Services and Applications
GLITTER provides the first real-time interactive data reduction for LAM-ICPMS analysis; it allows inspection and evaluation of each result before the next analysis spot is chosen.
GLITTER enables rapid selection of the best intervals for background and signal measurement. Time-resolved data for each analyte mass are displayed in a unique pixel-row display to allow quick recognition of inclusions and data spikes. Results in tables and plots change automatically when different integration intervals are selected.
With online analysis it provides calculation of the results for each analysis during the run. The first results are calculated as soon as one standard and one sample have been analysed. With each additional standard analysis, the data are instantaneously adjusted to take account of changes in the analytical conditions such as instrumental drift; no off-line reprocessing is required.
GLITTER also provides a variety of plotting and diagnostic options allowing the user to evaluate the quality and significance of each analysis during the run.
LAM-ICPMS in the Geosciences: Potential and limitations
The laser-ablation ICPMS microprobe (LAM-ICPMS) was introduced more than ten years ago, largely through the work of geologists (especially the group at Memorial University, Newfoundland), and is now becoming an important technology. The capability for rapid, sensitive, spatially-resolved in-situ trace-element analysis will have the same impact on the geosciences (and material sciences) as the spread of the electron microprobe (EMP) did in the 1970s. Today the EMP is found in nearly every significant geoscience laboratory in the world (academic, government, industry, commercial laboratories). An equivalent market potential exists for a well-designed, effective LAM-ICPMS.
The development of on-line, real-time data reduction was a major factor in the rapid spread of EMP laboratories in the 1970s. It enabled the user to view the results of an analysis within seconds of data acquisition, and to use that in put to guide further analytical strategy. Compared with the off-line data reduction available previously, this meant a great increase in productivity, flexibility and applicability. This interactive analytical environment is now taken for granted in EMP work.
A similar interactive environment has not been available for the LAM-ICPMS. To meet this need, GEMOC has now developed GLITTER, the GEMOC Laser ICPMS Total Trace Element Reduction software package. This new interactive program gives users of the laser ablation microprobe a unique analytical environment. It provides real-time on-line data reduction for the LAM-ICPMS, and features linked graphics and analysis tables, greatly improving both productivity and the flexibility of analysis. A variety of plotting options allows the user to evaluate the quality and significance of each analysis during the run, and to dynamically change the focus of the session if required.
GLITTER is written in the IDL programming language and provides cross-platform support for a number of environments, including Windows, MacOS, and Unix. The current release supports the Perkin Elmer ELAN 5100, 6000, 6100 and HP4500, Agilent 7500, Micromass, ThermoFinnigan Element, ThermoFinnigan Element II and VG-PQ2, utilising the time-resolved data output option. It can be readily adapted to other LA-ICPMS systems which can produce time-resolved signals.
GLITTER is currently compatible with the following ICP-MS instruments:
- Agilent Instruments running ChemStation or MassHunter, including MS/MS Models
- Thermo iCap Instruments (QTegra software), Element II/XR (.FIN2)
- Finnigan ME
- Nu AttoM, Plasma (PlasmaLab1, PlasmaLab2)
- Analytic Jena
If your ICP-MS instrument is not listed here, please contact us for information about adapting GLITTER to your systems. We are always interested in developing compatibility with new platforms as they become available.
U-Pb Dating of Zircons
GEMOC has developed an analytical protocol for the in situ dating of zircons by laser ablation ICP-MS using the U-Pb isotopic system (see "Analytical Methods". GLITTER allows the rapid reduction of these data, calculating age estimates from isotopic ratios and plotting a concordia diagram (see example below). Data are displayed as single isotopes or as isotope ratios in the "Review" window, and isotope ratios, age estimates and one sigma uncertainty estimates (ratios and ages) can be displayed in the table and exported to an ASCII text file. Further details and applications are included in (Jackson, S.E., 2001.;Knudsen, T.-L. et al., 2000. and Belousova, E.A. et al., 2001).
An example of the Concordia diagram in the
"Plot" window. Age estimates are viewed graphically
by plotting 208Pb/238U vs 207Pb/235U.
The curve represents the concordia and fixed ages (in units of
billions of years (Ga) are plotted as the purple asterisk symbols.
The data points (green crosses) in this particular dataset show
distinct age populations from 450 to 1750 Ma, with evidence of
Pb loss extending from the 1750
Ma population. Each data point is plotted on the concordia diagram within seconds of data acquisition, and discordant points can therefore be identified quickly and easily.
