Abstract
We report here the results of a series of inclusive chemical characterizations, including all elements except oxygen, for a suite of 54 tourmaline samples. A combination of analytical techniques was used to analyze for major and light elements (electron microprobe), Fe3 and Fe2t (Mössbauer spectroscopy), H (U extraction), and B, Li, and F (ion microprobe, or SIMS). The B content of the tourmalines studied ranges from 2.86 to 3.26 B per formula unit (pfu) with 31 anions; excess boron is believed to reside in the Si site. Li ranges from 0.0 to 1.44 Li pfu and F contents are 0.0-0.91 pfu. H contents range from nearly anhydrous up to 3.76 H pfu and do not correlate simply with Fe3t content. Mössbauer results show that tourmaline exhibits the entire range of Fe3+/2Fe from 0.0-1.0. Fe-+ is represented in the spectra by three doublets, with occupancy in at least three distinct types of Y sites (with different types of nearest and next nearest neighbors). Fe3+ was found in 26 of the 54 samples studied. Although Mössbauer data do not allow the distinction between Fe3t and
Cite
CITATION STYLE
Darby Dyar, M. (1998). Inclusive chemical characterization of tourmaline: Mössbauer study of Fe valence and site occupancy. American Mineralogist, 83(7–8), 848–864. https://doi.org/10.2138/am-1998-7-817
Register to see more suggestions
Mendeley helps you to discover research relevant for your work.