Prd. Mason et al., Determination of incompatible trace elements in mantle clinopyroxenes by LA-ICP-MS: A comparison of analytical performance with established techniques, GEOSTAND N, 23(2), 1999, pp. 157-172
Citations number
35
Categorie Soggetti
Earth Sciences
Journal title
GEOSTANDARDS NEWSLETTER-THE JOURNAL OF GEOSTANDARDS AND GEOANALYSIS
Incompatible trace element abundances have been determined in mantle-derive
d clinopyroxenes by laser ablation-inductively coupled plasma-mass spectrom
etry (LA-ICP-MS) in a comparative study with established microanalytical an
d bulk techniques. Individual clinopyroxene grains were sampled for the las
er ablation study from sieved mineral separate fractions from which similar
mineral grains had been previously extracted for microprobe (SIMS) and bul
k (INAA and ID-TIMS) analysis. Mineral grains were ablated with variable de
grees of surface spatial resolution (50-200 mu m) in order to maximise ICP-
MS analyte count rates and to improve detection limits. A comparison of res
ults from the different techniques reveals that for the most homogeneous sa
mples LA-ICP-MS can achieve excellent levels of agreement with other techni
ques (+/- 10%) and good precision for most of the studied elements (1-5% RS
D). Variations in calculated concentrations by LA-ICP-MS confirm inter- and
intra-mineral heterogeneity determined by SIMS, reflecting changes in samp
le composition and texture. The long-term reproducibility of the technique
is shown by the consistency of results for one sample analysed on thirteen
occasions over a period of nine months.