

    Chapter  Google Scholar 

  • Wilcox RR (1997) Introduction to robust estimation and hypothesis testing. Academic Press,San Diego, p 296

    Google Scholar 

Download references

Acknowledgments

We are grateful to Ben Snook and Ian Henderson who improved the English language of the manuscript.

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Flem, B., Müller, A. (2012). In Situ Analysis of Trace Elements in Quartz Using Laser Ablation Inductively Coupled Plasma Mass Spectrometry. In: Götze, J., Möckel, R. (eds) Quartz: Deposits, Mineralogy and Analytics. Springer Geology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-22161-3_10

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