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Synthetic fluid inclusions in natural quartz. IV. Chemical analyses of fluid inclusions by SEM/EDA: Evaluation of method

Journal Article · · Geochimica et Cosmochimica Acta; (USA)
 [1]; ;  [2]
  1. Univ. of Michigan, Ann Arbor (USA)
  2. Virginia Polytechnic Institute, Blacksburg (USA)
The compositions of individual synthetic fluid inclusions in the systems NaCl-KCl, NaCl-CaCl{sub 2} and NaCl-KCl-CaCl{sub 2} have been semi-quantitatively determined by energy dispersive analysis of precipitates produced during thermal decrepitation. Inclusions containing known mixtures of 20 wt.% total salinity were synthesized by healing fractures in natural quartz at 600-700{degree}C and 5-7 kbars for 7-10 days. The two-phase, daughter-free inclusions homogenized at 170-250{degree}C, began to decrepitate after about 100{degree} of overheating and by 360-420{degree}C a significant number of decrepitates had formed on the polished surface. Peak heights generated by EDA (raster mode) of these decrepitates were standardized using both single and mixed salt standards evaporated to dryness in a vacuum. Although the mixed salt standards better approximated the decrepitate compositions, difficulties were encountered in producing micron-scale homogeneity and the single salts yielded more reliable results.
OSTI ID:
5152747
Journal Information:
Geochimica et Cosmochimica Acta; (USA), Journal Name: Geochimica et Cosmochimica Acta; (USA) Vol. 52:5; ISSN GCACA; ISSN 0016-7037
Country of Publication:
United States
Language:
English