The Review window is shown below. It illustrates defining signal markers based on a plot of 207Pb/206Pb isotope ratios.
GLITTER: An Overview
GLITTER consists of five main interactive user interfaces ("windows"):
- The GLITTER "Main Window", containing the main menu options and the table of results.
- The "Standards" window, calling for the user to input the identity and values of the internal standard.
- The "Review" window, where the time-resolved laser signals are viewed and integration intervals are selected by the user.
- The "Plot" window(s), where data are visualised in various ways.
- The "Options" window, where the user can control the yield interpolation options, background fitting, magnitude of uncertainty estimates etc.
The "GLITTER", "Review" and "Plot" windows typically remain on the screen during a session, whereas "Standards" and "Options" only appears when needed or when called by the user. The size of datasets is unrestricted. Movement within a dataset also is unrestricted and all windows are dynamically linked. This means that:
- If marker positions are changed in the "Review" window, the table of results and all dataplots on the screen at the time are automatically updated to reflect these changes.
- The selected (highlighted) analysis number in "GLITTER" is also the selected analysis number in "Review" and "Plot", and vice versa.
Data can be written to disk as ASCII text at any time, for further off-line analysis in spreadsheet programs.
The main GLITTER window
The main GLITTER window is the front-end of the program from which all other operations are carried out. It also contains a table which can display various results, including trace element concentrations, one sigma uncertainty, detection limits, raw counts data etc. In "Isotope-ratio" mode, GLITTER displays the isotope ratios of interest (for example 207Pb/206Pb) as well as the age estimates (in Ma) calculated from the various ratios for each analysis.
When the dataset is first loaded the "Standards" window appears automatically and prompts the user to identify the internal standard and enter the values in the table provided. Internal standards can be changed at any time during the session. Up to three isotopes can be used as internal standards, and are chosen from droplists. Compositions of reference materials (such as the NIST 612 glass in the example below) are held in GLITTER's data library.
GLITTER selects a default set of integration intervals for the background, and signal, counts; these can be changed interactively by the user at any time in the "Review" window.
Analysis labels are displayed on the left and the time-resolved laser ablation signals on the right. The top pixelmap display shows all isotopes for the selected analysis (each row of pixels = one isotope), with colour representing signal intensity (blue represents low signal, yellow represents high signal). The bottom display shows the signal for a particular isotope (in this case47Ti) selected using the horizontal green marker in the pixelmap display. Integration intervals are selected by dragging the four vertical markers. The framed area at the bottom of the window contains context-sensitive on-line help.
Results can be viewed graphically in the "Plot" window(s) as:
- Chondrite-normalised plots, with a choice of trace-element order (as in the example below)
- X-Y scatter plots
- Run quality control data (drift, ablation rates, detection limits, backgrounds etc.)
- Concordia plots (for U-Pb dating)
The user has control over various aspects of the data reduction process, selected via the "Options" window. This includes:
- The type of yield interpolation to apply across the standard analyses
- Control over the background fitting procedures
- Enabling or disabling the 60s timed-save feature
- The magnitude of the relative uncertainty associated with the internal standard values and standard reference material values
- A fractionation test (useful to measure the relative fractionation between 2 isotopes of the same element, such as 24Mg and 25Mg)
On-line analysis means that the results for each analysis are calculated during the run as data are acquired. The first results are calculated as soon as one standard and one sample have been analysed. With each additional standard analysis, the data are instantaneously adjusted to take account of changes in the analytical conditions such as instrumental drift and no off-line reprocessing is required.
Jackson, S.E., 2001. The application of Nd:YAG lasers in LA-ICP-MS. Principles and Applications of Laser Ablation-Mass Spectrometry in the Earth. Mineralogical Association of Canada Short Course Series 29, 29-46
Knudsen, T.-L. et al., 2000. In situ hafnium and lead isotope analyses of detrital zircons from the Devonian sedimentary basin of NW Greenland: a record of repeated crustal reworking. Contributions to Mineralogy and Petrology, 141, 83-94
Belousova, E.A. et al., 2001. Two age populations of zircons from the Timber Creek kimberlites, Northern Territory, Australia, as determined by laser-ablation ICPMS analysis. Australian Journal of Earth Sciences, in press