Tetrahedral substitutions in tourmaline

Author(s)
Andreas Ertl, Darell J. Henry, Ekkehart Tillmanns
Abstract

The Si4+ cation, typically the overwhelming occupant of the tetrahedral site of the tourmaline structure, can be partially replaced by Al3+, B3+, and Be2+. Tetrahedrally coordinated Al (up to ~0.9 [4]Al atom per formula unit, apfu) has been found in different Mg- and/or Fe2+-rich tourmalines from high-temperature aluminous lithologies as well as in Li-rich pegmatites. It is relatively common for Li- and [4]Al-bearing tourmalines to also contain some [4]B. While the highest boron content (~0.8 [4]B apfu) in a natural tourmaline was found in an Al-rich tourmaline (olenite) from the Eastern Alps, Austria, much higher contents of up to ~2.8 apfu have been reported for synthetic Al-rich tourmalines. Natural tourmalines with a higher total Al content (> 7.2 Al apfu) can also contain significant [4]B. The highest verified beryllium content in a tourmaline is still below 100 ppm, but current data show that in pegmatitic tourmaline crystals the Be content is positively correlated with the overall Al content. Therefore Li-rich tourmalines can contain higher Be contents in pegmatites that originated from differentiated granitic magma, than in pegmatites that have evolved as granitic pegmatitic melts from the surrounding country-rocks during decompression.

Organisation(s)
Department of Mineralogy and Crystallography
External organisation(s)
Louisiana State University, Naturhistorisches Museum Wien (NHM)
Journal
European Journal of Mineralogy: an international journal of mineralogy, geochemistry and related sciences
Volume
30
Pages
465-470
No. of pages
6
ISSN
0935-1221
DOI
https://doi.org/10.1127/ejm/2018/0030-2732
Publication date
04-2018
Peer reviewed
Yes
Austrian Fields of Science 2012
105116 Mineralogy, 105113 Crystallography, 105120 Petrology
Keywords
ASJC Scopus subject areas
Geochemistry and Petrology
Portal url
https://ucrisportal.univie.ac.at/en/publications/172f8e59-7194-45a8-b52c-9dc1fc54bccf