The crystal structure of 45 tourmalines containing trivalent cations (Me3+: Cr3+, V3+, Fe3+) and 43 tourmalines containing divalent cations (Me2+: Fe2+, Mn2+, Co2+, Ni2+, Cu2+) of 3d elements were analysed. We establish that the incorporation of Me3+ cations is controlled by the ratio between the sizes of YO6 and ZO6 octahedra and does not exceed eight atoms per formula unit (apfu), while the incorporation of Me2+ cations is controlled by the charge balance and does not exceed 3 apfu. We prove that there are no structural constraints controlling the incorporation of Co, Ni and Cu cations into the tourmaline structure at concentrations of up to 1 apfu. We show that, when the limiting content (less or equal to 1 apfu and 1.6 apfu for divalent and trivalent cations, respectively) is reached, these cations start to occupy not only YO6, but also ZO6 octahedra, to maintain stability of the crystal structure. As the content of 3d-element cations increases further, the degree of disorder grows and, at a content of ~7 apfu, their distribution is close to statistical. An increase in the content of 3d cations, accompanied by their disordering, causes a decrease in disparity between sizes of YO6 and ZO6 octahedra and their deformations.
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Research Article|
September 01, 2018
Incorporation of 3d elements in tourmalines: structural adjustments and stability
Oleg S. Vereshchagin;
1
Institute of Earth Science, Saint Petersburg State University, Universitetskaya nab. 7/9
, Saint Petersburg199034, Russia
Corresponding author, e-mail: [email protected]
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Olga V. Frank-Kamenetskaya;
Olga V. Frank-Kamenetskaya
1
Institute of Earth Science, Saint Petersburg State University, Universitetskaya nab. 7/9
, Saint Petersburg199034, Russia
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Ira V. Rozhdestvenskaya;
Ira V. Rozhdestvenskaya
1
Institute of Earth Science, Saint Petersburg State University, Universitetskaya nab. 7/9
, Saint Petersburg199034, Russia
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Anatoly A. Zolotarev
Anatoly A. Zolotarev
1
Institute of Earth Science, Saint Petersburg State University, Universitetskaya nab. 7/9
, Saint Petersburg199034, Russia
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1
Institute of Earth Science, Saint Petersburg State University, Universitetskaya nab. 7/9
, Saint Petersburg199034, Russia
Olga V. Frank-Kamenetskaya
1
Institute of Earth Science, Saint Petersburg State University, Universitetskaya nab. 7/9
, Saint Petersburg199034, Russia
Ira V. Rozhdestvenskaya
1
Institute of Earth Science, Saint Petersburg State University, Universitetskaya nab. 7/9
, Saint Petersburg199034, Russia
Anatoly A. Zolotarev
1
Institute of Earth Science, Saint Petersburg State University, Universitetskaya nab. 7/9
, Saint Petersburg199034, Russia
Corresponding author, e-mail: [email protected]
Publisher: Deutsche Mineralogische Gesellschaft, Sociedad Española de Mineralogia, Societá Italiana di Mineralogia e Petrologia, Société Francaise de Minéralogie
Received:
09 Jan 2017
Revision Received:
04 Dec 2017
Accepted:
18 May 2018
First Online:
05 Nov 2018
Online ISSN: 1617-4011
Print ISSN: 0935-1221
© 2018 E. Schweizerbart’sche Verlagsbuchhandlung, 70176 Stuttgart, Germany
European Journal of Mineralogy (2018) 30 (5): 917–928.
Article history
Received:
09 Jan 2017
Revision Received:
04 Dec 2017
Accepted:
18 May 2018
First Online:
05 Nov 2018
Citation
Oleg S. Vereshchagin, Olga V. Frank-Kamenetskaya, Ira V. Rozhdestvenskaya, Anatoly A. Zolotarev; Incorporation of 3d elements in tourmalines: structural adjustments and stability. European Journal of Mineralogy 2018;; 30 (5): 917–928. doi: https://doi.org/10.1127/ejm/2018/0030-2781
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