Laser-Assisted APT of Deformed Minerals 405
the sample that is analyzed. This may be achieved by corre- lating electron backscattered diffraction (EBSD) and/or transmission Kikuchi diffraction (TKD) (Trimby, 2012) with APT. In this paper, we focus on the influence of APT analysis
parameters (laser pulse energy and frequency, base tem- perature) on the overall data quality and mass spectrum thermal tail. We discuss the important topic of ion identifi- cation in the APT mass spectrum and assess the Pb and U detection and quantification limits for two different zircons. Finally, we present a correlative EBSD, TKD, and APT approach for the study of trace element mobility in deformed zircons.
MATERIALS ANDMETHODS
The zircons used in this study come from two different regions: plastically deformed Archean zircons (~2.5Ga old) from the Napier complex in Antarctica and younger zircons from a decimeter wide high strain zone developed on the island of Krossey within the Bergen Arc of southwest Norway (age range ~760–405 Ma). The Archean zircons, namely DN5 and DN77 contain ~2,000ppma U, ~600ppma Pb, and ~150ppma U, ~60ppma Pb, respectively. In con- trast, those from the Bergen Arc contain ~10ppma U and ~1 ppma Pb. Supplementary Table 1 presents U, Pb, and Th composition measured by SIMS for the Krossey sample and by SHRIMP for DN5 and DN77.
Supplementary Table 1
Supplementary Table 1 can be found online. Please visit
journals.cambridge.org/jid_MAM The general microstructure of the zircons was char-
acterized using combined EBSD and energy dispersive X-ray spectroscopy (Oxford Instrument Aztec) in a Zeiss Ultra Plus field emission gun (FEG; Zeiss) scanning electron microscope (SEM). Thin sections of the samples (DN5, Krossey, and DN77) were mechanically polished down to 1 μm, and subsequently mechano-chemically polished using colloidal silica to allowEBSD analysis. The thin sections were coated with ~5–10nm carbon. Regions of interest (low-angle boundaries with small misorientations, <4°) were then selected based on the EBSD deformation maps. APT samples were prepared using a Zeiss-Auriga focused ion beam SEM (FIB-SEM) equipped with a Kleindiek micromanipulator system (Kleindiek). Bars of selected areas were lifted-out from milled cross-sections using the micromanipulator. Samples were milled from these bars, attached to electro- polished molybdenum grids and finally milled to form APT tips with a typical diameter of around 60nm (Felfer et al., 2012). The final ion beam milling step was carried out at low energies (typically 5 kV) in order to minimize Ga-implantation and damage. In cases where carbon contamination was an issue, the SEM chamber was plasma
cleaned for ~5min before TKD analyses using an on-chamber plasma cleaner (Evactron Zephyr; XEI Scientific). The defor- mation structures within each APT tip were analyzed in the FIB-SEM using TKD after the final annular milling. The APT experiments were conducted on a Cameca LEAP 4000× SiTM (Cameca) atom probe equipped with a picosecond-pulse ultraviolet laser (355nm, spot size <4 μm). The data were reconstructed using the Cameca IVAS 3.6.6 software.
RESULTS AND DISCUSSION
Effect of Laser Energy The influence of laser energy on the mass spectra quality was investigated to determine the optimum laser energy for zircon, as an example of a typicalmineral. A single tip of the Krossey zircon was used and the laser energy was progres- sively increased from 25 to 700 pJ. This experiment was carried out at a base temperature of 60 K, a laser pulse repetition rate of 250 kHz and an evaporation rate of 1%. A total of 1 million atoms per laser energy condition were collected. It is important to note that several factors such as tip radius and voltage are changing with laser energy increase. The tip radius is increasing slightly after each million atoms collected. The interaction volume with the laser becomes greater improving the thermal conductivity at the apex. However, this effect is thought to be minimal due to the small volume evaporated between each laser energy. The thermal tails are equally important for most of the spe- cies in the mass spectra. Their evolution with changing analysis parameters also follows exactly the same trend. We have arbitrarily chosen to show the thermal tails evolution for ZrO and SiO2. Figure 1a shows the mass spectra of the ZrO2+ and SiO2
+
peaks for data collected at different laser pulse energies. Laser-assisted field ionization is a thermal process inducing local heating of the tip, which in turn provokes a broadening of the peak tail (Vurpillot et al., 2009). The extent of the tail broadening (thermal tail) is function of the local heating intensity and tip cooling rate. The thermal tail after each peak only slightly increases
with increasing laser energy. We therefore conclude that the local heating of the tip due to the laser pulse is minimal, with only a limited effect on the extent of the tail behind each peak. It shows that mineral zircon has a sufficiently high thermal diffusivity and fast cooling rate when exposed to the picosecondUVlaser. The temperature conductivity of zircon was reported to have only a minimal dependency on temperature above 300–400K (Kingery et al., 1954). This explains the relatively fast thermal diffusivity of the zircons at high laser energy. The mass resolving power (mass resolution of a specific peak) in APT is usually measured as full-width half maximum (FWHM) and full-width tenth maximum (FWTM) on a peak around 30Da (Larson et al., 2013). The FWHM and FWTM measured at 32Da (O2
+)
increases with increasing laser energy and reaches a plateau from ~400 pJ with FWHM ~780 and FWTM ~320.
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