MAJOR-ELEMENT RATIOS IN SYNTHETIC FLUID INCLUSIONS BY SYNCHROTRON X-RAY-FLUORESCENCE MICROPROBE

Citation
Da. Vanko et al., MAJOR-ELEMENT RATIOS IN SYNTHETIC FLUID INCLUSIONS BY SYNCHROTRON X-RAY-FLUORESCENCE MICROPROBE, Chemical geology, 109(1-4), 1993, pp. 125-134
Citations number
18
Categorie Soggetti
Geology
Journal title
ISSN journal
00092541
Volume
109
Issue
1-4
Year of publication
1993
Pages
125 - 134
Database
ISI
SICI code
0009-2541(1993)109:1-4<125:MRISFI>2.0.ZU;2-R
Abstract
Individual fluid inclusions in quartz were investigated by synchrotron radiation X-ray fluorescence (SXRF) microprobe to develop protocols f or major-element microanalysis. Studies were conducted of synthetic fl uid inclusions in Brazilian quartz that contain fluids of known NaCl-C aCl2-H2O and KCl-H2O compositions. Inclusions were irradiated by synch rotron X-rays and the resulting energy-dispersive spectra were correct ed for fluorescence yield and absorption effects to obtain Ca/Cl and K /Cl ratios. Results are commonly better than +/- 30% relative to the n ominal ratio. Element ratios obtained by SXRF may be combined with res ults of heating and freezing studies to characterize non-destructively the bulk major-element composition of individual inclusions. Extensio n of the analytical protocol to elements of higher atomic number (e.g. , trace and transition elements) will result in better precision as ab sorption effects and peak overlaps become less problematic.