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Development of an extended matrix-matched calibration protocol for fast, high-resolution, quantitative chemical mapping of major and trace elements of polymineralic samples by laser-ablation coupled to time-of-flight-mass-spectrometry (LA-ICP-TOF-MS)

Savard Dany, Bédard L. Paul, Barnes Sarah-Jane et Petrus Joseph. (2021). Development of an extended matrix-matched calibration protocol for fast, high-resolution, quantitative chemical mapping of major and trace elements of polymineralic samples by laser-ablation coupled to time-of-flight-mass-spectrometry (LA-ICP-TOF-MS). Dans : Goldschmidt , 4-9 July 2021, Virtual.

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Résumé

In situ analysis conducted by LA-ICP-MS for the determination of trace elements in ore deposit studies provides precious information of chemical composition in a variety of minerals at the micrometer-scale. To date, most laser studies use quadrupole mass spectrometers (ICP-Q-MS) for the analysis of monomineral phases, using static spot (or line ablation), while chemical mapping can reveal important spatial (2D) information, such as growth zoning, exsolutions, micro-veins, micro-inclusions (Fig.1). However, peak jumping mode operation of ICP-Q-MS limits the acquisition speed and spatial resolution. Time-of-flight mass spectrometers (ICP-TOF-MS) can extract full mass range simultaneously at high rate (33,000 Hz), rendering the instrument attractive for routine analysis and allowing to take steps towards new research areas [1]. A new protocol was developed using a 193nm LA-system (RESOnetics, Applied Spectra) attached to an ICP-TOF-MS (TOFWERK) [2] to allow high-resolution quantitative mapping of polymineralic surfaces (Fig.1B-C). Simultaneous quantification of trace and major elements of different minerals (silicates, sulfides, oxides, zircon, apatite, calcite) within a single data processing, and without saturation of the ICP-TOF-MS detector, can be achieved by combining 7 reference materials of varied matrices (glasses, sulfide, apatite, zircon). Based on normalization of major elements without the use of an internal standard, a new data reduction scheme (DRS) was developed for IOLITE v4 software [3]. The DRS can recognize sulfide and calcite to apply appropriate Fe conversion factors or correct for “blind” element (CO2), respectively. Using a 7µm beam in raster mode, a 1mm2 area is covered in about 30 minutes.

Figure.1) Fe-Ti-oxide-apatite mineralisation (Sept-Iles Intrusion, Canada). [A] Reflected light microphotography. [B] LA-ICP-TOF-MS RGB composite image of Cu(red), Pb(blue) and Ni(green) revealing zonation in a pyrite grain in a late calcite-serpentine vein. Maximum intensity scales are Cu(500ppm), Pb(20ppm), Ni(150ppm). [C] Normalized Fe(%) distribution (LA-ICP-TOF-MS). Total map size is 2mm x 0.7mm, resolution is 7µm (28,600 pixels total), acquisition time ~50 minutes.

Type de document:Matériel de conférence (Non spécifié)
Date:6 Juillet 2021
Sujets:Sciences naturelles et génie > Génie
Sciences naturelles et génie > Sciences appliquées
Sciences naturelles et génie > Sciences naturelles > Sciences de la terre (géologie, géographie)
Département, module, service et unité de recherche:Départements et modules > Département des sciences appliquées > Unité d'enseignement en sciences de la Terre
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Déposé le:27 janv. 2023 21:16
Dernière modification:27 janv. 2023 21:16
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