10.01.2013 Views

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

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

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

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

Concentration (ppm)<br />

148<br />

146<br />

144<br />

142<br />

140<br />

138<br />

Integration Start<br />

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

320<br />

Zn<br />

Integration End<br />

2 4 6 8 10 12 14 16 18 20<br />

Time (s)<br />

The ideal output (i.e., complete absence of fractionation)<br />

would be a flat l<strong>in</strong>e (∆C/∆t = 0) where <strong>the</strong><br />

concentration (C) <strong>in</strong> each of <strong>the</strong> 10 slices is <strong>the</strong><br />

same. Additional plots also display <strong>the</strong> standard/<br />

element signal ratios. The signal ratio plots show<br />

<strong>the</strong> stability (or lack <strong>the</strong>reof) of <strong>the</strong> <strong>in</strong>tensity ratios<br />

dur<strong>in</strong>g <strong>the</strong> analysis.<br />

FLUID INCLUSION ANALYSIS AND DATA<br />

REDUCTION<br />

The logical steps followed dur<strong>in</strong>g analysis of<br />

fluid and melt <strong>in</strong>clusions are shown <strong>in</strong> Figure A5-4.<br />

The analysis of fluid or melt <strong>in</strong>clusions starts with<br />

detailed petrographic exam<strong>in</strong>ation of each sample to<br />

determ<strong>in</strong>e <strong>the</strong> relationship of <strong>the</strong> <strong>in</strong>clusions to <strong>the</strong><br />

FIG. A5-3. Fractionation<br />

plot produced by<br />

AMS show<strong>in</strong>g <strong>the</strong><br />

concentration of z<strong>in</strong>c<br />

as a function of time<br />

<strong>in</strong> <strong>the</strong> signal region of<br />

<strong>in</strong>terest.<br />

host m<strong>in</strong>eral phase and to <strong>the</strong> petrogenesis of <strong>the</strong><br />

sample (Bodnar 2003, Bodnar & Student 2006)<br />

(Fig. A5-4, box 1). After <strong>the</strong> fluid <strong>in</strong>clusions have<br />

been selected, <strong>the</strong> freez<strong>in</strong>g po<strong>in</strong>t depression or <strong>the</strong><br />

halite disappearance temperature of <strong>the</strong> <strong>in</strong>clusions is<br />

determ<strong>in</strong>ed by micro<strong>the</strong>rmometry (Fig. A5-4, box<br />

2). These temperatures are entered <strong>in</strong>to AMS,<br />

which <strong>the</strong>n uses published algorithms (Bodnar<br />

1993, Bodnar et al. 1989, Sterner et al. 1988) to<br />

calculate an NaCl-equivalent bulk sal<strong>in</strong>ity of <strong>the</strong><br />

<strong>in</strong>clusion (Fig. A5-4, box 3). The bulk sal<strong>in</strong>ity of<br />

<strong>the</strong> <strong>in</strong>clusion, <strong>in</strong> conjunction with elemental<br />

concentration ratios determ<strong>in</strong>ed by LA–ICP–MS<br />

analysis, is used to calculate <strong>the</strong> absolute element<br />

concentrations <strong>in</strong> <strong>the</strong> <strong>in</strong>clusion.<br />

1 8 12 15<br />

Petrography MI MI (Host Correction) Mixed (Host + MI signal)<br />

2<br />

FI Micro<strong>the</strong>rmometry<br />

(Tm, ice :Td,halite )<br />

3<br />

Bulk Sal<strong>in</strong>ity (NaCl eq.)<br />

4<br />

LA-ICP-MS Integrated Signal<br />

5<br />

Element Ratio (K/Na, Mg/Na, etc.<br />

NaCl eq = NaCl + KCl + MgCl + ...<br />

6<br />

Drift Correction<br />

7<br />

Absolute Element Conc.<br />

9<br />

Exposed MI<br />

10<br />

LA-ICP-MS Integrated Signal<br />

11<br />

Element Ratio (Si/Ca, Na/Ca, etc. )<br />

�<br />

Element conc. recast as:<br />

Oxides<br />

Carbonates<br />

Sulfides<br />

or<br />

pure MI<br />

signal<br />

= 100 %<br />

Element Ratios + EMPA conc. of one elem.<br />

13<br />

Host Only<br />

LA-ICP-MS<br />

Integrated Signal<br />

14<br />

Host Element Conc.<br />

16<br />

Mixed LA-ICP-MS Integrated signal)<br />

17<br />

Element Ratio (Si/Ca, Na/Ca, etc. )<br />

�<br />

Element conc. recast as:<br />

Oxides<br />

= 100 %<br />

Carbonates<br />

Sulfides<br />

18<br />

Mixed Element Conc.<br />

19<br />

Known Elem. Conc.<br />

e.g. Al <strong>in</strong> Host/MI<br />

20<br />

Proportionally<br />

allocate mix<br />

concentration us<strong>in</strong>g<br />

Al conc.<br />

FIG. A5-4. Flow chart show<strong>in</strong>g <strong>the</strong> sequence of tasks <strong>in</strong>volved <strong>in</strong> <strong>the</strong> analysis and data reduction for fluid and melt <strong>in</strong>clusions<br />

us<strong>in</strong>g AMS software.

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!