Research output: Contribution to journal › Article › peer-review
Ln3+ (Ln3+ = La, Nd, Eu, Yb) incorporation in synthetic tourmaline analogues: Towards tourmaline REE pattern explanation. / Vereshchagin, Oleg S.; Britvin, Sergey N. ; Wunder, Bernd; Frank-Kamenetskaya, Olga V. ; Wilke, Franziska; Vlasenko, Natalia S. ; Shilovskikh, Vladimir V. ; Bocharov, Vladimir N. ; Danilov, Denis V. .
In: Chemical Geology, Vol. 584, 120526, 05.12.2021, p. 120526.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - Ln3+ (Ln3+ = La, Nd, Eu, Yb) incorporation in synthetic tourmaline analogues: Towards tourmaline REE pattern explanation
AU - Vereshchagin, Oleg S.
AU - Britvin, Sergey N.
AU - Wunder, Bernd
AU - Frank-Kamenetskaya, Olga V.
AU - Wilke, Franziska
AU - Vlasenko, Natalia S.
AU - Shilovskikh, Vladimir V.
AU - Bocharov, Vladimir N.
AU - Danilov, Denis V.
N1 - Publisher Copyright: © 2021 Elsevier B.V.
PY - 2021/12/5
Y1 - 2021/12/5
N2 - Tourmaline rare-earth element (lanthanides + Y) patterns could provide valuable geological information as tourmalines are the most abundant borosilicates on Earth and are stable at extreme PT conditions. The lanthanide-bearing tourmalines were synthesized for the first time in a series of high- (4 GPa) and low-pressure (0.2 GPa) hydrothermal experiments. We have found that Ln-content (Ln = La 3+, Nd 3+, Eu 3+ and Yb 3+) in synthetic tourmalines varies significantly (1.13–8.35 wt% Ln 2O 3) with Yb < La ≤ Nd < Eu independent of pressure conditions. Ln-content in synthetic tourmalines, obtained at low pressure is 2–3 times higher, than those from high-pressure experiments. The Nd- and Eu-rich synthetic tourmalines exhibit cathodo- photoluminescence properties (blue and violet luminescence colors for Nd and Eu, respectively), which confirms trivalent state of Ln in tourmaline structure. Single-crystal X-ray diffraction data for synthetic tourmalines (Nd-rich a 15.893(1), c 7.130(1) Å; Eu-rich a 15.903(5), c 7.168(3) Å) show that Eu 3+ and Nd 3+ occupy the 9-coordinated X-site in the tourmaline structure. The general formula of obtained synthetic tourmalines can be expressed as Ln 3+ 1-x (Mg,Al) 3 (Al,Mg) 6 (Si 6O 18) (BO 3) 3 (OH,O) 3 (OH,O) (0.05 ≤ x ≤ 0.97). The crystal-chemical features and lanthanide speciation in synthesized tourmalines are herein discussed and compared to natural and synthetic compounds.
AB - Tourmaline rare-earth element (lanthanides + Y) patterns could provide valuable geological information as tourmalines are the most abundant borosilicates on Earth and are stable at extreme PT conditions. The lanthanide-bearing tourmalines were synthesized for the first time in a series of high- (4 GPa) and low-pressure (0.2 GPa) hydrothermal experiments. We have found that Ln-content (Ln = La 3+, Nd 3+, Eu 3+ and Yb 3+) in synthetic tourmalines varies significantly (1.13–8.35 wt% Ln 2O 3) with Yb < La ≤ Nd < Eu independent of pressure conditions. Ln-content in synthetic tourmalines, obtained at low pressure is 2–3 times higher, than those from high-pressure experiments. The Nd- and Eu-rich synthetic tourmalines exhibit cathodo- photoluminescence properties (blue and violet luminescence colors for Nd and Eu, respectively), which confirms trivalent state of Ln in tourmaline structure. Single-crystal X-ray diffraction data for synthetic tourmalines (Nd-rich a 15.893(1), c 7.130(1) Å; Eu-rich a 15.903(5), c 7.168(3) Å) show that Eu 3+ and Nd 3+ occupy the 9-coordinated X-site in the tourmaline structure. The general formula of obtained synthetic tourmalines can be expressed as Ln 3+ 1-x (Mg,Al) 3 (Al,Mg) 6 (Si 6O 18) (BO 3) 3 (OH,O) 3 (OH,O) (0.05 ≤ x ≤ 0.97). The crystal-chemical features and lanthanide speciation in synthesized tourmalines are herein discussed and compared to natural and synthetic compounds.
KW - Crystal chemistry
KW - End-member
KW - Geochemistry
KW - REE
KW - Synthesis
KW - Tourmaline
UR - http://www.scopus.com/inward/record.url?scp=85115953693&partnerID=8YFLogxK
U2 - 10.1016/j.chemgeo.2021.120526
DO - 10.1016/j.chemgeo.2021.120526
M3 - Article
VL - 584
SP - 120526
JO - Chemical Geology
JF - Chemical Geology
SN - 0009-2541
M1 - 120526
ER -
ID: 85871552