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Improved Accuracy for Trace Element Analysis of Al and Ti in Quartz by Electron Probe Microanalysis

Published online by Cambridge University Press:  04 February 2019

Ji-Qiang Cui
Affiliation:
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, PR China
Shui-Yuan Yang*
Affiliation:
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, PR China
Shao-Yong Jiang
Affiliation:
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, PR China Faculty of Earth Resources and Collaborative Innovation Center for Scarce and Strategic Mineral Resources, China University of Geosciences, Wuhan 430074, PR China
Jing Xie
Affiliation:
Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, PR China
*
*Author for correspondence: Shui-Yuan Yang, E-mail: shuiyuanyang@cug.edu.cn
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Abstract

The trace elements in quartz, Al and Ti, contain considerable information about mineral genesis, and determining their concentrations is of great importance in geology. Electron probe microanalysis has the advantages of non-destructive testing and high spatial resolution; however, it is a challenge to improve the accuracy and precision of trace element detection using this method. The important factors affecting accuracy include the fragility of quartz lattices at high beam currents and the methods used to determine the background. In this paper, the peaks of Al-Kα and Ti-Kα, and their backgrounds, were found to exhibit intensity variations at high beam currents and small beam diameters; therefore, it is necessary to select a large beam diameter (up to 20 µm) to avoid variations in intensity at high currents (500 nA). For background determination of Al, a multipoint background method is proposed to determine the background value, which greatly improves the accuracy of the results. For Ti, the choice of background measurement does not affect the result. In addition, it is verified that the background obtained from other quartz samples can be used as the background of an unknown quartz sample, which reduces the analysis time and minimizes sample damage.

Type
Materials Science Applications
Copyright
Copyright © Microscopy Society of America 2019 

