Ertlite, NaAl3Al6(Si4B2O18)(BO3)3(OH)3O, a new mineral species of the tourmaline supergroup

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F25%3A00141275" target="_blank" >RIV/00216224:14310/25:00141275 - isvavai.cz</a>

Výsledek na webu

<a href="https://pubs.geoscienceworld.org/msa/ammin/article-abstract/doi/10.2138/am-2025-9816/654751/Ertlite-NaAl3Al6-Si4B2O18-BO3-3-OH-3O-a-new?redirectedFrom=fulltext" target="_blank" >https://pubs.geoscienceworld.org/msa/ammin/article-abstract/doi/10.2138/am-2025-9816/654751/Ertlite-NaAl3Al6-Si4B2O18-BO3-3-OH-3O-a-new?redirectedFrom=fulltext</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.2138/am-2025-9816" target="_blank" >10.2138/am-2025-9816</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Ertlite, NaAl3Al6(Si4B2O18)(BO3)3(OH)3O, a new mineral species of the tourmaline supergroup

Popis výsledku v původním jazyce

Ertlite, ideally NaAl3Al6(Si4B2O18)(BO3)3(OH)3O, is a new, very B-rich mineral of the tourmaline supergroup. It was found at two localities; the holotype in the Sahatany Valley, central Madagascar, and a co-type specimen from Sakangyi, Mogok Township, Mandalay Region, Myanmar. At both localities, the mineral occurs as a late-stage hydrothermal phase in open pockets within highly fractionated, B-rich granitic pegmatites. The holotype occurs as pink to brownish grey or near colorless euhedral crystals and aggregates, up to 10 mm in diameter, with vitreous luster, conchoidal fracture, and white streak. The mineral is uniaxial (–). Holotype ertlite has a Mohs hardness of ca. 7–8, a calculated density of 3.128 g·cm−3 and an excellent compatibility index (1 − KP/KC = 0.018). Co-type ertlite has a Mohs hardness of ca. 7–8, a calculated density of 3.135 g·cm−3 and a superior compatibility index (1 − KP/KC = 0.001). Ertlite has trigonal symmetry, space group R3m, with a = 15.6509(8) Å, c = 7.0406(5) Å, V = 1493.55(19) Å3 (holotype) and a = 15.590(2) Å, c = 7.009(1) Å, V = 1475.3(4) Å3 (co-type, with the lowest unit-cell volume ever recorded for a natural tourmaline); Z = 3. The crystal structures were refined to R1 = 2.01 % and 3.74 %, respectively, using room temperature datasets collected with MoKα radiation. Crystal-chemical analysis obtained using electron probe microanalysis, laser ablation inductively coupled plasma mass spectroscopy, Raman spectrometry, and crystal structure refinement resulted in the following empirical holotype and co-type formulae, respectively: X(Na0.743Ca0.1090.146K0.002)Σ1.000 Y(Al2.836Li0.144Mn0.002Fe0.010)Σ2.992 Z(Al6.000)T(Si4.526B1.419Al0.055)Σ6.000O18 B(BO3)3 V(OH2.857O0.143)Σ3.000 W(O0.974F0.026)Σ1.000 (holotype); X(Na0.743Ca0.1090.146K0.002)Σ1.000 Y(Al2.836Li0.144Mn0.002Fe0.010)Σ2.992 Z(Al6.000) T(Si4.053B1.955)Σ6.008O18 B(BO3)3 V(OH)3.000 W(O0.716OH0.245F0.039)Σ1.000 (co-type). Ertlite is an oxy-species that belongs to the sodic-group of the tourmaline supergroup. The closest end-member compositions of valid tourmaline species are: olenite by the coupled substitution TSi4+ + VO2− → TB3+ + VOH− accompanied by the disorder exchange VO2− + WOH− → VOH− + wO2−, alumino-oxy-rossmanite by the coupled substitution X□ + TSi4+ + TAl3+ → XNa+ + 2(TB3+), and darrellhenryite by the coupled substitution YLi+ + 2(TSi4+) → YAl3+ + 2(TB3+). Ertlite was approved by the IMA-CNMNC (IMA 2023-086); the name honors the tourmaline specialist Dr. Andreas Ertl-Winand. Ertlite is closely related to synthetic excess-boron tourmalines. Holotype ertlite formed during a late stage of open pocket crystallization in a highly fractionated granitic pegmatite dike of lithium-cesium-tantalum-enriched type (LCT-type) of likely Pan-African age. Co-type ertlite crystallized in a very similar pegmatite environment.

