While the precision of the method cannot rival that of the benchmark isotope dilution thermal ionization mass spectrometry (ID-TIMS), and its spatial resolution cannot easily compete with less destructive secondary ion mass spectrometry (SIMS) techniques, for many applications these drawbacks are outweighed by the low cost and rapid sample throughput achieved by LA-ICPMS, and many research facilities now have in-house laser ablation capabilities. U-(Th)-Pb zircon geochronology by laser ablation inductively coupled plasma mass spectrometry (LA-ICPMS) has seen a dramatic rise in popularity in the last decade.
#IGOR PRO WORKING WITH DATA IN TABLES SOFTWARE#
We present a data reduction module for use with the Iolite software package that implements this methodology and which may provide the means for simpler interlaboratory comparisons and, perhaps most importantly, enable the rapid reduction of large quantities of data with maximum feedback to the user at each stage. We demonstrate that the use of more complex models of elemental fractionation such as exponential curves and smoothed cubic splines can efficiently correct complex fractionation trends, allowing detection of spatial heterogeneities, while simultaneously maintaining data quality. This approach has the versatility to treat data from any laboratory, regardless of the expression of downhole fractionation under any given set of analytical conditions. Here we investigate an alternate approach that aims to reverse the problem by first observing the elemental fractionation response and then applying an appropriate (and often unique) model to the data. A common feature of all these techniques, however, is that they impose an expected model of elemental fractionation behavior thus, any variance in actual fractionation response between laboratories, mineral types, or matrix types cannot be easily accommodated. Alternatively, other methods have been developed which attempt to correct for the effects of downhole elemental fractionation. Several methods have been proposed to minimize the degree of downhole fractionation, typically by rastering or limiting acquisition to relatively short intervals of time, but these compromise minimum target size or the temporal resolution of data.
Elemental fractionation effects during analysis are the most significant impediment to obtaining precise and accurate U-Pb ages by laser ablation ICPMS.
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