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References

Audétat, A (2013). Origin of Ti-rich rims in quartz phenocrysts from the Upper Bandelier Tuff and the Tunnel Spring Tuff, southwestern USA. Chem Geol 360–361, 99104.Google Scholar
Audétat, A, Garbe-Schönberg, D, Kronz, A, Pettke, T, Rusk, B, Donovan, JJ & Lowers, HA (2015). Characterisation of a natural quartz crystal as a reference material for microanalytical determination of Ti, Al, Li, Fe, Mn, Ga and Ge. Geostand Geoanal Res 39, 171184.Google Scholar
Batanova, VG, Sobolev, AV & Kuzmin, DV (2015). Trace element analysis of olivine: High precision analytical method for JEOL JXA-8230 electron probe microanalyser. Chem Geol 419, 149157.Google Scholar
Borisova, AY, Zagrtdenov, NR, Toplis, MJ, Donovan, JJ, Llovet, X, Asimow, PD, De Parseval, P & Gouy, S (2018). Secondary fluorescence effects in microbeam analysis and their impacts on geospeedometry and geothermometry. Chem Geol 490, 2229.Google Scholar
Breiter, K, Svojtka, M, Ackerman, L & Švecová, K (2012). Trace element composition of quartz from the Variscan Altenberg–Teplice caldera (Krušné hory/Erzgebirge Mts, Czech Republic/Germany): Insights into the volcano-plutonic complex evolution. Chem Geol 326–327, 3650.Google Scholar
Cruz-Uribe, AM, Mertz-Kraus, R, Zack, T, Feineman, MD, Woods, G & Jacob, DE (2017). A new LA-ICP-MS method for Ti in quartz: Implications and application to high pressure rutile-quartz veins from the Czech Erzgebirge. Geostand Geoanal Res 41, 2940.Google Scholar
Donovan, JJ, Lowers, HA & Rusk, BG (2011). Improved electron probe microanalysis of trace elements in quartz. Am Mineral 96, 274282.Google Scholar
Donovan, JJ, Singer, JW & Armstrong, JT (2016). A new EPMA method for fast trace element analysis in simple matrices. Am Mineral 101, 18391853.Google Scholar
Drivenes, K, Larsen, RB, Müller, A & Sørensen, BE (2016). Crystallization and uplift path of late Variscan granites evidenced by quartz chemistry and fluid inclusions: Example from the Land's End granite, SW England. Lithos 252–253, 5775.Google Scholar
Fournelle, J (2007). The problem of secondary fluorescence in EPMA in the application of the Ti-in-zircon geothermometer and the utility of PENEPMA Monte Carlo Program. Microsc Microanal 13(Suppl 2), 13901391.Google Scholar
Frelinger, SN, Ledvina, MD, Kyle, JR & Zhao, D (2015). Scanning electron microscopy cathodoluminescence of quartz: Principles, techniques and applications in ore geology. Ore Geol Rev 65, 840852.Google Scholar
Garate-Olave, I, Müller, A, Roda-Robles, E, Gil-Crespo, PP & Pesquera, A (2017). Extreme fractionation in a granite–pegmatite system documented by quartz chemistry: The case study of Tres Arroyos (Central Iberian Zone, Spain). Lithos 286, 162174.Google Scholar
Goemann, K, Vasyukova, OV, Kamenetsky, VS, Rae, CMM & Wilson, NC (2014). Determination of trace elements in quartz by combined EPMA and CL microspectrometry. Microsc Microanal 20, 718719.Google Scholar
Jercinovic, MJ & Williams, ML (2005). Analytical perils (and progress) in electron microprobe trace element analysis applied to geochronology: Background acquisition, interferences, and beam irradiation effects. Am Mineral 90, 526546.Google Scholar
Jercinovic, MJ, Williams, ML, Allaz, J & Donovan, JJ (2012). Trace analysis in EPMA. IOP Conference Series-Materials Science and Engineering 32, p. 1–22.Google Scholar
Jercinovic, MJ, Williams, ML & Lane, ED (2008). In-situ trace element analysis of monazite and other fine-grained accessory minerals by EPMA. Chem Geol 254, 197215.Google Scholar
Kronz, A, Van Den KERKHOF, AM & Müller, A, 2012. Analysis of low element concentrations in quartz by electron microprobe. In Quartz: Deposits, Mineralogy and Analytics, Götze, J. & Möckel, R. (Eds.), pp. 191217. Berlin, Heidelberg: Springer.Google Scholar
Larsen, RB, Henderson, I, Ihlen, PM & Jacamon, F (2004). Distribution and petrogenetic behaviour of trace elements in granitic pegmatite quartz from South Norway. Contrib Mineral Petrol 147, 615628.Google Scholar
Larsen, RB, Jacamon, F & Kronz, A (2009). Trace element chemistry and textures of quartz during the magmatic hydrothermal transition of Oslo Rift granites. Mineral Mag 73, 691707.Google Scholar
Llovet, X & Salvat, F (2017). PENEPMA: A Monte Carlo program for the simulation of X-ray emission in electron probe microanalysis. Microsc Microanal 23, 634646.Google Scholar
Müller, A, Herrington, R, Armstrong, R, Seltmann, R, Kirwin, DJ, Stenina, NG & Kronz, A (2010). Trace elements and cathodoluminescence of quartz in stockwork veins of Mongolian porphyry-style deposits. Miner Deposita 45, 707727.Google Scholar
Müller, A, Ihlen, PM, Snook, B, Larsen, RB, Flem, B, Bingen, B & Williamson, BJ (2015). The chemistry of quartz in granitic pegmatites of southern Norway: Petrogenetic and economic implications. Econ Geol 110, 17371757.Google Scholar
Müller, A, René, M, Behr, HJ & Kronz, A (2003a). Trace elements and cathodoluminescence of igneous quartz in topaz granites from the Hub Stock (Slavkovský Les Mts., Czech Republic). Miner Petrol 79, 167191.Google Scholar
Müller, A, Wiedenbeck, M, Van Den Kerkhof, AM, Kronz, A & Simon, K (2003b). Trace elements in quartz—a combined electron microprobe, secondary ion mass spectrometry, laser-ablation ICP-MS, and cathodoluminescence study. Eur J Mineral 15, 747763.Google Scholar
Reed, SJB (2000). Quantitative trace analysis by wavelength-dispersive EPMA. Microchim Acta 132, 145151.Google Scholar
Rusk, B, Koenig, A & Lowers, H (2011). Visualizing trace element distribution in quartz using cathodoluminescence, electron microprobe, and laser ablation-inductively coupled plasma-mass spectrometry. Am Mineral 96, 703708.Google Scholar
Rusk, BG, Lowers, HA & Reed, MH (2008). Trace elements in hydrothermal quartz: Relationships to cathodoluminescent textures and insights into vein formation. Geology 36, 547550.Google Scholar
Tanner, D, Henley, RW, Mavrogenes, JA & Holden, P (2013). Combining in situ isotopic, trace element and textural analyses of quartz from four magmatic-hydrothermal ore deposits. Contrib Mineral Petr 166, 11191142.Google Scholar
Van Den Kerkhof, AM, Kronz, A, Simon, K & Scherer, T (2004). Fluid-controlled quartz recovery in granulite as revealed by cathodoluminescence and trace element analysis (Bamble sector, Norway). Contrib Mineral Petr 146, 637652.Google Scholar
Wark, DA & Watson, EB (2006). Titaniq: A titanium-in-quartz geothermometer. Contrib Mineral Petr 152, 743754.Google Scholar
Wiebe, RA, Wark, DA & Hawkins, DP (2007). Insights from quartz cathodoluminescence zoning into crystallization of the Vinalhaven granite, coastal Maine. Contrib Mineral Petr 154, 439453.Google Scholar
Zhang, RX & Yang, SY (2016). A mathematical model for determining carbon coating thickness and its application in electron probe microanalysis. Microsc Microanal 22, 13741380.Google Scholar