Název v anglickém jazyce

Ertlite, NaAl3Al6(Si4B2O18)(BO3)3(OH)3O, a new mineral species of the tourmaline supergroup

Popis výsledku anglicky

Ertlite, ideally NaAl3Al6(Si4B2O18)(BO3)3(OH)3O, is a new, very B-rich mineral of the tourmaline supergroup. It was found at two localities; the holotype in the Sahatany Valley, central Madagascar, and a co-type specimen from Sakangyi, Mogok Township, Mandalay Region, Myanmar. At both localities, the mineral occurs as a late-stage hydrothermal phase in open pockets within highly fractionated, B-rich granitic pegmatites. The holotype occurs as pink to brownish grey or near colorless euhedral crystals and aggregates, up to 10 mm in diameter, with vitreous luster, conchoidal fracture, and white streak. The mineral is uniaxial (–). Holotype ertlite has a Mohs hardness of ca. 7–8, a calculated density of 3.128 g·cm−3 and an excellent compatibility index (1 − KP/KC = 0.018). Co-type ertlite has a Mohs hardness of ca. 7–8, a calculated density of 3.135 g·cm−3 and a superior compatibility index (1 − KP/KC = 0.001). Ertlite has trigonal symmetry, space group R3m, with a = 15.6509(8) Å, c = 7.0406(5) Å, V = 1493.55(19) Å3 (holotype) and a = 15.590(2) Å, c = 7.009(1) Å, V = 1475.3(4) Å3 (co-type, with the lowest unit-cell volume ever recorded for a natural tourmaline); Z = 3. The crystal structures were refined to R1 = 2.01 % and 3.74 %, respectively, using room temperature datasets collected with MoKα radiation. Crystal-chemical analysis obtained using electron probe microanalysis, laser ablation inductively coupled plasma mass spectroscopy, Raman spectrometry, and crystal structure refinement resulted in the following empirical holotype and co-type formulae, respectively: X(Na0.743Ca0.1090.146K0.002)Σ1.000 Y(Al2.836Li0.144Mn0.002Fe0.010)Σ2.992 Z(Al6.000)T(Si4.526B1.419Al0.055)Σ6.000O18 B(BO3)3 V(OH2.857O0.143)Σ3.000 W(O0.974F0.026)Σ1.000 (holotype); X(Na0.743Ca0.1090.146K0.002)Σ1.000 Y(Al2.836Li0.144Mn0.002Fe0.010)Σ2.992 Z(Al6.000) T(Si4.053B1.955)Σ6.008O18 B(BO3)3 V(OH)3.000 W(O0.716OH0.245F0.039)Σ1.000 (co-type). Ertlite is an oxy-species that belongs to the sodic-group of the tourmaline supergroup. The closest end-member compositions of valid tourmaline species are: olenite by the coupled substitution TSi4+ + VO2− → TB3+ + VOH− accompanied by the disorder exchange VO2− + WOH− → VOH− + wO2−, alumino-oxy-rossmanite by the coupled substitution X□ + TSi4+ + TAl3+ → XNa+ + 2(TB3+), and darrellhenryite by the coupled substitution YLi+ + 2(TSi4+) → YAl3+ + 2(TB3+). Ertlite was approved by the IMA-CNMNC (IMA 2023-086); the name honors the tourmaline specialist Dr. Andreas Ertl-Winand. Ertlite is closely related to synthetic excess-boron tourmalines. Holotype ertlite formed during a late stage of open pocket crystallization in a highly fractionated granitic pegmatite dike of lithium-cesium-tantalum-enriched type (LCT-type) of likely Pan-African age. Co-type ertlite crystallized in a very similar pegmatite environment.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10504 - Mineralogy

Projekt

<a href="/cs/project/EH23_015%2F0008175" target="_blank" >EH23_015/0008175: Inovace České infrastruktury pro integrativní strukturní biologii</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2025

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

American Mineralogist

ISSN

0003-004X

e-ISSN

1945-3027

Svazek periodika

110

Číslo periodika v rámci svazku

12

Stát vydavatele periodika

US - Spojené státy americké

Počet stran výsledku

12

Strana od-do

1865-1876

Kód UT WoS článku

001631098100001

EID výsledku v databázi Scopus

2-s2.0-105024219193