Open Access
Annexe A
Operating conditions for the LA-ICP-MS equipment for cassiterite analyses.
Protocole analytique LA-ICP-MS pour la cassitérite.
Laboratory & Sample Preparation | |
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Laboratory name | Géosciences Rennes, UMR CNRS 6118, Rennes, France |
Sample type/mineral | Cassiterite |
Sample preparation | In-context in thin-section and thick-section |
Imaging | CL: Relion CL instrument, Olympus Microscope and Leica Color Camera |
Laser ablation system | |
Make, Model & type | ESI NWR193UC, Excimer |
Ablation cell | ESI NWR TwoVol2 |
Laser wavelength | 193 nm |
Pulse width | < 5 ns |
Fluence | 6 J/cm2 |
Repetition rate | 5 Hz |
Spot size | 50 µm |
Sampling mode/pattern | Single spot |
Carrier gas | 100% He, Ar make-up gas and N2 (3 ml/mn) combined using in-house smoothing device |
Background collection | 20 s |
Ablation duration | 60 s |
Wash-out delay | 15 s |
Cell carrier gas flow (He) | 0.76 l/min |
ICP-MS Instrument | |
Make, Model & type | Agilent 7700x, Q-ICP-MS |
Sample introduction | Via conventional tubing |
RF power | 1350 W |
Sampler, skimmer cones | Ni |
Extraction lenses | X type |
Make-up gas flow (Ar) | 0.85 l/min |
Detection system | Single collector secondary electron multiplier |
Data acquisition protocol | Time-resolved analysis |
Scanning mode | Peak hopping, one point per peak |
Detector mode | Pulse counting, dead time correction applied, and analog mode when signal intensity>∼ 106 cps |
Masses measured | 204(Hg + Pb), 206Pb, 207Pb, 208Pb, 232Th, 238U |
Integration time per peak | 10–30 ms |
Sensitivity / Efficiency | 23 000 cps/ppm Pb (50 μm, 10 Hz) |
Data Processing | |
Gas blank | 20 s on-peak |
Calibration strategy | Phalaborwa Baddeleyite used as primary reference materials, Abbaretz Cassiterite used as secondary reference material (quality control) |
Common-Pb correction, composition and uncertainty | No common-Pb correction. |
Reference Material info | Phalaborwa (Heaman and Lecheminant, 1993) Abbaretz Cassiterite (in-house) |
Data processing package used | Iolite 4 (Paton et al., 2011), U-Pb Geochronology (Paton et al., 2010) |
Uncertainty level and propagation | Ages are quoted at 2 sigma absolute, propagation is by quadratic addition according to Horstwood et al. (2016). |
Quality control/Validation | Abbaretz: 324.5 ± 6.5 Ma (n = 25 ; MSWD = 3.1) |
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