Other
Scientific paper
Sep 2002
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002gecoa..66.2855w&link_type=abstract
Geochimica et Cosmochimica Acta, vol. 66, Issue 16, pp.2855-2863
Other
6
Scientific paper
Laser sulfur combustion in the presence of O 2 is the most commonly used method of in situ sulfur isotope analysis. Previous workers indicated that a small but reproducible fractionation of 34 S/ 32 S exists between the product SO 2 gas and the mineral. The magnitude of this fractionation varies with bond strength, as reflected in Gibbs free energy of formation at 298.15K. The correction factors are known for common sulfides and anhydrite but not, hitherto, for stibnite and the sulfosalt minerals, which are important constituents of many classes of ore deposits. We present the correction factors for the following chemically and crystallographically well-characterized minerals: stibnite (weighted MEAN = -1.2 ), bournonite (+0.6 ), tetrahedrite (+1.3 ), and boulangerite (+1.4 ). The Gibbs free energies of formation of these phases have been approximated by the sulfide summation method, and the correlation of G 298 0 with the correction factor for the sulfosalts fits well with the trend previously established for simple sulfides. There is an excellent correlation between the fractionation factor and mineral composition, a parameter that does result in bond strength variations (e.g., mol fraction of PbS in sulfosalts), allowing estimation of the correction factors for simple intermediate compositions. Finally, bond strength also varies with variation in interatomic distances, and we have, therefore, investigated the behaviour of stibnite, a strongly anisotropic mineral. Our results indicate that there is a significant variation in fractionation factor, depending on crystal orientation. The fractionation factor along the prismatic b-axis, which displays the strongest chemical bonds (as monitored by the shortest bond lengths), is more negative (-1.7 ) than along the other crystallographic directions (-0.7 to -1.0 ), which is in full agreement with theoretical predictions. We demonstrate the application of the technique in unravelling source- and process-related sulfur isotope systematics in two hydrothermal vein systems in the classic mining area of the NE Rhenish Massif, both studies requiring resolution beyond the scale of conventional sulfur isotope analysis.
Boyce Adrian J.
Fallick Anthony E.
Wagner Thomas
No associations
LandOfFree
Laser combustion analysis of 34 S of sulfosalt minerals: determination of the fractionation systematics and some crystal-chemical considerations does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.
If you have personal experience with Laser combustion analysis of 34 S of sulfosalt minerals: determination of the fractionation systematics and some crystal-chemical considerations, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Laser combustion analysis of 34 S of sulfosalt minerals: determination of the fractionation systematics and some crystal-chemical considerations will most certainly appreciate the feedback.
Profile ID: LFWR-SCP-O-1047288