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Laser Ablation–ICP–MS in the Earth Sciences ... - Virginia Tech

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<strong>in</strong>clusions by electron microprobe or LA–ICP–MS<br />

to obta<strong>in</strong> concentration values that can be used to<br />

reduce data from <strong>the</strong> rema<strong>in</strong><strong>in</strong>g <strong>in</strong>clusions.<br />

Alternatively, Halter et al. (2002) estimated <strong>the</strong><br />

concentration of one or more elements <strong>in</strong> <strong>the</strong> MI<br />

based on whole rock analysis and assumptions<br />

concern<strong>in</strong>g <strong>the</strong> relationship of <strong>the</strong> MI to <strong>the</strong> bulk<br />

rock composition. In <strong>the</strong> example here, <strong>the</strong><br />

concentration of Al <strong>in</strong> <strong>the</strong> MI is estimated to be<br />

17.26 wt% based on analyses of o<strong>the</strong>r MI <strong>in</strong> <strong>the</strong><br />

same MIA that were exposed at <strong>the</strong> surface. Next,<br />

select <strong>the</strong> “Host Concentrations” tab and <strong>the</strong>n click<br />

on “Use current results” to set <strong>the</strong> host<br />

concentrations – this uses <strong>the</strong> host concentrations<br />

determ<strong>in</strong>ed <strong>in</strong> <strong>the</strong> previous steps.<br />

Based on analyses of homogenized MI <strong>in</strong> this<br />

sample, we know that <strong>the</strong> MI conta<strong>in</strong> about 4 wt%<br />

H2O. Therefore, before analyz<strong>in</strong>g <strong>the</strong> mixed signal<br />

region we return to <strong>the</strong> options w<strong>in</strong>dow (e.g., Figure<br />

A5-5) and enter “96” (ra<strong>the</strong>r than 100) <strong>in</strong> <strong>the</strong> box<br />

S.R. MUTCHLER, L. FEDELE & R.J. BODNAR<br />

326<br />

“Use normalization to” <strong>in</strong> <strong>the</strong> Methods subsection.<br />

The f<strong>in</strong>al step before <strong>the</strong> results can be calculated is<br />

to return to <strong>the</strong> spectra w<strong>in</strong>dow and select <strong>the</strong> mixed<br />

signal region (Fig. A5-10). F<strong>in</strong>ally, click on <strong>the</strong><br />

“Analyze” button to complete <strong>the</strong> analysis. The<br />

results are <strong>the</strong>n displayed <strong>in</strong> <strong>the</strong> results w<strong>in</strong>dow<br />

(Fig. A5-11).<br />

The first eight columns <strong>in</strong> <strong>the</strong> results w<strong>in</strong>dow<br />

(Fig. A5-11) are <strong>the</strong> same as for <strong>the</strong> fluid <strong>in</strong>clusion<br />

analysis, except that <strong>in</strong> column 4, Weight % refers<br />

to weight percent oxide of <strong>the</strong> element.. Column 9<br />

(Mix (ppm)) shows <strong>the</strong> concentration of <strong>the</strong> element<br />

<strong>in</strong> <strong>the</strong> mixed (host + MI) signal. Column 10 (Host<br />

(ppm)) shows <strong>the</strong> concentration of <strong>the</strong> element <strong>in</strong><br />

<strong>the</strong> host. It is important to emphasize that <strong>the</strong><br />

concentrations shown <strong>in</strong> columns 2 to 4 are <strong>the</strong><br />

concentrations corrected for <strong>the</strong> host phase<br />

contribution. The host correction factor (0.53)<br />

<strong>in</strong>dicates that 53% of <strong>the</strong> mixed signal was from <strong>the</strong><br />

melt <strong>in</strong>clusion.<br />

FIG. A5-11. Results w<strong>in</strong>dow show<strong>in</strong>g <strong>the</strong> composition of a buried melt <strong>in</strong>clusion calculated with AMS. See text for<br />

description of each of <strong>the</strong> data columns.

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